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Images of Taiwan and Philippines and Goddard Space Flight Center (GSFC)
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Floods in Southern Taiwan
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Floods in Southern Taiwan |
| Description |
Once a powerful super typhoon packing winds of 125 knots (144 mph) as it approached the northern Philippines on June 29, 2004, Mindulle weakened as it moved across the West Pacific, leaving a path of destruction. The bulk of the damage, in the northern Philippines and Taiwan, was not due to Mindulle's strong winds, however, but to the heavy rains the storm generated that resulted in widespread flooding and mudslides. The storm was responsible for at least 31 fatalities in the Philippines, and 11 more are still missing. At least 22 fatalities occurred in Taiwan and 14 others are still missing. Almost all of the deaths were a direct result of flooding and mudslides. The Tropical Rainfall Measuring Mission [ http://trmm.gsfc.nasa.gov/ ] (TRMM) satellite has been monitoring rainfall over the global tropics since its launch in November of 1997 using both a microwave imager and the first precipitation radar in space. The TRMM-based, near-real time Multi-satellite Precipitation Analysis (MPA) at the NASA Goddard Space Flight Center provides quantitative rainfall estimates over the global tropics. MPA rainfall totals between June 23 and July 4, 2004 are shown for the West Pacific and surrounding areas. Mindulle's track is denoted by the cyclone symbols shown at the 00:00 UTC positions beginning at 00:00 UTC on June 23, 2004. Mindulle's path is also clearly identified by the trail of heavy rain (dark red areas) across the Philippine Sea. The storm's slow forward speed as evidenced by the closely positioned cyclone symbols was responsible for the near 20-inch rainfall totals (dark reds) that stretch across the far the western part of the Philippine Sea and over the northern part of the island of Luzon. Twenty-inch rainfall accumulations are also visible over central and southern parts of Taiwan. Significantly smaller amounts of rainfall occur along the northern part of Mindulle's path as the storm accelerated as it moved north of Taiwan and began moving much faster. TRMM is a joint mission between NASA and the Japanese space agency JAXA. Image produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC). |
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Floods in Southern Taiwan
| Title |
Floods in Southern Taiwan |
| Description |
Once a powerful super typhoon packing winds of 125 knots (144 mph) as it approached the northern Philippines on June 29, 2004, Mindulle weakened as it moved across the West Pacific, leaving a path of destruction. The bulk of the damage, in the northern Philippines and Taiwan, was not due to Mindulle's strong winds, however, but to the heavy rains the storm generated that resulted in widespread flooding and mudslides. The storm was responsible for at least 31 fatalities in the Philippines, and 11 more are still missing. At least 22 fatalities occurred in Taiwan and 14 others are still missing. Almost all of the deaths were a direct result of flooding and mudslides. The Tropical Rainfall Measuring Mission [ http://trmm.gsfc.nasa.gov/ ] (TRMM) satellite has been monitoring rainfall over the global tropics since its launch in November of 1997 using both a microwave imager and the first precipitation radar in space. The TRMM-based, near-real time Multi-satellite Precipitation Analysis (MPA) at the NASA Goddard Space Flight Center provides quantitative rainfall estimates over the global tropics. MPA rainfall totals between June 23 and July 4, 2004 are shown for the West Pacific and surrounding areas. Mindulle's track is denoted by the cyclone symbols shown at the 00:00 UTC positions beginning at 00:00 UTC on June 23, 2004. Mindulle's path is also clearly identified by the trail of heavy rain (dark red areas) across the Philippine Sea. The storm's slow forward speed as evidenced by the closely positioned cyclone symbols was responsible for the near 20-inch rainfall totals (dark reds) that stretch across the far the western part of the Philippine Sea and over the northern part of the island of Luzon. Twenty-inch rainfall accumulations are also visible over central and southern parts of Taiwan. Significantly smaller amounts of rainfall occur along the northern part of Mindulle's path as the storm accelerated as it moved north of Taiwan and began moving much faster. TRMM is a joint mission between NASA and the Japanese space agency JAXA. Image produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC). |
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Super Typhoon Sepat
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Super Typhoon Sepat |
| Description |
Super Typhoon Sepat came ashore in Taiwan on August 17, 2007, after bringing torrential rain and flooding to the Philippines the day before. Flights to and from Tapei, the island's capital, were canceled and Chinese authorities were calling all ships at sea to come back to shore in anticipation of the powerful typhoon, said news reports. The typhoon was classified as Category 5 typhoon, [ http://www.nhc.noaa.gov/aboutsshs.shtml ] the very top of the scale, with sustained winds of 184 kilometers per hour (114 miles per hour), according to CNN. At 10:25 a.m. local time (02:25 UTC) on August 16, 2007, when the Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Terra [ http://terra.nasa.gov/ ] satellite captured this image, Super Typhoon Sepat was still well away from its coming encounter with the Philippines and Taiwan. Winds were measured at a sustained speed as high as 257 km/hr (161 mph) at the time of this image, according to the University of Hawaii's Tropical Storm Information Center. [ http://www.solar.ifa.hawaii.edu/Tropical/ ] The storm's strength is evident in this image from its large size, well-defined spiral structure, and obvious large eye. Some clouds are present in the central eye: a completely clear eye is a tell-tale sign of the most powerful storms, though some clouds can be present in the eye of a powerful storm, as is the case here. NASA image by Jesse Allen, using data provided courtesy of the MODIS Rapid Response team [ http://rapidfire.sci.gsfc.nasa.gov ] at Goddard Space Flight Center. |
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Super Typhoon Wipha
| Title |
Super Typhoon Wipha |
| Description |
