Estimating Daily Net Radiation over Vegetation Canopy through Remote Sensing and Climatic Data

Net radiation ( Rn ) =key variable in hydrological studies. Measured net radiation data are rarely available and are often subject to error due to equipment calibration or failure. In addition, point measurements of net radiation do not represent the diversity of the regional net radiation values wh...

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Published inJournal of irrigation and drainage engineering Vol. 133; no. 4; pp. 291 - 297
Main Authors Samani, Zohrab, Bawazir, A. Salim, Bleiweiss, Max, Skaggs, Rhonda, Tran, Vien D
Format Journal Article
LanguageEnglish
Published Reston, VA American Society of Civil Engineers 01.08.2007
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ISSN0733-9437
1943-4774
DOI10.1061/(ASCE)0733-9437(2007)133:4(291)

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Abstract Net radiation ( Rn ) =key variable in hydrological studies. Measured net radiation data are rarely available and are often subject to error due to equipment calibration or failure. In addition, point measurements of net radiation do not represent the diversity of the regional net radiation values which are needed for large scale evapotranspiration mapping. A procedure has been developed to estimate daily net radiation using canopy temperature, albedo, short wave radiation and air temperature. This procedure makes it possible to estimate Rn by combining information from satellite and local weather stations. Three different methodologies are presented to estimate net radiation. Comparisons between net radiation using the three methods resulted in average error ranging from 1 to 30% and standard error of estimate ranging from 1.06 to 5.34 MJ∕ m2 ∕day .
AbstractList Net radiation (Rn)=key variable in hydrological studies. Measured net radiation data are rarely available and are often subject to error due to equipment calibration or failure. In addition, point measurements of net radiation do not represent the diversity of the regional net radiation values which are needed for large scale evapotranspiration mapping. A procedure has been developed to estimate daily net radiation using canopy temperature, albedo, short wave radiation and air temperature. This procedure makes it possible to estimate Rn by combining information from satellite and local weather stations. Three different methodologies are presented to estimate net radiation. Comparisons between net radiation using the three methods resulted in average error ranging from 1 to 30% and standard error of estimate ranging from 1.06 to 5.34 MJ/m2/day.
Net radiation ( Rn ) =key variable in hydrological studies. Measured net radiation data are rarely available and are often subject to error due to equipment calibration or failure. In addition, point measurements of net radiation do not represent the diversity of the regional net radiation values which are needed for large scale evapotranspiration mapping. A procedure has been developed to estimate daily net radiation using canopy temperature, albedo, short wave radiation and air temperature. This procedure makes it possible to estimate Rn by combining information from satellite and local weather stations. Three different methodologies are presented to estimate net radiation. Comparisons between net radiation using the three methods resulted in average error ranging from 1 to 30% and standard error of estimate ranging from 1.06 to 5.34 MJ∕ m2 ∕day .
Net radiation (R sub(n))=key variable in hydrological studies. Measured net radiation data are rarely available and are often subject to error due to equipment calibration or failure. In addition, point measurements of net radiation do not represent the diversity of the regional net radiation values which are needed for large scale evapotranspiration mapping. A procedure has been developed to estimate daily net radiation using canopy temperature, albedo, short wave radiation and air temperature. This procedure makes it possible to estimate R sub(n) by combining information from satellite and local weather stations. Three different methodologies are presented to estimate net radiation. Comparisons between net radiation using the three methods resulted in average error ranging from 1 to 30% and standard error of estimate ranging from 1.06 to 5.34 MJ/m super(2)/day.
Author Skaggs, Rhonda
Samani, Zohrab
Bawazir, A. Salim
Bleiweiss, Max
Tran, Vien D
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Issue 4
Keywords Irrigation
Climatic data
Satellite
Weather station
Remote sensing
Classification description
Drainage
Weather
Irrigation and drainage
Classification
Evapotranspiration
Water engineering
Net radiation
Solar radiation
Canopy(vegetation)
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Snippet Net radiation ( Rn ) =key variable in hydrological studies. Measured net radiation data are rarely available and are often subject to error due to equipment...
Net radiation (R sub(n))=key variable in hydrological studies. Measured net radiation data are rarely available and are often subject to error due to equipment...
Net radiation (Rn)=key variable in hydrological studies. Measured net radiation data are rarely available and are often subject to error due to equipment...
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SubjectTerms Agricultural and forest climatology and meteorology. Irrigation. Drainage
Agricultural and forest meteorology
Agronomy. Soil science and plant productions
air temperature
albedo (reflectance)
Biological and medical sciences
canopy
climatic factors
diurnal variation
equations
error analysis
estimation
evapotranspiration
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
irrigation and drainage
Irrigation. Drainage
leaf area index
methodology
New Mexico
prediction
remote sensing
satellites
solar radiation
TECHNICAL PAPERS
temperature
vegetation
Water balance and requirements. Evapotranspiration
weather stations
Title Estimating Daily Net Radiation over Vegetation Canopy through Remote Sensing and Climatic Data
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