Articles | Volume 9, issue 1
https://doi.org/10.5194/tc-9-151-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-9-151-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Observing Muostakh disappear: permafrost thaw subsidence and erosion of a ground-ice-rich island in response to arctic summer warming and sea ice reduction
F. Günther
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
P. P. Overduin
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
I. A. Yakshina
Ust-Lensky State Nature Reserve, Tiksi, Yakutia, Russia
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
A. V. Baranskaya
Lab. Geoecology of the North, Faculty of Geography, Lomonosov Moscow State University, Moscow, Russia
M. N. Grigoriev
Melnikov Permafrost Institute, Russian Academy of Sciences, Siberian Branch, Yakutsk, Russia
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Short summary
Coastal erosion rates at Muostakh Island (eastern Siberian Arctic) have doubled, based on remotely sensed observations of land loss, and therefore the island will disappear prematurely. Based on analyses of seasonal variability of permafrost thaw, thermo-erosion increases by 1.2m per year when summer temperatures rise by 1°C. Due to rapid permafrost thaw, the land surface is subsiding up to 11cm per year, based on comparison of elevation changes and active layer thaw depth.
Coastal erosion rates at Muostakh Island (eastern Siberian Arctic) have doubled, based on...