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Tropical Cyclone Clare
| Title |
Tropical Cyclone Clare |
| Description |
Tropical Cyclone Clare is a moderately strong storm system in the Indian Ocean off the Australian coast. When the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite observed the cyclone at 06:05 UTC (2:05 p.m. local time) on January 9, 2006, it was a well-developed system with peak sustained winds of around 100 kilometers per hour (60 miles per hour). The cyclone (the local term for a hurricane or typhoon) was about 200 kilometers offshore from Port Hedland in Western Australia, the nearest major city. NASA image created by Jesse Allen, Earth Observatory, using data obtained courtesy of the MODIS Rapid Response team. |
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Tropical Cyclone Emma
| Title |
Tropical Cyclone Emma |
| Description |
Tropical Cyclone Emma formed as a low-intensity storm system and built to cyclone strength only briefly. But Emma's brief cyclone status belied its size and rainfall. The Moderate Resolution Imaging Spectrometer (MODIS) instrument on the Aqua observed the storm system as it was losing strength, and hence its tropical cyclone status, on February 28, 2006, at 5:55 UTC (1:55 p.m. local time). At this time, the cyclone had peak winds of roughly 55 kilometers per hour (35 miles per hour). As the image shows, the storm system covered an enormous area, extending over almost the entire extent of Western Australia. With it came heavy rain and substantial flooding to the Pilbara Region, the northwestern corner of Western Australia, where the storm system came ashore. NASA image created by Jesse Allen, Earth Observatory, using data obtained from the Goddard Earth Sciences DAAC. |
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Tropical Cyclone Floyd
| Title |
Tropical Cyclone Floyd |
| Description |
Tropical Cyclone Floyd formed northwest of Australia in the Timor Sea on March 21, 2006. The cyclone gained power gradually and was heading west into the Indian Ocean. It was not predicted to travel over any large landmasses, though it may pose a threat to Christmas Island well off the Western Australia coast in the Indian Ocean. When the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Terra satellite observed the storm at 11:55 a.m. Australian Western Daylight Saving time (02:35 UTC) on March 22, 2006, Tropical Cyclone Floyd was continuing to slowly build power and size. When MODIS made this observation, the storm had peak winds of around 120 kilometers per hour (75 miles per hour), and forecasts at the time called for it to continue to gather strength for at least several days, with predicted peak winds of 170 kilometers per hour (105 mph), according to the University of Hawaii's Tropical Storm Information Center. NASA image created by Jesse Allen, Earth Observatory, using data obtained courtesy of the MODIS Rapid Response team. |
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Tropical Cyclone George
| Title |
Tropical Cyclone George |
| Description |
After crossing Australia's Northern Territory and triggering floods [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=14159 ], Cyclone George skimmed along the Australian coast, steadily gaining power. By the time the storm took a sharp turn towards shore and headed towards Port Hedland in northern Western Australia on March 8, 2007, the cyclone packed sustained winds of 200 kilometers per hour (127 miles per hour, 110 knots), with gusts to 250 km/hr (155 mph, 135 knots). The Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Terra [ http://terra.nasa.gov/ ] satellite captured this image on March 8 at 10:55 a.m. local time (1:55 UTC). Though the storm lacks a distinct eye, the dense concentration of swirling clouds attests to the storm's power. 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/?2007067-0308/George.A2007067.0155 ] You can also download a 250-meter-resolution Cyclone George KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Mar2007/George.A2007067.0155.250m.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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Tropical Cyclone George
| Title |
Tropical Cyclone George |
| Description |
Tropical Cyclone George came ashore on the remote Pilbara coast of Western Australia on the evening of March 8, 2007, as a very powerful Category 4 storm, [ http://www.nhc.noaa.gov/aboutsshs.shtml ] with wind speeds as high as 275 kilometers per hour (170 miles per hour). According to the online version of the Sydney Morning Herald, the storm was responsible for at least two deaths [ http://www.smh.com.au/news/national/cyclone-george-kills-two-jacob-advances/2007/03/09/1173166991751.html ] and many serious injuries as of March 10. This photo-like image of George was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on the Aqua [ http://aqua.nasa.gov/ ] satellite on March 9, 2007, at 1:25 p.m. local time (05:25 UTC). The storm was still a strong tropical cyclone with a circular shape and distinct eye at its center, despite the fact that the storm had been traveling over land for nearly a day when the image was captured. According to the University of Hawaii's Tropical Storm Information Center, [ http://www.solar.ifa.hawaii.edu/Tropical/ ] Cyclone George had sustained winds of 120 kilometers per hour (75 miles per hour) near the time this image was acquired. George was the worst storm to hit the area in 30 years, and the government declared the region a disaster area. Rescue and recovery efforts were expected to be complicated by the arrival of Cyclone Jacob. As a Category 2 storm, Jacob was smaller and weaker, and it was not expected to wreak the same kind of destruction as George. You can download a 250-meter-resolution Cyclone George KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Mar2007/george_amo_2007068.kmz ] for use with Google Earth. [ http://earth.google.com/download-earth.html ] NASA image created by Jesse Allen, using data provided courtesy of the MODIS Rapid Response [ http://rapidfire.sci.gsfc.gov/ ] team. |
