Determination of regional land surface heat fluxes over a heterogeneous landscape of the Jiddah area of Saudi Arabia by using Landsat-7 ETM data

2007 ◽  
Vol 21 (14) ◽  
pp. 1892-1900 ◽  
Author(s):  
Yaoming Ma ◽  
Hui Tian ◽  
Hirohiko Ishikawa ◽  
Ryohji Ohba ◽  
Hiromasa Ueda ◽  
...  
Keyword(s):  
Saudi Arabia ◽  
Land Surface ◽  
Surface Heat ◽  
Heat Fluxes ◽  
Surface Heat Fluxes ◽  
Heterogeneous Landscape ◽  
Landsat 7 ◽  
Regional Land ◽  
Land Surface Heat Fluxes

Remote sensing parameterization of regional land surface heat fluxes over arid area in northwestern China

2004 ◽  
Vol 57 (2) ◽  
pp. 257-273 ◽  
Author(s):  
Yao-ming Ma ◽  
Massimo Menenti ◽  
Osamu Tsukamoto ◽  
Hirohiko Ishikawa ◽  
Jie-min Wang ◽  
...  
Keyword(s):  
Remote Sensing ◽  
Land Surface ◽  
Surface Heat ◽  
Arid Area ◽  
Heat Fluxes ◽  
Northwestern China ◽  
Surface Heat Fluxes ◽  
Regional Land ◽  
Land Surface Heat Fluxes

Trends of land surface heat fluxes on the Tibetan Plateau from 2001 to 2012

2017 ◽  
Vol 37 (14) ◽  
pp. 4757-4767 ◽  
Author(s):  
Cunbo Han ◽  
Yaoming Ma ◽  
Xuelong Chen ◽  
Zhongbo Su
Keyword(s):  
Tibetan Plateau ◽  
Land Surface ◽  
Surface Heat ◽  
Heat Fluxes ◽  
The Tibetan Plateau ◽  
Surface Heat Fluxes ◽  
Land Surface Heat Fluxes

The progress on the observation and modeling of surface heat fluxes and evapotranspiration over heterogeneous landscapes of the Third Pole region

2020 ◽  
Author(s):  
Yaoming Ma
Keyword(s):  
Heat Flux ◽  
Latent Heat Flux ◽  
Land Surface ◽  
Sensible Heat Flux ◽  
Surface Heat ◽  
Heat Fluxes ◽  
Sensible Heat ◽  
Surface Heat Fluxes ◽  
The Third ◽  
Land Surface Heat Fluxes

<p>The exchange of heat and water vapor between land surface and atmosphere over the Third Pole region (Tibetan Plateau and nearby surrounding region) plays an important role in Asian monsoon, westerlies and the northern hemisphere weather and climate systems. Supported by various agencies in the People’s Republic of China, a Third Pole Environment (TPE) observation and research Platform (TPEORP) is now implementing over the Third Pole region. The background of the establishment of the TPEORP, the establishing and monitoring plan of long-term scale (5-10 years) of it will be shown firstly. Then the preliminary observational analysis results, such as the characteristics of land surface energy fluxes partitioning and the turbulent characteristics will also been shown in this study. Then, the parameterization methodology based on satellite data and the atmospheric boundary layer (ABL) observations has been proposed and tested for deriving regional distribution of net radiation flux, soil heat flux, sensible heat flux and latent heat flux (evapotranspiration (ET)) and their variation trends over the heterogeneous landscape of the Tibetan Plateau (TP) area. To validate the proposed methodology, the ground measured net radiation flux, soil heat flux, sensible heat flux and latent heat flux of the TPEORP are compared to the derived values. The results showed that the derived land surface heat fluxes over the study areas are in good accordance with the land surface status. These parameters show a wide range due to the strong contrast of surface feature. And the estimated land surface heat fluxes are in good agreement with ground measurements, and all the absolute percent difference in less than 10% in the validation sites. The sensible heat flux has increased slightly and the latent heat flux has decreased from 2001 to 2016 over the TP. It is therefore conclude that the proposed methodology is successful for the retrieval of land surface heat fluxes and ET over heterogeneous landscape of the TP area. Further improvement of the methodology and its applying field over the whole Third Pole region and Pan-Third Pole region were also discussed.</p>

Remote sensing parameterization of land surface heat fluxes over arid and semi-arid areas

2003 ◽  
Vol 20 (4) ◽  
pp. 530-539 ◽  
Author(s):  
Ma Yaoming ◽  
Wang Jiemin ◽  
Huang Ronghui ◽  
Wei Guoan ◽  
Massimo Menenti ◽  
...  
Keyword(s):  
Remote Sensing ◽  
Land Surface ◽  
Surface Heat ◽  
Heat Fluxes ◽  
Arid Areas ◽  
Surface Heat Fluxes ◽  
Semi Arid ◽  
Land Surface Heat Fluxes

scholarly journals Analysis of Land Surface Heat Fluxes Using the Orthonormal Wavelet Approach

1995 ◽  
Vol 31 (11) ◽  
pp. 2743-2749 ◽  
Author(s):  
Gabriel G. Katul ◽  
Marc B. Parlange
Keyword(s):  
Land Surface ◽  
Surface Heat ◽  
Heat Fluxes ◽  
Orthonormal Wavelet ◽  
Surface Heat Fluxes ◽  
Land Surface Heat Fluxes

scholarly journals Estimating surface fluxes over middle and upper streams of the Heihe River Basin with ASTER imagery

2009 ◽  
Vol 6 (3) ◽  
pp. 4619-4635 ◽  
Author(s):  
W. Ma ◽  
Y. Ma ◽  
Z. Hu ◽  
B. Su ◽  
J. Wang ◽  
...  
Keyword(s):  
Heat Flux ◽  
Land Surface ◽  
Sensible Heat Flux ◽  
Surface Heat ◽  
Surface Fluxes ◽  
Heat Fluxes ◽  
Heihe River ◽  
Surface Heat Fluxes ◽  
Aster Data ◽  
Land Surface Heat Fluxes

Abstract. Surface fluxes are important boundary conditions for climatological modeling and the Asian monsoon system. Recent availability of high-resolution, multi-band imagery from the ASTER (Advanced Space-borne Thermal Emission and Reflection Radiometer) sensor has enabled us to estimate surface fluxes to bridge the gap between local scale flux measurements using micrometeorological instruments and regional scale land-atmosphere exchanges of water and heat fluxes that are fundamental for the understanding of the water cycle in the Asian monsoon system. A Surface Energy Balance System (SEBS) method based on ASTER data and field observations has been proposed and tested for deriving net radiation flux (Rn), soil heat flux (G0), sensible heat flux (H) and latent heat flux (λ E) over heterogeneous land surface in this paper. As a case study, the methodology was applied to the experimental area of the WATER (Watershed Allied Telemetry Experimental Research), located at the mid-to-upstream sections of the Heihe River, northwest China. The ASTER data of 3 May and 4 June in 2008 was used in this paper for the case of mid-to-upstream sections of the Heihe River Basin. To validate the proposed methodology, the ground-measured land surface heat fluxes (net radiation flux (Rn), soil heat flux (G0), sensible heat flux (H) and latent heat flux (λ E)) were compared to the ASTER derived values. The results show that the derived surface variables and land surface heat fluxes in different months over the study area are in good accordance with the land surface status. It is therefore concluded that the proposed methodology is successful for the retrieval of land surface heat fluxes using the ASTER data and filed observation over the study area.

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