Spatially varying WIndow based maximum likelihood feature tracking (SWIFT) method for glacier surface velocity estimations
Glacier surface velocity is an important variable for glacier dynamics studies. Estimation of accurate surface velocity from remote sensing is a challenge, especially for glaciers with no in-situ observations. To overcome this challenge, a new method for glacier feature tracking named as Spatially v...
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ftdoajarticles:oai:doaj.org/article:e7ac05e05f6f4c7ea5fe74dfbf3364b5 2023-10-09T21:51:48+02:00 Spatially varying WIndow based maximum likelihood feature tracking (SWIFT) method for glacier surface velocity estimations Sangita S. Tomar Raaj Ramsankaran Jeffrey P. Walker 2022-12-01T00:00:00Z https://doi.org/10.1080/10106049.2022.2082556 https://doaj.org/article/e7ac05e05f6f4c7ea5fe74dfbf3364b5 EN eng Taylor & Francis Group http://dx.doi.org/10.1080/10106049.2022.2082556 https://doaj.org/toc/1010-6049 https://doaj.org/toc/1752-0762 1010-6049 1752-0762 doi:10.1080/10106049.2022.2082556 https://doaj.org/article/e7ac05e05f6f4c7ea5fe74dfbf3364b5 Geocarto International, Vol 37, Iss 26, Pp 13769-13796 (2022) glacier surface velocity feature tracking approach sar optical automated window size Physical geography GB3-5030 article 2022 ftdoajarticles https://doi.org/10.1080/10106049.2022.2082556 2023-09-24T00:39:24Z Glacier surface velocity is an important variable for glacier dynamics studies. Estimation of accurate surface velocity from remote sensing is a challenge, especially for glaciers with no in-situ observations. To overcome this challenge, a new method for glacier feature tracking named as Spatially varying WIndow based maximum likelihood Feature Tracking (SWIFT) has been proposed. This method utilizes both optical data (to automatically determine the window size [WS] using the concept of Object Based Image Analysis [OBIA]) and Synthetic Aperture Radar (SAR) data (to perform feature tracking). The proposed method uses a spatially varying WS unlike other existing softwares that cannot provide the flexibility of a spatially varying WS. The proposed method has been tested and validated at three different glaciers (South Glacier [SG], Canada; Chhota Shigri Glacier [CSG], India; and Tasman Glacier [TG], New Zealand) for which field measured data were available. The obtained results for all three glaciers showed consistent improvement in estimated velocity by SWIFT when compared with spatially fixed WS-based estimates from normalized cross correlation-based Correlation Image Analysis Software (CIAS). Considering the data availability, the proposed SWIFT method has been implemented using a variety of SAR and optical satellite data to understand its performance/effectiveness for glacier surface velocity estimation. When validated against field measurements, the results from SWIFT gave an RMSE of 12.8 m/years, 15.32 m/years and 67.1 m/years for SG, CSG and TG, respectively. Moreover, the RMSE of SWIFT estimates were observed to have an RMSE that was 19–36% lower than the best performing spatially fixed WS. Article in Journal/Newspaper glacier* Directory of Open Access Journals: DOAJ Articles Canada New Zealand Geocarto International 37 26 13769 13796 |
institution |
Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
glacier surface velocity feature tracking approach sar optical automated window size Physical geography GB3-5030 |
spellingShingle |
glacier surface velocity feature tracking approach sar optical automated window size Physical geography GB3-5030 Sangita S. Tomar Raaj Ramsankaran Jeffrey P. Walker Spatially varying WIndow based maximum likelihood feature tracking (SWIFT) method for glacier surface velocity estimations |
topic_facet |
glacier surface velocity feature tracking approach sar optical automated window size Physical geography GB3-5030 |
description |
Glacier surface velocity is an important variable for glacier dynamics studies. Estimation of accurate surface velocity from remote sensing is a challenge, especially for glaciers with no in-situ observations. To overcome this challenge, a new method for glacier feature tracking named as Spatially varying WIndow based maximum likelihood Feature Tracking (SWIFT) has been proposed. This method utilizes both optical data (to automatically determine the window size [WS] using the concept of Object Based Image Analysis [OBIA]) and Synthetic Aperture Radar (SAR) data (to perform feature tracking). The proposed method uses a spatially varying WS unlike other existing softwares that cannot provide the flexibility of a spatially varying WS. The proposed method has been tested and validated at three different glaciers (South Glacier [SG], Canada; Chhota Shigri Glacier [CSG], India; and Tasman Glacier [TG], New Zealand) for which field measured data were available. The obtained results for all three glaciers showed consistent improvement in estimated velocity by SWIFT when compared with spatially fixed WS-based estimates from normalized cross correlation-based Correlation Image Analysis Software (CIAS). Considering the data availability, the proposed SWIFT method has been implemented using a variety of SAR and optical satellite data to understand its performance/effectiveness for glacier surface velocity estimation. When validated against field measurements, the results from SWIFT gave an RMSE of 12.8 m/years, 15.32 m/years and 67.1 m/years for SG, CSG and TG, respectively. Moreover, the RMSE of SWIFT estimates were observed to have an RMSE that was 19–36% lower than the best performing spatially fixed WS. |
format |
Article in Journal/Newspaper |
author |
Sangita S. Tomar Raaj Ramsankaran Jeffrey P. Walker |
author_facet |
Sangita S. Tomar Raaj Ramsankaran Jeffrey P. Walker |
author_sort |
Sangita S. Tomar |
title |
Spatially varying WIndow based maximum likelihood feature tracking (SWIFT) method for glacier surface velocity estimations |
title_short |
Spatially varying WIndow based maximum likelihood feature tracking (SWIFT) method for glacier surface velocity estimations |
title_full |
Spatially varying WIndow based maximum likelihood feature tracking (SWIFT) method for glacier surface velocity estimations |
title_fullStr |
Spatially varying WIndow based maximum likelihood feature tracking (SWIFT) method for glacier surface velocity estimations |
title_full_unstemmed |
Spatially varying WIndow based maximum likelihood feature tracking (SWIFT) method for glacier surface velocity estimations |
title_sort |
spatially varying window based maximum likelihood feature tracking (swift) method for glacier surface velocity estimations |
publisher |
Taylor & Francis Group |
publishDate |
2022 |
url |
https://doi.org/10.1080/10106049.2022.2082556 https://doaj.org/article/e7ac05e05f6f4c7ea5fe74dfbf3364b5 |
geographic |
Canada New Zealand |
geographic_facet |
Canada New Zealand |
genre |
glacier* |
genre_facet |
glacier* |
op_source |
Geocarto International, Vol 37, Iss 26, Pp 13769-13796 (2022) |
op_relation |
http://dx.doi.org/10.1080/10106049.2022.2082556 https://doaj.org/toc/1010-6049 https://doaj.org/toc/1752-0762 1010-6049 1752-0762 doi:10.1080/10106049.2022.2082556 https://doaj.org/article/e7ac05e05f6f4c7ea5fe74dfbf3364b5 |
op_doi |
https://doi.org/10.1080/10106049.2022.2082556 |
container_title |
Geocarto International |
container_volume |
37 |
container_issue |
26 |
container_start_page |
13769 |
op_container_end_page |
13796 |
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1779314917275336704 |