Observed Energy Forcing Fields
These hourly meteorological data for 8 basins in the DMIP
domains are derived from the 1/8 degree gridded data files
developed at the University of Washington. These files are
named xxxxxxxx.dat, where xxxxxxxx are the 8-digit USGS
basin ID. The correspondence between basin names and USGS
ID are as follows:
03069500 CHEAT RIVER NEAR PARSONS, WV
07194800 ILLINOIS RIVER AT SAVOY, ARK.
07195500 ILLINOIS RIVER NEAR WATTS, OK
07196000 FLINT CREEK NEAR KANSAS, OK
07196500 ILLINOIS RIVER NEAR TAHLEQUAH
07196973 PEACHEATER CREEK AT CHRISTIE, OK (no data for this basins)
07197000 BARON FORK AT ELDON, OK
07189000 ELK RIVER NEAR TIFF CITY, MO
07332500 BLUE RIVER NEAR BLUE, OK
The data are hourly (one row for each hour) beginning January 1, 1992,
and continuing through July 31, 2000.
Each file contains 9 columns of data:
1) date and hour (in yyyymmddhh format)
2) precipitation (mm) (see note below)
3) air temperature (C)
4) incoming shortwave radiation (W/m^2)
5) incoming longwave radiation (W/m^2)
6) atmospheric density (kg/m^3)
7) atmospheric pressure (kPa)
8) atmospheric vapor pressure (kPa)
9) wind speed (m/s)
Note: The precipitation data provided here are different from the
NEXRAD data. It is recommended that NEXRAD data be used for DMIP.
For a more complete description of the source of these data, please see:
http://www.hydro.washington.edu/SurfaceWaterGroup/Data/gridded/index.html
Brief descriptions of the data:
2) NCDC Cooperative Observer station data, gridded to the grid cell
centers.
Each daily precipitation total, for this dataset, is simply divided
into
24 equal increments.
3) Maximum and minimum air temperature is also from NCDC Cooperative
Observer
stations, with an asymmetric hermite polynomial fitted through these
to
estimate hourly temperature.
4) Incoming shortwave is parameterized from the daily max/min
temperatures
and dew point, following Thornton and Running (1999)
5) Incoming longwave is calculated following Bras (1990), using air
temperature,
humidity, and atmospheric transmissivity (produced in 3).
6) Atmospheric density is estimated according to Shuttleworth (1993)
7) Atmospheric pressure is assumed constant here.
8) Vapor pressure is estimated iteratively using Kimball (1997) and
Thornton and
Running (1999).
9) Wind speed is the average daily 10m wind speed from NCEP/NCAR
Reanalysis
(resultant of u- and v-wind components), interpolated to the 1/8
degree cell
centers.
* External
Link. When you click on any of the following links you will
be leaving the HL Web site. You may wish to review the privacy
notice on those sites since their information may differ from
that of OHD and NOAA. In addition, our linking to this site
does not constitute an endorsement of any products, services
or the information found on the that site.
|