Legates and Willmott's (1990) station records of monthly and annual mean air
temperature (
T) were used to produce this archive. The number of
stations (and oceanic grid nodes) used was 24,941.
SPATIAL INTERPOLATION:
Station averages of air
temperature were interpolated (see below) to a 0.5 degree by 0.5 degree of
latitude/longitude grid, where the grid nodes are
centered on 0.25 degree. The number of nearby stations which influence
a grid-node estimate was
increased to an average of 20, from an average of 7 in earlier
applications. This resulted in smaller
cross-validation errors (see below) and visually more
realistic air-temperature fields. A more robust
neighbor finding algorithm, based on spherical distance,
also was developed and used.
Digital-elevation-model- or DEM-assisted interpolation of air
temperature was employed (Willmott and Matsuura, 1995).
Station air temperature was first "brought
down" to sea level at an average environmental lapse rate (6.0 deg C/Km).
Traditional interpolation then was performed on the
adjusted-to-sea-level station air temperatures.
It was accomplished with the spherical version of Shepard's algorithm,
which employs an enhanced distance-weighting method
(Shepard, 1968; Willmott et al., 1985).
Then, the gridded sea-level air temperatures were brought up to the
DEM-grid height, again, at an average environmental lapse rate.
This version (2.02) of our average air-temperature archive differs from the
previous DEM-assisted version (2.01) in that we employed an
alternate DEM and reduced the lapse rate by 0.5 degrees to 6.0 deg C/Km.
SPATIAL CROSS VALIDATION:
To indicate (roughly) the spatial interpolation errors, station-by-station
cross validation was employed (Willmott and Matsuura, 1995).
One station was removed at a time, and
air temperature was then interpolated to the
removed station location from the surrounding nearby stations.
The difference between the real station value and the
interpolated value is a local estimate of interpolation error.
After each station cross validation was made, the removed
station was put back into the network. To reduce network biases on
cross-validation results, absolute values of the errors at
the stations were interpolated to the same spatial resolution as
the air temperature field.
ARCHIVE STRUCTURE:
lw_temp_dem.clim: |
Average monthly and annual air temperature interpolated to a 0.5 by
0.5 degree grid resolution (centered on 0.25 degree). The format
of each record is
|
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 Air Temperature (deg C, Jan - Dec) |
12F8.1 |
15 |
113 - 120 |
Mean Annual Air Temperature |
F8.1 |
lw_temp_dem_cv.clim: |
Cross-validation errors associated with air temperatures
interpolated to a 0.5 by 0.5 degree grid resolution. The format of
each record is |
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 |
Cross-validation errors for Monthly Air Temperature (deg C , Jan - Dec) |
12F8.1 |
15 |
113 - 120 |
Cross-validation errors for Mean Annual Air Temperature |
F8.1 |
SELECTED REFERENCES:
Legates, D. R. and C. J. Willmott (1990) Mean Seasonal and Spatial Variability
Global Surface Air Temperature. Theoretical and Applied Climatology
, 41, 11-21.
Shepard, D. (1968) A two-dimensional Interpolation function for irregularly-spaced
Data. Proceedings, 1968 ACM National Conference, 517-523.
Willmott, C. J., C. M. Rowe and W. D. Philpot (1985) Small-Scale
Climate Maps: A Sensitivity Analysis of Some Common Assumptions Associated with
Grid-point Interpolation and Contouring.
American Cartographer, 12, 5-16.
Willmott, C. J. and K. Matsuura (1995) Smart Interpolation of Annually Averaged Air
Temperature in the United States. Journal of Applied Meteorology, 34, 2577-2586.