Super Typhoon Wipha was approaching the coast of China on the afternoon of September 18, 2007, when the Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Aqua [ http://aqua.nasa.gov/ ] satellite captured this photo-like image. At the time (12:40 p.m. local time, 4:40 UTC), Wipha had winds between 250 kilometers per hour (155 miles per hour or 135 knots) and 240 km/hr (150 mph or 130 knots), making it a strong Category 4 [ http://www.nhc.noaa.gov/aboutsshs.shtml ] storm and a Super Typhoon (a typhoon with winds of at least 130 knots). The storm weakened shortly after this image was taken and was forecast to weaken further before making landfall over the densely populated East China coast late on September 18 or early on September 19. Though the storm was weakening, it was anticipated to be the strongest storm to hit China in a decade, reported Xinhua, China's news agency. In preparation for the storm, the government evacuated about two million people in three provinces, said Xinhua. The storm had already started to soak Taiwan with heavy rains by the time this image was taken. The spiraling bands of rain clouds cover the island in this image, though the dark, well-defined eye remains offshore to the north. The image also reveals just how large Wipha was. Including its outer bands, which stretch from the Philippines (visible in the large image) in the south to the East China coast in the north, Wipha sprawls over several hundred kilometers. The high-resolution image provided above is at MODIS' full spatial resolution (level of detail) of 250 meters per pixel. The MODIS Rapid Response System provides this image at additional resolutions. You can also download a 250-meter-resolution KMZ file of Super Typhoon Wipia [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Sep2007/Wipha.A2007261.0440.250m.kmz ] suitable for use with Google Earth. [ http://earth.google.com/ ] NASA image by Jeff Schmaltz, MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center. |
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Flooding in Luzon, the Phili
…
| Title |
Flooding in Luzon, the Philippines |
| Description |
Melor became a tropical depression a few hundred miles east of the central Philippines on October 30, 2003. Moving towards the northwest, Melor strengthened into a minimal typhoon on October 31, just east of the Northern Philippine island of Luzon. Melor crossed over the northern part of Luzon with winds estimated at up to 85 miles per hour. At least four people lost their lives as a result of flooding due to the storm. The TRMM-based, near-real time Multi-satellite Precipitation Analysis (MPA) at the NASA Goddard Space Flight Center shows the rainfall totals associated with Melor's passage. A wide area of 6 inch plus rainfall (red areas) occurred over the northeastern part of the island along the coastline and east of the Cordillera Central mountains. After crossing the northern coastline, Melor headed north and weakened into a tropical storm before brushing the southeast coastline of Taiwan. White crosses show the track of Melor with tropical storm and typhoon symbols denoting the 00Z positions. Rainfall accumulations are for the period October 30 to November 4, 2003. TRMM is a joint mission between NASA and the Japanese space agency NASDA. Image generaged by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC) |
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Flooding in Luzon, the Phili
…
| Title |
Flooding in Luzon, the Philippines |
| Description |
Melor became a tropical depression a few hundred miles east of the central Philippines on October 30, 2003. Moving towards the northwest, Melor strengthened into a minimal typhoon on October 31, just east of the Northern Philippine island of Luzon. Melor crossed over the northern part of Luzon with winds estimated at up to 85 miles per hour. At least four people lost their lives as a result of flooding due to the storm. The TRMM-based, near-real time Multi-satellite Precipitation Analysis (MPA) at the NASA Goddard Space Flight Center shows the rainfall totals associated with Melor's passage. A wide area of 6 inch plus rainfall (red areas) occurred over the northeastern part of the island along the coastline and east of the Cordillera Central mountains. After crossing the northern coastline, Melor headed north and weakened into a tropical storm before brushing the southeast coastline of Taiwan. White crosses show the track of Melor with tropical storm and typhoon symbols denoting the 00Z positions. Rainfall accumulations are for the period October 30 to November 4, 2003. TRMM is a joint mission between NASA and the Japanese space agency NASDA. Image generaged by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC) |
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Typhoon Aere
| Title |
Typhoon Aere |
| Description |
The Tropical Rainfall Measuring Mission or TRMM satellite provided this image of Typhoon Aere over the western Philippine Sea as it was approaching Taiwan. Images and data collected by TRMM help to provide valuable estimates of storm location and intensity especially over remote ocean areas. This particular image was taken at 09:23 UTC on 23 August 2004. At the time of this image, Aere was a minimal Category 1 typhoon with winds estimated at 65 knots (75 mph) by the Joint Typhoon Warning Center. The image shows a top down view of the horizontal distribution of rain intensity obtained from the TRMM satellite. Rain rates in the center part of the swath are from the TRMM Precipitation Radar (PR), the first and only precipitation radar in space. The PR can provide fine resolution rainfall data and details on the vertical structure. Rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). TRMM reveals that Aere has a large, closed eye. However, only the southern portion of the eyewall contains any moderate (green) to heavy (red) rain. The northern portion of the eyewall contains only light (blue) rain and is almost open, which is supported by the IR data. It reveals that Aere is not a strong, well-organized storm and is unlikely to intensify at this time. The heaviest rainfall (darker reds) is contained in an outer rainband south of the center. Aere originally formed as a tropical depression on the 19th of August about 1000 km east of the central Philippines and never intensified beyond Category 1. TRMM is a joint mission between NASA and the Japanese space agency JAXA. NASA images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Ewiniar
| Title |
Typhoon Ewiniar |
| Description |
As of July 11, 2006, at least 30 people in China and 5 in Korea had died as a result of flooding and mudslides caused by Typhoon Ewiniar. The storm began as a tropical depression on June 30, 2006, southeast of Palau in the northern West Pacific. Ewiniar tracked generally north-northwestward before turning north to pass east of the Philippines and Taiwan. The storm made landfall in South Korea on July 10. Ewiniar was rated a Category 4 typhoon at its peak, with maximum sustained winds estimated at 240 kilometers per hour (150 miles per hour) while it was east of the Philippines on July 5. Ewiniar then slowly weakened as it passed by the coast of China before striking the Korean Peninsula as a tropical storm. Rainfall totals are shown here for the period June 29 to July 10, 2006, for the western Pacific region. The highest rainfall totals trace out Ewiniar's path, with maximum amounts around 600 millimeters or more (shown in red). These heavy amounts occurred offshore. The east-west oriented bands of moderate to isolated heavy rainfall (shown in green and red) over the east coast of China and southeast of Japan are associated with another weather system unrelated to Typhoon Ewiniar. That system brought rain to the same area during this period. The rainfall analysis above is from the Multi-satellite Precipitation Analysis, which uses data from NASA's Tropical Rainfall Measuring Mission (TRMM) satellite to calibrate precipitation estimates. This product was developed by the precipitation research team in the Laboratory for Atmosphere at NASA Goddard Space Flight Center. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. Image produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC). |