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Tropical Cyclone Glenda
| Title |
Tropical Cyclone Glenda |
| Description |
Tropical Cyclone Glenda formed off the northwestern coast of Australia on March 27, 2006. The storm quickly built into a powerful and well-defined cyclone during the next day. Powerful winds have whipped up surf along the coastline of Western Australia's Pilbara region, and the storm also brought heavy rain to the islands off the Kimberly coast. As of March 28, 2006, the storm had reached Category 4 status and was expected to build power and reach the maximum, Category 5, rating during the next day. This natural-color image was acquired by the Moderate Resolution Imaging Spectrometer (MODIS) on the Terra satellite on March 28, 2006, at 10:00 a.m. local time (02:00 UTC). It shows Cyclone Glenda as a well-developed storm, sitting 180 kilometers (150 miles) north of Broome. The storm was already large enough that Broome was covered by the edge of the cyclone. Sustained, peak winds in the storm system were roughly 165 kilometers per hour (105 miles per hour) at this time. The cyclone had been traveling roughly parallel to the coastline, putting the entire coastal area on alert. The area includes not only major pearl-diving operations and beaches that attract tourists, but it is also home to the Northwest Shelf, one of Australia's major oil fields. The oil fields are located off the coast near Dampier. According to news reports, operators were not expressing concern about the oil field but were planning for necessary shutdowns for safety. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of the MODIS Rapid Response team. |
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Tropical Cyclone Glenda
| Title |
Tropical Cyclone Glenda |
| Description |
Tropical Cyclone Glenda formed off the northwestern coast of Australia on March 27, 2006. The storm quickly built into a powerful and well-defined cyclone during the next day. Powerful winds have whipped up surf along the coastline of Western Australia's Pilbara, and the storm brought heavy rain to the islands off the Kimberly coast. As of March 29, 2006, the storm had reached Category 5 status, the maximum rating possible for a cyclone. This photo-like image was acquired by the Moderate Resolution Imaging Spectrometer (MODIS) on the Terra satellite on March 29, 2006, at 10:40 a.m. local time (02:40 UTC). It shows Cyclone Glenda as a well-developed storm, sitting 525 kilometers (330 miles) west of Broome. Clouds from the storm covered most of the northwest coastline of Western Australia. Sustained, peak winds in the storm system were roughly 220 kilometers per hour (140 miles per hour) at this time. The storm's spiraling clouds appear as a nearly solid white disk, but in several places, it appears as though some clouds are "boiling" up above the rest. Predictions as of 2:55 a.m. Australian Western Standard Time on March 30 were that the storm would cross the coast between Exmouth and Karatha on Thursday afternoon or night as a very dangerous storm. The Australian Bureau of Meteorology predicted that wind speeds near the storm center could reach 265 kilometers per hour (165 miles per hour) as the storm comes ashore. Many coastal communities were being evacuated by State Emergency Services ahead of the storm. NASA image created by Jesse Allen, Earth Observatory, using data provided by Liam Gumley, University of Wisconsin-Madison, and Geoscience Australia. |
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Tropical Cyclone Glenda
| Title |
Tropical Cyclone Glenda |
| Description |
Tropical Cyclone Glenda formed off the northwestern coast of Australia on March 27, 2006. Powerful winds whipped up surf along the coastline of Western Australia's Pilbara region, and the storm brought heavy rains to the islands off the Kimberly coast. On March 29, it was classified as a Category 5 storm, the highest rating on the cyclone-strength scale. However, as it came ashore a day later, it had lost a small fraction of its strength. By March 31, 2006, the storm had lost considerable power and was ranked as a mere tropical depression. This photo-like image was acquired by the Moderate Resolution Imaging Spectrometer (MODIS) on the Terra satellite on March 31, 2006, at 10:30 a.m. local time (02:30 UTC), roughly 40 hours after coming ashore near Onslow. The remnants of Cyclone Glenda still have a vaguely spiral appearance, but they lack the well-developed eye and tight-wound shape of the mature, powerful storm of previous days. Clouds from the storm cover most of the Indian Ocean coast of Western Australia. Sustained, peak winds in the storm system were considerably diminished, roughly 65 kilometers per hour (40 miles per hour) around the time the image was captured. Damage assessments in Onslow showed the town fared better than expected in the face of such a powerful storm. However, it will be many days before clean-up operations are concluded. Meteorologists were also concerned about the widespread flooding potential as the storm continued to travel inland. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of the MODIS Rapid Response team. |
