Diverse supraglacial drainage patterns on the Devon ice Cap, Arctic Canada
The Devon Ice Cap (DIC) is one of the largest ice masses in the Canadian Arctic. Each summer, extensive supraglacial river networks develop on the DIC surface and route large volumes of meltwater from ice caps to the ocean. Mapping their extent and understanding their temporal evolution are importan...
Published in: | Journal of Maps |
---|---|
Main Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Taylor & Francis Group
2020
|
Subjects: | |
Online Access: | https://doi.org/10.1080/17445647.2020.1838353 https://doaj.org/article/24695c1dc7d84df88b3130147b811be2 |
id |
ftdoajarticles:oai:doaj.org/article:24695c1dc7d84df88b3130147b811be2 |
---|---|
record_format |
openpolar |
spelling |
ftdoajarticles:oai:doaj.org/article:24695c1dc7d84df88b3130147b811be2 2023-05-15T14:49:33+02:00 Diverse supraglacial drainage patterns on the Devon ice Cap, Arctic Canada Yao Lu Kang Yang Xin Lu Laurence C. Smith Andrew J. Sole Stephen J. Livingstone Xavier Fettweis Manchun Li 2020-12-01T00:00:00Z https://doi.org/10.1080/17445647.2020.1838353 https://doaj.org/article/24695c1dc7d84df88b3130147b811be2 EN eng Taylor & Francis Group http://dx.doi.org/10.1080/17445647.2020.1838353 https://doaj.org/toc/1744-5647 1744-5647 doi:10.1080/17445647.2020.1838353 https://doaj.org/article/24695c1dc7d84df88b3130147b811be2 Journal of Maps, Vol 16, Iss 2, Pp 834-846 (2020) supraglacial rivers regional climate model (rcm) sentinel-2 devon ice cap arctic Maps G3180-9980 article 2020 ftdoajarticles https://doi.org/10.1080/17445647.2020.1838353 2022-12-31T06:55:12Z The Devon Ice Cap (DIC) is one of the largest ice masses in the Canadian Arctic. Each summer, extensive supraglacial river networks develop on the DIC surface and route large volumes of meltwater from ice caps to the ocean. Mapping their extent and understanding their temporal evolution are important for validating runoff routing and melt volumes predicted by regional climate models (RCMs). We use 10 m Sentinel-2 images captured on 28 July and 10/11 August 2016 to map supraglacial rivers across the entire DIC (12,100 km2). Both dendritic and parallel supraglacial drainage patterns are found, with a total length of 44,941 km and a mean drainage density (Dd) of 3.71 km−1. As the melt season progresses, Dd increases and supraglacial rivers form at progressively higher elevations. There is a positive correlation between RCM-derived surface runoff and satellite-mapped Dd, suggesting that supraglacial drainage density is primarily controlled by surface runoff. Article in Journal/Newspaper Arctic Ice cap Directory of Open Access Journals: DOAJ Articles Arctic Canada Devon Ice Cap ENVELOPE(-82.499,-82.499,75.335,75.335) Journal of Maps 16 2 834 846 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
supraglacial rivers regional climate model (rcm) sentinel-2 devon ice cap arctic Maps G3180-9980 |
spellingShingle |
supraglacial rivers regional climate model (rcm) sentinel-2 devon ice cap arctic Maps G3180-9980 Yao Lu Kang Yang Xin Lu Laurence C. Smith Andrew J. Sole Stephen J. Livingstone Xavier Fettweis Manchun Li Diverse supraglacial drainage patterns on the Devon ice Cap, Arctic Canada |
topic_facet |
supraglacial rivers regional climate model (rcm) sentinel-2 devon ice cap arctic Maps G3180-9980 |
description |
The Devon Ice Cap (DIC) is one of the largest ice masses in the Canadian Arctic. Each summer, extensive supraglacial river networks develop on the DIC surface and route large volumes of meltwater from ice caps to the ocean. Mapping their extent and understanding their temporal evolution are important for validating runoff routing and melt volumes predicted by regional climate models (RCMs). We use 10 m Sentinel-2 images captured on 28 July and 10/11 August 2016 to map supraglacial rivers across the entire DIC (12,100 km2). Both dendritic and parallel supraglacial drainage patterns are found, with a total length of 44,941 km and a mean drainage density (Dd) of 3.71 km−1. As the melt season progresses, Dd increases and supraglacial rivers form at progressively higher elevations. There is a positive correlation between RCM-derived surface runoff and satellite-mapped Dd, suggesting that supraglacial drainage density is primarily controlled by surface runoff. |
format |
Article in Journal/Newspaper |
author |
Yao Lu Kang Yang Xin Lu Laurence C. Smith Andrew J. Sole Stephen J. Livingstone Xavier Fettweis Manchun Li |
author_facet |
Yao Lu Kang Yang Xin Lu Laurence C. Smith Andrew J. Sole Stephen J. Livingstone Xavier Fettweis Manchun Li |
author_sort |
Yao Lu |
title |
Diverse supraglacial drainage patterns on the Devon ice Cap, Arctic Canada |
title_short |
Diverse supraglacial drainage patterns on the Devon ice Cap, Arctic Canada |
title_full |
Diverse supraglacial drainage patterns on the Devon ice Cap, Arctic Canada |
title_fullStr |
Diverse supraglacial drainage patterns on the Devon ice Cap, Arctic Canada |
title_full_unstemmed |
Diverse supraglacial drainage patterns on the Devon ice Cap, Arctic Canada |
title_sort |
diverse supraglacial drainage patterns on the devon ice cap, arctic canada |
publisher |
Taylor & Francis Group |
publishDate |
2020 |
url |
https://doi.org/10.1080/17445647.2020.1838353 https://doaj.org/article/24695c1dc7d84df88b3130147b811be2 |
long_lat |
ENVELOPE(-82.499,-82.499,75.335,75.335) |
geographic |
Arctic Canada Devon Ice Cap |
geographic_facet |
Arctic Canada Devon Ice Cap |
genre |
Arctic Ice cap |
genre_facet |
Arctic Ice cap |
op_source |
Journal of Maps, Vol 16, Iss 2, Pp 834-846 (2020) |
op_relation |
http://dx.doi.org/10.1080/17445647.2020.1838353 https://doaj.org/toc/1744-5647 1744-5647 doi:10.1080/17445647.2020.1838353 https://doaj.org/article/24695c1dc7d84df88b3130147b811be2 |
op_doi |
https://doi.org/10.1080/17445647.2020.1838353 |
container_title |
Journal of Maps |
container_volume |
16 |
container_issue |
2 |
container_start_page |
834 |
op_container_end_page |
846 |
_version_ |
1766320601843105792 |