C-Band SAR Imagery for Snow-Cover Monitoring at Treeline
Abstract: RADARSAT and ERS-2 data collected at multiple incidence angles are used to characterize the seasonal variations in the backscatter of snow-covered landscapes in the northern Hudson Bay Lowlands during the winters of 1997/98 and 1998/99. The study evaluates the usefulness of C-band SAR syst...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
2012
|
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.361.9288 http://www.mdpi.com/2072-4292/4/7/2133/pdf/ |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.361.9288 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.361.9288 2023-05-15T16:35:29+02:00 C-Band SAR Imagery for Snow-Cover Monitoring at Treeline Frédérique C. Pivot The Pennsylvania State University CiteSeerX Archives 2012 http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.361.9288 http://www.mdpi.com/2072-4292/4/7/2133/pdf/ en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.361.9288 http://www.mdpi.com/2072-4292/4/7/2133/pdf/ Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.mdpi.com/2072-4292/4/7/2133/pdf/ remote sensing snow SAR C-band backscatter RADARSAT ERS ground penetrating radar treeline forest-tundra ecotoneRemote Sens. 2012 4 2134 text 2012 ftciteseerx 2016-01-08T00:52:33Z Abstract: RADARSAT and ERS-2 data collected at multiple incidence angles are used to characterize the seasonal variations in the backscatter of snow-covered landscapes in the northern Hudson Bay Lowlands during the winters of 1997/98 and 1998/99. The study evaluates the usefulness of C-band SAR systems for retrieving the snow water equivalent under dry snow conditions in the forest–tundra ecotone. The backscatter values are compared against ground measurements at six sampling sites, which are taken to be representative of the land-cover types found in the region. The contribution of dry snow to the radar return is evident when frost penetrates the first 20 cm of soil. Only then does the backscatter respond positively to changes in snow water equivalent, at least in the open and forested areas near the coast, where 1-dB increases in backscatter for each approximate 5–10 mm of accumulated water equivalent are observed at 20–31 � incidence angles. Further inland, the backscatter shows either no change or a negative change with snow accumulation, which suggests that the radar signal there is dominated by ground surface scattering (e.g., fen) when not attenuated by vegetation (e.g., forested and transition). With high-frequency ground-penetrating radar, we demonstrate the presence of a 10–20-cm layer Text Hudson Bay Tundra Unknown Hudson Bay Hudson |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
remote sensing snow SAR C-band backscatter RADARSAT ERS ground penetrating radar treeline forest-tundra ecotoneRemote Sens. 2012 4 2134 |
spellingShingle |
remote sensing snow SAR C-band backscatter RADARSAT ERS ground penetrating radar treeline forest-tundra ecotoneRemote Sens. 2012 4 2134 Frédérique C. Pivot C-Band SAR Imagery for Snow-Cover Monitoring at Treeline |
topic_facet |
remote sensing snow SAR C-band backscatter RADARSAT ERS ground penetrating radar treeline forest-tundra ecotoneRemote Sens. 2012 4 2134 |
description |
Abstract: RADARSAT and ERS-2 data collected at multiple incidence angles are used to characterize the seasonal variations in the backscatter of snow-covered landscapes in the northern Hudson Bay Lowlands during the winters of 1997/98 and 1998/99. The study evaluates the usefulness of C-band SAR systems for retrieving the snow water equivalent under dry snow conditions in the forest–tundra ecotone. The backscatter values are compared against ground measurements at six sampling sites, which are taken to be representative of the land-cover types found in the region. The contribution of dry snow to the radar return is evident when frost penetrates the first 20 cm of soil. Only then does the backscatter respond positively to changes in snow water equivalent, at least in the open and forested areas near the coast, where 1-dB increases in backscatter for each approximate 5–10 mm of accumulated water equivalent are observed at 20–31 � incidence angles. Further inland, the backscatter shows either no change or a negative change with snow accumulation, which suggests that the radar signal there is dominated by ground surface scattering (e.g., fen) when not attenuated by vegetation (e.g., forested and transition). With high-frequency ground-penetrating radar, we demonstrate the presence of a 10–20-cm layer |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Frédérique C. Pivot |
author_facet |
Frédérique C. Pivot |
author_sort |
Frédérique C. Pivot |
title |
C-Band SAR Imagery for Snow-Cover Monitoring at Treeline |
title_short |
C-Band SAR Imagery for Snow-Cover Monitoring at Treeline |
title_full |
C-Band SAR Imagery for Snow-Cover Monitoring at Treeline |
title_fullStr |
C-Band SAR Imagery for Snow-Cover Monitoring at Treeline |
title_full_unstemmed |
C-Band SAR Imagery for Snow-Cover Monitoring at Treeline |
title_sort |
c-band sar imagery for snow-cover monitoring at treeline |
publishDate |
2012 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.361.9288 http://www.mdpi.com/2072-4292/4/7/2133/pdf/ |
geographic |
Hudson Bay Hudson |
geographic_facet |
Hudson Bay Hudson |
genre |
Hudson Bay Tundra |
genre_facet |
Hudson Bay Tundra |
op_source |
http://www.mdpi.com/2072-4292/4/7/2133/pdf/ |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.361.9288 http://www.mdpi.com/2072-4292/4/7/2133/pdf/ |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766025708930334720 |