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Super Typhoon Haitang
| Title |
Super Typhoon Haitang |
| Description |
Typhoon Haitang has been gradually building up strength in the northwest Pacific ocean several hundred kilometers from the Mariana Islands. This image was captured by the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite at 04:10 UTC on July 14, 2005 (20:10 Eastern Daylight Time on July 13, 2005). At this time, the typhoon was just beginning to acquire the spiral pattern of a tropical cyclone, with winds reaching 140 kilometers per hour (75 knots). Haitang was heading roughly westward at around 22 km/hr (12 knots) towards Luzon. However, its path is predicted to swing gradually northward to take it north of Taiwan and ultimately into the Chinese coastline near Shanghai. If the typhoon continues to strengthen according to predictions, it will have steady winds as high as 220 km/hr (120 knots) when it makes landfall. However, predicting hurricane strength and intensity remains an inexact science, so communities throughout the potentially affected area keep a wary eye on this threatening storm. NASA image created by Jesse Allen, Earth Observatory, using data obtained from the MODIS Rapid Response team. |
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Super Typhoon Haitang
| Title |
Super Typhoon Haitang |
| Description |
Super Typhoon Haitang is shown here on the morning of July 20, 2005. This image was captured by the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite at 05:15 UTC (3:15 p.m. local time), well after it come ashore onto mainland China and lost much of its power and been downgraded to a tropical storm. Four deaths in Taiwan are attributed to the storm as it passed over the island, and as many as 1 million people have been evacuated in mainland China. All flights out of the cities of Fuzhou and Quanzhou were cancelled in view of the danger of the storm. NASA image created by Jesse Allen, Earth Observatory, using data obtained from the MODIS Rapid Response team. |
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Super Typhoon Haitang
| Title |
Super Typhoon Haitang |
| Description |
Super Typhoon Haitang is shown here bearing down on Taiwan on the afternoon of July 17, 2005. This image was captured by the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite at 04:40 UTC (12:40 p.m. Taipei time). At this time, the typhoon had built into a Category 4 storm on the Saffir-Simpson scale, sufficient for it to be dubbed a super typhoon. Sustained winds were around 230 kilometers per hour (125 knots) with peak gusts as high as 280 km/hr (150 knots). The super typhoon by this time was projected to change course and come ashore in Taiwan. As it crosses the island, the storm will lose some of its strength, but may then rebuild as it crosses the Taiwan Straits and comes ashore again in eastern China. Projections call for it to land in Taiwan early on July 18, and then make landfall in mainland China on July 19. NASA image created by Jesse Allen, Earth Observatory, using data obtained from the MODIS Rapid Response team. |
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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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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 Man-Yi
| Title |
Typhoon Man-Yi |
| Description |
On July 12, 2007, Super Typhoon Man-Yi was a huge spiral of clouds, intense winds, and powerful thunderstorms as it arced northward over the western Pacific toward the southern end of the islands of Japan. Though far offshore, the Category 4 Super Typhoon [ http://www.nhc.noaa.gov/aboutsshs.shtml ] was large enough that the outer bands of storm clouds were bringing wind and rain to Taiwan. Forecasts as of July 12 were calling for the storm to weaken as it traveled through the island chain and to reach Tokyo as a milder, but still powerful, typhoon on or around July 15. 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 2:05 p.m. local time (5:05 UTC). Very near the same time MODIS was observing the storm, the Joint Typhoon Warning Center [ https://metocph.nmci.navy.mil/jtwc.php ] estimated Man-Yi's sustained winds to be over 240 kilometers per hour (145 miles per hour). The satellite image confirms that Man-Yi was a powerful Super Typhoon. The storm has the hallmark tightly wound arms that spiral around a well-defined, circular eye. The symmetrical spirals, clear eye, and intense storm clouds around the eyewall (innermost band of clouds) are all features regularly seen in satellite images of other particularly powerful typhoons. 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/?2007193-0712/Man-Yi.A2007193.0505 ] You can download a 250-meter-resolution Super Typhoon Man-Yi KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Jul2007/Man-Yi.A2007193.0505.250m.kmz ] for use with Google Earth. [ http://earth.google.com/download-earth.html ] NASA image by Jeff Schmaltz, MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center. |
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Typhoon Shanshan
| Title |
Typhoon Shanshan |
| Description |
