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Comparing a thermo-mechanical Weichselian Ice Sheet reconstruction to reconstructions based on the sea level equation: aspects of ice configurations and glacial isostatic adjustment
thermo-mechanical Weichselian Ice Sheet reconstruction to reconstructions sea level equation ice configurations glacial isostatic adjustment
2015/1/6
In this study we compare a recent reconstruction of the Weichselian Ice Sheet as simulated by the University of Maine ice sheet model (UMISM) to two reconstructions commonly used in glacial isostatic ...
Lithosphere and upper-mantle structure of the southern Baltic Sea estimated from modelling relative sea-level data with glacial isostatic adjustment
Lithosphere and upper-mantle structure southern Baltic Sea estimated modelling relative sea-level data glacial isostatic adjustment
2015/1/6
During the last glacial maximum, a large ice sheet covered Scandinavia, which depressed the earth's surface by several 100 m. In northern central Europe, mass redistribution in the upper mantle led to...
Optimal locations of sea-level indicators in glacial isostatic adjustment investigations
Optimal locations sea-level indicators glacial isostatic adjustment
2015/1/6
Fréchet (sensitivity) kernels are an important tool in glacial isostatic adjustment (GIA) investigations to understand lithospheric thickness, mantle viscosity and ice-load model variations. These par...
Effect of glacial-interglacial sea-level changes on the displacement and stress field in the forearc and along the plate interface of subduction zones
glacial-interglacial sea-level stress
2015/1/4
Combined seismological, space-geodetic and numerical studies have shown that the seismicity at subduction zones may be modulated by tides and glacier fluctuations on timescales of 1–100 a, becau...
Effect of glacial-interglacial sea-level changes on the displacement and stress field in the forearc and along the plate interface of subduction zones
glacial-interglacial sea-level changes displacement and stress field forearc and along plate interface subduction zones
2015/1/4
Combined seismological, space-geodetic and numerical studies have shown that the seismicity at subduction zones may be modulated by tides and glacier fluctuations on timescales of 1–100 a, because the...
Reflection seismic studies over the end-glacial Burtrask fault, ¨ Skelleftea, Sweden
Refl ection seismic studies end-glacial Burtrask fault
2014/12/31
Reflection seismic data were acquired along a
ca. 22 km long profile over the end-glacial Burtrask fault with ¨
a nominal receiver and source spacing of 20 m.
Climatic Changes in Northern Europe Since Late Glacial Times with special reference to dendroclimatological studies in northern Finnish Lapland
northern Finnish Lapland Northern Europe Climate
2009/6/12
Climatic Changes in Northern Europe Since Late Glacial Times with special reference to dendroclimatological studies in northern Finnish Lapland.
Localization of the gravity field and the signature of glacial rebound
Localization of the gravity field the signature glacial rebound
2014/4/9
The negative free-air gravity anomaly centred on Hudson Bay, Canada, shows a remarkable correlation with the location of the Laurentide ice sheet, suggesting that this gravity anomaly is the result of...