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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Published in:Earth System Science Data
Main Authors: K. D. Mankoff, B. Noël, X. Fettweis, A. P. Ahlstrøm, W. Colgan, K. Kondo, K. Langley, S. Sugiyama, D. van As, R. S. Fausto
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/essd-12-2811-2020
https://doaj.org/article/5f85b67af08d45a29832a106407d2224
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spelling 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
institution 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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