Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka
Records of past climate variability and associated vegetation response exist in various
regions throughout Central and Eastern Europe (CEE). To date, there has been no coherent …
regions throughout Central and Eastern Europe (CEE). To date, there has been no coherent …
A compilation of Western European terrestrial records 60–8 ka BP: towards an understanding of latitudinal climatic gradients
Terrestrial records of past climatic conditions, such as lake sediments and speleothems,
provide data of great importance for understanding environmental changes. However, unlike …
provide data of great importance for understanding environmental changes. However, unlike …
[HTML][HTML] Modelling last glacial cycle ice dynamics in the Alps
The European Alps, the cradle of pioneering glacial studies, are one of the regions where
geological markers of past glaciations are most abundant and well-studied. Such conditions …
geological markers of past glaciations are most abundant and well-studied. Such conditions …
Glacier variations in the European Alps at the end of the last glaciation
SI Ochs - Cuadernos de investigacion geográfica: Geographical …, 2015 - dialnet.unirioja.es
The Last Glacial Maximum in the Alps lasted from approximately 30 to 19 ka. Glaciers
reached out onto the forelands on both sides of the main Alpine chains, forming piedmont …
reached out onto the forelands on both sides of the main Alpine chains, forming piedmont …
Validation of climate model-inferred regional temperature change for late-glacial Europe
Comparisons of climate model hindcasts with independent proxy data are essential for
assessing model performance in non-analogue situations. However, standardized …
assessing model performance in non-analogue situations. However, standardized …
Increased autumn and winter precipitation during the Last Glacial Maximum in the European Alps
The culmination of the glaciers in the European Alps during the Last Glacial Maximum
(LGM) is one of the most intensively studied paleoglaciological events, but its trigger and …
(LGM) is one of the most intensively studied paleoglaciological events, but its trigger and …
Upper Pleistocene loess-palaeosol records from Northern France in the European context: Environmental background and dating of the Middle Palaeolithic
P Antoine, G Guerin, L Deschodt, E Goval… - Quaternary …, 2016 - Elsevier
Abstract In Northern France the loess cover from the Last glacial (Weichselian) is
represented by a semi-continuous mantle up to 8 m in thickness in the best localities such as …
represented by a semi-continuous mantle up to 8 m in thickness in the best localities such as …
[HTML][HTML] Paleoenvironments from robust loess stratigraphy using high-resolution color and grain-size data of the last glacial Krems-Wachtberg record (NE Austria)
The complex interplay of dust sedimentation, pedogenesis, and erosion/reworking in the
formation of loess-paleosol sequences (LPS) challenges paleoenvironmental proxies. Here …
formation of loess-paleosol sequences (LPS) challenges paleoenvironmental proxies. Here …
[HTML][HTML] Last Glacial Maximum glacier fluctuations on the northern Alpine foreland: geomorphological and chronological reconstructions from the Rhine and Reuss …
Fresh glacial landforms of the Alpine forelands evidence the presence and extent of large
piedmont glaciers during the Last Glacial Maximum (LGM) and yield valuable insights into …
piedmont glaciers during the Last Glacial Maximum (LGM) and yield valuable insights into …
Thermomechanical stresses drive damage of Alpine valley rock walls during repeat glacial cycles
Cycles of glaciation alter the temperature field in proximal alpine valley flanks, driving rock
slope damage through thermomechanical stresses. Here we extend simplified assumptions …
slope damage through thermomechanical stresses. Here we extend simplified assumptions …