Strong altitudinal control on the response of local glaciers to Holocene climate change in southwest Greenland

TY - JOUR

T1 - Strong altitudinal control on the response of local glaciers to Holocene climate change in southwest Greenland

AU - Larsen, Nicolaj K.

AU - Strunk, Astrid

AU - Levy, Laura B.

AU - Olsen, Jesper

AU - Bjork, Anders

AU - Lauridsen, Torben L.

AU - Jeppesen, Erik

AU - Davidson, Thomas A.

PY - 2017/7/15

Y1 - 2017/7/15

N2 - Accelerating ice loss during recent years has made the Greenland Ice Sheet one of the largest single contributors to global sea level rise, accounting for 0.5 of the total 3.2 mm yr −1. This loss is predicted to continue and will most likely increase in the future as a consequence of global warming. However, the sensitivity of glaciers and ice caps (GICs) in Greenland to prolonged warm periods is less well constrained and geological records documenting the long-term glacial history are needed to put recent observations into a broader perspective. Here we report the results from three proglacial lakes where fluctuations in local glaciers located at different altitudes in Kobbefjord, southwest Greenland have been recorded. Our results show that the lakes received meltwater from the initial deglaciation of the area ∼9.2 cal. ka BP until ∼8.7–7.9 cal. ka BP when the meltwater input ceased as the glaciers most likely disappeared. Regrowth of glaciers began again at ∼5.5 cal. ka BP at ∼1370 m a.s.l., ∼3.6 cal. ka at ∼1170 m a.s.l., and ∼1.6 cal. ka BP at ∼1000 m a.s.l., clearly reflecting strong altitudinal control of the GIC response to Neoglacial cooling. Our results highlight that GICs in Kobbefjord, southwest Greenland are primarily influenced by changes in summer air temperatures and winter precipitation and that they are facing a rapid decay that most likely will result in their disappearance within the next centuries as a consequence of global warming. If current 21st Century retreat rates continue, the GICs in the study area will be completely gone in ∼30–90 years, with the smallest GICs disappearing first.

AB - Accelerating ice loss during recent years has made the Greenland Ice Sheet one of the largest single contributors to global sea level rise, accounting for 0.5 of the total 3.2 mm yr −1. This loss is predicted to continue and will most likely increase in the future as a consequence of global warming. However, the sensitivity of glaciers and ice caps (GICs) in Greenland to prolonged warm periods is less well constrained and geological records documenting the long-term glacial history are needed to put recent observations into a broader perspective. Here we report the results from three proglacial lakes where fluctuations in local glaciers located at different altitudes in Kobbefjord, southwest Greenland have been recorded. Our results show that the lakes received meltwater from the initial deglaciation of the area ∼9.2 cal. ka BP until ∼8.7–7.9 cal. ka BP when the meltwater input ceased as the glaciers most likely disappeared. Regrowth of glaciers began again at ∼5.5 cal. ka BP at ∼1370 m a.s.l., ∼3.6 cal. ka at ∼1170 m a.s.l., and ∼1.6 cal. ka BP at ∼1000 m a.s.l., clearly reflecting strong altitudinal control of the GIC response to Neoglacial cooling. Our results highlight that GICs in Kobbefjord, southwest Greenland are primarily influenced by changes in summer air temperatures and winter precipitation and that they are facing a rapid decay that most likely will result in their disappearance within the next centuries as a consequence of global warming. If current 21st Century retreat rates continue, the GICs in the study area will be completely gone in ∼30–90 years, with the smallest GICs disappearing first.

KW - Greenland

KW - Glacier fluctuations

KW - Holocene

KW - Paleoclimate

KW - RELATIVE SEA-LEVEL

KW - ICE-SHEET MARGIN

KW - WEST GREENLAND

KW - ARCTIC CANADA

KW - SOUTHERN GREENLAND

KW - LATEST PLEISTOCENE

KW - BAFFIN-ISLAND

KW - EAST GREENLAND

KW - LAKE-SEDIMENTS

KW - EUROPEAN ALPS

UR - https://www.scopus.com/pages/publications/85019469948

U2 - 10.1016/j.quascirev.2017.05.008

DO - 10.1016/j.quascirev.2017.05.008

M3 - Journal article

SN - 0277-3791

VL - 168

SP - 69

EP - 78

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

ER -