|
Read Full Article (file size: 1577931 bytes) Cited by
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 110,
D21104,
doi:10.1029/2005JD005763,
2005
Diurnal cycle of tropical precipitation in Tropical Rainfall Measuring Mission (TRMM) satellite and ocean buoy rain gauge
data
Kenneth P. Bowman
Department of Atmospheric Sciences, Texas A&M University, College Station, Texas, USA
J. Craig Collier
Department of Atmospheric Sciences, Texas A&M University, College Station, Texas, USA
Gerald R. North
Department of Atmospheric Sciences, Texas A&M University, College Station, Texas, USA
Qiaoyan Wu
Department of Atmospheric Sciences, Texas A&M University, College Station, Texas, USA
Eunho Ha
Department of Atmospheric Sciences, Texas A&M University, College Station, Texas, USA
James Hardin
College of Science, Texas A&M University, College Station, Texas, USA
Abstract
The climatological diurnal cycle of precipitation in the tropics is analyzed using data from rain gauges on ocean buoys and
satellite measurements by the Tropical Rainfall Measuring Mission (TRMM) satellite. The ocean buoy data are from the NOAA/Pacific
Marine Environmental Laboratory Tropical Atmosphere-Ocean/Triangle Trans-Ocean buoy Network in the tropical Pacific Ocean.
TRMM data are from the precipitation radar (PR) and the TRMM microwave imager (TMI). Climatological hourly mean precipitation
rates are analyzed in terms of the diurnal and semidiurnal harmonics. Both data sets confirm an early morning peak in precipitation
over ocean regions. The amplitude of the diurnal harmonic over the oceans is typically less than 25% of the mean precipitation
rate. Over tropical land masses the rainfall peaks in the afternoon and evening hours. The relative amplitude of the diurnal
harmonic over land is larger than over the ocean, often exceeding 50% of the mean rain rate. Previously noted differences
between the TMI and PR rainfall retrievals persist in the diurnal cycle. On average the TMI measures more rainfall than the
PR and has a larger diurnal variation. Phase differences between the two instruments do not show a consistent bias.
Received 7
January
2005;
accepted 1
August
2005;
published 4
November
2005.
Keywords: precipitation;
diurnal cycle;
satellite.
Index Terms: 3354 Atmospheric Processes: Precipitation (1854); 3360 Atmospheric Processes: Remote sensing; 1836 Hydrology: Hydrological cycles and budgets (1218, 1655).
Read Full Article (file size: 1577931 bytes) Cited by
Citation: Bowman, K. P., J. C. Collier, G. R. North, Q. Wu, E. Ha, and J. Hardin
(2005),
Diurnal cycle of tropical precipitation in Tropical Rainfall Measuring Mission (TRMM) satellite and ocean buoy rain gauge
data,
J. Geophys. Res.,
110,
D21104,
doi:10.1029/2005JD005763.
Copyright 2005 by the American Geophysical Union.
|