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Typhoon Ewiniar
| Title |
Typhoon Ewiniar |
| Description |
As of July 11, 2006, at least 30 people in China and 5 in Korea had died as a result of flooding and mudslides caused by Typhoon Ewiniar. The storm began as a tropical depression on June 30, 2006, southeast of Palau in the northern West Pacific. Ewiniar tracked generally north-northwestward before turning north to pass east of the Philippines and Taiwan. The storm made landfall in South Korea on July 10. Ewiniar was rated a Category 4 typhoon at its peak, with maximum sustained winds estimated at 240 kilometers per hour (150 miles per hour) while it was east of the Philippines on July 5. Ewiniar then slowly weakened as it passed by the coast of China before striking the Korean Peninsula as a tropical storm. Rainfall totals are shown here for the period June 29 to July 10, 2006, for the western Pacific region. The highest rainfall totals trace out Ewiniar's path, with maximum amounts around 600 millimeters or more (shown in red). These heavy amounts occurred offshore. The east-west oriented bands of moderate to isolated heavy rainfall (shown in green and red) over the east coast of China and southeast of Japan are associated with another weather system unrelated to Typhoon Ewiniar. That system brought rain to the same area during this period. The rainfall analysis above is from the Multi-satellite Precipitation Analysis, which uses data from NASA's Tropical Rainfall Measuring Mission (TRMM) satellite to calibrate precipitation estimates. This product was developed by the precipitation research team in the Laboratory for Atmosphere at NASA Goddard Space Flight Center. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. Image produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC). |
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Typhoon Kaemi
| Title |
Typhoon Kaemi |
| Description |
) flew over the storm. At the time, Kaemi was over the central Philippine Sea. These images show the horizontal distribution of rain intensity within the storm and provide important clues about Kaemi's structure. In the top image, taken on July 21, TRMM reveals that Kaemi had a well-defined closed eye (center circular region) indicative of the kind of well-developed circulation that is commonly associated with a mature tropical cyclone. The image also shows that the rain field is very asymmetrical, with the bulk of the rain, including essentially all of the intense rain (shown by the darker reds), occurring in the southern half of storm. After the top image was taken on July 21, Kaemi continued to track northwest. Although the storm's center passed well to the north of the main island of Luzon in the northern Philippines, it did bring significant rains to the island. As Kaemi exited the Philippine Sea, it took a direct path over southern Taiwan, crossing over the island on the evening of July 24. By the time it struck, Kaemi had weakened to a Category 1 system. On July 25, Kaemi passed over the narrow Taiwan Straight between Taiwan and China before making landfall that afternoon (local time) near Jinjiang in Fujian Province on China's southeast coast. TRMM captured the lower image at 3:40 p.m. local time (7:40 UTC), just as Kaemi was making landfall on the coast of China. In this image, the center is poorly defined, with no closed eye visible. By this time, Kaemi had weakened to a tropical storm, with sustained winds estimated at just 93 km/hr (58 mph or 90 knots). There was, however, a broad area of light (blue) to moderate (green) rain wrapped around the northern and eastern side of the storm over mainland China. This rain eventually triggered flooding and mudslides in the region. Launched in November of 1997, TRMM was designed to measure rainfall over the global Tropics using a suite of active and passive sensors, including the world's first space-borne precipitation radar. TRMM has also proven to be extremely valuable for monitoring tropical cyclones, especially over remote parts of the open ocean. In these images, rain rates in the center swath are from the TRMM Precipitation Radar, while those in the outer swath are from the TRMM Microwave Imager. The rain rates are overlaid on infrared data from the TRMM Visible Infrared Scanner. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. NASA images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC)., Following a path similar to recent Tropical Storm Bilis, [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=13711 ] which triggered extensive inland flooding and landslides and has been blamed for more than 600 deaths in China, Typhoon Kaemi passed over Taiwan before striking the southeast coast of China. Kaemi means "ant" in Korean. The storm started out as a tropical depression on July 18, 2006, several hundred miles south-southeast of Guam, tracked generally to the northwest, and entered the Philippine Sea as a weak tropical storm on July 19. Over the next two days, Kaemi intensified into a Category 2 typhoon in the central Philippine Sea, with sustained winds estimated at 167 kilometers per hour (104 miles per hour or 90 knots) by the Joint Typhoon Warning Center. [ https://metoc.npmoc.navy.mil//jtwc.html ] While the typhoon was at Category 2 status on July 21, the Tropical Rainfall Measuring Mission satellite (TRMM [ http://trmm.gsfc.nasa.gov/ ] |
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Typhoon Kaemi
| Title |
Typhoon Kaemi |
| Description |
) flew over the storm. At the time, Kaemi was over the central Philippine Sea. These images show the horizontal distribution of rain intensity within the storm and provide important clues about Kaemi's structure. In the top image, taken on July 21, TRMM reveals that Kaemi had a well-defined closed eye (center circular region) indicative of the kind of well-developed circulation that is commonly associated with a mature tropical cyclone. The image also shows that the rain field is very asymmetrical, with the bulk of the rain, including essentially all of the intense rain (shown by the darker reds), occurring in the southern half of storm. After the top image was taken on July 21, Kaemi continued to track northwest. Although the storm's center passed well to the north of the main island of Luzon in the northern Philippines, it did bring significant rains to the island. As Kaemi exited the Philippine Sea, it took a direct path over southern Taiwan, crossing over the island on the evening of July 24. By the time it struck, Kaemi had weakened to a Category 1 system. On July 