Plant cover, soil temperature, freeze, water stress, and evapotranspiration conditions
The author has identified the following significant results. Procedures to edit cloud-contaminated pixels from those pixels representing Earth surface features were investigated. Because clouds are more reflective than Earth features and are colder than Earth surface features most of the year at 26...
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| creator | Wiegand, C. L. Nixon, P. R. Gausman, H. W. Namken, L. N. Leamer, R. W. Richardson, A. J. |
| description | The author has identified the following significant results. Procedures to edit cloud-contaminated pixels from those pixels representing Earth surface features were investigated. Because clouds are more reflective than Earth features and are colder than Earth surface features most of the year at 26 N latitude, either a raw digital count ratio or a ratio of reflectance percentage for the VIS band to the temperature works well. For this procedure, the two bands of data need to be registered to the ground scene. |
| format | Report |
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J.</creatorcontrib><description>The author has identified the following significant results. Procedures to edit cloud-contaminated pixels from those pixels representing Earth surface features were investigated. Because clouds are more reflective than Earth features and are colder than Earth surface features most of the year at 26 N latitude, either a raw digital count ratio or a ratio of reflectance percentage for the VIS band to the temperature works well. 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W.</creatorcontrib><creatorcontrib>Richardson, A. J.</creatorcontrib><title>Plant cover, soil temperature, freeze, water stress, and evapotranspiration conditions</title><description>The author has identified the following significant results. Procedures to edit cloud-contaminated pixels from those pixels representing Earth surface features were investigated. Because clouds are more reflective than Earth features and are colder than Earth surface features most of the year at 26 N latitude, either a raw digital count ratio or a ratio of reflectance percentage for the VIS band to the temperature works well. 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W. ; Namken, L. N. ; Leamer, R. W. ; Richardson, A. J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-nasa_ntrs_198000102473</frbrgroupid><rsrctype>reports</rsrctype><prefilter>reports</prefilter><language>eng</language><creationdate>1979</creationdate><topic>Earth Resources And Remote Sensing</topic><toplevel>online_resources</toplevel><creatorcontrib>Wiegand, C. L.</creatorcontrib><creatorcontrib>Nixon, P. R.</creatorcontrib><creatorcontrib>Gausman, H. W.</creatorcontrib><creatorcontrib>Namken, L. N.</creatorcontrib><creatorcontrib>Leamer, R. W.</creatorcontrib><creatorcontrib>Richardson, A. J.</creatorcontrib><collection>NASA Scientific and Technical Information</collection><collection>NASA Technical Reports Server</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Wiegand, C. L.</au><au>Nixon, P. R.</au><au>Gausman, H. W.</au><au>Namken, L. N.</au><au>Leamer, R. 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| source | NASA Technical Reports Server |
| subjects | Earth Resources And Remote Sensing |
| title | Plant cover, soil temperature, freeze, water stress, and evapotranspiration conditions |
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