Greenland liquid water discharge from 1958 through 2019
Greenland runoff, from ice mass loss and increasing rainfall, is increasing. That runoff, as discharge, impacts the physical, chemical, and biological properties of the adjacent fjords. However, where and when the discharge occurs is not readily available in an open database. Here we provide data se...
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Copernicus Publications
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Online Access: | https://doi.org/10.5194/essd-12-2811-2020 https://doaj.org/article/5f85b67af08d45a29832a106407d2224 |
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ftdoajarticles:oai:doaj.org/article:5f85b67af08d45a29832a106407d2224 2023-05-15T16:27:04+02:00 Greenland liquid water discharge from 1958 through 2019 K. D. Mankoff B. Noël X. Fettweis A. P. Ahlstrøm W. Colgan K. Kondo K. Langley S. Sugiyama D. van As R. S. Fausto 2020-11-01T00:00:00Z https://doi.org/10.5194/essd-12-2811-2020 https://doaj.org/article/5f85b67af08d45a29832a106407d2224 EN eng Copernicus Publications https://essd.copernicus.org/articles/12/2811/2020/essd-12-2811-2020.pdf https://doaj.org/toc/1866-3508 https://doaj.org/toc/1866-3516 doi:10.5194/essd-12-2811-2020 1866-3508 1866-3516 https://doaj.org/article/5f85b67af08d45a29832a106407d2224 Earth System Science Data, Vol 12, Pp 2811-2841 (2020) Environmental sciences GE1-350 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.5194/essd-12-2811-2020 2022-12-31T12:37:21Z Greenland runoff, from ice mass loss and increasing rainfall, is increasing. That runoff, as discharge, impacts the physical, chemical, and biological properties of the adjacent fjords. However, where and when the discharge occurs is not readily available in an open database. Here we provide data sets of high-resolution Greenland hydrologic outlets, basins, and streams, as well as a daily 1958 through 2019 time series of Greenland liquid water discharge for each outlet. The data include 24 507 ice marginal outlets and upstream basins and 29 635 land coast outlets and upstream basins, derived from the 100 m ArcticDEM and 150 m BedMachine. At each outlet there are daily discharge data for 22 645 d – ice sheet runoff routed subglacially to ice margin outlets and land runoff routed to coast outlets – from two regional climate models (RCMs; MAR and RACMO). Our sensitivity study of how outlet location changes for every inland cell based on subglacial routing assumptions shows that most inland cells where runoff occurs are not highly sensitive to those routing assumptions, and outflow location does not move far. We compare RCM results with 10 gauges from streams with discharge rates spanning 4 orders of magnitude. Results show that for daily discharge at the individual basin scale the 5 % to 95 % prediction interval between modeled discharge and observations generally falls within plus or minus a factor of 5 (half an order of magnitude, or +500 % <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>/</mo><mo>-</mo><mn mathvariant="normal">80</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="6ffec3eb5fe5b4a83b6d76b6e5dff91a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-12-2811-2020-ie00001.svg" width="32pt" height="14pt" ... Article in Journal/Newspaper Greenland Ice Sheet Directory of Open Access Journals: DOAJ Articles Greenland Earth System Science Data 12 4 2811 2841 |
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Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental sciences GE1-350 Geology QE1-996.5 K. D. Mankoff B. Noël X. Fettweis A. P. Ahlstrøm W. Colgan K. Kondo K. Langley S. Sugiyama D. van As R. S. Fausto Greenland liquid water discharge from 1958 through 2019 |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
Greenland runoff, from ice mass loss and increasing rainfall, is increasing. That runoff, as discharge, impacts the physical, chemical, and biological properties of the adjacent fjords. However, where and when the discharge occurs is not readily available in an open database. Here we provide data sets of high-resolution Greenland hydrologic outlets, basins, and streams, as well as a daily 1958 through 2019 time series of Greenland liquid water discharge for each outlet. The data include 24 507 ice marginal outlets and upstream basins and 29 635 land coast outlets and upstream basins, derived from the 100 m ArcticDEM and 150 m BedMachine. At each outlet there are daily discharge data for 22 645 d – ice sheet runoff routed subglacially to ice margin outlets and land runoff routed to coast outlets – from two regional climate models (RCMs; MAR and RACMO). Our sensitivity study of how outlet location changes for every inland cell based on subglacial routing assumptions shows that most inland cells where runoff occurs are not highly sensitive to those routing assumptions, and outflow location does not move far. We compare RCM results with 10 gauges from streams with discharge rates spanning 4 orders of magnitude. Results show that for daily discharge at the individual basin scale the 5 % to 95 % prediction interval between modeled discharge and observations generally falls within plus or minus a factor of 5 (half an order of magnitude, or +500 % <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>/</mo><mo>-</mo><mn mathvariant="normal">80</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="32pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="6ffec3eb5fe5b4a83b6d76b6e5dff91a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-12-2811-2020-ie00001.svg" width="32pt" height="14pt" ... |
format |
Article in Journal/Newspaper |
author |
K. D. Mankoff B. Noël X. Fettweis A. P. Ahlstrøm W. Colgan K. Kondo K. Langley S. Sugiyama D. van As R. S. Fausto |
author_facet |
K. D. Mankoff B. Noël X. Fettweis A. P. Ahlstrøm W. Colgan K. Kondo K. Langley S. Sugiyama D. van As R. S. Fausto |
author_sort |
K. D. Mankoff |
title |
Greenland liquid water discharge from 1958 through 2019 |
title_short |
Greenland liquid water discharge from 1958 through 2019 |
title_full |
Greenland liquid water discharge from 1958 through 2019 |
title_fullStr |
Greenland liquid water discharge from 1958 through 2019 |
title_full_unstemmed |
Greenland liquid water discharge from 1958 through 2019 |
title_sort |
greenland liquid water discharge from 1958 through 2019 |
publisher |
Copernicus Publications |
publishDate |
2020 |
url |
https://doi.org/10.5194/essd-12-2811-2020 https://doaj.org/article/5f85b67af08d45a29832a106407d2224 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_source |
Earth System Science Data, Vol 12, Pp 2811-2841 (2020) |
op_relation |
https://essd.copernicus.org/articles/12/2811/2020/essd-12-2811-2020.pdf https://doaj.org/toc/1866-3508 https://doaj.org/toc/1866-3516 doi:10.5194/essd-12-2811-2020 1866-3508 1866-3516 https://doaj.org/article/5f85b67af08d45a29832a106407d2224 |
op_doi |
https://doi.org/10.5194/essd-12-2811-2020 |
container_title |
Earth System Science Data |
container_volume |
12 |
container_issue |
4 |
container_start_page |
2811 |
op_container_end_page |
2841 |
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1766016125641949184 |