TRMM

Hurricane Kenneth (in the eastern Pacific Ocean) reached powerful category four hurricane strength with wind speeds of 125 kts (~144 mph) on Tuesday 22 November 2011. The TRMM satellite passed directly above Kenneth as it was rapidly weakening on Wednesday 23 November 2011 at 0455 UTC. A rainfall analysis from TRMM's Micrwave Imager (TMI) and Precipitation Radar (PR) instruments is shown overlaid on an infrared image from TRMM's Visible and InfraRed Scanner (VIRS). Very heavy rainfall of over 50mm/hr (~2 inches) is shown by this analysis occurring in the northeastern side of Kenneth's eye wall

The TRMM satellite had a good view of tropical storm Kenneth in the eastern Pacific Ocean when it passed above on 21 November 2011 at 0510 UTC (20 November 2011 9:10 PM PST). The National Hurricane Center (NHC) upgraded Kenneth to a hurricane on 21 November 2011 at 1500 UTC (7:00 AM PST) after determining that a ragged eye was forming. The image on the right shows a rainfall analysis derived from TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) instruments. TMI data show that heavy rainfall was occurring around the center of Kenneth's circulation.

Tornadoes are expected to accompany severe storms in the springtime in the U.S., but this time of year they also usually happen. When a line of severe thunderstorms associated with a cold front swept through the U.S. southeast on Nov. 16, TRMM collected rainfall data on the dangerous storms from space. TRMM's Precipitation Radar (PR) data was used to show the line of severe thunderstorms in 3-D. The line of storms were pushing through North and South Carolina on Nov. 16, 2011. Strong updrafts had pushed precipitation within some of these storms to heights of 15km (9.3 miles). Credit: SSAI/NASA

The TRMM satellite had a good look at tropical storm Sean when it flew over on 10 November 2011 at 0541 UTC (00:41 AM EST). TRMM's Precipitation Radar (PR) data were used in the image above to show a 3-D cross section through Sean. TRMM's PR revealed that heights of storms in the edge of Sean's center of circulation were reaching to about 11km (~6.8 miles). Radar Reflectivity values of up to 46.0 dBZ found in these storms also showed that rainfall was heavy in that area. The "top down" satellite view above shows that those storms in Sean's northwestern quadrant were the most powerful. The rest

The Joint Typhoon Warning Center (JTWC) issued it's last warning on dissipating tropical depression 04W in the Arabian Sea on 9 November 2011 at 1500 UTC. A rainfall analysis from TRMM data collected with a pass over 04A on 9 November 2011 at 1530 UTC is shown here. Data from TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) show that heavy rainfall was extending from 04A's location in the Arabian Sea north-eastward toward Pakistan.

The National Hurricane Center (NHC) upgraded a low pressure center in the Atlantic Ocean to subtropical storm Sean at 0900 UTC ( 4:00 AM EDT). The TRMM satellite flew directly above Sean a little earlier on 8 November 2011 at 0731 UTC ( 2:31 AM EDT) collecting data used in the precipitation analyses shown. TRMM Precipitation Radar (PR) data in the 3-D display above show that scattered moderate storms within Sean were reaching maximum heights of only about 11km (~6.8 miles). The "top down" view on the right above shows that Sean was well organized but most rainfall was of low to moderate

On November 2011 at 1541 UTC the TRMM satellite passed over another stormy area heading toward Oman from the Arabian sea . Another tropical cyclone may be forming in this area less than a week after deadly tropical storm Keila hit Oman. A rainfall analysis from TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) is shown in the image above. Rainfall derived from PR data, shown in a lighter shade, reveals that an area of extremely heavy rainfall was located in the center of this stormy area. TRMM's PR data were again used to show the 3-D structure of this stormy area. Some of these very

Tropical storm Kelia caused the reported deaths of at least 11 people when it came ashore in Oman on Thursday 3 November 2011. TRMM's Microwave Imager (TMI) had a good early morning view of Keila on 3 November 2011 at 0254 UTC. The TMI rainfall analysis from these data was overlaid on a sunlit visible and infrared image from TRMM's Visible and InfraRed Scanner (VIRS). This rainfall analysis shows a large band of moderate to heavy rainfall wrapping around the eastern side of the storm and drenching coastal Oman.

The TRMM satellite again flew over tropical storm Keila in the Arabian Sea on November 2, 2011 at 1842 UTC. Data received with that orbit shows that although Keila was weakening it was still producing some very powerful storms off the coast of Oman. A rainfall analysis from TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) indicates that these storms were dropping rain at a rate of over 50mm/hr (~2 inches). TRMM PR data were used in the image above to show the 3-D vertical structure of those storms. Some extremely powerful storms in the band of rainfall off the coast of Oman were

The TRMM satellite passed directly above a recently formed tropical cyclone in the Arabian Sea on November 2, 2011 at 0350 UTC. An analysis of rainfall from TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) instruments is shown in the image on the upper left. TRMM data shows that rainfall rates with tropical storm Keila ranged from light to moderate along the south-eastern coast of Oman. Moderate to heavy rainfall was revealed to be spiraling into Keila's center of circulation in the Arabian Sea near the southeastern coast of Oman. The image above is a rendering that shows Keila's