Area, elevation and mass changes of the two southernmost ice caps of the Canadian Arctic Archipelago between 1952 and 2014

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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.

Figures

  • Figure 1. Study area.
  • Figure 2. (a) Pléiades orthoimage of Grinnell Ice Cap (3 August 2014) superimposed with areal extents from 1952, 1999 and 2014. (b) Pléiades orthoimages of Terra Nivea Ice Cap (14 August 2014 on the east side and 26 August 2014 on the west side) superimposed with areal extents from 1958/59, 1998, 2007 and 2014. The overlapping area between the two orthoimages is represented by the black dashed polygon. (c) Historical and recent area changes for both ice caps. Error margins were estimated at 5 % for historical areas and at 3 % for 1998 and later outlines (Sect. 4.4.3.).
  • Table 1. Elevation data sets used in this study with the acquisition date and the purpose of their use for each ice cap.
  • Figure 3. Elevation change rates (m a−1) on Grinnell Ice Cap between August 1952 (Aerial photo DEM) and August 2014 (Pléiades DEM). For this figure as well as for the next ones, no color (i.e. hillshade is visible) represents no data.
  • Table 2. Historical and recent glacier-wide mass balances for both ice caps.
  • Figure 4. Elevation change rates (m a−1) on Grinnell Ice Cap between March/April 2004 (ICESat and in situ GPS points) and August 2014 (Pléiades DEM). Bottom right graph shows historical (1952–2004) and recent (2004–2014) rates of elevation changes along the 203 points contiguous with the 1952 DEM (represented as black dots on the map).
  • Figure 5. (a) Elevation change rates (dH /dt , m a−1) on Terra Nivea Ice Cap (TNIC) between 1958/59 (CDED) and 2007 (ASTER DEM). (b) dH /dt on TNIC between 1958/59 (CDED) and 2014 (Pléiades DEM). (c) dH /dt on TNIC between 2007 (ASTER DEM) and 2014 (Pléiades DEM). Note a different color scale for the lower panel (c).
  • Figure 6. (a) Historical averaged elevation change rates (dH /dtavg) measured for GRIC (1952–2014) and TNIC (1958/59–2014) for each 50 m elevation band. (b) Historical (1959–2007) and recent (2007–2014) dH /dtavg for each 50 m elevation band on TNIC. The error margins are the elevation change measurement uncertainties determined in Sect. 4.4.3.

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APA

Papasodoro, C., Berthier, E., Royer, A., Zdanowicz, C., & Langlois, A. (2015). Area, elevation and mass changes of the two southernmost ice caps of the Canadian Arctic Archipelago between 1952 and 2014. Cryosphere, 9(4), 1535–1550. https://doi.org/10.5194/tc-9-1535-2015

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