Increasing mass loss from Greenland's Mittivakkat Gletscher

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Standard

Increasing mass loss from Greenland's Mittivakkat Gletscher. / Hasholt, Bent; Mernild, S.H.; Knudsen, N.T.; Lipscomb, J.C.; Yde, J.; Malmros, J.K.; Jakobsen, Bjarne Holm.

I: The Cryosphere Discussions, Bind 5, Nr. 2, 2011, s. 341-348.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Hasholt, B, Mernild, SH, Knudsen, NT, Lipscomb, JC, Yde, J, Malmros, JK & Jakobsen, BH 2011, 'Increasing mass loss from Greenland's Mittivakkat Gletscher', The Cryosphere Discussions, bind 5, nr. 2, s. 341-348. https://doi.org/10.5194/tc-5-341-2011

APA

Hasholt, B., Mernild, S. H., Knudsen, N. T., Lipscomb, J. C., Yde, J., Malmros, J. K., & Jakobsen, B. H. (2011). Increasing mass loss from Greenland's Mittivakkat Gletscher. The Cryosphere Discussions, 5(2), 341-348. https://doi.org/10.5194/tc-5-341-2011

Vancouver

Hasholt B, Mernild SH, Knudsen NT, Lipscomb JC, Yde J, Malmros JK o.a. Increasing mass loss from Greenland's Mittivakkat Gletscher. The Cryosphere Discussions. 2011;5(2):341-348. https://doi.org/10.5194/tc-5-341-2011

Author

Hasholt, Bent ; Mernild, S.H. ; Knudsen, N.T. ; Lipscomb, J.C. ; Yde, J. ; Malmros, J.K. ; Jakobsen, Bjarne Holm. / Increasing mass loss from Greenland's Mittivakkat Gletscher. I: The Cryosphere Discussions. 2011 ; Bind 5, Nr. 2. s. 341-348.

Bibtex

@article{cd31d2da7ec14749a4af06febddf5941,
title = "Increasing mass loss from Greenland's Mittivakkat Gletscher",
abstract = "Warming in the Arctic during the past several decades has caused glaciers to thin and retreat, and recent mass loss from the Greenland Ice Sheet is well documented. Local glaciers peripheral to the ice sheet are also retreating, but few mass-balance observations are available to quantify that retreat and determine the extent to which these glaciers are out of equilibrium with present-day climate. Here, we document record mass loss in 2009/10 for the Mittivakkat Gletscher (henceforth MG), the only local glacier in Greenland for which there exist long-term observations of both the surface mass balance and glacier front fluctuations. We attribute this mass loss primarily to record high mean summer (June–August) temperatures in combination with lower-than-average winter precipitation. Also, we use the 15-yr mass-balance record to estimate present-day and equilibrium accumulation-area ratios for the MG. We show that the glacier is significantly out of balance and will likely lose at least 70% of its current area and 80% of its volume even in the absence of further climate changes. Temperature records from coastal stations in Southeast Greenland suggest that recent MG mass losses are not merely a local phenomenon, but are indicative of glacier changes in the broader region. Mass-balance observations for the MG therefore provide unique documentation of the general retreat of Southeast Greenland's local glaciers under ongoing climate warming.",
author = "Bent Hasholt and S.H. Mernild and N.T. Knudsen and J.C. Lipscomb and J. Yde and J.K. Malmros and Jakobsen, {Bjarne Holm}",
year = "2011",
doi = "10.5194/tc-5-341-2011",
language = "English",
volume = "5",
pages = "341--348",
journal = "The Cryosphere Discussions",
issn = "1994-0432",
publisher = "Copernicus GmbH",
number = "2",

}

RIS

TY - JOUR

T1 - Increasing mass loss from Greenland's Mittivakkat Gletscher

AU - Hasholt, Bent

AU - Mernild, S.H.

AU - Knudsen, N.T.

AU - Lipscomb, J.C.

AU - Yde, J.

AU - Malmros, J.K.

AU - Jakobsen, Bjarne Holm

PY - 2011

Y1 - 2011

N2 - Warming in the Arctic during the past several decades has caused glaciers to thin and retreat, and recent mass loss from the Greenland Ice Sheet is well documented. Local glaciers peripheral to the ice sheet are also retreating, but few mass-balance observations are available to quantify that retreat and determine the extent to which these glaciers are out of equilibrium with present-day climate. Here, we document record mass loss in 2009/10 for the Mittivakkat Gletscher (henceforth MG), the only local glacier in Greenland for which there exist long-term observations of both the surface mass balance and glacier front fluctuations. We attribute this mass loss primarily to record high mean summer (June–August) temperatures in combination with lower-than-average winter precipitation. Also, we use the 15-yr mass-balance record to estimate present-day and equilibrium accumulation-area ratios for the MG. We show that the glacier is significantly out of balance and will likely lose at least 70% of its current area and 80% of its volume even in the absence of further climate changes. Temperature records from coastal stations in Southeast Greenland suggest that recent MG mass losses are not merely a local phenomenon, but are indicative of glacier changes in the broader region. Mass-balance observations for the MG therefore provide unique documentation of the general retreat of Southeast Greenland's local glaciers under ongoing climate warming.

AB - Warming in the Arctic during the past several decades has caused glaciers to thin and retreat, and recent mass loss from the Greenland Ice Sheet is well documented. Local glaciers peripheral to the ice sheet are also retreating, but few mass-balance observations are available to quantify that retreat and determine the extent to which these glaciers are out of equilibrium with present-day climate. Here, we document record mass loss in 2009/10 for the Mittivakkat Gletscher (henceforth MG), the only local glacier in Greenland for which there exist long-term observations of both the surface mass balance and glacier front fluctuations. We attribute this mass loss primarily to record high mean summer (June–August) temperatures in combination with lower-than-average winter precipitation. Also, we use the 15-yr mass-balance record to estimate present-day and equilibrium accumulation-area ratios for the MG. We show that the glacier is significantly out of balance and will likely lose at least 70% of its current area and 80% of its volume even in the absence of further climate changes. Temperature records from coastal stations in Southeast Greenland suggest that recent MG mass losses are not merely a local phenomenon, but are indicative of glacier changes in the broader region. Mass-balance observations for the MG therefore provide unique documentation of the general retreat of Southeast Greenland's local glaciers under ongoing climate warming.

U2 - 10.5194/tc-5-341-2011

DO - 10.5194/tc-5-341-2011

M3 - Journal article

VL - 5

SP - 341

EP - 348

JO - The Cryosphere Discussions

JF - The Cryosphere Discussions

SN - 1994-0432

IS - 2

ER -

ID: 37972527