Supraglacial river discharge into Moulin L41A on the Greenland Ice Sheet measured in spring/summer 2012

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Main Authors: Chandler, David M, Wadham, Jemma, Nienow, Peter, Doyle, Samuel H, Tedstone, Andrew, Telling, Jon, Hawkings, Jonathan, Alcock, Jonathan, Linhoff, Benjamin, Hubbard, Alun L
Format: Dataset Open Access
Language:en
Published: PANGAEA 2021
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author Chandler, David M
Wadham, Jemma
Nienow, Peter
Doyle, Samuel H
Tedstone, Andrew
Telling, Jon
Hawkings, Jonathan
Alcock, Jonathan
Linhoff, Benjamin
Hubbard, Alun L
author_facet Chandler, David M
Wadham, Jemma
Nienow, Peter
Doyle, Samuel H
Tedstone, Andrew
Telling, Jon
Hawkings, Jonathan
Alcock, Jonathan
Linhoff, Benjamin
Hubbard, Alun L
collection Datos científicos de ciencias marinas y ambientales
contents Supraglacial river discharge was measured by monitoring water depth with a custom-built pressure sensor, at 1-minute intervals, and converting depth to discharge with a rating curve established from salt dilution gauging. Here we report 1-hour means of the 1-minute measurements. This method is well suited to supraglacial river gauging as the electrical conductivity of supraglacial melt water is very low. The pressure sensor was installed on the bottom of the channel and was able to move downwards with the ice surface as the channel gradually incised. Full details are provided in the online supplement to Wadham et al. (2016) at https://doi.org/10.5194/bg-13-6339-2016.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_926844
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Supraglacial river discharge into Moulin L41A on the Greenland Ice Sheet measured in spring/summer 2012
Chandler, David M
Wadham, Jemma
Nienow, Peter
Doyle, Samuel H
Tedstone, Andrew
Telling, Jon
Hawkings, Jonathan
Alcock, Jonathan
Linhoff, Benjamin
Hubbard, Alun L
Calculated after Wadham et al. (2016); DATE/TIME; Greenland; Greenland ice sheet; hydrology; ICEOBS; Ice observation; Ice Sheet; moulin; Moulin_L41A; River discharge, hourly maximum; River discharge, hourly mean; River discharge, hourly minimum; subglacial; tracing
Supraglacial river discharge was measured by monitoring water depth with a custom-built pressure sensor, at 1-minute intervals, and converting depth to discharge with a rating curve established from salt dilution gauging. Here we report 1-hour means of the 1-minute measurements. This method is well suited to supraglacial river gauging as the electrical conductivity of supraglacial melt water is very low. The pressure sensor was installed on the bottom of the channel and was able to move downwards with the ice surface as the channel gradually incised. Full details are provided in the online supplement to Wadham et al. (2016) at https://doi.org/10.5194/bg-13-6339-2016.
title Supraglacial river discharge into Moulin L41A on the Greenland Ice Sheet measured in spring/summer 2012
topic Calculated after Wadham et al. (2016); DATE/TIME; Greenland; Greenland ice sheet; hydrology; ICEOBS; Ice observation; Ice Sheet; moulin; Moulin_L41A; River discharge, hourly maximum; River discharge, hourly mean; River discharge, hourly minimum; subglacial; tracing
url https://doi.org/10.1594/PANGAEA.926844