Ablation observations for 2008-2011 from the Programme for Monitoring of the Greenland Ice Sheet (PROMICE)

Robert S. Fausto; Dirk van As; Andreas P. Ahlstrøm; Signe B. Andersen; Morten L. Andersen; Michele Citterio; Karen Edelvang; Signe H. Larsen; Horst Machguth; Søren Nielsen; Anker Weidick

doi:10.34194/geusb.v26.4765

Ablation observations for 2008-2011 from the Programme for Monitoring of the Greenland Ice Sheet (PROMICE)

Robert S. Fausto, Dirk van As, Andreas P. Ahlstrøm, Signe B. Andersen, Morten L. Andersen, Michele Citterio, Karen Edelvang, Signe H. Larsen, Horst Machguth, Søren Nielsen, Anker Weidick

Publikation: Bidrag til tidsskrift › Artikel › Forskning › peer review

38 Citationer (Scopus)

Abstrakt

Recent estimates from the glaciological community agree that the Greenland ice sheet is losing mass at an accelerated pace due to climate change (Velicogna 2009; Khan et al. 2010; Rignot et al. 2011). This has caught the attention of the public and policy makers due to the potential impact on sea-level rise (Dahl-Jensen et al. 2009). The mass loss can be attributed approximately equally to increases in meltwater runoff from surface melt and iceberg production (van den Broeke et al. 2009).

Originalsprog	Engelsk
Sider (fra-til)	73-76
Antal sider	4
Tidsskrift	Geological Survey of Denmark and Greenland Bulletin
Vol/bind	26
DOI	https://doi.org/10.34194/geusb.v26.4765
Status	Udgivet - 10 jul. 2012

Programområde

Programområde 5: Natur og klima

FN’s Verdensmål

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Adgang til dokumentet

10.34194/geusb.v26.4765Licens: CC BY

Citationsformater

Fausto, R. S., van As, D., Ahlstrøm, A. P., Andersen, S. B., Andersen, M. L., Citterio, M., Edelvang, K., Larsen, S. H., Machguth, H., Nielsen, S., & Weidick, A. (2012). Ablation observations for 2008-2011 from the Programme for Monitoring of the Greenland Ice Sheet (PROMICE). Geological Survey of Denmark and Greenland Bulletin, 26, 73-76. https://doi.org/10.34194/geusb.v26.4765

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abstract = "Recent estimates from the glaciological community agree that the Greenland ice sheet is losing mass at an accelerated pace due to climate change (Velicogna 2009; Khan et al. 2010; Rignot et al. 2011). This has caught the attention of the public and policy makers due to the potential impact on sea-level rise (Dahl-Jensen et al. 2009). The mass loss can be attributed approximately equally to increases in meltwater runoff from surface melt and iceberg production (van den Broeke et al. 2009).",

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doi = "10.34194/geusb.v26.4765",

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AU - Fausto, Robert S.

AU - van As, Dirk

AU - Ahlstrøm, Andreas P.

AU - Andersen, Signe B.

AU - Andersen, Morten L.

AU - Citterio, Michele

AU - Edelvang, Karen

AU - Larsen, Signe H.

AU - Machguth, Horst

AU - Nielsen, Søren

AU - Weidick, Anker

PY - 2012/7/10

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N2 - Recent estimates from the glaciological community agree that the Greenland ice sheet is losing mass at an accelerated pace due to climate change (Velicogna 2009; Khan et al. 2010; Rignot et al. 2011). This has caught the attention of the public and policy makers due to the potential impact on sea-level rise (Dahl-Jensen et al. 2009). The mass loss can be attributed approximately equally to increases in meltwater runoff from surface melt and iceberg production (van den Broeke et al. 2009).

AB - Recent estimates from the glaciological community agree that the Greenland ice sheet is losing mass at an accelerated pace due to climate change (Velicogna 2009; Khan et al. 2010; Rignot et al. 2011). This has caught the attention of the public and policy makers due to the potential impact on sea-level rise (Dahl-Jensen et al. 2009). The mass loss can be attributed approximately equally to increases in meltwater runoff from surface melt and iceberg production (van den Broeke et al. 2009).

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JO - Geological Survey of Denmark and Greenland Bulletin

JF - Geological Survey of Denmark and Greenland Bulletin

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ER -

Ablation observations for 2008-2011 from the Programme for Monitoring of the Greenland Ice Sheet (PROMICE)

Abstrakt

Programområde

FN’s Verdensmål

Adgang til dokumentet

Fingeraftryk

Citationsformater