Greenland Ice Sheet surface mass balance 1870 to 2010 based on Twentieth Century Reanalysis, and links with global climate forcing

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Standard

Greenland Ice Sheet surface mass balance 1870 to 2010 based on Twentieth Century Reanalysis, and links with global climate forcing. / Hanna, Edward; Huybrechts, Philippe; Cappelen, John; Steffen, Konrad; Bales, Roger C.; Burgess, Evan; McConnell, Joseph R.; Steffensen, Joergen Peder; Van Den Broeke, Michiel; Wake, Leanne; Bigg, Grant; Griffiths, Mike; Savas, Deniz.

I: Journal of Geophysical Research Atmospheres, Bind 116, Nr. 24, D24121, 01.01.2011.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Hanna, E, Huybrechts, P, Cappelen, J, Steffen, K, Bales, RC, Burgess, E, McConnell, JR, Steffensen, JP, Van Den Broeke, M, Wake, L, Bigg, G, Griffiths, M & Savas, D 2011, 'Greenland Ice Sheet surface mass balance 1870 to 2010 based on Twentieth Century Reanalysis, and links with global climate forcing', Journal of Geophysical Research Atmospheres, bind 116, nr. 24, D24121. https://doi.org/10.1029/2011JD016387

APA

Hanna, E., Huybrechts, P., Cappelen, J., Steffen, K., Bales, R. C., Burgess, E., McConnell, J. R., Steffensen, J. P., Van Den Broeke, M., Wake, L., Bigg, G., Griffiths, M., & Savas, D. (2011). Greenland Ice Sheet surface mass balance 1870 to 2010 based on Twentieth Century Reanalysis, and links with global climate forcing. Journal of Geophysical Research Atmospheres, 116(24), [D24121]. https://doi.org/10.1029/2011JD016387

Vancouver

Hanna E, Huybrechts P, Cappelen J, Steffen K, Bales RC, Burgess E o.a. Greenland Ice Sheet surface mass balance 1870 to 2010 based on Twentieth Century Reanalysis, and links with global climate forcing. Journal of Geophysical Research Atmospheres. 2011 jan. 1;116(24). D24121. https://doi.org/10.1029/2011JD016387

Author

Hanna, Edward ; Huybrechts, Philippe ; Cappelen, John ; Steffen, Konrad ; Bales, Roger C. ; Burgess, Evan ; McConnell, Joseph R. ; Steffensen, Joergen Peder ; Van Den Broeke, Michiel ; Wake, Leanne ; Bigg, Grant ; Griffiths, Mike ; Savas, Deniz. / Greenland Ice Sheet surface mass balance 1870 to 2010 based on Twentieth Century Reanalysis, and links with global climate forcing. I: Journal of Geophysical Research Atmospheres. 2011 ; Bind 116, Nr. 24.

Bibtex

@article{cc256ab3c84e4494b11154e2abbdb7fd,
title = "Greenland Ice Sheet surface mass balance 1870 to 2010 based on Twentieth Century Reanalysis, and links with global climate forcing",
abstract = "We present a reconstruction of the Greenland Ice Sheet surface mass balance (SMB) from 1870 to 2010, based on merged Twentieth Century Reanalysis (20CR) and European Centre for Medium-Range Weather Forecasts (ECMWF) meteorological reanalyses, and we compare our new SMB series with global and regional climate and atmospheric circulation indices during this period. We demonstrate good agreement between SMB annual series constructed from 20CR and ECMWF reanalyses for the common period of overlap and show statistically significant agreement of long-term modeled snowfall with ice-core-based accumulation data. We analyze variations in SMB for the last 140 years and highlight the periods with significantly increased runoff and decreased SMB since 1870, which have both been enhanced in the period since 1990, as well as interannual variations in SMB linked to Greenland climate fluctuations. We show very good agreement of our SMB series variations with existing, independently derived SMB series (RACMO2) variations for the past few decades of overlap but also a significant disparity of up to ∼200 km3 yr-1 in absolute SMB values due to poorly constrained modeled accumulation reflecting a lack of adequate validation data in southeast Greenland. There is no significant correlation between our SMB time series and a widely referenced time series of North Atlantic icebergs emanating from Greenland for the past century, which may reflect the complex nature of the relationship between SMB and ice dynamical changes. Finally, we discuss how our analysis sheds light on the sensitivity and response of the Greenland Ice Sheet to ongoing and future global climate change, and its contribution to global sea level rise.",
author = "Edward Hanna and Philippe Huybrechts and John Cappelen and Konrad Steffen and Bales, {Roger C.} and Evan Burgess and McConnell, {Joseph R.} and Steffensen, {Joergen Peder} and {Van Den Broeke}, Michiel and Leanne Wake and Grant Bigg and Mike Griffiths and Deniz Savas",
year = "2011",
month = jan,
day = "1",
doi = "10.1029/2011JD016387",
language = "English",
volume = "116",
journal = "Journal of Geophysical Research: Solid Earth",
issn = "0148-0227",
publisher = "American Geophysical Union",
number = "24",

