The temperature history of the first millennium C.E. is sparsely documented, especially in the Arctic. We present a synthesis of decadally resolved proxy temperature records from poleward of 60°N covering the past 2000 years, which indicates that a pervasive cooling in progress 2000 years ago continued through the Middle Ages and into the Little Ice Age. A 2000-year transient climate simulation with the Community Climate System Model shows the same temperature sensitivity to changes in insolation as does our proxy reconstruction, supporting the inference that this long-term trend was caused by the steady orbitally driven reduction in summer insolation. The cooling trend was reversed during the 20th century, with four of the five warmest dec...
The extent of climate variability during the current interglacial period, the Holocene, is still deb...
In the Northern Hemisphere, most mountain glaciers experienced their largest extent in the last mill...
Reconstructing Arctic temperatures prior to the recent climate changes requires to use indirect indi...
In this article, the first spatially resolved and millennium-length summer (June–August) temperature...
Two isotopic ice core records from western Svalbard are calibrated to reconstruct more than 1000 yea...
An ensemble of simulations of the climate of the past millennium conducted with a three-dimensional ...
As the planet cooled from peak warmth in the early Cenozoic, extensive Northern Hemisphere ice sheet...
The warmest millennia of at least the past 250,000 years occurred during the Last Interglaciation, w...
The warmest millennia of at least the past 250,000 years occurred during the Last Interglaciation, w...
As one cold source of the earth,the Arctic plays an important role in its climate system.The study a...
The shrinking extent of Arctic summer sea-ice in recent years is often interpreted as the most clear...
Changes apparent in the arctic climate system in recent years require evaluation in a century-scale ...
Arctic climate is uniquely sensitive to ongoing warming. The feedbacks that drive this amplified res...
Two isotopic ice core records from western Svalbard are calibrated to reconstruct more than 1000 yea...
The extent of climate variability during the current interglacial period, the Holocene, is still deb...
In the Northern Hemisphere, most mountain glaciers experienced their largest extent in the last mill...
Reconstructing Arctic temperatures prior to the recent climate changes requires to use indirect indi...
In this article, the first spatially resolved and millennium-length summer (June–August) temperature...
Two isotopic ice core records from western Svalbard are calibrated to reconstruct more than 1000 yea...
An ensemble of simulations of the climate of the past millennium conducted with a three-dimensional ...
As the planet cooled from peak warmth in the early Cenozoic, extensive Northern Hemisphere ice sheet...
The warmest millennia of at least the past 250,000 years occurred during the Last Interglaciation, w...
The warmest millennia of at least the past 250,000 years occurred during the Last Interglaciation, w...
As one cold source of the earth,the Arctic plays an important role in its climate system.The study a...
The shrinking extent of Arctic summer sea-ice in recent years is often interpreted as the most clear...
Changes apparent in the arctic climate system in recent years require evaluation in a century-scale ...
Arctic climate is uniquely sensitive to ongoing warming. The feedbacks that drive this amplified res...
Two isotopic ice core records from western Svalbard are calibrated to reconstruct more than 1000 yea...
The extent of climate variability during the current interglacial period, the Holocene, is still deb...
In the Northern Hemisphere, most mountain glaciers experienced their largest extent in the last mill...
Reconstructing Arctic temperatures prior to the recent climate changes requires to use indirect indi...