Long-term Soil Moisture Time Series Analyses based on Active Microwave Backscatter Measurements

Active microwave sensors operating at lower microwave frequencies in the range from 1 to 10 GHz provide backscatter measurements that are sensitive to the moisture content of the soil. Thanks to a series of European C-band (5.3 GHz) scatterometers, which were first flown on board of the European Rem...

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Main Authors: W. Wagner, C. Reimer, B. Bauer-Marschallinger, M. Enenkel, S. Hahn, T. Melzer, V. Naeimi, C. Paulik, W. Dorigo
Format: Article
Language:English
Published: Copernicus Publications 2015-04-01
Series:The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Online Access:http://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XL-7-W3/545/2015/isprsarchives-XL-7-W3-545-2015.pdf
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author W. Wagner
C. Reimer
B. Bauer-Marschallinger
M. Enenkel
S. Hahn
T. Melzer
V. Naeimi
C. Paulik
W. Dorigo
author_facet W. Wagner
C. Reimer
B. Bauer-Marschallinger
M. Enenkel
S. Hahn
T. Melzer
V. Naeimi
C. Paulik
W. Dorigo
author_sort W. Wagner
collection DOAJ
description Active microwave sensors operating at lower microwave frequencies in the range from 1 to 10 GHz provide backscatter measurements that are sensitive to the moisture content of the soil. Thanks to a series of European C-band (5.3 GHz) scatterometers, which were first flown on board of the European Remote Sensing satellites ERS-1 and ERS-2, and later on board of MetOp-A and MetOp -B, we are now in the possession of a long-term soil moisture time series starting in 1991. The creation of globally consistent long-term soil moisture time series is a challenging task. The TU-Wien soil moisture algorithm is adopted to tackle these challenges. In this paper we present two methodologies that were developed to ensure radiometric stability of the European C-band scatterometers. The objective of sensor intra-calibration is to monitor and correct for radiometric instabilities within one scatterometer mission, while sensor inter-calibration aims to remove radiometric differences across several missions. In addition, a novel vegetation modelling approach is presented that enables the estimation of vegetation parameters for each day across several years to account for yearly to longer-term changes in vegetation phenology and land cover.
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spelling doaj.art-96910914c24b49f4ba4b15695e3404b02022-12-22T03:11:43ZengCopernicus PublicationsThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences1682-17502194-90342015-04-01XL-7/W354555010.5194/isprsarchives-XL-7-W3-545-2015Long-term Soil Moisture Time Series Analyses based on Active Microwave Backscatter MeasurementsW. Wagner0C. Reimer1B. Bauer-Marschallinger2M. Enenkel3S. Hahn4T. Melzer5V. Naeimi6C. Paulik7W. Dorigo8Vienna University of Technology, Department of Geodesy and Geoinformation, Vienna, AustriaVienna University of Technology, Department of Geodesy and Geoinformation, Vienna, AustriaVienna University of Technology, Department of Geodesy and Geoinformation, Vienna, AustriaVienna University of Technology, Department of Geodesy and Geoinformation, Vienna, AustriaVienna University of Technology, Department of Geodesy and Geoinformation, Vienna, AustriaVienna University of Technology, Department of Geodesy and Geoinformation, Vienna, AustriaVienna University of Technology, Department of Geodesy and Geoinformation, Vienna, AustriaVienna University of Technology, Department of Geodesy and Geoinformation, Vienna, AustriaVienna University of Technology, Department of Geodesy and Geoinformation, Vienna, AustriaActive microwave sensors operating at lower microwave frequencies in the range from 1 to 10 GHz provide backscatter measurements that are sensitive to the moisture content of the soil. Thanks to a series of European C-band (5.3 GHz) scatterometers, which were first flown on board of the European Remote Sensing satellites ERS-1 and ERS-2, and later on board of MetOp-A and MetOp -B, we are now in the possession of a long-term soil moisture time series starting in 1991. The creation of globally consistent long-term soil moisture time series is a challenging task. The TU-Wien soil moisture algorithm is adopted to tackle these challenges. In this paper we present two methodologies that were developed to ensure radiometric stability of the European C-band scatterometers. The objective of sensor intra-calibration is to monitor and correct for radiometric instabilities within one scatterometer mission, while sensor inter-calibration aims to remove radiometric differences across several missions. In addition, a novel vegetation modelling approach is presented that enables the estimation of vegetation parameters for each day across several years to account for yearly to longer-term changes in vegetation phenology and land cover.http://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XL-7-W3/545/2015/isprsarchives-XL-7-W3-545-2015.pdf
spellingShingle W. Wagner
C. Reimer
B. Bauer-Marschallinger
M. Enenkel
S. Hahn
T. Melzer
V. Naeimi
C. Paulik
W. Dorigo
Long-term Soil Moisture Time Series Analyses based on Active Microwave Backscatter Measurements
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
title Long-term Soil Moisture Time Series Analyses based on Active Microwave Backscatter Measurements
title_full Long-term Soil Moisture Time Series Analyses based on Active Microwave Backscatter Measurements
title_fullStr Long-term Soil Moisture Time Series Analyses based on Active Microwave Backscatter Measurements
title_full_unstemmed Long-term Soil Moisture Time Series Analyses based on Active Microwave Backscatter Measurements
title_short Long-term Soil Moisture Time Series Analyses based on Active Microwave Backscatter Measurements
title_sort long term soil moisture time series analyses based on active microwave backscatter measurements
url http://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XL-7-W3/545/2015/isprsarchives-XL-7-W3-545-2015.pdf
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