Typhoon Shanshan formed on September 10, 2006, in the western Pacific off the coast of the Philippine Islands. Over the course of the next 36 hours, it grew from a tropical depression (area of low air pressure) to a typhoon, reaching Category 4 [ http://www.nhc.noaa.gov/aboutsshs.shtml ] strength as it passed Taiwan on September 15. Typhoon Shanshan stayed at Category 4 (a Super Typhoon) for two days, starting to subside only late in the day on September 16. As of September 19, the typhoon was projected to pass on a northeasterly track through the straits between the Korean Peninsula and southern Japan, and to curve east to cross Hokkaido. This photo-like image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on the Aqua [ http://aqua.nasa.gov/ ] satellite on September 18, 2006, at 1:25 p.m. local time (04:25 UTC). Shanshan at the time of this image had a well-defined spiral shape, with a distinct but cloud-filled ("closed") eye. Shanshan had sustained winds of around 140 kilometers per hour (85 miles per hour) at the time this satellite image was acquired, according to the University of Hawaii's Tropical Storm Information Center. [ http://www.solar.ifa.hawaii.edu/Tropical/tropical.html ] Though no longer a super typhoon by this time, Agence France Presse reported nine deaths in southern Japan attributed to the storm, as well at least 310 injuries, and one person missing. Risks for landslides, flooding, and strong storm surge along the western coast were expected to remain high as the storm traveled near the western coastline. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of the MODIS Rapid Response [ http://rapidfire.sci.gsfc.nasa.gov/ ] team. |
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Typhoon Talim
| Title |
Typhoon Talim |
| Description |
Typhoon Talim was a weakening typhoon in the Taiwan Straits when the Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Aqua [ http://aqua.nasa.gov/ ] satellite captured this image at 12:50 p.m. Tapei time on September 1, 2005. It had sustained winds of around 120 kilometers an hour (70 miles per hour). The typhoon was predicted to weaken to a tropical storm in the hours immediately after this image was acquired. The outer edge of the storm started to rain onto Taiwan on August 31, where it brought down very heavy rains throughout the eastern portions of the island. It is the 13th named storm of the Pacific typhoon season, which has seen a record number of storms, and in particular, super typhoons. NASA image created by Jesse Allen, Earth Observatory, using data obtained from the MODIS Rapid Response team. |
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Typhoon Fung-wong: Natural H
nasa, nasanaturalhazards
Typhoon Fung-Wong was lashin
fungwong_amo_2008210
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2008-07-28 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
fungwong_amo_2008210 |
|
Typhoon Shanshan: Natural Ha
nasa, nasanaturalhazards
Typhoon Shanshan formed on S
shanshan_amo_2005261
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2006-09-17 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
shanshan_amo_2005261 |
|
Typhoon Man-Yi: Natural Haza
nasa, nasanaturalhazards
On July 12, 2007, Super Typh
manyi_amo_2007193
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2007-07-12 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
manyi_amo_2007193 |
|
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 |
|
Typhoon Talim: Natural Hazar
nasa, nasanaturalhazards
Typhoon Talim was a weakenin
talim_tmo_01sep05
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2005-09-01 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
talim_tmo_01sep05 |
|
Super Typhoon Haitang: Natur
nasa, nasanaturalhazards
Haitang was heading roughly
haitang_amo_14jul05
| mediatype |
IMAGE |
| mediatype |
image |
| date |
July 14, 2005 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
haitang_amo_14jul05 |
|
Super Typhoon Haitang: Natur
nasa, nasanaturalhazards
The super typhoon by this ti
Haitang.A2005198.0440
| mediatype |
IMAGE |
| mediatype |
image |
| date |
July 17, 2005 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
Haitang.A2005198.0440 |
|
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 |
|
AIRS First Light Data: Typho
PIA00341
Sol (our sun)
Atmospheric Infrared Sounder
| Title |
AIRS First Light Data: Typhoon Ramasun, July 3, 2002 |
| Original Caption Released with Image |
Four images of Tropical Cyclone Ramasun were obtained July 3, 2002 by the Atmospheric Infrared Sounder experiment system onboard NASA's Aqua spacecraft. The AIRS experiment, with its wide spectral coverage in four diverse bands, provides the ability to obtain complete 3-D observations of severe weather, from the surface, through clouds to the top of the atmosphere with unprecedented accuracy. This accuracy is the key to understanding weather patterns and improving weather predictions. Viewed separately, none of these images can provide accurate 3-D descriptions of the state of the atmosphere because of interference from clouds. However, the ability to make simultaneous observations at a wide range of wavelengths allows the AIRS experiment to "see" through clouds. This visible light picture from the AIRS instrument provides important information about the location of the cyclone, cloud structure and distribution. The AIRS instrument image at 900 cm-1 (Figure 1) is from a 10 micron transparent "window channel" that is little affected by water vapor but still cannot see through clouds. In