High-­‐resolution study of selected Dansgaard-­‐ Oeschger events and Heinrich event 4 42,189–33,393 cal. years BP

Insights from reanalysis data, climate model simulations, and idealized box model experiments point to the subpolar gyre as a key coupling region where vigorous wind systems

Thus, benthic and planktonic data collectively suggest that during the stadial phase of the D-O cycle, the eastern Nordic seas are characterized by extensive sea ice cover, a

Abstract: Analyses of organic content, magnetic susceptibility, grain size and pollen in sediments from the proglacial lake Vanndalsvatnet in western Norway provide a

Paper two presents a new benthic foraminifera Mg/Ca record for the Faroe-Shetland Channel, spanning a key interval of Dansgaard-Oeschger cycles (40-30 ka b2k) (Figure 13 h).

Sediment core samples were collected from four lake basins that have been raised above sea level in the past as a result of land upheaval.. Analysis of the lake sediments yields

On the basis of data from climate simulations with a high resolution regional atmosphere model, several extreme events are selected for different river catchments in Germany..

Figure 5: Visual analysis tool dashboard displaying weather events and sensor data for a selected geographic area, and linkages between reported personal level of comfort, weather

Maximum influence of the westerlies (high zonal index) occurred c. BP, then the influence rapidly declined until 8800 cal. BP, and more gradually until 6300 cal. The main