TRMM Combination

The Tropical Rainfall Measurement Mission (TRMM) is being flown by the National Aeronautics and Space Administration (NASA, U.S.) and the National Aeronautics and Japan Aerospace Exploration Agency (JAXA, Japan) to improve our quantitative knowledge of the 3-dimensional distribution of precipitation in the tropics. TRMM has a passive microwave radiometer (TRMM Microwave Imager, TMI), the first active space-borne Precipitation Radar (PR), and a Visible-Infrared Scanner (VIRS), plus other instruments. Coordinated observations are intended to result in a "flying raingauge" capability.

Two of the products produced operationally in TRMM are the "TRMM and Other Satellites" precipitation estimate (Algorithm 3B-42) and the "TRMM and Other Sources" precipitation estimate (Algorithm 3B-43) described in Huffman et al. (2007). Algorithm 3B-42 uses the TRMM Multi-satellite Precipitation Analysis (TMPA) algorithm to calibrate the TMI (2A-12), SSM/I, AMSR-E, AMSU-B and IR to the TRMM best-estimate TCI (2B-31), and then optimally merge these satellite estimates to produce 3-hourly precipitation fields. Algorithm 3B-43 merges monthly averaged 3B-42 estimates with gauge data over land to produce the best-estimated monthly precipitation field. The data sets cover the period January 1998--present (with about a month delay). Both 3B-42 and 3B-43 products are observation-only datasets, that is, a gridded analysis based on satellite-only estimate of rainfall, and a combined satellite/rain gauge estimate of rainfall, respectively. There are two fields in each data set - estimates of surface precipitation and RMS random error.

The data set archive consists of binary data sets in Hierarchical Data Format (HDF). Each 3B-42 file contains a 3-hourly estimate and each 3B-43 file contains a one month estimate. The grid on which each field of values is presented is a 0.25degx0.25deg latitude--longitude (Cylindrical Equal Distance) array of points over the latitude range 50N-S. It is size 400x1440, with X (latitude) incrementing most rapidly South to North, and then Y (longitude) incrementing West to East from the Date Line. Grid edges are located at whole-degree values:

First point center      = (49.875S,179.875W)
Second point center = (49.625S,179.625W)
Last point center      = (49.875N,179.875E)

Missing values are denoted by the value -9999.9, and the units are mm/hour.

Technical documentation is available though the more information hot link at the bottom of the page, and the standard reference is:

Huffman, G.J., R.F. Adler, D.T. Bolvin, G. Gu, E.J. Nelkin, K.P. Bowman,

E.F. Stocker, D.B. Wolff, 2007: The TRMM Multi-satellite Precipitation

Analysis: Quasi-Global, Multi-Year, Combined-Sensor Precipitation

Estimates at Fine Scale. J. Hydrometeor., 8, 33-55.

The dataset creator is:

David T. Bolvin
Code 613.1
NASA Goddard Space Flight Center
Greenbelt, MD 20771 USA
Phone: +1 301-614-6323
Fax: +1 301-614-5492
Internet: david.t.bolvin@nasa.gov

More Information (pdf)

Data