NASA sees Tropical Cyclone Evan batter and drench Samoan IslandsDecember 14, 2012 in Earth / Earth Sciences
NASA's Tropical Rainfall Measuring Mission or TRMM satellite continues to provide rainfall and cloud height data on powerful Cyclone Evan as it crawls through the Samoan Islands with hurricane-force winds and heavy rains. NASA's TRMM satellite identified "hot towers" in the storm, hinting that it would continue to intensify.
On Dec. 14, American Samoa, Tonga and Fiji are all under warnings or alerts as Evan continues to move west. A gale warning is in effect for Tutuila and Aunuu. A high surf warning is in effect for all of American Samoa. A flash flood watch is in effect for Tutuila and Manua. A tropical cyclone alert is in force for Niuafo'ou and Fiji.
The TRMM satellite had an excellent view of tropical cyclone Evan on Dec. 12, 2012 at 1704 UTC when it was battering the Samoan Islands with hurricane force winds. Evan is predicted by the Joint Typhoon Warning Center (JTWC) to intensify and have winds of 130 knots (~150 mph) while remaining close to the islands. This wind speed would make it a strong Category 3 storm on the Saffir-Simpson Scale. A storm surge of 4.5 meters (14 feet) was already reported along the Samoan coast.
Evan's rainfall was analyzed using TRMM's Microwave Imager (TMI) and Precipitation Radar (PR) data. This analysis showed that the heaviest rainfall of over 80 mm (~3.1 inches) per hour was occurring in heavy rainfall within Evan's clear eye wall. Strong bands of thunderstorms were seen wrapping into the low level center of circulation.
TRMM's Precipitation Radar (PR) data sliced through Evan and were used to provide the 3-D cut-a-way view looking at Evan's northern side. The imagery clearly showed the vertical side surface of Evan's well-defined eye.
TRMM data revealed several "hot towers" or towering thunderstorms reaching heights of greater than 16.5 km (10.25 miles) within Evan's eye wall. A "hot tower" is a tall cumulonimbus cloud that reaches at least to the top of the troposphere, the lowest layer of the atmosphere which extends approximately nine miles (14.5 km) high in the tropics.
These towers are called "hot" because they rise to such altitude due to the large amount of latent heat. Water vapor releases this latent heat as it condenses into liquid. NASA research shows that a tropical cyclone with a hot tower in its eyewall was twice as likely to intensify within six or more hours, than a cyclone that lacked a hot tower.
On Dec. 14 at 1500 UTC (10 a.m. EST) Cyclone Evan had maximum sustained winds near 100 knots (115 mph/185 kph). Cyclone-force winds extend 35 nautical miles (40 miles/64.8 km) out from the center, while tropical-storm-force winds extend up to 105 miles (120.8 miles/194.5 km) from the center.
Evan was centered about 135 nautical miles (155.4 miles/250 km) northwest of Pago Pago, American Samoa, near 12.9 south latitude and 172.5 west longitude. Evan was moving slowly west at 5 knots. Evan is creating very rough seas with waves up to 32 feet (9.7 meters) high. Evan is a threat to American Samoa, Tonga and Fiji.
Evan is moving west away from American Samoa and will later turn southwest, away from American Samoa and is expected to continue to intensify as it moves just north-northwest of Fiji through Dec. 19.
Provided by NASA's Goddard Space Flight Center
"NASA sees Tropical Cyclone Evan batter and drench Samoan Islands" December 14, 2012 https://phys.org/news/2012-12-nasa-tropical-cyclone-evan-batter.html