A Millennium Symposium on Atmospheric Chemistry: Past, Present, and Future of Atmospheric Chemistry

3.1

Tropospheric ozone pollution from space: new views from the TOMS (Total Ozone Mapping Spectrometer) Instrument

Anne M. Thompson, NASA/GSFC, Greenbelt, MD; and R. D. Hudson, A. D. Frolov, J. C. Witte, and T. Kucsera

New products from the TOMS (Total Ozone Mapping Spectrometer) satellite instrument can resolve pollution events in tropical and mid-latitudes. Over the past several years, we have developed tropospheric ozone data sets by two methods. The modified-residual technique [Hudson and Thompson, 1998; Thompson and Hudson, 1999] uses v. 7 TOMS total ozone and is applicable to tropical regimes in which the wave-one pattern in total ozone is observed. The TOMS-direct method [Hudson et al., 2000] represents a new algorithm that uses TOMS radiances to extract tropospheric ozone in regions of constant stratospheric ozone and tropospheric ozone displaying high mixing ratios and variability characteristic of pollution. Absorbing aerosols (dust and smoke; Herman et al., 1997; Hsu et al., 1999), a standard TOMS product, provide transport and/or source marker information to interpret tropospheric ozone. For the Nimbus 7/TOMS observing period (1979-1992), modified-residual TTO (tropical tropospheric ozone) appears as two maps/month at 1-degree latitude x 2-degree longitude resolution at a homepage and digital data are available (20S to 20N) by ftp at http://metosrv2. umd.edu/~tropo/ 14y_data.d. Preliminary modified-residual TTO data from the operational Earth-Probe/TOMS (1996- present) are posted in near-real-time at the same website. Analyses with the new tropospheric ozone and aerosol data are illustrated by the following: (1) Signals in tropical tropospheric ozone column and smoke amount during ENSO (El Ni§o-Southern Oscillation) events, e.g. 1982-1983 and the intense ENSO-induced biomass fires of 1997-1998 over the Indonesian region [Thompson et al, 2000a; Thompson and Hudson, 1999]. (2) Trends in tropospheric ozone and smoke aerosols in various tropical regions (Atlantic, Pacific, Africa, Brazil). No significant trends were found for ozone from 1980-1990 [Thompson and Hudson, 1999] although smoke aerosols increased during the period [Hsu et al., 1999]. (3) Temporal and spatial offsets ("paradoxes") in tropical tropospheric ozone and smoke aerosol in regions of greatest tropical biomass burning [Thompson et al., 1996; 2000b]. (4) Trans-boundary pollution tracking. With an air parcel (trajectory) model, smoke aerosol and ozone and dust plumes can be tracked across oceans (e.g., Asia to North America; North America to Europe) and national boundaries, e.g. Indonesia to Singapore and Malaysia during the 1997 ENSO fires.

Session 3, The Role of Satellites in Tropospheric Chemistry Measurements
Tuesday, 16 January 2001, 9:00 AM-10:58 AM

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