Abstract

Abstract. Grinnell and Terra Nivea Ice Caps are located on the southern Baffin Island, Nunavut, in the Canadian Arctic Archipelago. These relatively small ice caps have received little attention compared to the much larger ice masses further north. Their evolution can, however, give valuable information about the impact of the recent Arctic warming at lower latitudes (i.e. ~ 62.5° N). In this paper, we measure or estimate historical and recent changes of area, elevation and mass of both ice caps using in situ, airborne and spaceborne data sets, including imagery from the Pléiades satellites. The area of Terra Nivea Ice Cap has decreased by 34 % since the late 1950s, while that of Grinnell Ice Cap has decreased by 20 % since 1952. For both ice caps, the areal reduction accelerated at the beginning of the 21st century. The estimated glacier-wide mass balance was −0.37 ± 0.21 m a−1 water equivalent (w.e.) over Grinnell Ice Cap for the 1952–2014 period, and −0.47 ± 0.16 m a−1 w.e. over Terra Nivea Ice Cap for the 1958/59–2014 period. Terra Nivea Ice Cap has experienced an accelerated rate of mass loss of −1.77 ± 0.36 m a−1 w.e. between 2007 and 2014. This rate is 5.9 times as negative when compared to the 1958/59–2007 period (−0.30 ± 0.19 m a−1 w.e.) and 2 times as negative when compared to the mass balance of other glaciers in the southern parts of Baffin Island over the 2003–2009 period. A similar acceleration in mass loss is suspected for the Grinnell Ice Cap, given the calculated elevation changes and the proximity to Terra Nivea Ice Cap. The recent increase in mass loss rates for these two ice caps is linked to a strong near-surface regional warming and a lengthening of the melt season into the autumn that may be indirectly strengthened by a later freezing of sea ice in the Hudson Strait sector. On a methodological level, our study illustrates the strong potential of Pléiades satellite data to unlock the under-exploited archive of old aerial photographs.

Highlights

  • With a glacierized area of ∼ 150 000 km2, the Canadian Arctic Archipelago (CAA) is one of the major glacier regions in the world (Pfeffer et al, 2014)

  • Since the ice-free zones on our Pléiades digital elevation models (DEMs) were not large enough to calculate an elevation accuracy with a sufficient number of ICESat points, we report here the vertical precisions obtained in recent glaciological studies

  • Grinnell Ice Cap (GRIC) experienced a mean rate of areal change of −0.10 ± 0.01 km2 a−1 between 1952 and 1999, whereas a mean rate of −0.59 ± 0.03 km2 a−1 is measured for Terra Nivea Ice Cap (TNIC) between 1958/59 and 1998

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Summary

Introduction

With a glacierized area of ∼ 150 000 km, the Canadian Arctic Archipelago (CAA) is one of the major glacier regions in the world (Pfeffer et al, 2014). In response to recent Arctic warming (Tingley and Huybers, 2013; Vaughan et al, 2013; Comiso and Hall, 2014), glaciers in the CAA have experienced an acceleration in their mass loss. Located in the southeastern part of the CAA, Baffin Island is the largest island of the archipelago (Andrews et al, 2002) and has a total ice-covered area of ∼ 37 000 km. In addition to two major ice caps, Barnes (∼ 5900 km2) and Penny (∼ 6400 km2), Baffin Island is covered by a num-

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