Strong Tropical Storm Harvey Comes Ashore

The TRMM satellite had an excellant daylight view of tropical storm Harvey on 20 August 2011 at 1744 UTC ( 1:44 PM EDT) as the storm was coming ashore in Belize. An Air Force Reserve aircraft reported to the National Hurricane Center that Harvey's winds had increased to 63 kts (~72.5 mph) just before landfall. TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) data show that heavy thunderstorms were occurring over land northwest of the storm's center.

Colder Water Chills Fernanda

Ocean water warmer than 26C is a necessary condition for tropical cyclones to support convection. A TMI based Sea Surface Temperature (SST) analysis for three days ending on 18 August 2011 is shown above. Tropical Storm Fernanda's path (overlaid in white) recently took it over ocean waters colder than 26 Celcius so it has weakened considerably. The TRMM satellite passed over Fernanda on 19 August 2011 at 0648 UTC. The TMI and PR rainfall analysis from this pass shows that there is now very little rainfall with the weakening storm. See earlier news about Tropical Storm Fernanda

Tropical Depression 08L Forms In The Caribbean

The TRMM satellite had a good daytime view of the tropical wave that was upgraded to the Atlantic Ocean basin's eighth tropical depression on 19 August 2011 at 0300 UTC (18 August 11 PM EDT). An image from TRMM's pass on 18 August 2011 at 1757 UTC (1:37 PM EDT) is displayed above and reveals that the precipitation pattern was getting a little better organized but heavy rainfall didn't cover a large portion of 08L at that time. Tropical depression 08L is predicted by the National Hurricane Center (NHC) to weaken to a remnant low in the next three days while producing rain over Honduras

Tropical Cyclone Forming in the Caribbean

On 18 August 2011 at 0307 UTC (11:07 PM EDT) the TRMM satellite traveled above an area of organized shower activity in the Caribbean Sea that the National Hurricane Center (NHC) forecasts will soon become a tropical cyclone. TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) data show that this tropical wave south of Jamaica contained several areas of convective thunderstorms that were dropping rainfall at the rate of over 40 mm/hr (~1.6 inches). TRMM's PR data show that some thunderstorm towers in this stormy area were higher than 13 km (~8 miles).

Tropical Storm Greg Forms

A tropical depression (7E) off the southern coast of Mexico was upgraded by the National Hurricane Center (NHC) to tropical storm Greg shortly after the TRMM satellite saw it on 17 August 2011 at 0534 UTC. TRMM's Microwave Imager (TMI) showed that intense convective thunderstorms within the developing storm were dropping rainfall at rates greater than 30mm/hr (1.2 inches) in an area near the center of the storm. Greg is expected to enhance rainfall over the southwest coastline of mexico for the next day or so. Greg is forecast by the NHC to intensify to hurricane strength within 24 hours while

High Gain Antenna System (HGAS) Completes Deployment Testing

The High Gain Antenna System (HGAS) onboard the GPM Core Observatory finished acoustics and post-environmental deployment testing at NASA Goddard Space Flight Center. The HGAS will then undergo Thermal Vacuum testing before it is completed and delivered in mid-September. The below video shows a test of the High Gain Antenna System as it will deploy once in orbit aboard the GPM Core Observatory. Learn more about the HGAS and the GPM Core Observatory

TD06 Becomes Tropical Storm Fernanda

The National Hurricane Center (NHC) upgraded tropical depression 06E to tropical storm Fernanda on 16 August 2011 at 0800 UTC after seeing data from a TRMM pass at that time. A rainfall analysis from TRMM Microwave Imager (TMI) rainfall data shows that Fernanda contains areas of heavy rainfall. Fernanda was located about 2378 km (~1478 miles) east-southeast of the Hawaiian Islands with wind speeds of about 45 kts (~52 mph) and was moving toward the west at about 8 kts (~9.2 mph). The NHC discussion says that computer guidance indicates considerably more intensification is possible with