A ten-year record of supraglacial lake evolution and rapid drainage in West Greenland using an automated processing algorithm for multispectral imagery
The rapid drainage of supraglacial lakes introduces large pulses of meltwater to the subglacial environment and creates moulins, surface-to-bed conduits for future melt. Introduction of water to the subglacial system has been shown to affect ice flow, and modeling suggests that variability in water...
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fttriple:oai:gotriple.eu:oai:doaj.org/article:76823ef745da4b7db1be3290c0d24cac 2023-05-15T16:21:28+02:00 A ten-year record of supraglacial lake evolution and rapid drainage in West Greenland using an automated processing algorithm for multispectral imagery B. F. Morriss R. L. Hawley J. W. Chipman L. C. Andrews G. A. Catania M. J. Hoffman M. P. Lüthi T. A. Neumann 2013-12-01 https://doi.org/10.5194/tc-7-1869-2013 http://www.the-cryosphere.net/7/1869/2013/tc-7-1869-2013.pdf https://doaj.org/article/76823ef745da4b7db1be3290c0d24cac en eng Copernicus Publications 1994-0416 1994-0424 doi:10.5194/tc-7-1869-2013 http://www.the-cryosphere.net/7/1869/2013/tc-7-1869-2013.pdf https://doaj.org/article/76823ef745da4b7db1be3290c0d24cac undefined The Cryosphere, Vol 7, Iss 6, Pp 1869-1877 (2013) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2013 fttriple https://doi.org/10.5194/tc-7-1869-2013 2023-01-22T17:50:33Z The rapid drainage of supraglacial lakes introduces large pulses of meltwater to the subglacial environment and creates moulins, surface-to-bed conduits for future melt. Introduction of water to the subglacial system has been shown to affect ice flow, and modeling suggests that variability in water supply and delivery to the subsurface play an important role in the development of the subglacial hydrologic system and its ability to enhance or mitigate ice flow. We developed a fully automated method for tracking meltwater and rapid drainages in large (> 0.125 km2) perennial lakes and applied it to a 10 yr time series of ETM+ and MODIS imagery of an outlet glacier flow band in West Greenland. Results indicate interannual variability in maximum coverage and spatial evolution of total lake area. We identify 238 rapid drainage events, occurring most often at low (< 900 m) and middle (900–1200 m) elevations during periods of net filling or peak lake coverage. We observe a general progression of both lake filling and draining from lower to higher elevations but note that the timing of filling onset, peak coverage, and dissipation are also variable. Lake coverage is sensitive to air temperature, and warm years exhibit greater variability in both coverage evolution and rapid drainage. Mid-elevation drainages in 2011 coincide with large surface velocity increases at nearby GPS sites, though the relationships between ice-shed-scale dynamics and meltwater input are still unclear. Article in Journal/Newspaper glacier Greenland The Cryosphere Unknown Greenland Peak Lake ENVELOPE(-106.984,-106.984,56.250,56.250) The Cryosphere 7 6 1869 1877 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
geo envir |
spellingShingle |
geo envir B. F. Morriss R. L. Hawley J. W. Chipman L. C. Andrews G. A. Catania M. J. Hoffman M. P. Lüthi T. A. Neumann A ten-year record of supraglacial lake evolution and rapid drainage in West Greenland using an automated processing algorithm for multispectral imagery |
topic_facet |
geo envir |
description |
The rapid drainage of supraglacial lakes introduces large pulses of meltwater to the subglacial environment and creates moulins, surface-to-bed conduits for future melt. Introduction of water to the subglacial system has been shown to affect ice flow, and modeling suggests that variability in water supply and delivery to the subsurface play an important role in the development of the subglacial hydrologic system and its ability to enhance or mitigate ice flow. We developed a fully automated method for tracking meltwater and rapid drainages in large (> 0.125 km2) perennial lakes and applied it to a 10 yr time series of ETM+ and MODIS imagery of an outlet glacier flow band in West Greenland. Results indicate interannual variability in maximum coverage and spatial evolution of total lake area. We identify 238 rapid drainage events, occurring most often at low (< 900 m) and middle (900–1200 m) elevations during periods of net filling or peak lake coverage. We observe a general progression of both lake filling and draining from lower to higher elevations but note that the timing of filling onset, peak coverage, and dissipation are also variable. Lake coverage is sensitive to air temperature, and warm years exhibit greater variability in both coverage evolution and rapid drainage. Mid-elevation drainages in 2011 coincide with large surface velocity increases at nearby GPS sites, though the relationships between ice-shed-scale dynamics and meltwater input are still unclear. |
format |
Article in Journal/Newspaper |
author |
B. F. Morriss R. L. Hawley J. W. Chipman L. C. Andrews G. A. Catania M. J. Hoffman M. P. Lüthi T. A. Neumann |
author_facet |
B. F. Morriss R. L. Hawley J. W. Chipman L. C. Andrews G. A. Catania M. J. Hoffman M. P. Lüthi T. A. Neumann |
author_sort |
B. F. Morriss |
title |
A ten-year record of supraglacial lake evolution and rapid drainage in West Greenland using an automated processing algorithm for multispectral imagery |
title_short |
A ten-year record of supraglacial lake evolution and rapid drainage in West Greenland using an automated processing algorithm for multispectral imagery |
title_full |
A ten-year record of supraglacial lake evolution and rapid drainage in West Greenland using an automated processing algorithm for multispectral imagery |
title_fullStr |
A ten-year record of supraglacial lake evolution and rapid drainage in West Greenland using an automated processing algorithm for multispectral imagery |
title_full_unstemmed |
A ten-year record of supraglacial lake evolution and rapid drainage in West Greenland using an automated processing algorithm for multispectral imagery |
title_sort |
ten-year record of supraglacial lake evolution and rapid drainage in west greenland using an automated processing algorithm for multispectral imagery |
publisher |
Copernicus Publications |
publishDate |
2013 |
url |
https://doi.org/10.5194/tc-7-1869-2013 http://www.the-cryosphere.net/7/1869/2013/tc-7-1869-2013.pdf https://doaj.org/article/76823ef745da4b7db1be3290c0d24cac |
long_lat |
ENVELOPE(-106.984,-106.984,56.250,56.250) |
geographic |
Greenland Peak Lake |
geographic_facet |
Greenland Peak Lake |
genre |
glacier Greenland The Cryosphere |
genre_facet |
glacier Greenland The Cryosphere |
op_source |
The Cryosphere, Vol 7, Iss 6, Pp 1869-1877 (2013) |
op_relation |
1994-0416 1994-0424 doi:10.5194/tc-7-1869-2013 http://www.the-cryosphere.net/7/1869/2013/tc-7-1869-2013.pdf https://doaj.org/article/76823ef745da4b7db1be3290c0d24cac |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-7-1869-2013 |
container_title |
The Cryosphere |
container_volume |
7 |
container_issue |
6 |
container_start_page |
1869 |
op_container_end_page |
1877 |
_version_ |
1766009467568128000 |