Spatial and temporal soil water estimation considering soil variability and evapotranspiration uncertainity
Lack of accurate information stemming from soil variability and climatic uncertainty obstructs efficient irrigation management. State-space models of soil water balance and potential evapotranspiration were used in the application of spatial-temporal estimation methods to reduce uncertainty. Tempora...
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Veröffentlicht in: | Water resources research 1992, Vol.28 (3), p.803-814 |
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description | Lack of accurate information stemming from soil variability and climatic uncertainty obstructs efficient irrigation management. State-space models of soil water balance and potential evapotranspiration were used in the application of spatial-temporal estimation methods to reduce uncertainty. Temporal soil water storage estimates and estimation errors were obtained by the Kalman filter (KF). Spatial estimates were obtained by the conditional multivariate normal method. These spatial and temporal estimates were combined by an additional KF step that considers spatial estimates as measurements. Time-dependent soil water spatial covariance was approximated by assuming a constant correlation range and by using measurements variance to estimate the variogram "sill." Simulation and field results indicate that soil water storage estimates by the proposed method agreed better with measurements than estimates based on either spatial or temporal information only. The proposed estimation scheme can be extended to other systems with a simple physical model and a known spatial structure where only a few field measurements are available. |
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State-space models of soil water balance and potential evapotranspiration were used in the application of spatial-temporal estimation methods to reduce uncertainty. Temporal soil water storage estimates and estimation errors were obtained by the Kalman filter (KF). Spatial estimates were obtained by the conditional multivariate normal method. These spatial and temporal estimates were combined by an additional KF step that considers spatial estimates as measurements. Time-dependent soil water spatial covariance was approximated by assuming a constant correlation range and by using measurements variance to estimate the variogram "sill." Simulation and field results indicate that soil water storage estimates by the proposed method agreed better with measurements than estimates based on either spatial or temporal information only. The proposed estimation scheme can be extended to other systems with a simple physical model and a known spatial structure where only a few field measurements are available.</description><identifier>ISSN: 0043-1397</identifier><identifier>EISSN: 1944-7973</identifier><language>eng</language><subject>decision making ; evapotranspiration ; irrigation ; irrigation management ; mathematical models ; prediction ; simulation ; soil water balance ; soil water storage ; spatial distribution ; spatial variation ; temporal variation ; water availability</subject><ispartof>Water resources research, 1992, Vol.28 (3), p.803-814</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,4010</link.rule.ids></links><search><creatorcontrib>Or, D</creatorcontrib><creatorcontrib>Hanks, R.J</creatorcontrib><title>Spatial and temporal soil water estimation considering soil variability and evapotranspiration uncertainity</title><title>Water resources research</title><description>Lack of accurate information stemming from soil variability and climatic uncertainty obstructs efficient irrigation management. State-space models of soil water balance and potential evapotranspiration were used in the application of spatial-temporal estimation methods to reduce uncertainty. Temporal soil water storage estimates and estimation errors were obtained by the Kalman filter (KF). Spatial estimates were obtained by the conditional multivariate normal method. These spatial and temporal estimates were combined by an additional KF step that considers spatial estimates as measurements. Time-dependent soil water spatial covariance was approximated by assuming a constant correlation range and by using measurements variance to estimate the variogram "sill." Simulation and field results indicate that soil water storage estimates by the proposed method agreed better with measurements than estimates based on either spatial or temporal information only. The proposed estimation scheme can be extended to other systems with a simple physical model and a known spatial structure where only a few field measurements are available.</description><subject>decision making</subject><subject>evapotranspiration</subject><subject>irrigation</subject><subject>irrigation management</subject><subject>mathematical models</subject><subject>prediction</subject><subject>simulation</subject><subject>soil water balance</subject><subject>soil water storage</subject><subject>spatial distribution</subject><subject>spatial variation</subject><subject>temporal variation</subject><subject>water availability</subject><issn>0043-1397</issn><issn>1944-7973</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1992</creationdate><recordtype>article</recordtype><recordid>eNqFy90KgjAYxvERBdnHNbQbEDY3HR5H0bl1HG865S3dZFtGd59k5x09PPD7z0jEcyljlSsxJxFjUsRc5GpJVt7fGeMyzVREHkUPAaGlYCoadNdbNx5vsaUvCNpR7QN2I7GGltZ4rLRD00xiAIdwwxbD-9vrAXobHBjfo5uapym1C4BmNBuyqKH1evvbNdkdD-f9Ka7BXqFx6K-XImFcMK5SyZJM_BcfwNBG_Q</recordid><startdate>1992</startdate><enddate>1992</enddate><creator>Or, D</creator><creator>Hanks, R.J</creator><scope>FBQ</scope></search><sort><creationdate>1992</creationdate><title>Spatial and temporal soil water estimation considering soil variability and evapotranspiration uncertainity</title><author>Or, D ; Hanks, R.J</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-fao_agris_US2013017540263</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1992</creationdate><topic>decision making</topic><topic>evapotranspiration</topic><topic>irrigation</topic><topic>irrigation management</topic><topic>mathematical models</topic><topic>prediction</topic><topic>simulation</topic><topic>soil water balance</topic><topic>soil water storage</topic><topic>spatial distribution</topic><topic>spatial variation</topic><topic>temporal variation</topic><topic>water availability</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Or, D</creatorcontrib><creatorcontrib>Hanks, R.J</creatorcontrib><collection>AGRIS</collection><jtitle>Water resources research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Or, D</au><au>Hanks, R.J</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatial and temporal soil water estimation considering soil variability and evapotranspiration uncertainity</atitle><jtitle>Water resources research</jtitle><date>1992</date><risdate>1992</risdate><volume>28</volume><issue>3</issue><spage>803</spage><epage>814</epage><pages>803-814</pages><issn>0043-1397</issn><eissn>1944-7973</eissn><abstract>Lack of accurate information stemming from soil variability and climatic uncertainty obstructs efficient irrigation management. State-space models of soil water balance and potential evapotranspiration were used in the application of spatial-temporal estimation methods to reduce uncertainty. Temporal soil water storage estimates and estimation errors were obtained by the Kalman filter (KF). Spatial estimates were obtained by the conditional multivariate normal method. These spatial and temporal estimates were combined by an additional KF step that considers spatial estimates as measurements. Time-dependent soil water spatial covariance was approximated by assuming a constant correlation range and by using measurements variance to estimate the variogram "sill." Simulation and field results indicate that soil water storage estimates by the proposed method agreed better with measurements than estimates based on either spatial or temporal information only. The proposed estimation scheme can be extended to other systems with a simple physical model and a known spatial structure where only a few field measurements are available.</abstract></addata></record> |
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subjects | decision making evapotranspiration irrigation irrigation management mathematical models prediction simulation soil water balance soil water storage spatial distribution spatial variation temporal variation water availability |
title | Spatial and temporal soil water estimation considering soil variability and evapotranspiration uncertainity |
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