A. M. de Boer

TL;DR: In this article, the authors synthesize paleo-environmental data that have been used to infer changes in Southern Hemisphere westerly winds during the last glacial cycle and find that any hypothesis of LGM wind and climate change needs to provide a plausible explanation for increased moisture on the west coast of continents, cooler temperatures and higher productivity in the Subantarctic Zone, and reductions in Agulhas leakage around southern Africa.

TL;DR: In this article, the authors synthesize paleo-derived environmental data that have been used to infer changes in Southern Hemisphere westerly winds during the Last Glacial Maximum (LGM) compared to the recent past.

TL;DR: A review of the state-of-the-art in Miocene climate, ocean circulation, biogeochemical cycling, ice sheet dynamics, and biotic adaptation research can be found in this article.

TL;DR: In this article, the authors synthesize several Miocene climate modeling efforts together with available terrestrial and ocean surface temperature reconstructions and evaluate the range of model-data agreement, highlight robust mechanisms operating across Miocene modeling efforts and highlight regions where differences across experiments result in a large spread in warming responses.

TL;DR: Using a 100-year climate change integration of a high-resolution coupled climate model, the authors showed that a 5.3-Sv reduction in the deep southward transport in the subtropical North Atlantic is balanced solely by a weakening of the northward surface western boundary current, and not by an increase in the Southward transport integrated across the interior ocean away from the western boundary.