USGS monthly water balance model inputs and outputs for the conterminous United States, 1895-2020, based on ClimGrid data
January 26, 2022
This NetCDF represents the monthly inputs and outputs from a United States Geological Survey water-balance model (McCabe and Wolock, 2011) for the conterminous United States for the period 1895-01-01 to 2020-12-31. The source data used to run the water balance model is based on the National Oceanic and Atmospheric Administration's(NOAA, 2020) ClimGrid data for precipitation and temperature. This NetCDF contains the following monthly inputs: temperature (degrees Celsius) and precipitation (millimeters, mm) and the following outputs (all in mm): runoff, soil moisture storage, actual evapotranspiration, potential evapotranspiration, snow water equivalent, and snowfall. The spatial reference for this data set is ESPG 4326.
Citation Information
Publication Year | 2022 |
---|---|
Title | USGS monthly water balance model inputs and outputs for the conterminous United States, 1895-2020, based on ClimGrid data |
DOI | 10.5066/P9JTV1T6 |
Authors | Michael E Wieczorek, Richard P Signell, Gregory J McCabe, David M Wolock |
Product Type | Data Release |
Record Source | USGS Asset Identifier Service (AIS) |
USGS Organization | MD-DE-DC Water Science Center |
Rights | This work is marked with CC0 1.0 Universal |
Related
Peak streamflow trends in Iowa and their relation to changes in climate, water years 1921–2020
This study summarizes trends and change points for peak and daily streamflow in Iowa from water years 1921 through 2020. Nonstationarity in peak streamflow in Iowa can include monotonic trends, change points, and changes in seasonality. Spatial patterns of nonstationarity in peak streamflow, daily streamflow, and monthly climatic data (observed and modeled) were examined across four temporal perio
Authors
Padraic S. O'Shea
Related
Peak streamflow trends in Iowa and their relation to changes in climate, water years 1921–2020
This study summarizes trends and change points for peak and daily streamflow in Iowa from water years 1921 through 2020. Nonstationarity in peak streamflow in Iowa can include monotonic trends, change points, and changes in seasonality. Spatial patterns of nonstationarity in peak streamflow, daily streamflow, and monthly climatic data (observed and modeled) were examined across four temporal perio
Authors
Padraic S. O'Shea