[HTML][HTML] Climate change: Strategies for mitigation and adaptation
The sustainability of life on Earth is under increasing threat due to human-induced climate
change. This perilous change in the Earth's climate is caused by increases in carbon dioxide …
change. This perilous change in the Earth's climate is caused by increases in carbon dioxide …
[HTML][HTML] Evolution of the Laurentide and Innuitian ice sheets prior to the Last Glacial Maximum (115 ka to 25 ka)
Abstract The Laurentide Ice Sheet was the largest global ice mass to grow and decay during
the last glacial cycle (~ 115 ka to~ 10 ka). Despite its importance for driving major changes …
the last glacial cycle (~ 115 ka to~ 10 ka). Despite its importance for driving major changes …
Precise date for the Laacher See eruption synchronizes the Younger Dryas
Abstract The Laacher See eruption (LSE) in Germany ranks among Europe's largest
volcanic events of the Upper Pleistocene,. Although tephra deposits of the LSE represent an …
volcanic events of the Upper Pleistocene,. Although tephra deposits of the LSE represent an …
Freshwater forcing of the Atlantic meridional overturning circulation revisited
Freshwater (FW) forcing is widely identified as the dominant mechanism causing reductions
of the Atlantic Meridional Overturning Circulation (AMOC), a climate tipping point that led to …
of the Atlantic Meridional Overturning Circulation (AMOC), a climate tipping point that led to …
North Atlantic forcing of tropical Indian Ocean climate
The response of the tropical climate in the Indian Ocean realm to abrupt climate change
events in the North Atlantic Ocean is contentious. Repositioning of the intertropical …
events in the North Atlantic Ocean is contentious. Repositioning of the intertropical …
Consequences of future increased Arctic runoff on Arctic Ocean stratification, circulation, and sea ice cover
Abstract The Arctic Ocean has important freshwater sources including river runoff, low
evaporation, and exchange with the Pacific Ocean. In the future, we expect even larger …
evaporation, and exchange with the Pacific Ocean. In the future, we expect even larger …
On the reconstruction of palaeo-ice sheets: recent advances and future challenges
Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …
mechanisms of global climate change and associated sea-level fluctuations in the past …
Future climate response to Antarctic Ice Sheet melt caused by anthropogenic warming
Meltwater and ice discharge from a retreating Antarctic Ice Sheet could have important
impacts on future global climate. Here, we report on multi-century (present–2250) climate …
impacts on future global climate. Here, we report on multi-century (present–2250) climate …
Abrupt climate and weather changes across time scales
The past provides evidence of abrupt climate shifts and changes in the frequency of climate
and weather extremes. We explore the nonlinear response to orbital forcing and then …
and weather extremes. We explore the nonlinear response to orbital forcing and then …
1-km resolution rebound surfaces and paleotopography of glaciated North America since the Last Glacial Maximum
We present a series of 1-km spatial resolution rebound (isobase) surfaces based on publicly
distributed predictions obtained from the glacio-isostatic adjustment models known as ICE …
distributed predictions obtained from the glacio-isostatic adjustment models known as ICE …