Browse All : Tropical Cyclone and Aqua from 2007

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Tropical Cyclone Favio
Title Tropical Cyclone Favio
Description Tropical Cyclone Favio formed in the western Indian Ocean about 1,200 kilometers from Madagascar on February 14, 2007. It gradually moved southwest, passing well offshore of Reunion and Mauritius Islands. By February 20, it was just off the southern shore of Madagascar as a well-formed, mature storm. While the storm system had largely skirted around populated areas to that point, forecasters were concerned about its behavior as it entered the warmer waters of the Mozambique Channel. The storm was forecast to reach Category Four [ http://www.nhc.noaa.gov/aboutsshs.shtml ] strength before coming ashore and tracking inland through Zimbabwe and Zambia, bringing heavy rains to already flooded areas. [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=14115 ] 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 February 20, 2007, at 2:15 p.m. local time (11:15 UTC). The storm was turning north around the southern end of Madagscar, headed for the Mozambique Channel. Favio had the recognizable shape of a southern-hemisphere tropical cyclone, with spiral arms showing its clockwise rotation. The spiral arms are well-defined and tightly wound. A distinct eye at the center of the storm is only partially filled with clouds (a "partially closed" eye). These are all signs of a well-developed and powerful storm, consistent with the cyclone's strength. According to the University of Hawaii's Tropical Storm Information Center, [ http:/NaturalHazards/natural_hazards_v2.php3 www.solar.ifa.hawaii.edu/Tropical/ ] Favio had steady winds of around 160 kilometers per hour (100 miles per hour) around the time MODIS made this observation. 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 Cyclone Favio KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Feb2007/Favio.A2007051.1115.250m.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.
Tropical Cyclone Favio
Title Tropical Cyclone Favio
Description Tropical Cyclone Favio came ashore on the coast of Mozambique on the morning of February 22, 2007. At the time it crossed the shoreline, Favio had lost some strength from its peak the previous day, but still had extremely powerful winds. The cyclone continued to weaken as it passed over land, becoming a tropical depression. As of 8:00 a.m. local time (0600 UTC), winds were down to 60 kilometers per hour (38 miles per hour), according to the South African Weather Service. [ http://www.weathersa.co.za/ ] 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 February 23, 2007, at 1:45 p.m. local time (11:45 UTC), as the tropical depression was crossing into Zimbabwe. The storm still has a distinct balled-up form left over from its cyclone state the previous day, but once over land, the strong circular eye and powerful eyewall storms typical of a cylone were gone. As it traveled farther inland towards the Zambezi River valley, the storm brought heavy rains to Zimbabwe. This region had already suffered from heavy rains associated with the onset of the monsoon, and severe flooding along the Zambezi River [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=14115 ] in mid-February killed dozens of people and forced more than a hundred thousand people to evacuate, according to reports [ http://www.reliefweb.int/rw/RWB.NSF/db900SID/LSGZ-6YMDSC?OpenDocument ] from the International Federation of Red Cross and Red Crescent Societies posted online by ReliefWeb. [ http://www.reliefweb.int/rw/dbc.nsf/doc100?OpenForm ] There had been widespread additional evacuations ahead of Cyclone Favio's arrival. You can download a 250-meter-resolution Cyclone Favio KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Feb2007/favio_amo_2007054.kmz ] for use with Google Earth. [ http://earth.google.com/download-earth.html ] NASA image by Jesse Allen, using data provided courtesy of the MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center.
