Glacier response to the Little Ice Age during the Neoglacial cooling in Greenland

Author:

Kjær Kurt H.,Bjørk Anders A.,Kjeldsen Kristian K.,Hansen Eric S.,Andresen Camilla S.,Siggaard-Andersen Marie-Louise,Khan Shfaqat A.,Søndergaard Anne Sofie,Colgan William,Schomacker Anders,Woodroffe Sarah,Funder Svend,Rouillard Alexandra,Jensen Jens Fog,Larsen Nicolaj K.

Funder

Research Council of Norway

Villum Foundation

DFF

Geocenter Danmark

DNRF

Horizon 2020 Marie Skłodowska-Curie Actions

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference324 articles.

1. Palaeohydrology of Kangerlussuaq (Søndre Strømfjord), West Greenland during the last ~8000 years;Aebly;Holocene,2009

2. Continental-scale temperature variability during the past two millennia;Ahmed;Nat. Geosci.,2013

3. Late Holocene sea surface instabilities in the Disko Bugt Area, West Greenland, in phase with δ 18 O oscillations at Camp Century;Allan,2018

4. The 8k event: cause and consequences of a major Holocene abrupt climate change;Alley;Quat. Sci. Rev.,2005

5. Variations in melt-layer frequency in the GISP2 ice core: implications for Holocene summer temperatures in central Greenland;Alley;Ann. Glaciol.,1995

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