Simulating tropical bare soil surface temperature using the force-restore method

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1. Verfasser: Olaniran, Jonathan Matthew
Format: Abschlussarbeit
Sprache:Englisch
Veröffentlicht: Obafemi Awolowo University 2019
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Online-Zugang:https://ir.oauife.edu.ng/handle/123456789/4315
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author Olaniran, Jonathan Matthew
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spelling oai:ir.oauife.edu.ng:123456789-43152023-05-13T11:31:08Z Simulating tropical bare soil surface temperature using the force-restore method Olaniran, Jonathan Matthew Tropical Bare Soil Force Restore Method Obafemi Awolowo University Teaching and Research Farm Temperature Soil Force restore viii,48 The force-restore (FR) method is a simple and efficient approximation procedure that can be used for predicting soil thermal characteristics such as ground heat flux and the surface temperature. It uses a prognostic energy-balance equation and the response to a periodic heating caused by diurnal variation of the solar radiation. Several variants of the FR method exist and have been developed and tested for the high latitude regions, but is rare for the tropical areas. In this particular study, a force-restore (FR) model is adapted to simulate bare soil surface temperature and other thermal properties at an experimental site a (tropical location) chosen inside the Teaching and Research Farm of Obafemi Awolowo University Ile-Ife, Nigeria (7.55oN, 4.56oE). In the model, the surface energy balance equation used does not contain the latent heat flux term. Thus it was assumed that evaporation/condensation processes at the surface was neglected. The relative contributions of the imposed initial conditions; deep ground temperature, soil thermal characteristics, surface temperature, and cloud cover fractions, were used to investigate the performance of the FR model. The numerical simulations of the energy fluxes and surface temperature were then compared with the observed field data. The FR method worked quite well for estimating the diurnal variation of bare (dry) soil surface temperature within a range of ± 2.0oC from actual values. On clear and relatively dry days, the simulated net radiative flux attained a maximum value of (420± 10)Wm-2 at about 1400hrs local time. It was found that the bare soil surface temperature depends essentially on the soil thermal properties, deep soil temperature and the cloud cover fractions. The result of this study is found useful for agrometeorological purposes particularly for predicting the soil surface temperature and frost conditions. 2019-07-03T08:10:14Z 2019-07-03T08:10:14Z 2006 Thesis Olaniran, J.M. (2006). Simulating tropical bare soil surface temperature using the force-restore method https://ir.oauife.edu.ng/handle/123456789/4315 en application/pdf Obafemi Awolowo University
spellingShingle Tropical Bare Soil
Force Restore Method
Obafemi Awolowo University Teaching and Research Farm
Temperature
Soil
Force restore
Olaniran, Jonathan Matthew
Simulating tropical bare soil surface temperature using the force-restore method
title Simulating tropical bare soil surface temperature using the force-restore method
title_full Simulating tropical bare soil surface temperature using the force-restore method
title_fullStr Simulating tropical bare soil surface temperature using the force-restore method
title_full_unstemmed Simulating tropical bare soil surface temperature using the force-restore method
title_short Simulating tropical bare soil surface temperature using the force-restore method
title_sort simulating tropical bare soil surface temperature using the force restore method
topic Tropical Bare Soil
Force Restore Method
Obafemi Awolowo University Teaching and Research Farm
Temperature
Soil
Force restore
url https://ir.oauife.edu.ng/handle/123456789/4315
work_keys_str_mv AT olaniranjonathanmatthew simulatingtropicalbaresoilsurfacetemperatureusingtheforcerestoremethod