25, Kaemi passed over the narrow Taiwan Straight between Taiwan and China before making landfall that afternoon (local time) near Jinjiang in Fujian Province on China's southeast coast. TRMM captured the lower image at 3:40 p.m. local time (7:40 UTC), just as Kaemi was making landfall on the coast of China. In this image, the center is poorly defined, with no closed eye visible. By this time, Kaemi had weakened to a tropical storm, with sustained winds estimated at just 93 km/hr (58 mph or 90 knots). There was, however, a broad area of light (blue) to moderate (green) rain wrapped around the northern and eastern side of the storm over mainland China. This rain eventually triggered flooding and mudslides in the region. Launched in November of 1997, TRMM was designed to measure rainfall over the global Tropics using a suite of active and passive sensors, including the world's first space-borne precipitation radar. TRMM has also proven to be extremely valuable for monitoring tropical cyclones, especially over remote parts of the open ocean. In these images, rain rates in the center swath are from the TRMM Precipitation Radar, while those in the outer swath are from the TRMM Microwave Imager. The rain rates are overlaid on infrared data from the TRMM Visible Infrared Scanner. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. NASA images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC)., Following a path similar to recent Tropical Storm Bilis, [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=13711 ] which triggered extensive inland flooding and landslides and has been blamed for more than 600 deaths in China, Typhoon Kaemi passed over Taiwan before striking the southeast coast of China. Kaemi means "ant" in Korean. The storm started out as a tropical depression on July 18, 2006, several hundred miles south-southeast of Guam, tracked generally to the northwest, and entered the Philippine Sea as a weak tropical storm on July 19. Over the next two days, Kaemi intensified into a Category 2 typhoon in the central Philippine Sea, with sustained winds estimated at 167 kilometers per hour (104 miles per hour or 90 knots) by the Joint Typhoon Warning Center. [ https://metoc.npmoc.navy.mil//jtwc.html ] While the typhoon was at Category 2 status on July 21, the Tropical Rainfall Measuring Mission satellite (TRMM [ http://trmm.gsfc.nasa.gov/ ] |
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Typhoon Krosa
| Title |
Typhoon Krosa |
| Description |
Typhoon Krosa was a powerful tropical storm (the generic name for typhoons, hurricanes, and cyclones) on the morning of October 4, 2007. With sustained winds of over 210 kilometers per hour (130 miles per hour), it was just at the crest of being classified a Category 4 [ http://www.nhc.noaa.gov/aboutsshs.shtml ] Super Typhoon when NASA's Aqua satellite flew over Krosa in the afternoon. The storm had been intensifying over the northeastern Philippine Sea for several days, and was expected, as of October 4, to head towards northern Taiwan and the Chinese mainland coast. The Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Aqua [ http://aqua.nasa.gov/ ] satellite acquired this photo-like image at 12:40 p.m. local time (4:40 UTC) on October 4, 2007. A sprawling system with tightly wound spiral arms and a large but cloud-filled ("closed") eye, Krosa bore all the hallmarks of a large and powerful typhoon. Although the storm was observed by MODIS to be brushing up against the Philippines, it was not projected to pass over the islands. The outer bands of the storm will certainly bring rains to Luzon, the northernmost island in the Philippine chain. The high-resolution image provided above is at MODIS' full spatial resolution (level of detail) of 250 meters per pixel. The MODIS Rapid Response System provides this image at additional resolutions. [ http://rapidfire.sci.gsfc.nasa.gov/gallery/?2007277-1004/Krosa.A2007277.0440 ] You can also download a 250-meter-resolution KMZ file of Typhoon Krosa [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Oct2007/ Krosa.A2007277.0440.250m.kmz ] suitable for use with Google Earth. [ http://earth.google.com/ ] NASA image by Jeff Schmaltz, MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center. |
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Typhoon Mindulle
| Title |
Typhoon Mindulle |
| Description |
The MODIS instrument onboard NASA's Terra satellite captured this true-color image of Typhoon Mindulle on June 29, 2004 at 2:20 UTC as the storm was located approximately 450 miles south-southeast of Tapei, Taiwan. At the time this image was taken, Mindulle had sustained winds of 144 mph with higher gusts to 173 mph. Mindulle was expected to drift towards the west and make landfall over the northern Philippines. Image courtesy Jeff Schmaltz, MODIS Land Rapid Response Team at NASA GSFC. |
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Typhoon Mindulle
| Title |
Typhoon Mindulle |
| Description |
As the northern Philippines island of Luzon recovers from its brush with Typhoon Mindulle, the island nation of Taiwan now bears the brunt of the storm. Mindulle was responsible for 16 fatalities and 17 missing persons in the Philippines mainly from flash floods and is now hitting the east coast of Taiwan with 75 mph winds. Mindulle formed into a tropical depression from a monsoon gyre back on the 23rd of June 2004 just west of the Northern Mariana Islands. Mindulle quickly reached tropical storm strength but only slowly intensified over the next few days before finally becoming a minimal typhoon on the 27th in the Philippine Sea. Next came a period of rapid development as Mindulle's maximum sustained winds increased from 65 knots (75 mph) to 125 knots (144 mph) within a span of just 30 hours, and it's forward speed decreased dramatically as it approached the northern Philippines. Up until this point, Mindulle had been moving mainly due west but now turned north taking it through the Babuyan and Batan islands north of the main island of Luzon. The storm increased its forward speed slowly and began to weaken as it passed through the Bashi Channel headed for Taiwan. Mindulle passed by the Hengchun Peninsula at the southern tip of Taiwan on the evening (local time) of the 30th of June before continuing up along the east coast of Taiwan. The Tropical Rainfall Measuring Mission (TRMM) satellite has been fulfilling its mission of monitoring rainfall over the global tropics since its launch back in November of 1997. With its passive and active sensors, TRMM is able to capture unique images of tropical cyclones providing a one of a kind perspective on their structures as seen by this series of images of Mindulle. The first image was taken at 15:39 UTC on 23 June 2004 when Mindulle was still just a tropical storm west of the Northern Mariana Islands with maximum sustained winds estimated at 35 knots (40 mph) by the Joint Typhoon Warning Center. The image shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), the first and only precipitation radar in space, and those in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). This