Supraglacial stream discharge measurements from six catchments within the Pâqitsoq region of Sermeq Avannarleq, western Greenland Ice Sheet 2017 -2018 ...

Meltwater produced on the Greenland Ice Sheet (GrIS) surface is routed through complex networks of supraglacial streams across the ice surface. Most of the supraglacial streams on the GrIS terminate into moulins. Moulins are vertical conduits that penetrate through the entire ice thickness and deliv...

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Main Authors: Trunz, Celia, Mejia, Jessica, Covington, Matthew, Siegel, Victoria, Conlon, Brandon, Gulley, Jason
Format: Dataset
Language:English
Published: NSF Arctic Data Center 2021
Subjects:
Online Access:https://dx.doi.org/10.18739/a2d21rk53
https://arcticdata.io/catalog/view/doi:10.18739/A2D21RK53
id ftdatacite:10.18739/a2d21rk53
record_format openpolar
spelling ftdatacite:10.18739/a2d21rk53 2023-10-01T03:56:19+02:00 Supraglacial stream discharge measurements from six catchments within the Pâqitsoq region of Sermeq Avannarleq, western Greenland Ice Sheet 2017 -2018 ... Trunz, Celia Mejia, Jessica Covington, Matthew Siegel, Victoria Conlon, Brandon Gulley, Jason 2021 text/xml https://dx.doi.org/10.18739/a2d21rk53 https://arcticdata.io/catalog/view/doi:10.18739/A2D21RK53 en eng NSF Arctic Data Center Discharge Supraglacial stream unit hydrograph hydrology glacial hydrology supraglacial catchment Dataset dataset 2021 ftdatacite https://doi.org/10.18739/a2d21rk53 2023-09-04T15:18:52Z Meltwater produced on the Greenland Ice Sheet (GrIS) surface is routed through complex networks of supraglacial streams across the ice surface. Most of the supraglacial streams on the GrIS terminate into moulins. Moulins are vertical conduits that penetrate through the entire ice thickness and deliver meltwater to the ice sheet's bed where water pressure fluctuations can modulate sliding speed. A poorly constrained parameter in glacial hydrological models is the timing and the volume of meltwater entering moulins within the GrIS ablation area. Here, we present direct measurements of supraglacial stream discharge within six catchments within the GrIS ablation area during the 2017 and 2018 melt seasons. In 2017 we measured stream discharge using a fluorescent dye dilution method. We continuously injected a Rhodamine WT solution (known concentration and pumping rate) into supraglacial streams and measured the dye concentration with a Cyclops fluorometer installed 50-100 meters downstream of the dye injection ... Dataset Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Avannarleq ENVELOPE(-49.100,-49.100,62.133,62.133) Greenland Sermeq Avannarleq ENVELOPE(-50.833,-50.833,71.033,71.033)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Discharge
Supraglacial stream
unit hydrograph
hydrology
glacial hydrology
supraglacial
catchment
spellingShingle Discharge
Supraglacial stream
unit hydrograph
hydrology
glacial hydrology
supraglacial
catchment
Trunz, Celia
Mejia, Jessica
Covington, Matthew
Siegel, Victoria
Conlon, Brandon
Gulley, Jason
Supraglacial stream discharge measurements from six catchments within the Pâqitsoq region of Sermeq Avannarleq, western Greenland Ice Sheet 2017 -2018 ...
topic_facet Discharge
Supraglacial stream
unit hydrograph
hydrology
glacial hydrology
supraglacial
catchment
description Meltwater produced on the Greenland Ice Sheet (GrIS) surface is routed through complex networks of supraglacial streams across the ice surface. Most of the supraglacial streams on the GrIS terminate into moulins. Moulins are vertical conduits that penetrate through the entire ice thickness and deliver meltwater to the ice sheet's bed where water pressure fluctuations can modulate sliding speed. A poorly constrained parameter in glacial hydrological models is the timing and the volume of meltwater entering moulins within the GrIS ablation area. Here, we present direct measurements of supraglacial stream discharge within six catchments within the GrIS ablation area during the 2017 and 2018 melt seasons. In 2017 we measured stream discharge using a fluorescent dye dilution method. We continuously injected a Rhodamine WT solution (known concentration and pumping rate) into supraglacial streams and measured the dye concentration with a Cyclops fluorometer installed 50-100 meters downstream of the dye injection ...
format Dataset
author Trunz, Celia
Mejia, Jessica
Covington, Matthew
Siegel, Victoria
Conlon, Brandon
Gulley, Jason
author_facet Trunz, Celia
Mejia, Jessica
Covington, Matthew
Siegel, Victoria
Conlon, Brandon
Gulley, Jason
author_sort Trunz, Celia
title Supraglacial stream discharge measurements from six catchments within the Pâqitsoq region of Sermeq Avannarleq, western Greenland Ice Sheet 2017 -2018 ...
title_short Supraglacial stream discharge measurements from six catchments within the Pâqitsoq region of Sermeq Avannarleq, western Greenland Ice Sheet 2017 -2018 ...
title_full Supraglacial stream discharge measurements from six catchments within the Pâqitsoq region of Sermeq Avannarleq, western Greenland Ice Sheet 2017 -2018 ...
title_fullStr Supraglacial stream discharge measurements from six catchments within the Pâqitsoq region of Sermeq Avannarleq, western Greenland Ice Sheet 2017 -2018 ...
title_full_unstemmed Supraglacial stream discharge measurements from six catchments within the Pâqitsoq region of Sermeq Avannarleq, western Greenland Ice Sheet 2017 -2018 ...
title_sort supraglacial stream discharge measurements from six catchments within the pâqitsoq region of sermeq avannarleq, western greenland ice sheet 2017 -2018 ...
publisher NSF Arctic Data Center
publishDate 2021
url https://dx.doi.org/10.18739/a2d21rk53
https://arcticdata.io/catalog/view/doi:10.18739/A2D21RK53
long_lat ENVELOPE(-49.100,-49.100,62.133,62.133)
ENVELOPE(-50.833,-50.833,71.033,71.033)
geographic Avannarleq
Greenland
Sermeq Avannarleq
geographic_facet Avannarleq
Greenland
Sermeq Avannarleq
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_doi https://doi.org/10.18739/a2d21rk53
_version_ 1778525728906674176