HR: 0800h
AN: A11C-0598    [Abstracts]
TI: Simulations of Tropospheric NO2 by the Global Modeling Initiative (GMI) Model Utilizing Assimilated and Forecast Meteorological Fields: Comparison to Ozone Monitoring Instrument (OMI) measurements
AU: * Rodriguez, J M
EM: Jose.M.Rodriguez@nasa.gov
AF: NASA/Goddard Space Flight Center, Code 613.3 NASA/Goddard Space Flight Center Greenbelt Road, Greenbelt, MD 20740, United States
AU: Yoshida, Y
EM: yyoshida@hyperion.gsfc.nasa.gov
AF: University of Maryland/Baltimore County, Code 613.3 NASA/Goddard Space Flight Center Greenbelt Road, Greenbelt, MD 20771, United States
AU: Duncan, B N
EM: Bryan.N.Duncan@nasa.gov
AF: University of Maryland/Baltimore County, Code 613.3 NASA/Goddard Space Flight Center Greenbelt Road, Greenbelt, MD 20771, United States
AU: Bucsela, E J
EM: Eric.J.Bucsela@nasa.gov
AF: University of Maryland/Baltimore County, Code 613.3 NASA/Goddard Space Flight Center Greenbelt Road, Greenbelt, MD 20771, United States
AU: Gleason, J F
EM: James.F.Gleason@nasa.gov
AF: NASA/Goddard Space Flight Center, Code 613.3 NASA/Goddard Space Flight Center Greenbelt Road, Greenbelt, MD 20740, United States
AU: Allen, D
EM: allen@atmos.umd.edu
AF: University of Maryland/College Park, Department of Atmospheric and Oceanic Science 3411 Computer and Space Science Building, College Park, MD 20740, United States
AU: Pickering, K E
EM: Kenneth.E.Pickering@nasa.gov
AF: NASA/Goddard Space Flight Center, Code 613.3 NASA/Goddard Space Flight Center Greenbelt Road, Greenbelt, MD 20740, United States
AB: We present simulations of the tropospheric composition for the years 2004 and 2005, carried out by the GMI Combined Stratosphere-Troposphere (Combo) model, at a resolution of 2°x2.5°. The model includes a new parameterization of lightning sources of NOx which is coupled to the cloud mass fluxes in the adopted meteorological fields. These simulations use two different sets of input meteorological fields: a)late-look assimilated fields from the Global Modeling and Assimilation Office (GMAO), GEOS-4 system and b) 12-hour forecast fields initialized with the assimilated data. Comparison of the forecast to the assimilated fields indicates that the forecast fields exhibit less vigorous convection, and yield tropical precipitation fields in better agreement with observations. Since these simulations include a complete representation of the stratosphere, they provide realistic stratosphere-tropospheric fluxes of O3 and NOy. Furthermore, the stratospheric contribution to total columns of different troposheric species can be subtracted in a consistent fashion, and the spatial and temporal patterns of the lightning production of NOx will depend on the adopted meteorological field. We concentrate here on the simulated tropospheric columns of NO2, and compare them to observations by the OMI instrument for the years 2004 and 2005. The comparison is used to address these questions: a) is there a significant difference in the agreement/disagreement between simulations for these two different meteorological fields, and if so, what causes these differences?; b) how do the simulations compare to OMI observations, and does this comparison indicate an improvement in simulations with the forecast fields? c) what are the implications of these simulations for our understanding of the NO2 emissions over continental polluted regions?
DE: 0365 Troposphere: composition and chemistry
DE: 0368 Troposphere: constituent transport and chemistry
SC: Atmospheric Sciences [A]
MN: 2007 Fall Meeting