By American Geophysical Union

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Towtry, and M. R. Snell, Measurement of convective mean rainfall over small areas using high-density raingagesand radar, d. Appl. , 18, 1316-1326, 1979. , Use of digital radar data in operational hydrology, paper presentedat National Water ResourcesEngineeringMeeting, Am. Soc. , 1973. , and V. L. Patterson, GATE radar rainfall atlas, NOAA Spec. , Natl. Oceanic and Atmos. , 1979. , D. R. Greene, P. R. Ahnert, W. F. Krajewski, T. R. Sivaramakrishnan,E. R. Johnson,and M. R. Dias, Proposed"offsite" precipitation processingsystemfor NEXRAD, iv.

Clim. Appl. , 25, 284307, 1986. Wetzel, P. , and R. H. Woodward, Soil moisture estimation using GOES-VISSR infrared data: A case study with a simple statistical method, J. Clirn. Appl. , 26, 107-117, 1987. Wetzel, P. , D. Atlas, and R. H. Woodward, Determining soil moisture from geosynchronoussatellite infrared data: A feasibility study, J. Clirn. Appl. , 23, 375-391, 1984. T. N. Carlson and A. L. , Pennsylvania State University, University Park, PA 16802. Benjamin, S. , and T. N. Carlson, Some effects of surface heating and topography on the regional severestorm environment, I, 3-D simulation, Mon.

Clearly, there was a large increasein M and API over the period betweenDecember24 and January 18. Correlations %00 hooo KM Fig. 3. Target area for Argentina case study. 4. Rectangles showtheboundaries oftheGOESsubset images, anddotsindicate thelocation of thegroundprecipitation measurements. (Bottom)Isopleths of thechange in antecedent precipitation index(AAPI) betweenDecember24, 1981,and January 18, 1982,in unitsof millimeters. The relationshipfor Argentinayieldssimilar 4. ' BRIEFREPORT herent uncertainties in the method.

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