Numerical solution of a complete surface energy balance model for simulation of heat fluxes and surface temperature under bare soil environment

Zhihao Qin; Pedro Berliner; Arnon Karnieli

doi:10.1016/S0096-3003(01)00089-3

Numerical solution of a complete surface energy balance model for simulation of heat fluxes and surface temperature under bare soil environment

Zhihao Qin, Pedro Berliner, Arnon Karnieli

Research output: Contribution to journal › Article › peer-review

32 Scopus citations

Abstract

The numerical solution of a complete surface energy balance model for simulation of heat fluxes and surface temperature under bare soil environment was presented. The surface energy balance model was an essential approach for heat flux and evaporation estimation in applied meterology and hydrology. The iterative computation of Newton-Raphson method was used for the approximation of latent heat flux and surface temperature from the balances. Results proved the validity of the model and method used for the numerical solution.

Original language	English
Pages (from-to)	171-200
Number of pages	30
Journal	Applied Mathematics and Computation
Volume	130
Issue number	1
DOIs	https://doi.org/10.1016/S0096-3003(01)00089-3
State	Published - 25 Jul 2002

Keywords

Heat fluxes
Israeli desert
Numerical solution
Surface energy balance model
Surface temperature

ASJC Scopus subject areas

Computational Mathematics
Applied Mathematics

Access to Document

10.1016/S0096-3003(01)00089-3

Cite this

@article{b1549541698f434b985df62f2f869046,

title = "Numerical solution of a complete surface energy balance model for simulation of heat fluxes and surface temperature under bare soil environment",

abstract = "The numerical solution of a complete surface energy balance model for simulation of heat fluxes and surface temperature under bare soil environment was presented. The surface energy balance model was an essential approach for heat flux and evaporation estimation in applied meterology and hydrology. The iterative computation of Newton-Raphson method was used for the approximation of latent heat flux and surface temperature from the balances. Results proved the validity of the model and method used for the numerical solution.",

keywords = "Heat fluxes, Israeli desert, Numerical solution, Surface energy balance model, Surface temperature",

author = "Zhihao Qin and Pedro Berliner and Arnon Karnieli",

note = "Funding Information: The authors would like to thank the International Center for Desert Research, J. Blaustein Institute for Desert Research, Ben Gurion University of the Negev for offering a fellowship to Qin Zhihao to conduct the research. We also would like to extend our thanks to the Laboratory of Desert Meteorology, Dept. of Environmental Physics J. Blaustein Institute for Desert Research, Ben Gurion University of the Negev for providing the required meteorological data used in the study.",

year = "2002",

month = jul,

day = "25",

doi = "10.1016/S0096-3003(01)00089-3",

language = "English",

volume = "130",

pages = "171--200",

journal = "Applied Mathematics and Computation",

issn = "0096-3003",

publisher = "Elsevier Inc.",

number = "1",

}

TY - JOUR

T1 - Numerical solution of a complete surface energy balance model for simulation of heat fluxes and surface temperature under bare soil environment

AU - Qin, Zhihao

AU - Berliner, Pedro

AU - Karnieli, Arnon

N1 - Funding Information: The authors would like to thank the International Center for Desert Research, J. Blaustein Institute for Desert Research, Ben Gurion University of the Negev for offering a fellowship to Qin Zhihao to conduct the research. We also would like to extend our thanks to the Laboratory of Desert Meteorology, Dept. of Environmental Physics J. Blaustein Institute for Desert Research, Ben Gurion University of the Negev for providing the required meteorological data used in the study.

PY - 2002/7/25

Y1 - 2002/7/25

N2 - The numerical solution of a complete surface energy balance model for simulation of heat fluxes and surface temperature under bare soil environment was presented. The surface energy balance model was an essential approach for heat flux and evaporation estimation in applied meterology and hydrology. The iterative computation of Newton-Raphson method was used for the approximation of latent heat flux and surface temperature from the balances. Results proved the validity of the model and method used for the numerical solution.

AB - The numerical solution of a complete surface energy balance model for simulation of heat fluxes and surface temperature under bare soil environment was presented. The surface energy balance model was an essential approach for heat flux and evaporation estimation in applied meterology and hydrology. The iterative computation of Newton-Raphson method was used for the approximation of latent heat flux and surface temperature from the balances. Results proved the validity of the model and method used for the numerical solution.

KW - Heat fluxes

KW - Israeli desert

KW - Numerical solution

KW - Surface energy balance model

KW - Surface temperature

UR - http://www.scopus.com/inward/record.url?scp=0037173502&partnerID=8YFLogxK

U2 - 10.1016/S0096-3003(01)00089-3

DO - 10.1016/S0096-3003(01)00089-3

M3 - Article

AN - SCOPUS:0037173502

VL - 130

SP - 171

EP - 200

JO - Applied Mathematics and Computation

JF - Applied Mathematics and Computation

SN - 0096-3003

IS - 1

ER -

Numerical solution of a complete surface energy balance model for simulation of heat fluxes and surface temperature under bare soil environment

Abstract

Keywords

ASJC Scopus subject areas

Access to Document

Other files and links

Fingerprint

Cite this