image shows that Mindulle is not very organized yet with no evidence of an eye in the rain field. However, some banding is visible in the moderate rain rates (green areas) and a sizeable area of intense rain is present (dark red areas). The second image was taken at 06:01 UTC on the 28th and shows a mature typhoon with a large, well- defined eye surrounded by a definitive eyewall that contains areas of heavy rain (semicircle with dark red areas). At this time Mindulle was a Category 4 storm with sustained winds estimated at 115 knots (132 mph) as it was approaching the the the northern Philippines. The next image at this same time shows a vertical cross section, through the center of the storm from the PR looking northeast. It shows the intense rain (black area) in the western eyewall and a broad rain shield of moderate intensity rain (yellow areas) west of the center. Also evident is a bright band (horizontal yellow areas) wherein ice particle begin to melt as they fall through the freezing level. The final image was taken at 4:51 UTC on 1 July 2004. It shows a greatly weakened Mindulle hugging the east coast of Taiwan. The eyewall is gone and the center is surrounded by a large swirl of mostly light rain (blue areas). The heaviest rain rates are part of a large rain band that extends southwest of the center into the northern South China Sea. At this time, the maximum estimated winds were down to 75 knots (86 mph). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Mindulle
| Title |
Typhoon Mindulle |
| Description |
As the northern Philippines island of Luzon recovers from its brush with Typhoon Mindulle, the island nation of Taiwan now bears the brunt of the storm. Mindulle was responsible for 16 fatalities and 17 missing persons in the Philippines mainly from flash floods and is now hitting the east coast of Taiwan with 75 mph winds. Mindulle formed into a tropical depression from a monsoon gyre back on the 23rd of June 2004 just west of the Northern Mariana Islands. Mindulle quickly reached tropical storm strength but only slowly intensified over the next few days before finally becoming a minimal typhoon on the 27th in the Philippine Sea. Next came a period of rapid development as Mindulle's maximum sustained winds increased from 65 knots (75 mph) to 125 knots (144 mph) within a span of just 30 hours, and it's forward speed decreased dramatically as it approached the northern Philippines. Up until this point, Mindulle had been moving mainly due west but now turned north taking it through the Babuyan and Batan islands north of the main island of Luzon. The storm increased its forward speed slowly and began to weaken as it passed through the Bashi Channel headed for Taiwan. Mindulle passed by the Hengchun Peninsula at the southern tip of Taiwan on the evening (local time) of the 30th of June before continuing up along the east coast of Taiwan. The Tropical Rainfall Measuring Mission (TRMM) satellite has been fulfilling its mission of monitoring rainfall over the global tropics since its launch back in November of 1997. With its passive and active sensors, TRMM is able to capture unique images of tropical cyclones providing a one of a kind perspective on their structures as seen by this series of images of Mindulle. The first image was taken at 15:39 UTC on 23 June 2004 when Mindulle was still just a tropical storm west of the Northern Mariana Islands with maximum sustained winds estimated at 35 knots (40 mph) by the Joint Typhoon Warning Center. The image shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), the first and only precipitation radar in space, and those in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). This image shows that Mindulle is not very organized yet with no evidence of an eye in the rain field. However, some banding is visible in the moderate rain rates (green areas) and a sizeable area of intense rain is present (dark red areas). The second image was taken at 06:01 UTC on the 28th and shows a mature typhoon with a large, well- defined eye surrounded by a definitive eyewall that contains areas of heavy rain (semicircle with dark red areas). At this time Mindulle was a Category 4 storm with sustained winds estimated at 115 knots (132 mph) as it was approaching the the the northern Philippines. The next image at this same time shows a vertical cross section, through the center of the storm from the PR looking northeast. It shows the intense rain (black area) in the western eyewall and a broad rain shield of moderate intensity rain (yellow areas) west of the center. Also evident is a bright band (horizontal yellow areas) wherein ice particle begin to melt as they fall through the freezing level. The final image was taken at 4:51 UTC on 1 July 2004. It shows a greatly weakened Mindulle hugging the east coast of Taiwan. The eyewall is gone and the center is surrounded by a large swirl of mostly light rain (blue areas). The heaviest rain rates are part of a large rain band that extends southwest of the center into the northern South China Sea. At this time, the maximum estimated winds were down to 75 knots (86 mph). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Mindulle
| Title |
Typhoon Mindulle |
| Description |
As the northern Philippines island of Luzon recovers from its brush with Typhoon Mindulle, the island nation of Taiwan now bears the brunt of the storm. Mindulle was responsible for 16 fatalities and 17 missing persons in the Philippines mainly from flash floods and is now hitting the east coast of Taiwan with 75 mph winds. Mindulle formed into a tropical depression from a monsoon gyre back on the 23rd of June 2004 just west of the Northern Mariana Islands. Mindulle quickly reached tropical storm strength but only slowly intensified over the next few days before finally becoming a minimal typhoon on the 27th in the Philippine Sea. Next came a period of rapid development as Mindulle's maximum sustained winds increased from 65 knots (75 mph) to 125 knots (144 mph) within a span of just 30 hours, and it's forward speed decreased dramatically as it approached the northern Philippines. Up until this point, Mindulle had been moving mainly due west but now turned north taking it through the Babuyan and Batan islands north of the main island of Luzon. The storm increased its forward speed slowly and began to weaken as it passed through the Bashi Channel headed for Taiwan. Mindulle passed by the Hengchun Peninsula at the southern tip of Taiwan on the evening (local time) of the 30th of June before continuing up along the east coast of Taiwan. The Tropical Rainfall Measuring Mission (TRMM) satellite has been fulfilling its mission of monitoring rainfall over the global tropics since its launch back in November of 1997. With its passive and active sensors, TRMM is able to capture unique images of tropical cyclones providing a one of a kind perspective on their structures as seen by this series of images of Mindulle. The first image was taken at 15:39 UTC on 23 June 2004 when Mindulle was still just a tropical storm west of the Northern Mariana Islands with maximum