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Tropical Cyclone Glenda
| Title |
Tropical Cyclone Glenda |
| Description |
Tropical Cyclone Glenda formed off the northwestern coast of Australia on March 27, 2006. The storm quickly built into a powerful and well-defined cyclone during the next day. Powerful winds have whipped up surf along the coastline of Western Australia's Pilbara region, and the storm has brought heavy rains to the islands off the Kimberly coast. As of March 30, 2006, the storm had lost some power and was ranked as a powerful Category 4 storm, after having peaked the previous day. This photo-like image was acquired by the Moderate Resolution Imaging Spectrometer (MODIS) on the Aqua satellite on March 30, 2006, at 2:10 p.m. local time (06:10 UTC). It shows Cyclone Glenda as a well-developed storm, sitting just off the coastline about 300 kilometers (185 miles) from Port Hedland. Clouds from the storm covered most of the northwest coastline of Western Australia. Sustained, peak winds in the storm system were roughly 195 kilometers per hour (120 miles per hour) at this time. The storm's spiraling clouds appear as a nearly solid white disk, and the faint bluish eye is poised just off the coastline. Observations as of 8:00 p.m. Australian Western Standard Time on March 30 were that the storm was crossing the coast near Onslow. The town was bearing the brunt of the worst winds near the cyclone's center. The Australian Bureau of Meteorology predicted that wind speeds could gust as high as 235 kilometers per hour (140 miles per hour) as the storm continued to come ashore. Residents in coastal communities who were not yet evacuated were directed to stay put, as the severe winds would make attempting to move extremely dangerous. Australian news services are comparing Glenda to the famous and destructive cyclones Larry and Tracy. Larry struck the Queensland coast just two weeks before Glenda, while Tracy remains imprinted on Australia's memory as the storm that flattened Darwin on Christmas Eve 1974. Glenda is large and more powerful than either of these storms, but striking in a much more sparsely populated area. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of the MODIS Rapid Response team. |
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Tropical Cyclone Kara
| Title |
Tropical Cyclone Kara |
| Description |
Tropical Cyclone Kara was poised just offshore of the Pilbara coast of Western Australia on March 27, 2007. Kara was not a particularly severe storm, but was prepared to hit the same area that powerful Cyclone George [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=14163 ] and Category 2 Cyclone Jacob [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=14162 ] hit two weeks earlier. This photo-like image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on the Terra [ http://terra.nasa.gov/ ] satellite on March 27, 2007, at 10:25 a.m. local time (02:25 UTC). The storm was a tropical cyclone with a circular shape and distinct eye at its center. According to the University of Hawaii's Tropical Storm Information Center, [ http://www.solar.ifa.hawaii.edu/Tropical/ ] Cyclone Kara had sustained winds of 145 kilometers per hour (90 miles per hour) near the time this image was acquired. 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/?2007086-0327/Kara.A2007086.0225 ] You can download a 250-meter-resolution Cyclone Kara KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Mar2007/kara_tmo_2007086.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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Tropical Cyclone Larry
| Title |
Tropical Cyclone Larry |
| Description |
Tropical Cyclone Larry formed off the northeastern coast of Australia on March 18, 2006. The cyclone gained power rapidly and came ashore on Queensland's eastern coastline, where it hammered beaches with heavy surf, tore roofs off buildings, and perhaps most destructively, flattened trees in banana plantations over a wide area. The Melbourne Age reported estimates that as much as 80 percent of the Australian banana crop has been destroyed. Since many trees have been uprooted, it may be many years before the banana industry recovers. When the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite observed the storm at 3:05 p.m. Australian Eastern Daylight Savings Time (04:05 UTC) on March 21, 2006, Larry had been downgraded to a tropical depression several hours before, and wind speeds had dropped to below 60 kilometers per hour (40 miles per hour). But while Larry's winds had dropped down to much less destructive levels, the storm system was still bringing significant rainfall in the upper reaches of the Darling River basin, and it retained the classical spiral form of a tropical storm even as it continued to become less organized. NASA image created by Jesse Allen, Earth Observatory, using data obtained courtesy of the MODIS Rapid Response team. |
