Articles | Volume 10, issue 2
The Cryosphere, 10, 523–534, 2016
The Cryosphere, 10, 523–534, 2016

Research article 08 Mar 2016

Research article | 08 Mar 2016

Recent summer sea ice thickness surveys in Fram Strait and associated ice volume fluxes

T. Krumpen1, R. Gerdes1,2, C. Haas3, S. Hendricks1, A. Herber1, V. Selyuzhenok1, L. Smedsrud4, and G. Spreen5,a T. Krumpen et al.
  • 1Alfred Wegener Institute, Busse Str. 24, 27570 Bremerhaven, Germany
  • 2Jacobs University, Earth and Environmental Sciences Faculty, Campus Ring 1, 28759 Bremen, Germany
  • 3York University, Earth & Space Science & Engineering, Petrie 105, 4700 Keele St, Toronto, ON M3J 1P3, Canada
  • 4Geophysical Institute, University Bergen, Allegt. 70, 5020 Bergen, Norway
  • 5Norwegian Polar Institute, Fram Centre, Postbox 6606 Langnes, 9296 Tromsø, Norway
  • anow at: University of Bremen, Institute of Environmental Physics, Otto-Hahn-Allee 1, 28359 Bremen, Germany

Abstract. Fram Strait is the main gateway for sea ice export out of the Arctic Ocean, and therefore observations there give insight into the composition and properties of Arctic sea ice in general and how it varies over time. A data set of ground-based and airborne electromagnetic ice thickness measurements collected during summer between 2001 and 2012 is presented here, including long transects well into the southern part of the Transpolar Drift obtained using fixed-wing aircrafts. The primary source of the surveyed sea ice leaving Fram Strait is the Laptev Sea and its age has decreased from 3 to 2 years between 1990 and 2012. The thickness data consistently also show a general thinning of sea ice for the last decade, with a decrease in modal thickness of second year and multiyear ice, and a decrease in mean thickness and fraction of ice thicker than 3 m. Local melting in the strait was investigated in two surveys performed in the downstream direction, showing a decrease in sea ice thickness of 0.19 m degree−1 latitude south of 81° N. Further north variability in ice thickness is more related to differences in age and deformation. The thickness observations were combined with ice area export estimates to calculate summer volume fluxes of sea ice. While satellite data show that monthly ice area export had positive trends since 1980 (10.9  ×  103 km2 decade−1), the summer (July and August) ice area export is low with high uncertainties. The average volume export amounts to 16.78 km3. Naturally, the volume flux estimates are limited to the period when airborne thickness surveys are available. Nevertheless, we could show that the combination of satellite data and airborne observations can be used to determine volume fluxes through Fram Strait and as such, can be used to bridge the lack of satellite-based sea ice thickness information in summer.

Short summary
We present an extensive data set of ground-based and airborne electromagnetic ice thickness measurements covering Fram Strait in summer between 2001 and 2012. An investigation of back trajectories of surveyed sea ice using satellite-based sea ice motion data allows us to examine the connection between thickness variability, ice age and source area. In addition, we determine across and along strait gradients in ice thickness and associated volume fluxes.