Terrestrial Water Balance Data Archive:
Regridded Monthly Climatologies
(Version 1.02)
produced and documented by
Cort. J. Willmott and Kenji Matsuura
(with support from NASA's Seasonal to Interannual ESIP)
For additional information concerning this archive,
please contact us at:
Center for Climatic Research
Department of Geography
University of Delaware
Newark, DE 19716
(302) 831-2294
or
kenjisan@udel.edu
Archive (Version 1.02) released July 1, 2001
GRIDDED DATA SOURCES:
Gridded monthly air temperature (
T) and unadjusted
(for raingage undercatch) precipitation (
P) (at a 0.5 x 0.5 degree
resolution) were taken from the
Terrestrial Air Temperature and Precipitation: Monthly and Annual Climatologies
(V. 3.02) which are based on 50 years of monthly
T and
P
observations. Interpolations to the grid were made using CAI.
Our estimates of the climatic water balance were made from
these 0.5x0.5 degree
T and
P fields and are available for
85,974 land grid points.
GRIDDED WATER-BUDGET ESTIMATES:
Average-monthly water-balance fields were estimated from the
gridded average-monthly T and P fields according to Willmott et
al.'s (1985) modified version of the Thornthwaite water-balance
procedure. The computational algorithm was derived from Willmott
(1977). Climatic water-balance calculations were separately made
for each of the 85,974 grid nodes, thereby conserving mass (in z
only) at each grid node.
These 0.5-degree
resolution water-balance estimates are based on semi-empirical
relationships between observed average monthly P and an
estimated average monthly potential evapotranspiration (Eo),
derived from an average monthly T. Soil water-holding capacity
(w*) was held constant at 150 mm. A snow-cover water budget
also was evaluated and coupled with the soil-moisture balance
according to Willmott et al. (1985). Water-balance variables
estimated and archived here include: average-monthly Eo in mm,
average-monthly actual evapotranspiration (E) in mm, average-monthly
deficit (def) in mm, mid-monthly soil-moisture depth (w) in
mm, mid-monthly water equivalent of the snow pack (ws) in mm,
average-monthly snow melt (M) in mm, and average-monthly surplus
(S) in mm.
ARCHIVE STRUCTURE:
Water balance climatologies were
produced and archived for a single soil water-holding
capacity, w*=150mm.
There are seven files in the archive.
The beginning of each file name describes the content of the file
as follows.
| def150.clim: | deficit |
| E150.clim : | actual evapotranspiration |
| Eo150.clim : | adjusted potential evapotranspiration |
| M150.clim : | snow melt |
| S150.clim : | surplus |
| w150.clim : | mid-monthly soil moisture |
| ws150.clim : | mid-monthly snow cover |
All files have the structure.
| Field |
Columns |
Variable |
Fortran Format
|
| 1 |
1 - 8 |
Longitude (decimal degrees) |
F8.3 |
| 2 |
9 - 16 |
Latitude (decimal degrees) |
F8.3 |
| 3-14 |
17 - 112 |
Monthly values (mm) |
12F8.1 |
SELECTED REFERENCES:
Willmott, C. J., 1977. WATBUG: A FORTRAN IV Algorithm for
Calculating the Climatic Water Budget. Pubs. in Climatology, 30,
1-55. (Also published as Report 1 in The Use of the Climatic Water
Budget in Water Resources Management and Control. Newark, DE:
University of Delaware, Water Resources Center, 1977).
Willmott, C. J., C. M. Rowe, and Y. Mintz, 1985. Climatology of
the Terrestrial Seasonal Water Cycle. Journal of Climatology, 5,
589-606.