Tropical Cyclone Gamede
Title Tropical Cyclone Gamede
Description Tropical Cyclone Gamede was in the western Indian Ocean off the shore of Madagascar on February 26, 2007. This powerful storm had been moving southward parallel to the eastern coast of Madagascar for two days at this time, bringing heavy rains and strong surf to Madagascar and the two major Mascarene Islands, Reunion and Mauritius. The storm seemed to be staying away from settled areas, but reports from the Joint Typhoon Warning Center [ https://metocph.nmci.navy.mil/jtwc.php ] and U.K. Accuweather [ http://ukie.accuweather.com/ ] noted strong surf on the coast and island shorelines, as well as heavy rain. This same area was brushed by Cyclone Favio [ http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=14136 ] just days before, and it suffered a series of severe storms and cyclones in preceding months. Unlike Favio, Gamede was predicted to continue on its generally southward track and not turn towards mainland Africa. 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 February 26, 2007, at 11:50 a.m. local time (9:50 UTC). The storm was a mature and powerful tropical cyclone, with a well-defined eye at its center and far-reaching, tightly wound spiral arms. According to the University of Hawaii's Tropical Storm Information Center, [ http://www.solar.ifa.hawaii.edu/Tropical/ ] Cylone Gamede has sustained winds of 175 kilometers per hour (110 miles per hour) around the eyewall at the time this image was acquired. Forecasts at the time called for the storm to avoid landfall, but to continue its grazing path between the Mascarene Islands and Madagascar, with winds continuing to intensify as the storm traveled south over warm waters. NASA image by Jesse Allen, using data provided courtesy of the MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center.
Tropical Cyclone Gamede
Title Tropical Cyclone Gamede
Description Tropical Cyclone Gamede was sitting in the western Indian Ocean off the shore of Madagascar on February 25, 2007. This powerful storm had been bringing heavy rains and strong surf to eastern Madagascar and the two major Mascarene Islands of Reunion and Mauritius. No settled land areas were experiencing the full brunt of of the sustained winds in the eyewall of the storm (reported at 195 kilometers per hour (120 miles per hour) by the Joint Typhoon Warning Center, [ https://metocph.nmci.navy.mil/jtwc.php ]) but damaging winds of 60 to 100 km/hr were recorded on the islands. One rainfall gauge measured totals as high as 47 centimeters over the three days Gamede was in the area, according to U.K. Accuweather. [ http://ukie.accuweather.com/ ] This photo-like image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on NASA's Aqua [ http://aqua.nasa.gov/ ] satellite on February 25, 2007, at 11:50 a.m. local time (9:50 UTC), as the storm sat in the region between the small islands and Madagascar. At that time, it appeared the storm would head roughly south, bringing more winds and rain to the Mascarene Islands but not coming ashore onto Madagascar. Since the island had been pummeled by a series of tropical cyclones and storms in preceding months, Gamede was being watched with great care and concern by residents of the islands. The image provided above is at 1 kilometer resolution, less than the full level of detail possible from the MODIS instrument. The MODIS Rapid Response System provides this image at additional resolutions. [ http://rapidfire.sci.gsfc.nasa.gov/gallery/?2007056-0225/ ] Their image collection also includes the distant, but neighboring Cyclone Humba in the central Indian Ocean. NASA image by Jeff Schmaltz, MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center.
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.
Tropical Cyclone Gonu
Title Tropical Cyclone Gonu
Description MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center., You might expect to see a storm with near-perfect symmetry and a well-defined eye hovering over the warm waters of the Caribbean or in the South Pacific, but Tropical Cyclone Gonu showed up in an unusual place. On June 4, 2007, when the Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Aqua [ http://aqua.nasa.gov/ ] satellite captured this image, Tropical Cyclone Gonu was approaching the northeastern shore of Oman, a region better known for hot desert conditions. Though rare, cyclones like Gonu are not unheard of in the northern Indian Ocean basin. Most cyclones that form in the region form over the Bay of Bengal, east of India. Those that take shape over the Arabian Sea, west of the Indian peninsula, tend to be small and fizzle out before coming ashore. Cyclone Gonu is a rare exception. As of June 4, 2007, the powerful storm had reached a dangerous Category 4 [ http://www.nhc.noaa.gov/aboutsshs.shtml ] status, and it was forecast to graze Oman's northeastern shore, following the Gulf of Oman. According to storm statistics maintained on Unisys Weather, [ http://weather.unisys.com/hurricane/ ] the last storm of this size to form over the Arabian Sea was Cyclone 01A, which tracked northwest along the coast of India between May 21 and May 28, 2001. Unlike Gonu's forecasted track, Cyclone 01A's path never brought it ashore. MODIS acquired this photo-like image at 12:00 p.m. local time (9:00 UTC), a few hours after the Joint Typhoon Warning Center [ https://metocph.nmci.navy.mil/jtwc.php ] estimated Gonu's sustained winds to be over 240 kilometers per hour (145 miles per hour). The satellite image confirms that Gonu was a super-powerful cyclone. The storm has the hallmark tightly wound arms that spiral around a well-defined, circular eye. The eye is surrounded by a clear wall of towering clouds that cast shadows on the surrounding clouds. Called hot towers, [ http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=17662 ] these clouds are a sign of the powerful uplift that feeds the storm. The symmetrical spirals, clear eye, and towering clouds are all features regularly seen in satellite images of other particularly powerful cyclones, which are also known as typhoons or hurricanes when they form in other parts of the world. 