4.7 Article

A method to estimate diurnal surface soil heat flux from MODIS data for a sparse vegetation and bare soil

Journal

JOURNAL OF HYDROLOGY
Volume 511, Issue -, Pages 139-150

Publisher

ELSEVIER
DOI: 10.1016/j.jhydrol.2014.01.019

Keywords

Surface soil heat flux; Surface temperature; Real soil thermal inertia; MODIS; Heihe River Basin

Funding

  1. National Natural Scientific Foundations of China [91025007]
  2. Strategic Priority Research Program-Climate Change: Carbon Budget and Related Issues of the Chinese Academy of Sciences [XDA05050109]
  3. Remote Sensing Investigation and Assessment Project of National Eco-Environmental Variation during the Past Ten Years [STSN-01-11]
  4. NASA Goddard Space Flight Center (GSFC)
  5. Distributed Active Archive Center (GDAAC)

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This paper proposes a mathematical method based on a one-dimensional diffusion equation to derive diurnal variation of surface soil heat flux using cloudless MODIS data for a sparse vegetation and bare soil. Diurnal variation of the surface temperature and near-surface real soil thermal inertia are both simulated from the MODIS data. The study was carried out for the Yingke oasis plains area and the Arou alpine meadow area, which are located in the midstream and upstream, respectively, of the Heihe River Basin. Statistical results showed that the proposed method performs well to estimate soil heat flux for both study areas. In the oasis plains case, the coefficient of determination (R-2) was 0.958 and the index of agreement (d) was 0.989. In the alpine meadow case, the coefficient of determination (R-2) was 0.972 and the index of agreement (d) was 0.993. Close agreement of the estimated surface soil heat flux with measured observations indicates that the method is promising. Future work will focus on scaling this mathematical method to create a diurnal surface soil heat flux map. Crown Copyright (c) 2014 Published by Elsevier B.V. All rights reserved.

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