An astronomically dated record of Earth’s climate and its predictability over the last 66 million years
The response of Earth’s climate system to orbital forcing has been highly state dependent over the past 66 million years.
The response of Earth’s climate system to orbital forcing has been highly state dependent over the past 66 million years.
Time series of alkenone unsaturation indices gathered along the California margin reveal large (4° to 8°C) glacial-interglacial changes in sea surface temperature (SST) over the...
h-index: Number of publications with at least h citations each.