}

RIS

TY - JOUR

T1 - Greenland Ice Sheet surface mass balance 1870 to 2010 based on Twentieth Century Reanalysis, and links with global climate forcing

AU - Hanna, Edward

AU - Huybrechts, Philippe

AU - Cappelen, John

AU - Steffen, Konrad

AU - Bales, Roger C.

AU - Burgess, Evan

AU - McConnell, Joseph R.

AU - Steffensen, Joergen Peder

AU - Van Den Broeke, Michiel

AU - Wake, Leanne

AU - Bigg, Grant

AU - Griffiths, Mike

AU - Savas, Deniz

PY - 2011/1/1

Y1 - 2011/1/1

N2 - We present a reconstruction of the Greenland Ice Sheet surface mass balance (SMB) from 1870 to 2010, based on merged Twentieth Century Reanalysis (20CR) and European Centre for Medium-Range Weather Forecasts (ECMWF) meteorological reanalyses, and we compare our new SMB series with global and regional climate and atmospheric circulation indices during this period. We demonstrate good agreement between SMB annual series constructed from 20CR and ECMWF reanalyses for the common period of overlap and show statistically significant agreement of long-term modeled snowfall with ice-core-based accumulation data. We analyze variations in SMB for the last 140 years and highlight the periods with significantly increased runoff and decreased SMB since 1870, which have both been enhanced in the period since 1990, as well as interannual variations in SMB linked to Greenland climate fluctuations. We show very good agreement of our SMB series variations with existing, independently derived SMB series (RACMO2) variations for the past few decades of overlap but also a significant disparity of up to ∼200 km3 yr-1 in absolute SMB values due to poorly constrained modeled accumulation reflecting a lack of adequate validation data in southeast Greenland. There is no significant correlation between our SMB time series and a widely referenced time series of North Atlantic icebergs emanating from Greenland for the past century, which may reflect the complex nature of the relationship between SMB and ice dynamical changes. Finally, we discuss how our analysis sheds light on the sensitivity and response of the Greenland Ice Sheet to ongoing and future global climate change, and its contribution to global sea level rise.

AB - We present a reconstruction of the Greenland Ice Sheet surface mass balance (SMB) from 1870 to 2010, based on merged Twentieth Century Reanalysis (20CR) and European Centre for Medium-Range Weather Forecasts (ECMWF) meteorological reanalyses, and we compare our new SMB series with global and regional climate and atmospheric circulation indices during this period. We demonstrate good agreement between SMB annual series constructed from 20CR and ECMWF reanalyses for the common period of overlap and show statistically significant agreement of long-term modeled snowfall with ice-core-based accumulation data. We analyze variations in SMB for the last 140 years and highlight the periods with significantly increased runoff and decreased SMB since 1870, which have both been enhanced in the period since 1990, as well as interannual variations in SMB linked to Greenland climate fluctuations. We show very good agreement of our SMB series variations with existing, independently derived SMB series (RACMO2) variations for the past few decades of overlap but also a significant disparity of up to ∼200 km3 yr-1 in absolute SMB values due to poorly constrained modeled accumulation reflecting a lack of adequate validation data in southeast Greenland. There is no significant correlation between our SMB time series and a widely referenced time series of North Atlantic icebergs emanating from Greenland for the past century, which may reflect the complex nature of the relationship between SMB and ice dynamical changes. Finally, we discuss how our analysis sheds light on the sensitivity and response of the Greenland Ice Sheet to ongoing and future global climate change, and its contribution to global sea level rise.

UR - http://www.scopus.com/inward/record.url?scp=84855336557&partnerID=8YFLogxK

U2 - 10.1029/2011JD016387

DO - 10.1029/2011JD016387

M3 - Journal article

AN - SCOPUS:84855336557

VL - 116

JO - Journal of Geophysical Research: Solid Earth

JF - Journal of Geophysical Research: Solid Earth

SN - 0148-0227

IS - 24

M1 - D24121

ER -

ID: 232014494