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Tropical Cyclone Monica
| Title |
Tropical Cyclone Monica |
| Description |
Tropical Cyclone Monica formed off the northeastern coast of Australia on April 17, 2006. This is the same general area where Cyclone Larry [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=13431 ] formed a month earlier. Larry caused devastation to Queenland's coastal communities and destroyed a large fraction of the banana trees in the region. Cyclone Monica was not predicted to be anywhere near as destructive as Larry, and according to the Australian Bureau of Meteorology [ http://www.bom.gov.au/ ], Monica was expected to cross Cape York in northern Queensland well away from most settled areas, limiting the damage it was predicted to cause. This photo-like image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on the Terra [ http://terra.nasa.gov/ ] satellite on April 18, 2006, at 10:35 a.m. local time (00:35 UTC). Cyclone Monica at this time had a basic spiral form, but lacked the well-developed eye and tight-wound shape of a powerful storm. Sustained, peak winds in the storm system were roughly 100 kilometers per hour (65 miles per hour) around the time the image was captured. NASA image by Jesse Allen, Earth Observatory, using data obtained from the Goddard Earth Sciences DAAC. [ http://daac.gsfc.nasa.gov/ ] |
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Tropical Cyclone Monica
| Title |
Tropical Cyclone Monica |
| Description |
Tropical Cyclone Monica formed off the northeastern coast of Australia on April 17, 2006. This is the same general area where Cyclone Larry [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=13431 ] formed a month earlier. Cyclone Monica was not anywhere near as destructive as Larry when it crossed Cape York Peninsula, but when the tropical cyclone reached the warm waters of the Gulf of Carpentaria on the other side, it re-organized and re-intensified. Cyclone Monica became the strongest storm of the 2006 Australian cyclone season with wind gusts reaching 350 kilometers per hour (215 miles per hour) according to the Australian Bureau of Meteorology's Cyclone Warning Centre. The Category 5 cyclone came ashore on the sparsely populated coastline of the Northern Territory, missing the city of Darwin, which had been bracing for a record storm. This photo-like image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on the Terra [ http://terra.nasa.gov/ ] satellite on April 26, 2006, at 10:55 a.m. Australian Central Standard Time (01:25 UTC). Monica by this point had fallen apart quite rapidly, and it was already below cyclone strength. Only vague remnants of its tight spiral formation could be made out in this image. However, it continued to bring very heavy rains as it traveled across the Northern Territory, with record rainfalls throughout the region. It is unusual for such a strong storm to show up so late in the season: the Northern Territory's "wet" season (the local name for the five months from December through April when heavy rains and cyclones are common) has only a few more days left. NASA image by Jesse Allen, Earth Observatory, using data obtained from the Goddard Earth Sciences DAAC. [ http://daac.gsfc.nasa.gov/ ] |
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Tropical Cyclone Monty
| Title |
Tropical Cyclone Monty |
| Description |
The Multi-angle Imaging SpectroRadiometer (MISR) acquired these natural color images and cloud top height measurements for Monty before and after the storm made landfall over the remote Pilbara region of Western Australia, on February 29 and March 2, 2004 (shown as the left and right-hand image sets, respectively). On February 29, Monty was upgraded to category 4 cyclone status. After traveling inland about 300 kilometers to the south, the cyclonic circulation had decayed considerably, although category 3 force winds were reported on the ground. Some parts of the drought-affected Pilbara region received more than 300 millimeters of rainfall, and serious and extensive flooding has occurred. The natural color images cover much of the same area, although the right-hand panels are offset slightly to the east. Automated stereoscopic processing of data from multiple MISR cameras was utilized to produce the cloud-top height fields. The distinctive spatial patterns of the clouds provide the necessary contrast to enable automated feature matching between images acquired at different view angles. The height retrievals are at this stage uncorrected for the effects of the high winds associated with cyclone rotation. Areas where heights could not be retrieved are shown in dark gray. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously and every 9 days views the entire globe between 82 degrees north and 82 degrees south latitude. These data products were generated from a portion of the imagery acquired during Terra orbits 22335 and 22364. The panels cover an area of about 380 kilometers x 985 kilometers, and utilize data from blocks 105 to 111 within World Reference System-2 paths 115 and 113. MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center, Greenbelt, MD. JPL is a division of the California Institute of Technology. Image courtesy NASA/GSFC/LaRC/JPL MISR Team [ http://www-misr.jpl.nasa.gov/ ], caption courtesy Clare Averill, Raytheon/Jet Propulsion Laboratory. |
