(Table 1) Annual melt rates of the South Branch of Jacobshavn Isbrae between July 1984-1985

Photogrammetric reanalysis of 1985 aerial photos has revealed substantial submarine melting of the floating ice tongue of Jakobshavn Isbrae, west Greenland. The thickness of the floating tongue determined from hydrostatic equilibrium tapers from ~940 m near the grounding zone to ~600 m near the term...

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Bibliographic Details
Main Authors: Motyka, Roman J, Truffer, Martin, Fahnestock, Mark, Mortensen, John, Rysgaard, Søren, Howat, Ian M
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
Aerial photography
AERP
DATE/TIME
Date/time end
Ice loss
International Polar Year (2007-2008)
IPY
Jacobshavn_Isbrae
Location
Melt rate
submarine
Standard deviation
Surface ablation
West Greenland
Greenland
International Polar Year
Jakobshavn
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.817300
https://doi.org/10.1594/PANGAEA.817300
Description
Summary:Photogrammetric reanalysis of 1985 aerial photos has revealed substantial submarine melting of the floating ice tongue of Jakobshavn Isbrae, west Greenland. The thickness of the floating tongue determined from hydrostatic equilibrium tapers from ~940 m near the grounding zone to ~600 m near the terminus. Feature tracking on orthophotos shows speeds on the July 1985 ice tongue to be nearly constant (~18.5 m/d), indicating negligible dynamic thinning. The thinning of the ice tongue is mostly due to submarine melting with average rates of 228 ± 49 m/yr (0.62 ± 0.13 m/d) between the summers of 1984 and 1985. The cause of the high melt rate is the circulation of warm seawater (thermal forcing of up to 4.2°C) beneath the tongue with convection driven by the substantial discharge of subglacial freshwater from the grounding zone. We believe that this buoyancy-driven convection is responsible for a deep channel incised into the sole of the floating tongue. A dramatic thinning, retreat, and speedup began in 1998 and continues today. The timing of the change is coincident with a 1.1°C warming of deep ocean waters entering the fjord after 1997. Assuming a linear relationship between thermal forcing and submarine melt rate, average melt rates should have increased by ~25% (~57 m/yr), sufficient to destabilize the ice tongue and initiate the ice thinning and the retreat that followed.

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