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/?2007155-0604/Gonu.A2007155.0900 ] You can download a 250-meter-resolution Cyclone Gonu KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Jun2007/Gonu.A2007155.0900.250m.kmz ] for use with Google Earth. [ http://earth.google.com/download-earth.html ] NASA image by Jeff Schmaltz,
Tropical Cyclone Gonu
Title Tropical Cyclone Gonu
Description A cyclonic storm like Tropical Cyclone Gonu might not seem an odd sight until you consider that Gonu is heading northwest into the Gulf of Oman. The most recent storm of this magnitude to hit the Sultanate of Oman was in 1977, according to AlJazerra.net (English language). [ http://english.aljazeera.net/English/ ] Given the rarity of these storms in the area, many shore facilities were never constructed to deal with the severe winds, strong rains, and high storm surge. At 10:15 a.m. local time (07:15 UTC) on June 6, 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, Tropical Cyclone Gonu was grazing the gulf shore of Oman. At this time, the powerful storm had lost considerable power and was considered a Category 1 [ http://www.nhc.noaa.gov/aboutsshs.shtml ] cyclone. Sustained winds were measured at 140 kilometers per hour (85 miles per hour) according to the University of Hawaii's Tropical Storm Information Center. [ http://www.solar.ifa.hawaii.edu/Tropical/ ] The satellite image shows Gonu bringing rain to both Oman and Iran even as the storm center remains offshore in the Gulf of Oman. Hemmed in by hot desert lands and mountains on both sides of the Gulf, Gonu was predicted to continue to move up the Gulf and lose power before making landfall in southeastern Iran. Because such storms are virtually unheard of in this part of the world, authorities treated the storm with considerable caution: government offices in Oman and most private businesses declared a holiday from June 5 until June 9. They recommended people stay in their homes as much as possible and stock basic supplies and emergency needs, according to Middle East Online. [ http://www.middle-east-online.com ] Residents in low-lying coastal areas in southeastern Iran were also being evacuated, while the fishing fleet in neighboring Pakistan was ordered to stay in as waves battered the shores. Gonu, however, did not appear poised to reach the Straits of Hormuz, and oil shipping from the Persian Gulf had not been significantly disrupted as of June 6, according to a number of news services. 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.
Tropical Cyclone Gonu
Title Tropical Cyclone Gonu
Description A cyclonic storm like Tropical Cyclone Gonu might not seem an odd sight until you consider that Gonu occurred in the Gulf of Oman and made landfall in Iran, a nation not known for cyclones. The most recent storm of Gonu's magnitude hit the neighboring Sultanate of Oman was in 1977, according to the news service AlJazerra.net [ http://english.aljazeera.net/English/ ] (English language).Given the rarity of these storms in the area, many shore facilities were never constructed to deal with the severe winds, strong rains, and high storm surge. At 12:55 p.m. local time (09:55 UTC) on June 7, 2007, when the Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Aqua [ http://aqua.nasa.gov/ ] satellite captured this image, Tropical Cyclone Gonu was crossing the Gulf of Oman and heading northward towards the Iranian coast. By this time, the powerful storm had lost considerable power and was considered a mere powerful tropical storm. Sustained winds were measured at 60 kilometers per hour (40 miles per hour) according to the University of Hawaii's Tropical Storm Information Center. [ http://www.solar.ifa.hawaii.edu/Tropical/ ] The satellite image shows Gonu bringing rain to both Oman and Iran as it heads north to the Iranian coastline. Because such storms are virtually unheard of in this part of the world, authorities have treated the storm with considerable caution: government offices in Oman and most private businesses declared a holiday from June 5 until June 9. They recommended people stay in their homes as much as possible and stock basic supplies and emergency needs, according to Middle East Online. [ http://www.middle-east-online.com ] Residents in low-lying coastal areas in southeastern Iran were also being evacuated, while the fishing fleet in neighboring Pakistan was ordered to stay in as waves battered the shores. Gonu, however, did not appear poised to reach the Straits of Hormuz, and oil shipping from the Persian Gulf had not been significantly disrupted as of June 6, according to a number of news services. You can download a 250-meter-resolution Cyclone Gonu KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Jun2007/gonu_amo_2007158.kmz ] for use with Google Earth. [ http://earth.google.com/download-earth.html ] 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.
