Hydrogeochemistry of Greenlandic proglacial and nonglacial streams

This project assesses how weathering varies across deglacial and proglacial watersheds in western and southern Greenland to evaluate the impact of ice sheet retreat on isotopic and nutrient fluxes to the ocean and atmospheric CO2 exchange. Deglacial watersheds are separated from the ice sheet by hyd...

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Bibliographic Details
Main Authors: Andrea Pain, Martin Jonathan, Ellen Martin, Shaily Rahman
Format: Dataset
Language:unknown
Published: Arctic Data Center 2019
Subjects:
Ice
Online Access:https://search.dataone.org/view/urn:uuid:da29e478-9980-4335-8154-8f2e528b1e81
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record_format openpolar
spelling dataone:urn:uuid:da29e478-9980-4335-8154-8f2e528b1e81 2024-06-03T18:46:51+00:00 Hydrogeochemistry of Greenlandic proglacial and nonglacial streams Andrea Pain Martin Jonathan Ellen Martin Shaily Rahman Watson River, Greenland Lake Helen watershed, Greenland Sisimiut watersheds, Greenland Quornup Kua watershed, Greenland Kiagtut Sermiat watershed, Greenland ENVELOPE(-50.68259,-50.05655,67.15853,67.00917) BEGINDATE: 2017-01-01T00:00:00Z ENDDATE: 2018-01-01T00:00:00Z 2019-01-01T00:00:00Z https://search.dataone.org/view/urn:uuid:da29e478-9980-4335-8154-8f2e528b1e81 unknown Arctic Data Center Dataset 2019 dataone:urn:node:ARCTIC 2024-06-03T18:16:01Z This project assesses how weathering varies across deglacial and proglacial watersheds in western and southern Greenland to evaluate the impact of ice sheet retreat on isotopic and nutrient fluxes to the ocean and atmospheric CO2 exchange. Deglacial watersheds are separated from the ice sheet by hydrologic divides and drain only annual snow and permafrost melt, while proglacial watersheds convey supraglacial and subglacial water to the ocean. Previous studies of high latitude weathering focused almost exclusively on proglacial and subglacial systems; however, preliminary work suggests deglacial watersheds in western Greenland transport similar volumes of water with higher solute concentrations than the proglacial system, and weathering extent increases from inland to the coast. Greenland Ice Sheet (GrIS) retreat will increase the areal extent of deglacial watersheds, particularly those with coastal weathering characteristics, thereby altering weathering fluxes. This project aims to test the hypothesis that differences in weathering reactions and extent within deglacial, and between deglacial and proglacial environments, will produce predictable changes in isotopic, solute and nutrient fluxes as the ice sheet retreats. We compare stream discharge and water chemistry between Greenlandic proglacial and nonglacial streams during the spring (2017), summer (2018) and fall (2017) melt seasons between two rivers directly draining the Greenland Ice Sheet (proglacial rivers) and six streams draining deglaciated catchments that are disconnected from the ice (nonglacial streams). This dataset includes DOC and CDOM characteristics analyzed with spectroscopic (UV (ultraviolet) absorbance and fluorescence) measurements, biogeochemical solute concentrations, major cations and anions, trace metals, radiogenic isotopes, and stream discharge information. Dataset Greenland greenlandic Ice Ice Sheet permafrost Sisimiut Arctic Data Center (via DataONE) Greenland Sisimiut ENVELOPE(-53.674,-53.674,66.939,66.939) ENVELOPE(-50.68259,-50.05655,67.15853,67.00917)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
description This project assesses how weathering varies across deglacial and proglacial watersheds in western and southern Greenland to evaluate the impact of ice sheet retreat on isotopic and nutrient fluxes to the ocean and atmospheric CO2 exchange. Deglacial watersheds are separated from the ice sheet by hydrologic divides and drain only annual snow and permafrost melt, while proglacial watersheds convey supraglacial and subglacial water to the ocean. Previous studies of high latitude weathering focused almost exclusively on proglacial and subglacial systems; however, preliminary work suggests deglacial watersheds in western Greenland transport similar volumes of water with higher solute concentrations than the proglacial system, and weathering extent increases from inland to the coast. Greenland Ice Sheet (GrIS) retreat will increase the areal extent of deglacial watersheds, particularly those with coastal weathering characteristics, thereby altering weathering fluxes. This project aims to test the hypothesis that differences in weathering reactions and extent within deglacial, and between deglacial and proglacial environments, will produce predictable changes in isotopic, solute and nutrient fluxes as the ice sheet retreats. We compare stream discharge and water chemistry between Greenlandic proglacial and nonglacial streams during the spring (2017), summer (2018) and fall (2017) melt seasons between two rivers directly draining the Greenland Ice Sheet (proglacial rivers) and six streams draining deglaciated catchments that are disconnected from the ice (nonglacial streams). This dataset includes DOC and CDOM characteristics analyzed with spectroscopic (UV (ultraviolet) absorbance and fluorescence) measurements, biogeochemical solute concentrations, major cations and anions, trace metals, radiogenic isotopes, and stream discharge information.
format Dataset
author Andrea Pain
Martin Jonathan
Ellen Martin
Shaily Rahman
spellingShingle Andrea Pain
Martin Jonathan
Ellen Martin
Shaily Rahman
Hydrogeochemistry of Greenlandic proglacial and nonglacial streams
author_facet Andrea Pain
Martin Jonathan
Ellen Martin
Shaily Rahman
author_sort Andrea Pain
title Hydrogeochemistry of Greenlandic proglacial and nonglacial streams
title_short Hydrogeochemistry of Greenlandic proglacial and nonglacial streams
title_full Hydrogeochemistry of Greenlandic proglacial and nonglacial streams
title_fullStr Hydrogeochemistry of Greenlandic proglacial and nonglacial streams
title_full_unstemmed Hydrogeochemistry of Greenlandic proglacial and nonglacial streams
title_sort hydrogeochemistry of greenlandic proglacial and nonglacial streams
publisher Arctic Data Center
publishDate 2019
url https://search.dataone.org/view/urn:uuid:da29e478-9980-4335-8154-8f2e528b1e81
op_coverage Watson River, Greenland
Lake Helen watershed, Greenland
Sisimiut watersheds, Greenland
Quornup Kua watershed, Greenland
Kiagtut Sermiat watershed, Greenland
ENVELOPE(-50.68259,-50.05655,67.15853,67.00917)
BEGINDATE: 2017-01-01T00:00:00Z ENDDATE: 2018-01-01T00:00:00Z
long_lat ENVELOPE(-53.674,-53.674,66.939,66.939)
ENVELOPE(-50.68259,-50.05655,67.15853,67.00917)
geographic Greenland
Sisimiut
geographic_facet Greenland
Sisimiut
genre Greenland
greenlandic
Ice
Ice Sheet
permafrost
Sisimiut
genre_facet Greenland
greenlandic
Ice
Ice Sheet
permafrost
Sisimiut
_version_ 1800872081690198016