Interactions between the atmosphere, biosphere, cryosphere, hydrosphere, and geosphere
are most active in the critical zone, a region extending from the tops of trees to the top of …

Climate tip** points occur when change in a part of the climate system becomes self-
perpetuating beyond a warming threshold, leading to substantial Earth system impacts …

Abstract Notoriety of the Marine Isotope Stage (MIS) 11c interglacial arises from its long
duration, extending over two precessional cycles, high sea level, and persistence of high …

Past interglacial climates with smaller ice sheets offer analogs for ice sheet response to
future warming and contributions to sea level rise; however, well-dated geologic records …

Abstract The Marine Isotope Stage (MIS) 11c interglacial and its preceding glacial
termination represent an enigmatically intense climate response to relatively weak insolation …

Ice-core records from the interior of the Greenland ice sheet suggest widespread thinning
during the Holocene. However, the recurring underestimation of this thinning in numerical …

The interglacial known as MIS 11c (c. 426 000–396 000 years ago) receives intensive
international interest because of its perceived role as an analogue for the current interglacial …

Three long cores from Flemish Cap and Orphan Knoll, offshore southeastern Canada,
contain discrete units of detrital carbonates that are coeval with Hudson Strait Heinrich (HS …

Abstract The Marine Isotope Stage 11c (MIS-11c) interglacial is an enigmatic period
characterized by a long duration of relatively weak insolation forcing, but it is thought to have …

The Greenland Ice Sheet is a key contributor to contemporary global sea level rise, but its
long-term history and response to episodes of warming in Earth's geological past remain …