clear areas (like the eye of the cyclone and over northwest Australia) it measures a surface temperature of about 300K (color encoded red). In cloudy areas it measures the cloud top temperature, about 200K for the cyclone, which translates to a cloud top height of about 50,000 feet. On the other hand, most clouds are relatively transparent in microwave, and the Advanced Microwave Sounding Instrument channel image (Figure 2) can see through all but the densest clouds. For example, Taiwan, which is covered by clouds, is clearly visible. The Humidity Sounder for Brazil instrument channel (Figure 3), also in the microwave, is more sensitive to both clouds and humidity. Only in clear, dry regions, such as the eye of the cyclone or the area north of Australia, does it see the surface. It is also severely affected by suspended ice particles formed by strong convection, which causes scattering and appears to be extremely cold. These blue areas indicate intense precipitation. The Atmospheric Infrared Sounder is an instrument onboard NASA's Aqua satellite under the space agency's Earth Observing System. The sounding system is making highly accurate measurements of air temperature, humidity, clouds and surface temperature. Data will be used to better understand weather and climate. It will also be used by the National Weather Service and the National Oceanic and Atmospheric Administration to improve the accuracy of their weather and climate models. The instrument was designed and built by Lockheed Infrared Imaging Systems (recently acquired by British Aerospace) under contract with JPL. The Aqua satellite mission is managed by NASA's Goddard Space Flight Center. |
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AIRS First Light Data: Typho
PIA00341
Sol (our sun)
Atmospheric Infrared Sounder
| Title |
AIRS First Light Data: Typhoon Ramasun, July 3, 2002 |
| Original Caption Released with Image |
Four images of Tropical Cyclone Ramasun were obtained July 3, 2002 by the Atmospheric Infrared Sounder experiment system onboard NASA's Aqua spacecraft. The AIRS experiment, with its wide spectral coverage in four diverse bands, provides the ability to obtain complete 3-D observations of severe weather, from the surface, through clouds to the top of the atmosphere with unprecedented accuracy. This accuracy is the key to understanding weather patterns and improving weather predictions. Viewed separately, none of these images can provide accurate 3-D descriptions of the state of the atmosphere because of interference from clouds. However, the ability to make simultaneous observations at a wide range of wavelengths allows the AIRS experiment to "see" through clouds. This visible light picture from the AIRS instrument provides important information about the location of the cyclone, cloud structure and distribution. The AIRS instrument image at 900 cm-1 (Figure 1) is from a 10 micron transparent "window channel" that is little affected by water vapor but still cannot see through clouds. In clear areas (like the eye of the cyclone and over northwest Australia) it measures a surface temperature of about 300K (color encoded red). In cloudy areas it measures the cloud top temperature, about 200K for the cyclone, which translates to a cloud top height of about 50,000 feet. On the other hand, most clouds are relatively transparent in microwave, and the Advanced Microwave Sounding Instrument channel image (Figure 2) can see through all but the densest clouds. For example, Taiwan, which is covered by clouds, is clearly visible. The Humidity Sounder for Brazil instrument channel (Figure 3), also in the microwave, is more sensitive to both clouds and humidity. Only in clear, dry regions, such as the eye of the cyclone or the area north of Australia, does it see the surface. It is also severely affected by suspended ice particles formed by strong convection, which causes scattering and appears to be extremely cold. These blue areas indicate intense precipitation. The Atmospheric Infrared Sounder is an instrument onboard NASA's Aqua satellite under the space agency's Earth Observing System. The sounding system is making highly accurate measurements of air temperature, humidity, clouds and surface temperature. Data will be used to better understand weather and climate. It will also be used by the National Weather Service and the National Oceanic and Atmospheric Administration to improve the accuracy of their weather and climate models. The instrument was designed and built by Lockheed Infrared Imaging Systems (recently acquired by British Aerospace) under contract with JPL. The Aqua satellite mission is managed by NASA's Goddard Space Flight Center. |
|
AIRS First Light Data: Typho
PIA00341
Sol (our sun)
Atmospheric Infrared Sounder
| Title |
AIRS First Light Data: Typhoon Ramasun, July 3, 2002 |
| Original Caption Released with Image |
