ARCUS | Arctic Research Consortium of the United States

7th Annual ARCUS Award for Arctic Research Excellence


Submitted by   Matthias Prange
Authors   Matthias Prange and G. Lohmann
Category   Physical Science
Title   Effects of Mid-Holocene River Runoff on the Arctic Ocean-Sea Ice System: A Numerical Model Study
Affiliation   Geosciences Department, University of Bremen, Bremen, Br, Germany

Abstract

Recent geological studies have revealed that the freshwater input to the Arctic Ocean was highly variable during the Holocene. In the present study, the influence of mid-Holocene river runoff on large-scale Arctic ocean-sea ice dynamics is examined using a general circulation model. A paleohydrological forcing for the time interval around 6 ka BP (radiocarbon time scale) is constructed by compiling data from the available literature. Keeping all other forcing fields and bottom topography of the ocean model at present-day values, the effect of a changed freshwater input to the Arctic Ocean is isolated. The model shows that freshwater supply is vitally important for the polar oceanic circulation. In particular, a close connection between Siberian river runoff and the path of the Transpolar Drift (TPD) is found. Consistent with paleoceanographic findings of driftwood delivery to the Canadian Archipelago and Baffin Bay, the model results suggest that enhanced freshwater discharge during the mid-Holocene caused an eastward shift of the TPD with strengthened outflow through Fram Strait.