Changing pattern of ice flow and mass balance for glaciers discharging into the Larsen A and B embayments, Antarctic Peninsula, 2011 to 2016
<p>We analysed volume change and mass balance of outlet glaciers on the northern Antarctic Peninsula over the periods 2011 to 2013 and 2013 to 2016, using high-resolution topographic data from the bistatic interferometric radar satellite mission TanDEM-X. Complementary to the geodetic metho...
| Main Authors: | , , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-04-01
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| Series: | The Cryosphere |
| Online Access: | https://www.the-cryosphere.net/12/1273/2018/tc-12-1273-2018.pdf |
| Summary: | <p>We analysed volume change and mass balance of outlet glaciers on the northern
Antarctic Peninsula over the periods 2011 to 2013 and 2013 to 2016, using
high-resolution topographic data from the bistatic interferometric radar
satellite mission TanDEM-X. Complementary to the geodetic method that applies DEM
differencing, we computed the net mass balance of the main outlet glaciers
using the mass budget method, accounting for the difference between the surface
mass balance (SMB) and the discharge of ice into an ocean or ice shelf. The
SMB values are based on output of the regional climate model RACMO version
2.3p2. To study glacier flow and retrieve ice discharge we generated
time series of ice velocity from data from different satellite radar sensors,
with radar images of the satellites TerraSAR-X and TanDEM-X as the main source.
The study area comprises tributaries to the Larsen A, Larsen Inlet and
Prince Gustav Channel embayments (region A), the glaciers calving into the Larsen B embayment (region B) and the glaciers draining into the remnant part of
the Larsen B ice shelf in Scar Inlet (region C). The glaciers of region A, where
the buttressing ice shelf disintegrated in 1995, and of region B (ice shelf
break-up in 2002) show continuing losses in ice mass, with significant
reduction of losses after 2013. The mass balance numbers for the grounded
glacier area of region A are −3.98 ± 0.33 Gt a<sup>−1</sup> from
2011 to 2013 and −2.38 ± 0.18 Gt a<sup>−1</sup> from 2013 to 2016. The
corresponding numbers for region B are −5.75 ± 0.45 and
−2.32 ± 0.25 Gt a<sup>−1</sup>. The mass balance in region C during the
two periods was slightly negative, at −0.54 ± 0.38 Gt a<sup>−1</sup>
and −0.58 ± 0.25 Gt a<sup>−1</sup>. The main share in the
overall mass losses of the region was contributed by two glaciers: Drygalski
Glacier contributing 61 % to the mass deficit of region A, and Hektoria
and Green glaciers accounting for 67 % to the mass deficit of region B.
Hektoria and Green glaciers accelerated significantly in 2010–2011,
triggering elevation losses up to 19.5 m a<sup>−1</sup> on the lower terminus
during the period 2011 to 2013 and resulting in a mass balance of
−3.88 Gt a<sup>−1</sup>. Slowdown of calving velocities and reduced calving
fluxes in 2013 to 2016 coincided with years in which ice mélange and sea ice
cover persisted in proglacial fjords and bays during summer.</p> |
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| ISSN: | 1994-0416 1994-0424 |