sustained winds estimated at 35 knots (40 mph) by the Joint Typhoon Warning Center. The image shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), the first and only precipitation radar in space, and those in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). This image shows that Mindulle is not very organized yet with no evidence of an eye in the rain field. However, some banding is visible in the moderate rain rates (green areas) and a sizeable area of intense rain is present (dark red areas). The second image was taken at 06:01 UTC on the 28th and shows a mature typhoon with a large, well- defined eye surrounded by a definitive eyewall that contains areas of heavy rain (semicircle with dark red areas). At this time Mindulle was a Category 4 storm with sustained winds estimated at 115 knots (132 mph) as it was approaching the the the northern Philippines. The next image at this same time shows a vertical cross section, through the center of the storm from the PR looking northeast. It shows the intense rain (black area) in the western eyewall and a broad rain shield of moderate intensity rain (yellow areas) west of the center. Also evident is a bright band (horizontal yellow areas) wherein ice particle begin to melt as they fall through the freezing level. The final image was taken at 4:51 UTC on 1 July 2004. It shows a greatly weakened Mindulle hugging the east coast of Taiwan. The eyewall is gone and the center is surrounded by a large swirl of mostly light rain (blue areas). The heaviest rain rates are part of a large rain band that extends southwest of the center into the northern South China Sea. At this time, the maximum estimated winds were down to 75 knots (86 mph). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Mindulle
| Title |
Typhoon Mindulle |
| Description |
As the northern Philippines island of Luzon recovers from its brush with Typhoon Mindulle, the island nation of Taiwan now bears the brunt of the storm. Mindulle was responsible for 16 fatalities and 17 missing persons in the Philippines mainly from flash floods and is now hitting the east coast of Taiwan with 75 mph winds. Mindulle formed into a tropical depression from a monsoon gyre back on the 23rd of June 2004 just west of the Northern Mariana Islands. Mindulle quickly reached tropical storm strength but only slowly intensified over the next few days before finally becoming a minimal typhoon on the 27th in the Philippine Sea. Next came a period of rapid development as Mindulle's maximum sustained winds increased from 65 knots (75 mph) to 125 knots (144 mph) within a span of just 30 hours, and it's forward speed decreased dramatically as it approached the northern Philippines. Up until this point, Mindulle had been moving mainly due west but now turned north taking it through the Babuyan and Batan islands north of the main island of Luzon. The storm increased its forward speed slowly and began to weaken as it passed through the Bashi Channel headed for Taiwan. Mindulle passed by the Hengchun Peninsula at the southern tip of Taiwan on the evening (local time) of the 30th of June before continuing up along the east coast of Taiwan. The Tropical Rainfall Measuring Mission (TRMM) satellite has been fulfilling its mission of monitoring rainfall over the global tropics since its launch back in November of 1997. With its passive and active sensors, TRMM is able to capture unique images of tropical cyclones providing a one of a kind perspective on their structures as seen by this series of images of Mindulle. The first image was taken at 15:39 UTC on 23 June 2004 when Mindulle was still just a tropical storm west of the Northern Mariana Islands with maximum sustained winds estimated at 35 knots (40 mph) by the Joint Typhoon Warning Center. The image shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), the first and only precipitation radar in space, and those in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). This image shows that Mindulle is not very organized yet with no evidence of an eye in the rain field. However, some banding is visible in the moderate rain rates (green areas) and a sizeable area of intense rain is present (dark red areas). The second image was taken at 06:01 UTC on the 28th and shows a mature typhoon with a large, well- defined eye surrounded by a definitive eyewall that contains areas of heavy rain (semicircle with dark red areas). At this time Mindulle was a Category 4 storm with sustained winds estimated at 115 knots (132 mph) as it was approaching the the the northern Philippines. The next image at this same time shows a vertical cross section, through the center of the storm from the PR looking northeast. It shows the intense rain (black area) in the western eyewall and a broad rain shield of moderate intensity rain (yellow areas) west of the center. Also evident is a bright band (horizontal yellow areas) wherein ice particle begin to melt as they fall through the freezing level. The final image was taken at 4:51 UTC on 1 July 2004. It shows a greatly weakened Mindulle hugging the east coast of Taiwan. The eyewall is gone and the center is surrounded by a large swirl of mostly light rain (blue areas). The heaviest rain rates are part of a large rain band that extends southwest of the center into the northern South China Sea. At this time, the maximum estimated winds were down to 75 knots (86 mph). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Mindulle
| Title |
Typhoon Mindulle |
| Description |
As the northern Philippines island of Luzon recovers from its brush with Typhoon Mindulle, the island nation of Taiwan now bears the brunt of the storm. Mindulle was responsible for 16 fatalities and 17 missing persons in the Philippines mainly from flash floods and is now hitting the east coast of Taiwan with 75 mph winds. Mindulle formed into a tropical depression from a monsoon gyre back on the 23rd of June 2004 just west of the Northern Mariana Islands. Mindulle quickly reached tropical storm strength but only slowly intensified over the next few days before finally becoming a minimal typhoon on the 27th in the Philippine Sea. Next came a period of rapid development as Mindulle's maximum sustained winds increased from 65 knots (75 mph) to 125 knots (144 mph) within a span of just 30 hours, and it's forward speed decreased dramatically as it approached the northern Philippines. Up until this point, Mindulle had been moving mainly due west but now turned north taking it through the Babuyan and Batan islands north of the main island of Luzon. The storm increased its forward speed slowly and began to weaken as it passed through the Bashi Channel headed for Taiwan. Mindulle passed by the Hengchun Peninsula at the southern tip of Taiwan on the evening (local time) of the 30th of June before continuing up along the east coast of Taiwan. The Tropical Rainfall Measuring Mission (TRMM) satellite has been fulfilling its mission of monitoring rainfall over the global tropics since its launch back in November of 1997. With its passive and active sensors, TRMM is able to capture unique images of tropical