TRMM News

Tropical Storm Rafael Getting Stronger A low pressure center in the eastern Caribbean Sea became tropical storm Rafael on Friday October 12, 2012. The tropical storm wasn't very well organized until today but the National Hurricane Center (NHC) predicts that Rafael will become a hurricane this evening. The TRMM satellite saw most of Rafael on October 15, 2012 at 0218 UTC (10:18 PM EDT October 14) and collected data used in the rainfall analysis on the right.

Hurricane Rafael has started to pick up speed after it passed to the east of Bermuda. This image shows a TRMM rainfall analysis that used data collected from two recent passes above Hurricane Rafael. The first orbit was on Tuesday October 16, 2012 at 2250 UTC (6:50 PM EDT). The second orbit received data when TRMM passed over on Wednesday October 17, 2012 at 0028 UTC (8:28 PM EDT on October 16, 2012). TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) data show that Rafael was producing rainfall over a large area of the Atlantic. Bermuda was shown getting light to moderate rain showers

Yesterday Sandy dropped to tropical storm intensity but the National Hurricane Center (NHC) decided on October 27,2012 at 1500 UTC (11 AM EDT) that Sandy was again a minimal hurricane. The rainfall analysis on the right was made from TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) data collected when TRMM flew above less than an hour later at 1552 UTC (11:52 AM EDT). This analysis includes some rainfall that was beyond the reach of land based radar observations.

Hurricane Sandy, located east of the Carolina's, has maintained minimal hurricane strength while following it's forecast track toward the northeast. The National Hurricane Center (NHC) predicts that Sandy will make a turn toward the Mid-Atlantic coast tomorrow. As a post-tropical low Sandy is then predicted to produce extremely heavy rainfall and dangerously high winds over a large area of the North-East after landfall. The TRMM satellite collected data when it flew over hurricane Sandy again today at 1456 UTC (10:56 AM EDT). An analysis of rainfall from TRMM's Microwave Imager (TMI) and

The reported death toll from hurricane Sandy's flooding and high winds has now reached above 120. Over 70 deaths were caused by Sandy in the Caribbean and recent reports bring the total to greater than 50 in the United States. Much of the recent deadly flooding along the northeastern United States coastlines was caused by super storm Sandy's storm surge. Strong winds from Sandy persistently pushed Atlantic ocean waters toward the coast. High tides that occurred at the same time also magnified the effects of the storm surge. Some flooding was also caused by long periods of heavy rainfall that

Over the past two weeks, a combination of the southwest monsoon and tropical cyclones passing in the vicinity of the northern Philippines has resulted in massive flooding in and around the Philippine capital. It is the worst flooding there since Typhoon Ketsana in 2009, which devastated Manila and killed over 400 people throughout the country. The current flooding began at the end of July with the passing of Typhoon Saola (known as Gener in the Philippines) northeast of Luzon. Although the center of Saola made landfall in northern Taiwan and passed well to the east of Luzon, the storm's

The TRMM satellite saw Ernesto on August 9, 2012 at 0656 UTC ( 2:36 AM EDT) after the tropical storm had moved from the Yucatan Peninsula into the Gulf of Mexico. An analysis of TRMM Microwave Imager (TMI) and Precipitation Radar (PR) rainfall is shown in the image above. This analysis shows that powerful convective thunderstorms were dropping rain at a rate greater than 50mm/hr (~2 inches) north of the storm's center. TRMM Precipitation Radar (PR) data were used in the image below to show a 3-D view of Ernesto's vertical structure. This PR view shows that a few of the powerful convective

The TRMM satellite passed over tropical storm Ernesto on 7 august 2012 at 0711 UTC ( 3:11 AM EDT) as it was heading toward the Yucatan Peninsula. TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) instruments show that Ernesto was a little better organized with bands of moderate to occasionally heavy rainfall spiraling into the center of the storm's circulation. A few powerful convective storms are shown located in these widely separated rain bands. The National Hurricane Center (NHC) predicts that Ernesto will be a category one hurricane on the Saffir-Simpson scale with winds of about

The TRMM satellite had a good view of Typhoon Haikui on August 6, 2012 at 1857 UTC as it was moving toward China. At that time Haikui was a category one typhoon on the Saffir-Simpson hurricane intensity scale with wind speeds of 65 kts (~75 mph). Data from TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) instruments show bands of moderate to heavy rainfall around Haikui's large eye. TRMM PR data were also used to show a 3-D cross section through Haikui's eye. This view shows that intense rainfall (45 dBZ) was occurring in the eastern side of Haikui's eye. Typhoon Haikui weakened

The South Pacific hurricane season normally ends in April but tropical cyclone 21P has developed in the South Pacific Ocean between Papua New Guinea and the Solomon Islands. The center of the tropical cyclone was directly beneath the TRMM satellite when it passed over on 28 June 2012 at 2225 UTC (~8:25 AM Local time). A rainfall analysis using data from TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) instruments shows that the tropical cyclone, although small, was well organized and contained some intense convective storms dropping rainfall at a rate of over 50mm/hr (~2 inches). A 3