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DOI | 10.3390/rs70708250 |
Estimation of Surface Soil Moisture from Thermal Infrared Remote Sensing Using an Improved Trapezoid Method | |
Yang, Yuting; Guan, Huade; Long, Di; Liu, Bing; Qin, Guanghua; Qin, Jun; Batelaan, Okke | |
通讯作者 | Yang, YT (通讯作者) |
发表日期 | 2015 |
EISSN | 2072-4292 |
起始页码 | 8250 |
结束页码 | 8270 |
卷号 | 7期号:7 |
英文摘要 | Surface soil moisture (SM) plays a fundamental role in energy and water partitioning in the soil-plant-atmosphere continuum. A reliable and operational algorithm is much needed to retrieve regional surface SM at high spatial and temporal resolutions. Here, we provide an operational framework of estimating surface SM at fine spatial resolutions (using visible/thermal infrared images and concurrent meteorological data) based on a trapezoidal space defined by remotely sensed vegetation cover (F-c) and land surface temperature (LST). Theoretical solutions of the wet and dry edges were derived to achieve a more accurate and effective determination of the F-c/LST space. Subjectivity and uncertainty arising from visual examination of extreme boundaries can consequently be largely reduced. In addition, theoretical derivation of the extreme boundaries allows a per-pixel determination of the VI/LST space such that the assumption of uniform atmospheric forcing over the entire domain is no longer required. The developed approach was tested at the Tibetan Plateau Soil Moisture/Temperature Monitoring Network (SMTMN) site in central Tibet, China, from August 2010 to August 2011 using Moderate Resolution Imaging Spectroradiometer (MODIS) Terra images. Results indicate that the developed trapezoid model reproduced the spatial and temporal patterns of observed surface SM reasonably well, with showing a root-mean-square error of 0.06 m(3)center dot m(-3) at the site level and 0.03 m(3)center dot m(-3) at the regional scale. In addition, a case study on 2 September 2010 highlighted the importance of the theoretically calculated wet and dry edges, as they can effectively obviate subjectivity and uncertainties in determining the F-c/LST space arising from visual interpretation of satellite images. Compared with Land Surface Models (LSMs) in Global Land Data Assimilation System-1, the remote sensing-based trapezoid approach gave generally better surface SM estimates, whereas the LSMs showed systematic underestimation. Sensitivity analyses suggested that the trapezoid method is most sensitive to field capacity and temperature but less sensitive to other meteorological observations and parameters. |
关键词 | TRIANGLE METHODENERGY FLUXESWATER STORAGEMODELEVAPOTRANSPIRATIONRETRIEVALSNETWORKTEMPERATUREPREDICTIONALGORITHM |
语种 | 英语 |
WOS研究方向 | Environmental Sciences & Ecology ; Geology ; Remote Sensing ; Imaging Science & Photographic Technology |
WOS类目 | Environmental Sciences ; Geosciences, Multidisciplinary ; Remote Sensing ; Imaging Science & Photographic Technology |
WOS记录号 | WOS:000360919900001 |
来源期刊 | REMOTE SENSING |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258584 |
推荐引用方式 GB/T 7714 | Yang, Yuting,Guan, Huade,Long, Di,et al. Estimation of Surface Soil Moisture from Thermal Infrared Remote Sensing Using an Improved Trapezoid Method[J]. 中国科学院青藏高原研究所,2015,7(7). |
APA | Yang, Yuting.,Guan, Huade.,Long, Di.,Liu, Bing.,Qin, Guanghua.,...&Batelaan, Okke.(2015).Estimation of Surface Soil Moisture from Thermal Infrared Remote Sensing Using an Improved Trapezoid Method.REMOTE SENSING,7(7). |
MLA | Yang, Yuting,et al."Estimation of Surface Soil Moisture from Thermal Infrared Remote Sensing Using an Improved Trapezoid Method".REMOTE SENSING 7.7(2015). |
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