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DAILY SIMULATED RUNOFF FROM PAN-ARCTIC WATER BALANCE MODEL (Serreze, Rawlins)
SummaryDaily runoff is generated using the Pan-Arctic Water Balance Model (P/WBM) [Rawlins et al., 2003]. The P/WBM simulates the high-latitude water cycle by utilizing gridded fields of plant rooting depth, soil characteristics (texture, organic content), vegetation, and daily time series of precipitation [Serreze et al., 2003] and air temperature. Model inputs and outputs are defined at 29,926 grids of ~25 km (628 km^2) resolution across the Pan-Arctic on the Equal-Area Scalable Grid known as EASE-Grid [Brodzik and Knowles, 2002]. The P/WBM includes a simple scheme for simulating daily changes in soil frozen and liquid water amounts, which is driven by air temperature, modeled soil moisture content, and physiographic data. The climate time series (precipitation and air temperature) originate from the National Center for Environmental Prediction (NCEP) reanalysis project [Kalnay et al., 1996], with the precipitation inputs described in Serreze et al., 2003.
The data is presented in 24 sub-datasets of different spatial and temporal
aggregations (see aggregation description below).
Data AccessORDER data for delivery by FTP.
* - This Dataset was submitted to or acquired by ArcticRIMS from a third party Research Institution. Data AggregationThere are two distinct methods to produce data aggregation along the "time" axis of the cube. These are -
Each aggregated data file in a dataset has a notation of a method (mean or sum) used to produce the file. The notation included in the first (top) line of the file. Please, pay attention to that. Aggregation along the "spatial scale" axis of the cube is
done using simple mean (average) over all grid cells of each basin (river, sea
basin, or continent) from an appropriate grid cell file. Additional Information
Temporal Coverage
Spatial CoverageMinimum latitude: 45.00000000, Minimum longitude: -180.00000000Maximum latitude: 90.00000000, Maximum longitude: 180.00000000
Point of Contact
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