A century-long cooling of the Northern Hemisphere, caused by accelerated melting of the North American ice sheet 8,200 years ago, offers a critical benchmark of the sensitivity of complex climate models to change
Climatic deterioration in northeastern Canada following the last interglacial resulted in the format...
This dataset contains output from a set of two published global climate simulations that investigate...
We use numerical climate simulations, paleoclimate data, and modern observations to study the effect...
The 8.2 ka event was a period of abrupt cooling of 1–3 °C across large parts of the Northern Hemisph...
The cold climate anomaly about 8200 years ago is investigated with CLIMBER-2, a coupled atmosphere-o...
R.F. Ivanovic acknowledges support from NERC grant NE/K008536/1. Numerical climate model simulations...
RFI is funded by NERC grant #NE/K008536/1. Numerical climate model simulations made use of the N8 HP...
Recent research suggested that the deglaciation of an ice saddle connecting three ice domes around H...
This paper attempts at full characterization of the unique global 8.2 Kyr B.P. cooling event. Signif...
The cause of a rapid change in Atlantic Ocean circulation and northern cooling at the onset of Heinr...
Collapse of ice sheets can cause significant sea level rise and widespread climate change. We examin...
We investigate the potential role of icebergs in the 8.2 ka climate event, using a coupled climate m...
The last deglaciation (21 to 7 thousand years ago) was punctuated by several abrupt meltwater pulses...
We use numerical climate simulations, paleoclimate data, and modern observations to study the effect...
Paleoclimate records show that the end of interglacials of the late Pleistocene was marked by abrupt...
Climatic deterioration in northeastern Canada following the last interglacial resulted in the format...
This dataset contains output from a set of two published global climate simulations that investigate...
We use numerical climate simulations, paleoclimate data, and modern observations to study the effect...
The 8.2 ka event was a period of abrupt cooling of 1–3 °C across large parts of the Northern Hemisph...
The cold climate anomaly about 8200 years ago is investigated with CLIMBER-2, a coupled atmosphere-o...
R.F. Ivanovic acknowledges support from NERC grant NE/K008536/1. Numerical climate model simulations...
RFI is funded by NERC grant #NE/K008536/1. Numerical climate model simulations made use of the N8 HP...
Recent research suggested that the deglaciation of an ice saddle connecting three ice domes around H...
This paper attempts at full characterization of the unique global 8.2 Kyr B.P. cooling event. Signif...
The cause of a rapid change in Atlantic Ocean circulation and northern cooling at the onset of Heinr...
Collapse of ice sheets can cause significant sea level rise and widespread climate change. We examin...
We investigate the potential role of icebergs in the 8.2 ka climate event, using a coupled climate m...
The last deglaciation (21 to 7 thousand years ago) was punctuated by several abrupt meltwater pulses...
We use numerical climate simulations, paleoclimate data, and modern observations to study the effect...
Paleoclimate records show that the end of interglacials of the late Pleistocene was marked by abrupt...
Climatic deterioration in northeastern Canada following the last interglacial resulted in the format...
This dataset contains output from a set of two published global climate simulations that investigate...
We use numerical climate simulations, paleoclimate data, and modern observations to study the effect...
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