HR: 1340h
AN: SA43A-1065 [Abstracts]
TI: Looking at the November 20, 2003 super storm with TIMED/GUVI: Comparison with the TIMEGCM
AU: Meier, R R
EM: meier@uap2.nrl.navy.mil
AF: George Mason University, School of Computational Sciences
4400 University Drive, Fairfax, VA 22030
United States
AU: * Crowley, G
EM: gcrowley@swri.org
AF: Southwest Research Institute, 6220 Culebra Rd, San Antonio, TX 78238
United States
AU: Strickland, D J
EM: dstrick@cpi.com
AF: Computational Physics Inc., 8001 Braddock Rd
Suite 210, Springfield, VA 22151
United States
AU: Christensen, A
EM: andy.christensen@ngc.com
AF: Northrop Grumman Space Technology, One Space Park, Redondo Beach, CA 90278
United States
AU: Paxton, L
EM: larry.paxton@jhuapl.edu
AF: Johns Hopkins University Applied Physics Laboratory, Johns Hopkins Road, Laurel, MD 20723
United States
AU: Morrison, D
EM: danny.morrison@jhuapl.edu
AF: Johns Hopkins University Applied Physics Laboratory, Johns Hopkins Road, Laurel, MD 20723
United States
AB:
During October and November 2003, Earth was subjected to record-class solar flares and geo-effective coronal mass ejections
that caused massive perturbations of the upper atmosphere and ionosphere. Observations of the storm effects are available
from the NASA TIMED satellite. Among the four TIMED instruments is the Global Ultra Violet Imager (GUVI), a far ultraviolet
(FUV) spectrograph that can be operated in imaging or spectrograph modes. GUVI produces images of the far ultraviolet (FUV)
dayglow on both the Earth disk below the satellite and on the limb. Among ionospheric and thermospheric parameters that can
be extracted from the imaging data are maps of the atomic oxygen to molecular nitrogen column density ratio and
altitude-latitude images of the number density and temperature profiles on the limb. GUVI recorded dramatic changes in these
quantities on November 20 and 21, a period when the TIMED orbit was favorable for retrieving composition and temperature from
the limb dayglow. We will review GUVI observations during that storm, showing examples of composition and temperature. These
will be compared with the initial predictions of the Thermosphere Ionosphere Mesosphere Electrodynamics General Circulation
Model. This preliminary comparison reveals many similarities between the model and data. High temperatures seen in the GUVI
data are reproduced in the model. And significant perturbations in the composition are also reproduced by the TIMEGCM. But
significant differences are also noticed in several areas. In particular, GUVI observes a much less rapid recovery of the
perturbed thermosphere than predicted. These and other quantitative conclusions demonstrate that FUV imaging will ultimately
play a major role space weather imaging analogous to that of visible or infrared monitoring in tropospheric weather.
DE: 0310 Airglow and aurora
DE: 0355 Thermosphere--composition and chemistry
DE: 0358 Thermosphere--energy deposition
SC: SPA-Aeronomy [SA]
MN: 2004 AGU Fall Meeting