Warmer–wetter climate drives shift in δD–δ18O composition of precipitation across the Queen Elizabeth Islands, Arctic Canada

Arctic Science

David Fisher¹  Laura Thomson²  Luke Copland³  Denis Lacelle³  Brittany Main³  Frances Delaney³  David Burgess⁴ 

[1] Department of Earth Sciences, University of Ottawa, Ottawa, ON K1N 6N5, Canada.;Department of Geography and Planning, Queen’s University, Kingston, ON K7L 3N6, Canada.;Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, ON K1N 6N5, Canada.;Natural Resources Canada, Ottawa, ON K1A 0E8, Canada.;

关键词: oxygen isotopes;    snow;    ice cores;    climate change;   

DOI  :  10.1139/as-2020-0009

来源: DOAJ

【 摘 要 】

We examine how recent increases in air temperature and precipitation, together with reductions in sea ice extent, may have affected the regional δD–δ18O composition of precipitation. In spring 2014, 80 snow samples were collected from six glaciers and ice caps across the Queen Elizabeth Islands, and in 2009 and 2014, two shallow ice cores were collected from Agassiz Ice Cap and White Glacier, respectively. The snow samples showed average δ18O values from 2013 to 2014 to be approximately 2‰–3‰ higher than those recorded in 1973–1974 in nearby locations, with the ice cores showing similar trends in δ18O values. A zonal average water isotope model was used to help understand the causes of the increased δ18O values, using inputs calibrated for observed changes in temperature, vapour flux, and sea ice extent. Model results indicate that atmospheric temperature changes account for <1‰ of the observed change in δ18O values, and that changes in local water input and precipitation driven by changes in sea ice extent only have an effect in coastal regions. Enhanced meridional vapour flux to the Queen Elizabeth Islands is, therefore, also required to explain the observed increases in δ18O values, with fluxes ∼7% higher today than in the 1970s, consistent with the change in precipitation.

【 授权许可】

Unknown