Holocene climate conditions and glacier variation in central Iceland from physical modelling and empirical evidence

Gwenn E. Flowers, Helgi Björnsson, Áslaug Geirsdóttir, Gifford H. Miller, Jessica L. Black, Garry K.C. Clarke

Research output: Contribution to journalArticlepeer-review

45 Scopus citations

Abstract

Lacustrine sediment cores from proglacial lake Hvítárvatn, central Iceland, reveal a detailed chronology of Holocene sedimentation, from which environmental conditions and the attendant fluctuations of Langjökull ice cap have been interpreted. We apply a numerical ice-sheet model to determine the climatic conditions under which the empirical reconstruction is glaciologically plausible. Modelling constraints are derived from core records of diatom concentration, benthic diatom fraction, and ice-rafted debris occurrence, as well as lake bottom morphology and the present-day ice-cap geometry. Holocene simulations driven by the NGRIP δ18 O record that are consistent with the empirical constraints show the most extensive advance of Langjökull ice cap to be its most recent, beginning somewhere between 5 and 3 ka BP. Ice advance in response to the 8.2 ka BP cold event is followed by several thousand years of nearly ice-free conditions in the mid-Holocene. All simulations suggest that the maximum Holocene stand of the ice cap occurred during the Little Ice Age (LIA); those consistent with the constraints show little to no ice advance into Hvítárvatn before ∼ 1 ka BP and indicate the lake area occupied by ice was much greater during the LIA than at any previous time. The most plausible simulation results were obtained for a maximum Holocene warming of 3-4 {ring operator} C relative to the 1961-1990 reference, twice the Arctic average, and for Holocene Thermal Maximum (HTM) precipitation amounts comparable to or slightly greater than the modern. Reconciling the simulated subglacial discharge record to the empirically derived sediment volumes and emplacement times requires mean Holocene sediment concentrations of 0.8-1.6 kg m- 3. These estimates increase to 1.4-2.0 kg m- 3 when sedimentation rates are highest.

Original languageEnglish (US)
Pages (from-to)797-813
Number of pages17
JournalQuaternary Science Reviews
Volume27
Issue number7-8
DOIs
StatePublished - Apr 2008

Bibliographical note

Funding Information:
This paper is a contribution to “Warm times/Cold times: Reconstructing Iceland's climate and environment since the last glaciation to evaluate the impacts of future climate change” which was jointly funded by the Research Council of Iceland (RANNIS), the University of Iceland Research Fund and the U.S. National Science Foundation (OPP-0138010, ATM-0318479). G. Flowers also received support from the Natural Sciences and Engineering Research Council of Canada during a postdoctoral fellowship at the University of British Columbia, and from the Canada Research Chairs Program in her current position at Simon Fraser University. This work would not have been possible without the ice-sheet model code contributed by Shawn Marshall (University of Calgary), the high-resolution NGRIP δ 18 O data generously provided by Bo Vinther and Sigfús Johnsen (Niels Bohr Institute, Copenhagen) and the digital elevation models of Langjökull from Finnur Pálsson (Institute of Earth Sciences, University of Iceland). Two anonymous reviewers are gratefully acknowledged for providing valuable feedback.

Copyright:
Copyright 2008 Elsevier B.V., All rights reserved.

Fingerprint Dive into the research topics of 'Holocene climate conditions and glacier variation in central Iceland from physical modelling and empirical evidence'. Together they form a unique fingerprint.

Cite this