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Tropical Cyclone Monty
| Title |
Tropical Cyclone Monty |
| Description |
The Multi-angle Imaging SpectroRadiometer (MISR) acquired these natural color images and cloud top height measurements for Tropical cyclone Monty before and after the storm made landfall over the remote Pilbara region of Western Australia, on February 29 and March 2, 2004 (shown as the left and right-hand image sets, respectively). On February 29, Monty was upgraded to category 4 cyclone status. After traveling inland about 300 kilometers to the south, the cyclonic circulation had decayed considerably, although category 3 force winds were reported on the ground. Some parts of the drought-affected Pilbara region received more than 300 millimeters of rainfall, and serious and extensive flooding has occurred. The natural color images cover much of the same area, although the right-hand panels are offset slightly to the east. Automated stereoscopic processing of data from multiple MISR cameras was utilized to produce the cloud-top height fields. The distinctive spatial patterns of the clouds provide the necessary contrast to enable automated feature matching between images acquired at different view angles. The height retrievals are at this stage uncorrected for the effects of the high winds associated with cyclone rotation. Areas where heights could not be retrieved are shown in dark gray. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously and every 9 days views the entire globe between 82 degrees north and 82 degrees south latitude. The MISR Browse Image Viewer [ http://earthobservatory.nasa.gov/cgi-bin/redirect?http://eosweb.larc.nasa.gov/MISRBR/ ] provides access to low-resolution true-color versions of these images. These data products were generated from a portion of the imagery acquired during Terra orbits 22335 and 22364. The panels cover an area of about 380 kilometers x 985 kilometers, and utilize data from blocks 105 to 111 within World Reference System-2 paths 115 and 113. Image courtesy NASA/GSFC/LaRC/JPL, MISR Team. [ http://earthobservatory.nasa.gov/cgi-bin/redirect?http://www-misr.jpl.nasa.gov/ ] Text by Clare Averill (Raytheon/JPL). |
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Tropical Cyclone Wati
| Title |
Tropical Cyclone Wati |
| Description |
Tropical Cyclone Wati formed northeast of New Caledonia on March 19, 2006. The cyclone gained power gradually and had been heading towards the coast of Australia along a track similar to the very destructive Cyclone Larry, which came ashore in Queensland at the same time Wati was building power. However, forecasts as of March 22 projected that while Wati would continue to gain strength, it would turn sharply south and east, staying well away from the Australian mainland and New Calendonia. When the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite observed the storm at 3:05 p.m. Australian Eastern Daylight Savings Time (04:05 UTC) on March 21, 2006, Tropical Cyclone Wati was continuing to slowly build power and size. When MODIS made this observation, the storm had peak winds of around 150 kilometers per hour (90 miles per hour), and forecasts at the time called for it to continue to gather power for at least another day. It was predicted to slowly weaken as it headed south and traveled over cooler water. In this image, the scattered and unorganized remnants of Tropical Cyclone Larry can still be seen over Queensland, well east of Cyclone Wati. NASA image created by Jesse Allen, Earth Observatory, using data obtained courtesy of the MODIS Rapid Response team. |
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Tropical Cyclone Wati
| Title |
Tropical Cyclone Wati |
| Description |
Tropical Cyclone Wati formed northeast of New Caledonia on March 19, 2006. The cyclone gained power gradually and had been heading towards the coast of Australia along a track similar to the very destructive Cyclone Larry, which came ashore in Queensland at the same time Wati was building power. However, forecasts as of March 21 projected that while Wati would continue to gain strength, it would turn sharply south and east, staying well away from the Australian mainland and New Calendonia. When the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite observed the storm at 2:55 p.m. Australian Eastern Daylight Savings Time (03:55 UTC) on March 21, 2006, Tropical Cyclone Wati was continuing to slowly build power and size. When MODIS made this observation, the storm had peak winds of around 120 kilometers per hour (75 miles per hour), and forecasts at the time called for it to continue to gather power for at least another day. It was predcited to slowly weaken as it headed south and traveled over cooler water. NASA image created by Jesse Allen, Earth Observatory, using data obtained courtesy of the MODIS Rapid Response team. |
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