Evapotranspiration in the Upper Klamath Basin for April 2013

The evapotranspiration (ET) datasets were created under contract for this study by the University of Idaho. A high-resolution remote sensing technique known as Mapping Evapotranspiration at High Resolution and Internalized Calibration (METRIC) was used to create estimates of the spatial distribution of ET. The METRIC technique uses thermal infrared Landsat imagery to quantify actual evapotranspiration at a 30-meter resolution that can be related to individual irrigated fields. Because evaporation uses heat energy, ground surfaces with large ET rates are left cooler as a result of ET than ground surfaces that have less ET. As a consequence, irrigated fields appear in the Landsat images as cooler than nonirrigated fields. Products produced from this study include total seasonal and total monthly (April-October) actual evapotranspiration maps for 2013.

Data and Resources

Field Value
accessLevel public
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identifier USGS:5642472ae4b0831b7d62eafb
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publisher U.S. Geological Survey
publisher_hierarchy Department of the Interior > U.S. Geological Survey
resource-type Dataset
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theme {geospatial}
Groups
  • AmeriGEOSS
  • National Provider
  • North America
Tags
  • amerigeo
  • amerigeoss
  • california
  • ckan
  • evapotranspiration
  • geo
  • geoss
  • inlandwaters
  • landsat
  • lost-river-basin
  • metric
  • national
  • north-america
  • oregon
  • remote-sensing
  • sprague-river-basin
  • united-states
  • upper-klamath-basin
  • usgs-5642472ae4b0831b7d62eafb
  • williamson-river-basin
  • wood-river-basin
isopen False
license_id notspecified
license_title License not specified
maintainer Jonathan Haynes
maintainer_email jhaynes@usgs.gov
metadata_created 2025-11-21T05:57:37.780845
metadata_modified 2025-11-21T05:57:37.780849
notes The evapotranspiration (ET) datasets were created under contract for this study by the University of Idaho. A high-resolution remote sensing technique known as Mapping Evapotranspiration at High Resolution and Internalized Calibration (METRIC) was used to create estimates of the spatial distribution of ET. The METRIC technique uses thermal infrared Landsat imagery to quantify actual evapotranspiration at a 30-meter resolution that can be related to individual irrigated fields. Because evaporation uses heat energy, ground surfaces with large ET rates are left cooler as a result of ET than ground surfaces that have less ET. As a consequence, irrigated fields appear in the Landsat images as cooler than nonirrigated fields. Products produced from this study include total seasonal and total monthly (April-October) actual evapotranspiration maps for 2013.
num_resources 2
num_tags 21
title Evapotranspiration in the Upper Klamath Basin for April 2013