Using stable isotopes and continuous meltwater river monitoring to investigate the hydrology of a rapidly retreating Icelandic outlet glacier

Alan MacDonald (Lead / Corresponding author), Andrew Black, Brighid Ó Dochartaigh, Verity Flett, WG Darling, Jez Everest

Research output: Contribution to conferenceAbstract

Abstract

Virkisjökull is an outlet glacier draining the western flanks of Öræfajökull on the southern extremity of the Vatnajökull ice cap in SE Iceland. The glacier is highly sensitive to environmental change and has been shown to be in rapid retreat since 2005. Since 2011 there has been continuous measurements of flow in the proglacial meltwater channel, daily photographs of the snout and regular campaigns to sample water chemistry and stable isotopes from the meltwater, ice and groundwater. Ice- and snowmelt dominate the summer flows, but significant flow is also observed in winter due to periodic snowmelt and winter storms. The data indicate a highly efficient glacial drainage system, which makes use of a series of permanent englacial channels within active and buried ice throughout the year. Groundwater contributions to river flow can also be distinguished using stable isotopes and forms an important source of baseflow to the river at low flows. The efficient and year round drainage network may be a contributory factor to the grounding and subsequent rapid retreat of the glacier.
Original languageEnglish
Number of pages1
Publication statusPublished - 22 Jun 2015
EventInternational Symposium on Hydrology of Glaciers and Ice Sheets - Hotel Vatnajökull at Lindarbakki, Höfn in Hornafjörður, Iceland
Duration: 21 Jun 201526 Jun 2015
http://en.vedur.is/conferences/igs-2015

Conference

ConferenceInternational Symposium on Hydrology of Glaciers and Ice Sheets
CountryIceland
CityHöfn in Hornafjörður
Period21/06/1526/06/15
Internet address

Fingerprint

meltwater
glacier
hydrology
stable isotope
snowmelt
ice
monitoring
river
groundwater
drainage network
winter
ice cap
baseflow
river flow
water chemistry
low flow
photograph
environmental change
summer

Cite this

MacDonald, A., Black, A., Ó Dochartaigh, B., Flett, V., Darling, WG., & Everest, J. (2015). Using stable isotopes and continuous meltwater river monitoring to investigate the hydrology of a rapidly retreating Icelandic outlet glacier. Abstract from International Symposium on Hydrology of Glaciers and Ice Sheets, Höfn in Hornafjörður, Iceland.
MacDonald, Alan ; Black, Andrew ; Ó Dochartaigh, Brighid ; Flett, Verity ; Darling, WG ; Everest, Jez. / Using stable isotopes and continuous meltwater river monitoring to investigate the hydrology of a rapidly retreating Icelandic outlet glacier. Abstract from International Symposium on Hydrology of Glaciers and Ice Sheets, Höfn in Hornafjörður, Iceland.1 p.
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title = "Using stable isotopes and continuous meltwater river monitoring to investigate the hydrology of a rapidly retreating Icelandic outlet glacier",
abstract = "Virkisj{\"o}kull is an outlet glacier draining the western flanks of {\"O}r{\ae}faj{\"o}kull on the southern extremity of the Vatnaj{\"o}kull ice cap in SE Iceland. The glacier is highly sensitive to environmental change and has been shown to be in rapid retreat since 2005. Since 2011 there has been continuous measurements of flow in the proglacial meltwater channel, daily photographs of the snout and regular campaigns to sample water chemistry and stable isotopes from the meltwater, ice and groundwater. Ice- and snowmelt dominate the summer flows, but significant flow is also observed in winter due to periodic snowmelt and winter storms. The data indicate a highly efficient glacial drainage system, which makes use of a series of permanent englacial channels within active and buried ice throughout the year. Groundwater contributions to river flow can also be distinguished using stable isotopes and forms an important source of baseflow to the river at low flows. The efficient and year round drainage network may be a contributory factor to the grounding and subsequent rapid retreat of the glacier.",
author = "Alan MacDonald and Andrew Black and {{\'O} Dochartaigh}, Brighid and Verity Flett and WG Darling and Jez Everest",
note = "Presented at session: Glacier catchment hydrology; International Symposium on Hydrology of Glaciers and Ice Sheets ; Conference date: 21-06-2015 Through 26-06-2015",
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MacDonald, A, Black, A, Ó Dochartaigh, B, Flett, V, Darling, WG & Everest, J 2015, 'Using stable isotopes and continuous meltwater river monitoring to investigate the hydrology of a rapidly retreating Icelandic outlet glacier' International Symposium on Hydrology of Glaciers and Ice Sheets, Höfn in Hornafjörður, Iceland, 21/06/15 - 26/06/15, .

