Model simulated hydrological estimates for the North Slope drainage basin, Alaska, 1980-2010

• Main Authors: Beaufort Lagoon Ecosystems LTER, Michael Rawlins
• Format: Dataset
• Language: unknown
• Published: Arctic Data Center 2019
• Subjects: movement of inorganic matter; discharge; hydrologic processes; hydrology; permafrost; runoff; seasonality; snow water equivalent; soil temperature; water balance; Beaufort Sea; Canning River; Colville River; Kuparuk River; Meade River; Beaufort Lagoon Ecosystems LTER; BLE; LTER; Delta River; Mackenzie River; Meade; Merra; Barrow; Mackenzie river; north slope; Alaska
• Online Access: https://search.dataone.org/view/urn:uuid:bd090a42-f1f6-4dcf-95d5-5f47544acdec

Estimates of runoff, river discharge, snow water equivalent (SWE), subsurface runoff, and soil temperatures are drawn from the Permafrost Water Balance Model (PWBM). The simulation and derived data span the period 1980-2010. The model was forced with daily gridded meteorological data obtained from the Modern-Era Retrospective analysis for Research and Applications (MERRA) reanalysis (version 5.2.0). The estimates of total runoff (daily), soil temperature (daily), subsurface runoff (monthly), and SWE (monthly) are expressed on a spatial grid (N=312; 25x25 km EASE-Grid version 1, Northern Hemisphere) over the North Slope drainage basin, with the coastline extending from Utqiagvik (formerly Barrow) to just west of the Mackenzie River delta. River discharge, calculated as a volume flux of runoff at each grid cell, was routed through the river network defined on a simulated topological network (STN). Archived files contain discharge flux through the grid cell representing the outlet of each of forty-two basins defined across the region on the 25 km resolution EASE-Grid. Details of the PWBM, forcing variables, model validation and results of analysis are described in Rawlins et al. (2019).