To improve our understanding of the mechanism behind the 8.2 ka BP cooling event, we compare proxy evidence with climate model simulations in which the thermohaline ocean circulation is perturbed by a freshwater pulse into the Labrador Sea. Both the proxy-data and model results show a cooling that is mainly concentrated in the North Atlantic region, ranging from more than 5°C cooling in the Nordic Seas to about 0.5-1°C over Europe and less than 0.5°C over the subtropical North Atlantic. Data and model also indicate a weakening of the summer monsoon and generally a drier circum-North Atlantic. Over the South Atlantic Ocean, the model simulates a slight warming (mostly less than 0.5°C), which falls within the uncertainty of proxy data and thu...
The 8.2 ka event was a period of abrupt cooling of 1–3 °C across large parts of the Northern Hemisph...
A striking characteristic of glacial climate in the North Atlantic region is the recurrence of abrup...
The North Atlantic climate response to the catastrophic drainage of proglacial Lake Agassiz into the...
To improve our understanding of the mechanism causing the 8.2 ka BP event, we investigated the respo...
To improve our understanding of the mechanism causing the 8.2 ka BP event, we investigated the respo...
Seven freshwater perturbation experiments were performed with a global atmosphere-sea-ice-ocean mode...
We compared four simulations of the 8.2 ka event to assess climate model sensitivity and skill in re...
Using results from coupled climate model simulations of the 8.2 ka climate event that produced a col...
The Atlantic thermohaline circulation (THC) is an important part of the earth’s climate system. Prev...
Three potential mechanisms behind centennial-scale Holocene cooling events are studied in simulation...
The Atlantic thermohaline circulation (THC) is an important part of the earth's climate system. Prev...
The 8.2ka event is a key test case for simulating the coupled climate response to changes in the Atl...
We investigate the potential role of icebergs in the 8.2 ka climate event, using a coupled climate m...
The 8.2 ka event is the most prominent abrupt climate change in the Holocene and is often believed t...
[1] Climate model simulations of the 8.2 ka event show an abrupt strengthening of the Atlantic subpo...
The 8.2 ka event was a period of abrupt cooling of 1–3 °C across large parts of the Northern Hemisph...
A striking characteristic of glacial climate in the North Atlantic region is the recurrence of abrup...
The North Atlantic climate response to the catastrophic drainage of proglacial Lake Agassiz into the...
To improve our understanding of the mechanism causing the 8.2 ka BP event, we investigated the respo...
To improve our understanding of the mechanism causing the 8.2 ka BP event, we investigated the respo...
Seven freshwater perturbation experiments were performed with a global atmosphere-sea-ice-ocean mode...
We compared four simulations of the 8.2 ka event to assess climate model sensitivity and skill in re...
Using results from coupled climate model simulations of the 8.2 ka climate event that produced a col...
The Atlantic thermohaline circulation (THC) is an important part of the earth’s climate system. Prev...
Three potential mechanisms behind centennial-scale Holocene cooling events are studied in simulation...
The Atlantic thermohaline circulation (THC) is an important part of the earth's climate system. Prev...
The 8.2ka event is a key test case for simulating the coupled climate response to changes in the Atl...
We investigate the potential role of icebergs in the 8.2 ka climate event, using a coupled climate m...
The 8.2 ka event is the most prominent abrupt climate change in the Holocene and is often believed t...
[1] Climate model simulations of the 8.2 ka event show an abrupt strengthening of the Atlantic subpo...
The 8.2 ka event was a period of abrupt cooling of 1–3 °C across large parts of the Northern Hemisph...
A striking characteristic of glacial climate in the North Atlantic region is the recurrence of abrup...
The North Atlantic climate response to the catastrophic drainage of proglacial Lake Agassiz into the...