FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3193562989> ?p ?o ?g. }

• W3193562989 endingPage "126805" @default.
• W3193562989 startingPage "126805" @default.
• W3193562989 abstract "• Simple contextual model is attractive for the estimation of evapotranspiration (ET). • An operational new parameterization scheme based on feature space is proposed. • The scale dependencies are investigated by boundary parameters and ET performance. • The proposed method is superior to traditional method and has temporal continuity. • Large-scale ET distributions are obtained and are consistent with other products. A recent review has suggested relatively simple contextual models would remain attractive in the estimation of evapotranspiration (ET). The surface temperature-vegetation index feature space model is a typical representative since it provides direct monitoring of ET using simply and effective contextual information. However, the temporally continuous estimation and large-scale application issues are not well identified at previous studies. Under this background, the main motivation for this study is to develop an operational new parameterization scheme within the feature space framework for large-scale temporally continuous ET estimation. Specifically, the spatial domain division strategy was first designed to obtain the optimal grid division size for large-scale ET estimation. The model boundaries of these sub-regions were parameterized using spatial domain based temporal domain information at seasonal scale. The applicability of new method was demonstrated over the entire contiguous United States (CONUS) in the year 2008 using Moderate Resolution Imaging Spectroradiometer (MODIS) and Global Land Surface Satellite (GLASS) products. The comparison between present method and traditional method indicates that the new parameterization scheme produced at different reference spatial domains has a slight accuracy improvement over the 14 FLUXNET sites. In addition, the new method holds unique advantages in its simplicity and continuity, especially superior in the temporally continuous estimation of ET over a large extended region. The validation results of 14 FLUXNET sites indicate the correlation coefficient ( r ), mean absolute error ( MAE ), root mean square error ( RMSE ) the mean bias ( B ) values for continuous estimation of daily ET were 0.62, 28.430 W/m 2 , 36.133 W/m 2 and −0.059, respectively. The comparison results with existing ET product also demonstrated the comparable of ET distribution and estimates. Meanwhile, the boundary parameters obtained at seasonal scale also enhanced the physical meanings of feature space model. Consequently, the new parameterization scheme proposed in this study can be regarded as a suitable tool to provide large-scale temporally continuous estimation of ET." @default.
• W3193562989 created "2021-08-30" @default.
• W3193562989 creator A5021658618 @default.
• W3193562989 creator A5031590177 @default.
• W3193562989 date "2021-11-01" @default.
• W3193562989 modified "2023-10-13" @default.
• W3193562989 title "An operational parameterization scheme of surface temperature-vegetation index contextual model for large-scale temporally continuous evapotranspiration estimation: The case study of contiguous United States" @default.
• W3193562989 cites W1096706567 @default.
• W3193562989 cites W1480975298 @default.
• W3193562989 cites W1966664222 @default.
• W3193562989 cites W1968796030 @default.
• W3193562989 cites W1975768883 @default.
• W3193562989 cites W1977741125 @default.
• W3193562989 cites W1981072855 @default.
• W3193562989 cites W1985479415 @default.
• W3193562989 cites W1987269713 @default.
• W3193562989 cites W1995598225 @default.
• W3193562989 cites W2000204314 @default.
• W3193562989 cites W2002694429 @default.
• W3193562989 cites W2025667458 @default.
• W3193562989 cites W2028847099 @default.
• W3193562989 cites W2036091850 @default.
• W3193562989 cites W2039340172 @default.
• W3193562989 cites W2043809497 @default.
• W3193562989 cites W2052069508 @default.
• W3193562989 cites W2059254542 @default.
• W3193562989 cites W2060082190 @default.
• W3193562989 cites W2064616890 @default.
• W3193562989 cites W2065454207 @default.
• W3193562989 cites W2068371905 @default.
• W3193562989 cites W2073861093 @default.
• W3193562989 cites W2074330348 @default.
• W3193562989 cites W2081276204 @default.
• W3193562989 cites W2085250887 @default.
• W3193562989 cites W2086756300 @default.
• W3193562989 cites W2095505091 @default.
• W3193562989 cites W2114059122 @default.
• W3193562989 cites W2116310314 @default.
• W3193562989 cites W2117199485 @default.
• W3193562989 cites W2119895530 @default.
• W3193562989 cites W2129859781 @default.
• W3193562989 cites W2131372757 @default.
• W3193562989 cites W2132009606 @default.
• W3193562989 cites W2135685863 @default.
• W3193562989 cites W2140628086 @default.
• W3193562989 cites W2157245283 @default.
• W3193562989 cites W2159889702 @default.
• W3193562989 cites W2161425513 @default.
• W3193562989 cites W2166134628 @default.
• W3193562989 cites W2214587583 @default.
• W3193562989 cites W2304445877 @default.
• W3193562989 cites W2517674203 @default.
• W3193562989 cites W2519117257 @default.
• W3193562989 cites W2550427149 @default.
• W3193562989 cites W2557410000 @default.
• W3193562989 cites W2567491594 @default.
• W3193562989 cites W2572951874 @default.
• W3193562989 cites W2592917969 @default.
• W3193562989 cites W2595433512 @default.
• W3193562989 cites W2609446845 @default.
• W3193562989 cites W2609470236 @default.
• W3193562989 cites W2728254824 @default.
• W3193562989 cites W2754395170 @default.
• W3193562989 cites W2776608098 @default.
• W3193562989 cites W2790511636 @default.
• W3193562989 cites W2801531238 @default.
• W3193562989 cites W2809524951 @default.
• W3193562989 cites W2887176132 @default.
• W3193562989 cites W2900898478 @default.
• W3193562989 cites W2907203129 @default.
• W3193562989 cites W2914489851 @default.
• W3193562989 cites W2936443558 @default.
• W3193562989 cites W2966224244 @default.
• W3193562989 cites W2971638684 @default.
• W3193562989 cites W2995687014 @default.
• W3193562989 cites W3009198333 @default.
• W3193562989 cites W3014541478 @default.
• W3193562989 cites W3016799330 @default.
• W3193562989 cites W3019514966 @default.
• W3193562989 cites W3021367644 @default.
• W3193562989 cites W3047838136 @default.
• W3193562989 cites W3109588733 @default.
• W3193562989 doi "https://doi.org/10.1016/j.jhydrol.2021.126805" @default.
• W3193562989 hasPublicationYear "2021" @default.
• W3193562989 type Work @default.
• W3193562989 sameAs 3193562989 @default.
• W3193562989 citedByCount "4" @default.
• W3193562989 countsByYear W31935629892022 @default.
• W3193562989 countsByYear W31935629892023 @default.
• W3193562989 crossrefType "journal-article" @default.
• W3193562989 hasAuthorship W3193562989A5021658618 @default.
• W3193562989 hasAuthorship W3193562989A5031590177 @default.
• W3193562989 hasBestOaLocation W31935629891 @default.
• W3193562989 hasConcept C127313418 @default.
• W3193562989 hasConcept C136764020 @default.
• W3193562989 hasConcept C142724271 @default.
• W3193562989 hasConcept C153294291 @default.
• W3193562989 hasConcept C1549246 @default.

• next