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Data from the Tropical Rainfall Measuring Mission’s (TRMM) Precipitation Radar (PR) were employed to identify warm<br />

season rainfall (1998-2000) patterns around Atlanta, Montgomery, Nashville, San Antonio, Waco, and Dallas. Results reveal<br />

an average increase of -28\% in monthly rainfall rates within 30-60 kilometers downwind of the metropolis with a modest<br />

increase of 5.6\% over the metropolis. Portions of the downwind area exhibit increases as high as 51\%. The percentage<br />

changes are relative to an upwind control area. It was also found that maximum rainfall rates in the downwind impact area<br />

exceeded the mean value in the upwind control area by 48\% - 116\%. The maximum value was generally found at an average<br />

distance of 39 km from the edge of the urban center or 64 km from the center of the city. Results are consistent with<br />

METROMEX studies of St. Louis almost two decades ago and with more recent studies near Atlanta. Future work is extending<br />

the investigation to Phoenix, Arizona, an arid U.S. city, and several international cities like Mexico City, Johannesburg, and<br />

Brasilia. The study establishes the possibility of utilizing satellite-based rainfall estimates for examining rainfall modification<br />

by urban areas on global scales and over longer time periods. Such research has implications for weather forecasting, urban<br />

planning, water resource management, and understanding human impact on the environment and climate.<br />

Author<br />

Rain; Resources Management; Water Resources; Wind Direction<br />

20030032196 NASA Goddard Space Flight Center, Greenbelt, MD, USA<br />

A Comparison of the Lower Stratospheric Age-Spectra Derived from a General Circulation Model and Two Data<br />

Assimilation Systems<br />

Schoeberl, Mark R.; Douglass, Anne R.; Zhu, Zhengxin; Pawson, Steven; [2002]; 2 pp.; In English; AGU 2002 Fall Meeting,<br />

6-10 Dec. 2002, San Francisco, CA, USA; Copyright; Avail: Other Sources; Abstract Only<br />

We use kinematic and diabatic back trajectory calculations, driven by winds from a general circulation model (GCM) and<br />

two different data assimilation systems (DAS), to compute the age spectrum at three latitudes in the lower stratosphere. The<br />

age-spectra are compared to chemical transport model (CTM) calculations, and the mean ages from all of these studies are<br />

compared to observations. The age spectra computed using the GCM winds show a reasonably isolated tropics in good<br />

agreement with observations; however, the age spectra determined from the DAS differ from the GCM spectra. For the DAS<br />

diabatic trajectory calculations there is too much exchange between the tropics and mid-latitudes. The age spectrum is thus<br />

too broad and the tropical mean age is too old as a result of mixing older mid latitude air with tropical air. Likewise the mid<br />

latitude mean age is too young due to the in mixing of tropical air. The DAS kinematic trajectory calculations show excessive<br />

vertical dispersion of parcels in addition to excessive exchange between the tropics and mid latitudes. Because air is moved<br />

rapidly to the troposphere from the vertical dispersion, the age spectrum is shifted toward the young side. The excessive<br />

vertical and meridional dispersion compensate in the kinematic case giving a reasonable tropical mean age. The CTM<br />

calculation of the age spectrum using the DAS winds shows the same vertical and meridional dispersive characteristics of the<br />

kinematic trajectory calculation. These results suggest that the current DAS products will not give realistic trace gas<br />

distributions for long integrations; they also help explain why the extra tropical mean ages determined in a number of previous<br />

DAS driven CTM s are too young compared with observations. Finally, we note trajectory-generated age spectra . show<br />

significant age anomalies correlated with the seasonal cycles. These anomalies can be linked to year-to-year variations in the<br />

tropical heating rate. The anomalies are suppressed in the CTM spectra suggesting that the CTM transport scheme is too<br />

diffusive.<br />

Author<br />

Atmospheric General Circulation Models; Cycles; Computation; Latitude; Stratosphere; Spectra; Trace Contaminants<br />

20030032234 NASA Goddard Space Flight Center, Greenbelt, MD, USA<br />

Visions of our Planet’s Atmosphere, Land & Oceans<br />

Hasler, Arthur F.; January 2002; 1 pp.; In English; The 107th STANYS Annual Convention, 3-5 Nov. 2002, Ellenville, NY,<br />

USA; No Copyright; Avail: Other Sources; Abstract Only<br />

The NASA/NOAA Electronic Theater presents Earth science observations and visualizations in a historical perspective.<br />

Fly in from outer space to South Africa, Cape Town and Johannesburg using NASA Terra MODIS data, Landsat data and 1m<br />

IKONOS ’Spy Satellite‘ data. Zoom in to any place South Africa using Earth Viewer 3D from Keyhole Inc. and Landsat data<br />

at 30 m resolution. Go back to the early weather satellite images from the 1960s and see them contrasted with the latest US<br />

and international global satellite weather movies including hurricanes & ’tornadoes‘. See the latest visualizations of<br />

spectacular images from NASA/NOAA remote sensing missions like Terra, GOES, TRMM, SeaWiFS, Landsat 7 including<br />

1 - min GOES rapid scan image sequences of Nov 9th 2001 Midwest tornadic thunderstorms and have them explained. See<br />

how High-Definition Television (HDTV) is revolutionizing the way we present science to the public. See dust storms and<br />

flooding in Africa and smoke plumes from fires in Mexico. See visualizations featured on the covers of Newsweek, TIME,<br />

91

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