Artigo Revisado por pares

Sensitivity of soil surface temperature in a force-restore equation to heat fluxes and deep soil temperature

1999; Wiley; Volume: 19; Issue: 14 Linguagem: Inglês

10.1002/(sici)1097-0088(19991130)19

ISSN

1097-0088

Autores

Dragutin T. Mihailović, George Kallos, Ilija Arsenić, Branislava Lalić, Borivoj Rajković, Αναστάσιος Παπαδόπουλος,

Tópico(s)

Landslides and related hazards

Resumo

International Journal of ClimatologyVolume 19, Issue 14 p. 1617-1632 Research Article Sensitivity of soil surface temperature in a force-restore equation to heat fluxes and deep soil temperature Dragutin T. Mihailović, Corresponding Author Dragutin T. Mihailović Faculty of Agriculture, University of Novi Sad and Center for Meteorology and Environmental Modelling, CIMS, University of Novi Sad, 21000 Novi Sad, YugoslaviaFaculty of Agriculture, University of Novi Sad and Center for Meteorology and Environmental Modelling, CIMS, University of Novi Sad, 21000 Novi Sad, YugoslaviaSearch for more papers by this authorGeorge Kallos, George Kallos Department of Applied Physics, University of Athens, 15874 Athens, GreeceSearch for more papers by this authorIlija D. Arsenić, Ilija D. Arsenić Faculty of Agriculture, University of Novi Sad and Center for Meteorology and Environmental Modelling, CIMS, University of Novi Sad, 21000 Novi Sad, YugoslaviaSearch for more papers by this authorBranislava Lalić, Branislava Lalić Faculty of Agriculture, University of Novi Sad and Center for Meteorology and Environmental Modelling, CIMS, University of Novi Sad, 21000 Novi Sad, YugoslaviaSearch for more papers by this authorBorivoj Rajković, Borivoj Rajković Faculty of Physics, University of Belgrade, 11000 Belgrade, YugoslaviaSearch for more papers by this authorAtanasios Papadopoulos, Atanasios Papadopoulos Department of Applied Physics, University of Athens, 15874 Athens, GreeceSearch for more papers by this author Dragutin T. Mihailović, Corresponding Author Dragutin T. Mihailović Faculty of Agriculture, University of Novi Sad and Center for Meteorology and Environmental Modelling, CIMS, University of Novi Sad, 21000 Novi Sad, YugoslaviaFaculty of Agriculture, University of Novi Sad and Center for Meteorology and Environmental Modelling, CIMS, University of Novi Sad, 21000 Novi Sad, YugoslaviaSearch for more papers by this authorGeorge Kallos, George Kallos Department of Applied Physics, University of Athens, 15874 Athens, GreeceSearch for more papers by this authorIlija D. Arsenić, Ilija D. Arsenić Faculty of Agriculture, University of Novi Sad and Center for Meteorology and Environmental Modelling, CIMS, University of Novi Sad, 21000 Novi Sad, YugoslaviaSearch for more papers by this authorBranislava Lalić, Branislava Lalić Faculty of Agriculture, University of Novi Sad and Center for Meteorology and Environmental Modelling, CIMS, University of Novi Sad, 21000 Novi Sad, YugoslaviaSearch for more papers by this authorBorivoj Rajković, Borivoj Rajković Faculty of Physics, University of Belgrade, 11000 Belgrade, YugoslaviaSearch for more papers by this authorAtanasios Papadopoulos, Atanasios Papadopoulos Department of Applied Physics, University of Athens, 15874 Athens, GreeceSearch for more papers by this author First published: 30 November 1999 https://doi.org/10.1002/(SICI)1097-0088(19991130)19:14 3.0.CO;2-BCitations: 17AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onEmailFacebookTwitterLinkedInRedditWechat Abstract The ‘force-restore’ approach is commonly used in order to calculate the surface temperature in atmospheric models. A critical point in this method is how to calculate the deep soil temperature which appears in the restore term of the ‘force-restore’ equation. If the prognostic equation for calculating the deep soil temperature is used, some errors in surface temperature calculation and consequently in partitioning the surface energy and land surface water can be introduced. Usually, these errors should appear as a result of incorrect parameterization of surface energy terms in the prognostic equation based on ‘force-restore’ approach. In this paper, the sensitivity of the ‘force-restore’ model for surface temperature to the: (a) changes of soil heat flux; (b) variations of deep soil temperature and (c) changes in soil water evaporation is examined. In addition, the impact of the deep soil temperature variations on partitioning the surface energy and land surface water is discussed. Finally, a new procedure for calculating the deep soil temperature based, on climatological data of soil temperature and its exponential attenuation in the deep soil layers is suggested. All numerical experiments with the LAPS land surface scheme were performed using two data sets, obtained from the micrometeorological measurements over a bare soil at Rimski Šančevi (Yugoslavia), RS, and Caumont (France), HAPEX. Copyright © 1999 Royal Meteorological Society References Acs, F., Mihailović, D.T. and Rajkovic, B. 1991. ‘A coupled soil moisture and surface temperature model’, J. Appl. Meteorol., 30, 812–822. 10.1175/1520-0450(1991)030 2.0.CO;2 Web of Science®Google Scholar Bhumralkar, C.M. 1975. ‘Numerical experiments on the computation of ground surface temperature in an atmospheric general circulation model’, J. Appl. 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