Using stable isotopes and continuous meltwater river monitoring to investigate the hydrology of a rapidly retreating Icelandic outlet glacier. / MacDonald, Alan (Lead / Corresponding author); Black, Andrew; Ó Dochartaigh, Brighid ; Flett, Verity; Darling, WG; Everest, Jez.

2015. Abstract from International Symposium on Hydrology of Glaciers and Ice Sheets, Höfn in Hornafjörður, Iceland.

Research output: Contribution to conferenceAbstract

TY - CONF

T1 - Using stable isotopes and continuous meltwater river monitoring to investigate the hydrology of a rapidly retreating Icelandic outlet glacier

AU - MacDonald, Alan

AU - Black, Andrew

AU - Ó Dochartaigh, Brighid

AU - Flett, Verity

AU - Darling, WG

AU - Everest, Jez

N1 - Presented at session: Glacier catchment hydrology

PY - 2015/6/22

Y1 - 2015/6/22

N2 - Virkisjökull is an outlet glacier draining the western flanks of Öræfajökull on the southern extremity of the Vatnajökull ice cap in SE Iceland. The glacier is highly sensitive to environmental change and has been shown to be in rapid retreat since 2005. Since 2011 there has been continuous measurements of flow in the proglacial meltwater channel, daily photographs of the snout and regular campaigns to sample water chemistry and stable isotopes from the meltwater, ice and groundwater. Ice- and snowmelt dominate the summer flows, but significant flow is also observed in winter due to periodic snowmelt and winter storms. The data indicate a highly efficient glacial drainage system, which makes use of a series of permanent englacial channels within active and buried ice throughout the year. Groundwater contributions to river flow can also be distinguished using stable isotopes and forms an important source of baseflow to the river at low flows. The efficient and year round drainage network may be a contributory factor to the grounding and subsequent rapid retreat of the glacier.

AB - Virkisjökull is an outlet glacier draining the western flanks of Öræfajökull on the southern extremity of the Vatnajökull ice cap in SE Iceland. The glacier is highly sensitive to environmental change and has been shown to be in rapid retreat since 2005. Since 2011 there has been continuous measurements of flow in the proglacial meltwater channel, daily photographs of the snout and regular campaigns to sample water chemistry and stable isotopes from the meltwater, ice and groundwater. Ice- and snowmelt dominate the summer flows, but significant flow is also observed in winter due to periodic snowmelt and winter storms. The data indicate a highly efficient glacial drainage system, which makes use of a series of permanent englacial channels within active and buried ice throughout the year. Groundwater contributions to river flow can also be distinguished using stable isotopes and forms an important source of baseflow to the river at low flows. The efficient and year round drainage network may be a contributory factor to the grounding and subsequent rapid retreat of the glacier.

UR - https://www.igsoc.org/symposia/2015/iceland/proceedings/procsfiles/procabstracts_67.html#A1704

UR - https://www.igsoc.org/symposia/2015/iceland/proceedings/fullprogramme.html

M3 - Abstract

ER -

MacDonald A, Black A, Ó Dochartaigh B, Flett V, Darling WG, Everest J. Using stable isotopes and continuous meltwater river monitoring to investigate the hydrology of a rapidly retreating Icelandic outlet glacier. 2015. Abstract from International Symposium on Hydrology of Glaciers and Ice Sheets, Höfn in Hornafjörður, Iceland.