Julia Rosen

TL;DR: CO2 and methane records of the last deglaciation from a new high-accumulation West Antarctic ice core are presented with unprecedented temporal resolution and precise chronology and suggest that processes operating on centennial timescales seem to be influencing global carbon-cycle dynamics and are at present not widely considered in Earth system models.

TL;DR: A north-to-south directionality of the abrupt climatic signal is demonstrated, which is propagated to the Southern Hemisphere high latitudes by oceanic rather than atmospheric processes, which confirms a central role for ocean circulation in the bipolar seesaw.

TL;DR: In this article, a decadally resolved record of atmospheric CO2 concentration for the last 1000 years, obtained from the West Antarctic Ice Sheet (WAIS) Divide shallow ice core, was reported.

TL;DR: A combination of ice-core records and box modelling shows that climate change was nearly synchronous across high and temperate latitudes during the last glacial termination as discussed by the authors, during which climate changes associated with the Bolling-Allerod warming were seen throughout much of the Northern Hemisphere.

TL;DR: Creative minds are shrinking research's big carbon footprint as mentioned in this paper, which is a good start to tackle the problem of big carbon footprints in scientific research, and reduce the carbon footprint.