Four images of Tropical Cyclone Ramasun were obtained July 3, 2002 by the Atmospheric Infrared Sounder experiment system onboard NASA's Aqua spacecraft. The AIRS experiment, with its wide spectral coverage in four diverse bands, provides the ability to obtain complete 3-D observations of severe weather, from the surface, through clouds to the top of the atmosphere with unprecedented accuracy. This accuracy is the key to understanding weather patterns and improving weather predictions. Viewed separately, none of these images can provide accurate 3-D descriptions of the state of the atmosphere because of interference from clouds. However, the ability to make simultaneous observations at a wide range of wavelengths allows the AIRS experiment to "see" through clouds. This visible light picture from the AIRS instrument provides important information about the location of the cyclone, cloud structure and distribution. The AIRS instrument image at 900 cm-1 (Figure 1) is from a 10 micron transparent "window channel" that is little affected by water vapor but still cannot see through clouds. In clear areas (like the eye of the cyclone and over northwest Australia) it measures a surface temperature of about 300K (color encoded red). In cloudy areas it measures the cloud top temperature, about 200K for the cyclone, which translates to a cloud top height of about 50,000 feet. On the other hand, most clouds are relatively transparent in microwave, and the Advanced Microwave Sounding Instrument channel image (Figure 2) can see through all but the densest clouds. For example, Taiwan, which is covered by clouds, is clearly visible. The Humidity Sounder for Brazil instrument channel (Figure 3), also in the microwave, is more sensitive to both clouds and humidity. Only in clear, dry regions, such as the eye of the cyclone or the area north of Australia, does it see the surface. It is also severely affected by suspended ice particles formed by strong convection, which causes scattering and appears to be extremely cold. These blue areas indicate intense precipitation. The Atmospheric Infrared Sounder is an instrument onboard NASA's Aqua satellite under the space agency's Earth Observing System. The sounding system is making highly accurate measurements of air temperature, humidity, clouds and surface temperature. Data will be used to better understand weather and climate. It will also be used by the National Weather Service and the National Oceanic and Atmospheric Administration to improve the accuracy of their weather and climate models. The instrument was designed and built by Lockheed Infrared Imaging Systems (recently acquired by British Aerospace) under contract with JPL. The Aqua satellite mission is managed by NASA's Goddard Space Flight Center. |
|
AIRS First Light Data: Typho
PIA00341
Sol (our sun)
Atmospheric Infrared Sounder
| Title |
AIRS First Light Data: Typhoon Ramasun, July 3, 2002 |
| Original Caption Released with Image |
Four images of Tropical Cyclone Ramasun were obtained July 3, 2002 by the Atmospheric Infrared Sounder experiment system onboard NASA's Aqua spacecraft. The AIRS experiment, with its wide spectral coverage in four diverse bands, provides the ability to obtain complete 3-D observations of severe weather, from the surface, through clouds to the top of the atmosphere with unprecedented accuracy. This accuracy is the key to understanding weather patterns and improving weather predictions. Viewed separately, none of these images can provide accurate 3-D descriptions of the state of the atmosphere because of interference from clouds. However, the ability to make simultaneous observations at a wide range of wavelengths allows the AIRS experiment to "see" through clouds. This visible light picture from the AIRS instrument provides important information about the location of the cyclone, cloud structure and distribution. The AIRS instrument image at 900 cm-1 (Figure 1) is from a 10 micron transparent "window channel" that is little affected by water vapor but still cannot see through clouds. In clear areas (like the eye of the cyclone and over northwest Australia) it measures a surface temperature of about 300K (color encoded red). In cloudy areas it measures the cloud top temperature, about 200K for the cyclone, which translates to a cloud top height of about 50,000 feet. On the other hand, most clouds are relatively transparent in microwave, and the Advanced Microwave Sounding Instrument channel image (Figure 2) can see through all but the densest clouds. For example, Taiwan, which is covered by clouds, is clearly visible. The Humidity Sounder for Brazil instrument channel (Figure 3), also in the microwave, is more sensitive to both clouds and humidity. Only in clear, dry regions, such as the eye of the cyclone or the area north of Australia, does it see the surface. It is also severely affected by suspended ice particles formed by strong convection, which causes scattering and appears to be extremely cold. These blue areas indicate intense precipitation. The Atmospheric Infrared Sounder is an instrument onboard NASA's Aqua satellite under the space agency's Earth Observing System. The sounding system is making highly accurate measurements of air temperature, humidity, clouds and surface temperature. Data will be used to better understand weather and climate. It will also be used by the National Weather Service and the National Oceanic and Atmospheric Administration to improve the accuracy of their weather and climate models. The instrument was designed and built by Lockheed Infrared Imaging Systems (recently acquired by British Aerospace) under contract with JPL. The Aqua satellite mission is managed by NASA's Goddard Space Flight Center. |
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