Evaluation of Soil Moisture Retrieval from the ERS and Metop Scatterometers in the Lower Mekong Basin

The natural environment and livelihoods in the Lower Mekong Basin (LMB) are significantly affected by the annual hydrological cycle. Monitoring of soil moisture as a key variable in the hydrological cycle is of great interest in a number of Hydrological and agricultural applications. In this study w...

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Main Authors: Heiko Apel, Claudia Kuenzer, Wolfgang Wagner, Daniel Sabel, Patrick Leinenkugel, Vahid Naeimi
Format: Article
Language:English
Published: MDPI AG 2013-03-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/5/4/1603
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spelling doaj-6739130ca6fd466c835e697b1e9ee1bb2020-11-24T22:29:11ZengMDPI AGRemote Sensing2072-42922013-03-01541603162310.3390/rs5041603Evaluation of Soil Moisture Retrieval from the ERS and Metop Scatterometers in the Lower Mekong BasinHeiko ApelClaudia KuenzerWolfgang WagnerDaniel SabelPatrick LeinenkugelVahid NaeimiThe natural environment and livelihoods in the Lower Mekong Basin (LMB) are significantly affected by the annual hydrological cycle. Monitoring of soil moisture as a key variable in the hydrological cycle is of great interest in a number of Hydrological and agricultural applications. In this study we evaluated the quality and spatiotemporal variability of the soil moisture product retrieved from C-band scatterometers data across the LMB sub-catchments. The soil moisture retrieval algorithm showed reasonable performance in most areas of the LMB with the exception of a few sub-catchments in the eastern parts of Laos, where the land cover is characterized by dense vegetation. The best performance of the retrieval algorithm was obtained in agricultural regions. Comparison of the available in situ evaporation data in the LMB and the Basin Water Index (BWI), an indicator of the basin soil moisture condition, showed significant negative correlations up to R = −0.85. The inter-annual variation of the calculated BWI was also found corresponding to the reported extreme hydro-meteorological events in the Mekong region. The retrieved soil moisture data show high correlation (up to R = 0.92) with monthly anomalies of precipitation in non-irrigated regions. In general, the seasonal variability of soil moisture in the LMB was well captured by the retrieval method. The results of analysis also showed significant correlation between El Niño events and the monthly BWI anomaly measurements particularly for the month May with the maximum correlation of R = 0.88.http://www.mdpi.com/2072-4292/5/4/1603soil moistureScatterometerASCATMekong
collection DOAJ
language English
format Article
sources DOAJ
author Heiko Apel
Claudia Kuenzer
Wolfgang Wagner
Daniel Sabel
Patrick Leinenkugel
Vahid Naeimi
spellingShingle Heiko Apel
Claudia Kuenzer
Wolfgang Wagner
Daniel Sabel
Patrick Leinenkugel
Vahid Naeimi
Evaluation of Soil Moisture Retrieval from the ERS and Metop Scatterometers in the Lower Mekong Basin
Remote Sensing
soil moisture
Scatterometer
ASCAT
Mekong
author_facet Heiko Apel
Claudia Kuenzer
Wolfgang Wagner
Daniel Sabel
Patrick Leinenkugel
Vahid Naeimi
author_sort Heiko Apel
title Evaluation of Soil Moisture Retrieval from the ERS and Metop Scatterometers in the Lower Mekong Basin
title_short Evaluation of Soil Moisture Retrieval from the ERS and Metop Scatterometers in the Lower Mekong Basin
title_full Evaluation of Soil Moisture Retrieval from the ERS and Metop Scatterometers in the Lower Mekong Basin
title_fullStr Evaluation of Soil Moisture Retrieval from the ERS and Metop Scatterometers in the Lower Mekong Basin
title_full_unstemmed Evaluation of Soil Moisture Retrieval from the ERS and Metop Scatterometers in the Lower Mekong Basin
title_sort evaluation of soil moisture retrieval from the ers and metop scatterometers in the lower mekong basin
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2013-03-01
description The natural environment and livelihoods in the Lower Mekong Basin (LMB) are significantly affected by the annual hydrological cycle. Monitoring of soil moisture as a key variable in the hydrological cycle is of great interest in a number of Hydrological and agricultural applications. In this study we evaluated the quality and spatiotemporal variability of the soil moisture product retrieved from C-band scatterometers data across the LMB sub-catchments. The soil moisture retrieval algorithm showed reasonable performance in most areas of the LMB with the exception of a few sub-catchments in the eastern parts of Laos, where the land cover is characterized by dense vegetation. The best performance of the retrieval algorithm was obtained in agricultural regions. Comparison of the available in situ evaporation data in the LMB and the Basin Water Index (BWI), an indicator of the basin soil moisture condition, showed significant negative correlations up to R = −0.85. The inter-annual variation of the calculated BWI was also found corresponding to the reported extreme hydro-meteorological events in the Mekong region. The retrieved soil moisture data show high correlation (up to R = 0.92) with monthly anomalies of precipitation in non-irrigated regions. In general, the seasonal variability of soil moisture in the LMB was well captured by the retrieval method. The results of analysis also showed significant correlation between El Niño events and the monthly BWI anomaly measurements particularly for the month May with the maximum correlation of R = 0.88.
topic soil moisture
Scatterometer
ASCAT
Mekong
url http://www.mdpi.com/2072-4292/5/4/1603
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