HR: 11:35h
AN: AE32A-05 [Abstracts]
TI: Electric Field and Microphysics of Hurricanes
AU: * Bateman, M G
EM: monte.bateman@msfc.nasa.gov
AF: Universities Space Research Association, 320 Sparkman Dr, Huntsville, AL 35805
United States
AU: Blakeslee, R J
EM: richard.blakeslee@nasa.gov
AF: NASA/MSFC, 320 Sparkman Dr, Huntsville, AL 35805
United States
AU: Mach, D M
EM: doug.mach@msfc.nasa.gov
AF: University of Alabama in Huntsville, 320 Sparkman Dr, Huntsville, AL 35805
United States
AU: Bailey, J C
EM: jeff.bailey@msfc.nasa.gov
AF: Raytheon/ITSS, 320 Sparkman Dr, Huntsville, AL 35805
United States
AB:
The Tropical Cloud Systems and Processes (TCSP) project was a campaign to primarily study tropical storm and hurricane
genesis, based in San José, Costa Rica, during July 2005. The main research platform was a NASA ER-2, high altitude
(~21 km) aircraft, which carried a number of instruments, including the Lightning Instrument Package consisting of
electric field mills and an air conductivity probe, two Doppler radar systems, and the Advanced Microwave Precipitation
Radiometer (AMPR). The field mills allow us to determine the vector electric field along the aircraft path. The AMPR allows
us to determine ice particle concentration from passive microwave ice scattering signatures. TCSP was the third program in
which we have measured electrification above hurricanes. In the previous programs, we have found oceanic hurricanes to be at
most only weakly electrified with little or no lightning in the central part of the storm. During the flight over Hurricane
Emily (17 July 2005) we found strong electrification and significant lightning flash rates (over 9 flashes/min) in the eye
wall. The ER-2 made several passes over and around the eyewall of Hurricane Emily during the flight. During the overpasses,
the hurricane was almost constantly producing lightning. Vaisala's long range lightning detection system indicated that this
remarkable lightning activity in the storm core persisted for several hours. We present the vector electric field, lightning
rates, passive microwave microphysics, and Doppler radar data from Hurricane Emily and compare these observations with data
from other hurricanes we have studied. We will address the question as to why Hurricane Emily was electrically so different
from the other tropical storms.
UR: http://tcsp.nsstc.nasa.gov
DE: 0320 Cloud physics and chemistry
DE: 3304 Atmospheric electricity
DE: 3324 Lightning
DE: 3339 Ocean/atmosphere interactions (0312, 4504)
DE: 3374 Tropical meteorology
SC: Atmospheric and Space Electricity [AE]
MN: Fall Meeting 2005