Abstract
Accurate estimation of latent heat flux (LE) based on remote sensing data is critical in characterizing terrestrial ecosystems and modeling land surface processes. Many LE products were released during the past few decades, but their quality might not meet the requirements in terms of data consistency and estimation accuracy. Merging multiple algorithms could be an effective way to improve the quality of existing LE products. In this paper, we present a data integration method based on modified empirical orthogonal function (EOF) analysis to integrate the Moderate Resolution Imaging Spectroradiometer (MODIS) LE product (MOD16) and the Priestley-Taylor LE algorithm of Jet Propulsion Laboratory (PT-JPL) estimate. Twenty-two eddy covariance (EC) sites with LE observation were chosen to evaluate our algorithm, showing that the proposed EOF fusion method was capable of integrating the two satellite data sets with improved consistency and reduced uncertainties. Further efforts were needed to evaluate and improve the proposed algorithm at larger spatial scales and time periods, and over different land cover types.
Highlights
Terrestrial latent heat flux (LE), the flux of heat from the Earth’s surface to the atmosphere that is associated with soil evaporation and plant transpiration, and is a key component of the hydrological and carbon cycles [1, 2]
LE estimates from MOD16 and Priestley-Taylor LE algorithm of Jet Propulsion Laboratory (PT-JPL) based on both tower-measured meteorology data and modern-era retrospective analysis for research and applications (MERRA) meteorology data were compared
The correlation coefficients, R2, of the TP-JPL and MOD16 using in situ meteorology data are higher than 0.6, which corresponds to a good correlation to the measured LE values
Summary
Terrestrial latent heat flux (LE), the flux of heat from the Earth’s surface to the atmosphere that is associated with soil evaporation and plant transpiration, and is a key component of the hydrological and carbon cycles [1, 2]. Accurate and temporally continuous estimation of LE is PLOS ONE | DOI:10.1371/journal.pone.0160150. A Function-Based Algorithm for Estimating Terrestrial Latent Heat Flux. Accurate and temporally continuous estimation of LE is PLOS ONE | DOI:10.1371/journal.pone.0160150 July 29, 2016
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