Tropical Cyclone Jaya
Title Tropical Cyclone Jaya
Description Tropical Cyclone Jaya came ashore in northern Madagascar in the morning of April 2, 2007 at around 11:00 a.m. local time (08:00 UTC). The storm formed in the Indian Ocean on March 30 and traveled westward toward Madagascar as predicted. What was not predicted, however, was its explosive growth in power from a strong tropical storm to a powerful Category 3 cyclone [ http://www.nhc.noaa.gov/aboutsshs.shtml ] in just 36 hours, according to figures provided by the University of Hawaii's Tropical Storm Information Center. [ http://www.solar.ifa.hawaii.edu/Tropical/tropical.html ]Fortunately, the intensification took place while Jaya was still far from Madagascar. 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 April 3, 2007, at 1:15 p.m. local time (10:15 UTC). The storm was a tropical cyclone with a circular shape, but no distinct eye at its center. According to the University of Hawaii's Tropical Storm Information Center, [ http://www.solar.ifa.hawaii.edu/Tropical/ ] Cyclone Jaya's sustained winds had fallen in strength to roughly 125 kilometers per hour (80 mph) at the time this image was acquired. When the storm made landfall on Madagascar, sustained winds were around 150 kilometers per hour (90 miles per hour), a marked change from 200 km/hr (125 mph) just twelve hours earlier. While much weakened, Jaya remained a powerful storm. Furthermore, it struck the northern part of Madagascar where a series of other cyclones have also come ashore in recent months. Forecasters were concerned that Jaya might reform after crossing the island and head inland into Mozambique, where residents are recovering from floods caused by recent heavy rains. 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/?2007093-0403/Jaya.A2007093.1015 ] You can download a 250-meter-resolution Cyclone Jaya KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Apr2007/Jaya.A2007093.1015.250m.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.
Tropical Cyclone Sidr
Title Tropical Cyclone Sidr
Description Tropical Cyclone Sidr was moving north toward the Mouths of the Ganges at a speed of 17 kilometers per hour (10 miles per hour) on November 15, 2007. Winds in the storm's center were raging at 240 km/hr (150 mph), making it a very strong Category 4 [ http://www.nhc.noaa.gov/aboutsshs.shtml ] tropical cyclone, according to the Joint Typhoon Warning Center. [ https://metocph.nmci.navy.mil/jtwc.php ] 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 1:25 p.m. local time (6:55 UTC) on November 15, 2007. With its densely wound clouds and distinct eye, Tropical Cyclone Sidr has the appearance of a well-developed system. The northernmost fringes of the storm already cloud the skies over Bangladesh and India. Western Bangladesh, where the storm appeared to be headed as of November 15, is the most heavily populated low-lying area in the world, with a history of severe causalities from previous storms due to both direct flooding and storm surge. The Joint Typhoon Warning Center [ https://metocph.nmci.navy.mil/jtwc.php ] predicted that the storm would weaken as it made landfall, but would maintain hurricane-force winds well after it moves inland. In 1970, a Category 3 storm that made landfall in the same vicinity caused 300,000 deaths and was one of the most deadly natural disasters in modern history. Another 138,000 people perished in 1991 from a similar cyclone. NASA image created by Jesse Allen, using data provided courtesy of the MODIS Rapid Response [ http://rapidfire.sci.gsfc.nasa.gov/ ] team.
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