cyclones providing a one of a kind perspective on their structures as seen by this series of images of Mindulle. The first image was taken at 15:39 UTC on 23 June 2004 when Mindulle was still just a tropical storm west of the Northern Mariana Islands with maximum sustained winds estimated at 35 knots (40 mph) by the Joint Typhoon Warning Center. The image shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), the first and only precipitation radar in space, and those in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). This image shows that Mindulle is not very organized yet with no evidence of an eye in the rain field. However, some banding is visible in the moderate rain rates (green areas) and a sizeable area of intense rain is present (dark red areas). The second image was taken at 06:01 UTC on the 28th and shows a mature typhoon with a large, well- defined eye surrounded by a definitive eyewall that contains areas of heavy rain (semicircle with dark red areas). At this time Mindulle was a Category 4 storm with sustained winds estimated at 115 knots (132 mph) as it was approaching the the the northern Philippines. The next image at this same time shows a vertical cross section, through the center of the storm from the PR looking northeast. It shows the intense rain (black area) in the western eyewall and a broad rain shield of moderate intensity rain (yellow areas) west of the center. Also evident is a bright band (horizontal yellow areas) wherein ice particle begin to melt as they fall through the freezing level. The final image was taken at 4:51 UTC on 1 July 2004. It shows a greatly weakened Mindulle hugging the east coast of Taiwan. The eyewall is gone and the center is surrounded by a large swirl of mostly light rain (blue areas). The heaviest rain rates are part of a large rain band that extends southwest of the center into the northern South China Sea. At this time, the maximum estimated winds were down to 75 knots (86 mph). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
|
Typhoon Nanmadol
| Title |
Typhoon Nanmadol |
| Description |
Powerful Typhoon Nanmadol was preparing to make landfall in the Philippines on December 2, 2004, over the already battered Aurora province. Over the past two weeks, Luzon, the main island in the Philippines, has been lashed with three tropical storms—Nanmadol is number four. The toll from the first three storms, the most recent of which was Monday, is well over 1,000 with 479 dead and 560 missing, according to Reuters. Many of the deaths occurred along Luzon's east coast where floods and landslides buried three towns. Nanmadol's effects were already being felt over Luzon's east coast late on December 2, and many fear that the storm will make the situation worse. The government of the Philippines has already requested international aid to meet the needs of those whose homes were destroyed. This Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) image shows Typhoon Nanmadol at 4:45 UTC, 12:45 p.m. in Manila. At that time, the storm had sustained winds of 240 kilometers per hour (150 mph) with gusts up to 296 kph (184 mph). Later in the day, the Joint Typhoon Warning Center reported that the storm's winds had slowed to 204 kph (127 mph) with gusts to 250 kph (155 mph). The storm is expected to move northwest over the Philippines, then turn northeast over Taiwan. NASA image created by Jesse Allen, Earth Observatory, using data obtained from the MODIS Rapid Response team. |
|
Typhoon Soudelor
| Title |
Typhoon Soudelor |
| Description |
*animations:* small movie (972 KB MPEG)large movie [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Jun2003/soudelor.qt ] (2.5 MB QuickTime) After traversing through the western Pacific over the past week, Tropical Cyclone Soudelor (07W) was beginning the end of its life cycle as it passed through the Korean Strait. Soudelor was named a Tropical Storm just west of the central Philippines at 12:00 UTC on the June 13, 2003. In the days following, the storm slowly skirted east of the Philippines where it delivered several inches of rain to the central islands as seen in the TRMM-based, near-real time Multi-satellite Precipitation Analysis (MPA) from the NASA Goddard Space Flight Center. Once past the Philippines, Soudelor took a more northerly track staying well east of the island of Taiwan and was elevated to typhoon status at 18:00 UTC on the June 16. After briefly reaching a strength of category 4 on the June 18, Soudelor began to weaken as it left the East China Sea and passed through the Korean Strait into the Sea of Japan. TRMM was able to capture Soudelor's the swath of heavy rainfall extending from east of the Philippines all the way into southern Japan where the cyclone interacted with a frontal system. This rainmap shows the total rainfall accumulation for the period June 13-20, 2003. The heaviest rainfall totals were found just off the southern coast of Korea and were a result of Soudelor's interaction with the frontal system. Although parts of southern Japan are shown to have received several inches of rain, fortunately the heaviest amounts remained offshore. NASA's TRMM or Tropical Rainfall Measurement Mission features a spaceborne weather radar built by the Japanese space agency NASDA. In operation for five years, TRMM has provided unprecedented views of tropical rain events around the globe. For more information on TRMM, please visit the TRMM website. Image and movie courtesy of Hal Pierce, TRMM Project, NASA Goddard Space Flight Center. |
|
Typhoon Soudelor
| Title |
Typhoon Soudelor |
| Description |
*animations:* small movie (972 KB MPEG)large movie [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Jun2003/soudelor.qt ] (2.5 MB QuickTime) After traversing through the western Pacific over the past week, Tropical Cyclone Soudelor (07W) was beginning the end of its life cycle as it passed through the Korean Strait. Soudelor was named a Tropical Storm just west of the central Philippines at 12:00 UTC on the June 13, 2003. In the days following, the storm slowly skirted east of the Philippines where it delivered several inches of rain to the central islands as seen in the TRMM-based, near-real time Multi-satellite Precipitation Analysis (MPA) from the NASA Goddard Space Flight Center. Once past the Philippines, Soudelor took a more northerly track staying well east of the island of Taiwan and was elevated to typhoon status at 18:00 UTC on the June 16. After briefly reaching a strength of category 4 on the June 18, Soudelor began to weaken as it left the East China Sea and passed through the Korean Strait into the Sea of Japan. TRMM was able to capture Soudelor's the swath of heavy rainfall extending from east of the Philippines all the way into southern Japan where the cyclone interacted with a frontal system. This rainmap shows the total rainfall accumulation for the period June 13-20, 2003. The heaviest rainfall totals were found just off the southern coast of Korea and were a result of Soudelor's interaction with the frontal system. Although parts of southern Japan are shown to have received several inches of rain, fortunately the heaviest amounts remained offshore. NASA's TRMM or Tropical Rainfall Measurement Mission features a spaceborne weather radar built by the Japanese space agency NASDA. In operation for five years, TRMM has provided unprecedented views of tropical rain events around the globe. For more information on TRMM, please visit the TRMM website. Image and movie courtesy of Hal Pierce, TRMM Project, NASA Goddard Space Flight Center. |
