Interannual modulation of seasonal glacial velocity variations in the Eastern Karakoram detected by ALOS-1/2 data

Unlike in most other regions, Karakoram glaciers are either stable or advancing, a phenomenon known as the Karakoram anomaly. Despite studies of glacier surges and the derivation of surface velocity maps, the spatiotemporal variability of glacier dynamics still remains poorly understood, particularl...

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Published in:Journal of Glaciology
Main Authors: USMAN, MUHAMMAD, FURUYA, MASATO
Format: Article in Journal/Newspaper
Language:English
Subjects:
452
Online Access:http://hdl.handle.net/2115/71934
https://doi.org/10.1017/jog.2018.39
id fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/71934
record_format openpolar
spelling fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/71934 2023-05-15T16:57:25+02:00 Interannual modulation of seasonal glacial velocity variations in the Eastern Karakoram detected by ALOS-1/2 data USMAN, MUHAMMAD FURUYA, MASATO http://hdl.handle.net/2115/71934 https://doi.org/10.1017/jog.2018.39 eng eng http://hdl.handle.net/2115/71934 Journal of Glaciology, 64(245): 465-476 http://dx.doi.org/10.1017/jog.2018.39 https://creativecommons.org/licenses/by-nc-nd/4.0/ CC-BY-NC-ND glacier velocity interannual modulation L-band SAR pixel offset summer speed-up 452 article fthokunivhus https://doi.org/10.1017/jog.2018.39 2022-11-18T01:04:56Z Unlike in most other regions, Karakoram glaciers are either stable or advancing, a phenomenon known as the Karakoram anomaly. Despite studies of glacier surges and the derivation of surface velocity maps, the spatiotemporal variability of glacier dynamics still remains poorly understood, particularly in the Eastern Karakoram Range. We use Advanced Land Observing Satellite/the Phased Array type L-band Synthetic Aperture Radar (ALOS/PALSAR)-1/2 data from 2007 to 2011 and 2014 to 2015 to examine detailed surface velocity patterns of the Siachen, Baltoro, Kundos, Singkhu and Gasherbrum Glaciers. The first three glaciers show considerable velocity variability (20–350 m a−1), with clear seasonal patterns. Although all glaciers, except for Baltoro, flow slowest in 2015, the velocity structures are individual and vary in space and time. In Gasherbrum Glacier, peak surge-phase velocities are seasonally modulated, with maxima in summers 2006 and 2007, suggesting surface melt plays an important role in maintaining the active phase. Given the relatively close proximity of these glaciers, we assume that surface melt timing and rates are comparable. We therefore argue that the observed spatiotemporal and interannual velocity patterns are determined by local and internal mechanisms, including englacial and subglacial hydrology, thermal processes and tributary configuration of each individual glacier. Article in Journal/Newspaper Journal of Glaciology Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Glacier Peak ENVELOPE(-128.637,-128.637,54.700,54.700) Journal of Glaciology 64 245 465 476
institution Open Polar
collection Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP)
op_collection_id fthokunivhus
language English
topic glacier velocity
interannual modulation
L-band SAR
pixel offset
summer speed-up
452
spellingShingle glacier velocity
interannual modulation
L-band SAR
pixel offset
summer speed-up
452
USMAN, MUHAMMAD
FURUYA, MASATO
Interannual modulation of seasonal glacial velocity variations in the Eastern Karakoram detected by ALOS-1/2 data
topic_facet glacier velocity
interannual modulation
L-band SAR
pixel offset
summer speed-up
452
description Unlike in most other regions, Karakoram glaciers are either stable or advancing, a phenomenon known as the Karakoram anomaly. Despite studies of glacier surges and the derivation of surface velocity maps, the spatiotemporal variability of glacier dynamics still remains poorly understood, particularly in the Eastern Karakoram Range. We use Advanced Land Observing Satellite/the Phased Array type L-band Synthetic Aperture Radar (ALOS/PALSAR)-1/2 data from 2007 to 2011 and 2014 to 2015 to examine detailed surface velocity patterns of the Siachen, Baltoro, Kundos, Singkhu and Gasherbrum Glaciers. The first three glaciers show considerable velocity variability (20–350 m a−1), with clear seasonal patterns. Although all glaciers, except for Baltoro, flow slowest in 2015, the velocity structures are individual and vary in space and time. In Gasherbrum Glacier, peak surge-phase velocities are seasonally modulated, with maxima in summers 2006 and 2007, suggesting surface melt plays an important role in maintaining the active phase. Given the relatively close proximity of these glaciers, we assume that surface melt timing and rates are comparable. We therefore argue that the observed spatiotemporal and interannual velocity patterns are determined by local and internal mechanisms, including englacial and subglacial hydrology, thermal processes and tributary configuration of each individual glacier.
format Article in Journal/Newspaper
author USMAN, MUHAMMAD
FURUYA, MASATO
author_facet USMAN, MUHAMMAD
FURUYA, MASATO
author_sort USMAN, MUHAMMAD
title Interannual modulation of seasonal glacial velocity variations in the Eastern Karakoram detected by ALOS-1/2 data
title_short Interannual modulation of seasonal glacial velocity variations in the Eastern Karakoram detected by ALOS-1/2 data
title_full Interannual modulation of seasonal glacial velocity variations in the Eastern Karakoram detected by ALOS-1/2 data
title_fullStr Interannual modulation of seasonal glacial velocity variations in the Eastern Karakoram detected by ALOS-1/2 data
title_full_unstemmed Interannual modulation of seasonal glacial velocity variations in the Eastern Karakoram detected by ALOS-1/2 data
title_sort interannual modulation of seasonal glacial velocity variations in the eastern karakoram detected by alos-1/2 data
url http://hdl.handle.net/2115/71934
https://doi.org/10.1017/jog.2018.39
long_lat ENVELOPE(-128.637,-128.637,54.700,54.700)
geographic Glacier Peak
geographic_facet Glacier Peak
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_relation http://hdl.handle.net/2115/71934
Journal of Glaciology, 64(245): 465-476
http://dx.doi.org/10.1017/jog.2018.39
op_rights https://creativecommons.org/licenses/by-nc-nd/4.0/
op_rightsnorm CC-BY-NC-ND
op_doi https://doi.org/10.1017/jog.2018.39
container_title Journal of Glaciology
container_volume 64
container_issue 245
container_start_page 465
op_container_end_page 476
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