|
Typhoon Tingting
| Title |
Typhoon Tingting |
| Description |
Typhoons Mindulle and Tingting spin side by side in the Pacific Ocean on June 30, 2004. Mindulle (image left) left seven dead and two missing (according to news reports) after it scraped across the Philippines on June 29 with winds reaching up to 173 miles per hour. When the Moderate Resolution Imaging Spectroradiometer [ http://modis.gsfc.nasa.gov ] (MODIS) on NASA?s Terra [ http://terra.nasa.gov/ ] satellite snapped this image the next day, the maximum wind speed had slowed to 125 miles per hour. Mindulle appears to be moving towards Taiwan and the eastern coast of China, shown in the upper left corner of this image. On June 29 and 30, Typhoon Tingting was dumping heavy rain on Guam and the Northern Marianas. The Joint Typhoon Warning Center [ https://metoc.npmoc.navy.mil//jtwc.html ] reported that the storm had maximum sustained winds of 75 miles per hour with gusts up to 92 miles per hour. This true-color MODIS image was acquired on June 30, 2004. It is available in multiple resolutions from the MODIS Rapid Response Team [ javascript:openNASAWindow('http://rapidfire.sci.gsfc.nasa.gov/gallery/?2004182-0630/MindulleTingting.A2004182.0430') ] at Goddard Space Flight Center. Image courtesy Jeff Schmaltz, MODIS Land Rapid Response Team [ http://rapidfire.sci.gsfc.nasa.gov ] at NASA GSFC |
|
Typhoon Tingting
| Title |
Typhoon Tingting |
| Description |
Typhoons Mindulle and Tingting spin side by side in the Pacific Ocean on June 30, 2004. Mindulle (image left) left seven dead and two missing (according to news reports) after it scraped across the Philippines on June 29 with winds reaching up to 173 miles per hour. When the Moderate Resolution Imaging Spectroradiometer [ http://modis.gsfc.nasa.gov ] (MODIS) on NASA?s Terra [ http://terra.nasa.gov/ ] satellite snapped this image the next day, the maximum wind speed had slowed to 125 miles per hour. Mindulle appears to be moving towards Taiwan and the eastern coast of China, shown in the upper left corner of this image. On June 29 and 30, Typhoon Tingting was dumping heavy rain on Guam and the Northern Marianas. The Joint Typhoon Warning Center [ https://metoc.npmoc.navy.mil//jtwc.html ] reported that the storm had maximum sustained winds of 75 miles per hour with gusts up to 92 miles per hour. This true-color MODIS image was acquired on June 30, 2004. It is available in multiple resolutions from the MODIS Rapid Response Team [ javascript:openNASAWindow('http://rapidfire.sci.gsfc.nasa.gov/gallery/?2004182-0630/MindulleTingting.A2004182.0430') ] at Goddard Space Flight Center. Image courtesy Jeff Schmaltz, MODIS Land Rapid Response Team [ http://rapidfire.sci.gsfc.nasa.gov ] at NASA GSFC |
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Typhoon Kalmaegi: Natural Ha
…
nasa, nasanaturalhazards
Typhoon Kalmaegi dumped heav
…
kalmaegi_trmm_2008200
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2008-07-18 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
kalmaegi_trmm_2008200 |
|
Typhoon Mindulle: Natural Ha
…
nasa, nasanaturalhazards
* eoimages.gsfc.nasa.gov/ima
…
trmm_mindulle_23june1539
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-06-23 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
trmm_mindulle_23june1539 |
|
Typhoon Ewiniar: Natural Haz
…
nasa, nasanaturalhazards
* eoimages.gsfc.nasa.gov/ima
…
ewiniar_mpa_2006191
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2006-07-10 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
ewiniar_mpa_2006191 |
|
Super Typhoon Sepat: Natural
…
nasa, nasanaturalhazards
Super Typhoon Sepat came ash
…
sepat_tmo_2007228
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2007-08-16 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
sepat_tmo_2007228 |
|
Typhoon Conson (07W): Natura
…
nasa, nasanaturalhazards
* eoimages.gsfc.nasa.gov/ima
…
trmm_conson_5june1732
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-06-05 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
trmm_conson_5june1732 |
|
Typhoon Krosa: Natural Hazar
…
nasa, nasanaturalhazards
Typhoon Krosa was a powerful
…
krosa_amo_2007277
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2007-10-04 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
krosa_amo_2007277 |
|
Floods in Southern Taiwan: N
…
nasa, nasanaturalhazards
* eoimages.gsfc.nasa.gov/ima
…
taiwan_TRMM_04jul04
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-07-04 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
taiwan_TRMM_04jul04 |
|
Flooding in Luzon, the Phili
…
nasa, nasanaturalhazards
Melor became a tropical depr
…
phillipine_melor_TRMM200330
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-11-04 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
phillipine_melor_TRMM200330 |
|
Flooding in Luzon, the Phili
…
nasa, nasanaturalhazards
Melor became a tropical depr
…
phillipine_melor_TRMM200330
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-11-04 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
phillipine_melor_TRMM200330 |
|
Typhoon Soudelor: Natural Ha
…
nasa, nasanaturalhazards
animations: /NaturalHazards/
…
soudelor_trm2003170
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-06-19 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
soudelor_trm2003170 |
|
Mindulle Leaves Behind Devas
…
nasa, nasaimageofthedaygalle
…
* eoimages.gsfc.nasa.gov/ima
…
mindulle_trm_2004186
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-06-29 |
| creator |
NASA -- Image courtesy Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC). |
| identifier |
mindulle_trm_2004186 |
|
Typhoon Kaemi: Natural Hazar
…
nasa, nasanaturalhazards
* eoimages.gsfc.nasa.gov/ima
…
kaemi_TRM_2006206
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2006-07-25 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
kaemi_TRM_2006206 |
|
Super Typhoon Wipha: Natural
…
nasa, nasanaturalhazards
Super Typhoon Wipha was appr
…
wipha_amo_2007261
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2007-09-18 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
wipha_amo_2007261 |
|
Typhoon Tingting: Natural Ha
…
nasa, nasanaturalhazards
Typhoons Mindulle and Tingti
…
MindulleTingting_TMO2004182
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-06-30 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
MindulleTingting_TMO2004182 |
|
Typhoon Tingting: Natural Ha
…
nasa, nasanaturalhazards
Typhoons Mindulle and Tingti
…
MindulleTingting_TMO2004182
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-06-30 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
MindulleTingting_TMO2004182 |
|
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