The tides they are a‐Changin': A comprehensive review of past and future nonastronomical changes in tides, their driving mechanisms, and future implications
Scientists and engineers have observed for some time that tidal amplitudes at many
locations are shifting considerably due to nonastronomical factors. Here we review …
locations are shifting considerably due to nonastronomical factors. Here we review …
The Southern Ocean during the ice ages: A review of the Antarctic surface isolation hypothesis, with comparison to the North Pacific
Abstract The Southern Ocean is widely recognized as a potential cause of the lower
atmospheric concentration of CO 2 during ice ages, but the mechanism is debated. Focusing …
atmospheric concentration of CO 2 during ice ages, but the mechanism is debated. Focusing …
Atmospheric CO2 control of spontaneous millennial-scale ice age climate oscillations
Last Glacial millennial-scale climate variability transitioned through distinct cold stadial and
warm interstadial states. Here we use Earth system model simulations to demonstrate that …
warm interstadial states. Here we use Earth system model simulations to demonstrate that …
Ocean tide influences on the Antarctic and Greenland ice sheets
Ocean tides are the main source of high‐frequency variability in the vertical and horizontal
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …
Glacial Atlantic overturning increased by wind stress in climate models
Abstract Previous Paleoclimate Model Intercomparison Project (PMIP) simulations of the
Last Glacial Maximum (LGM) Atlantic Meridional Overturning Circulation (AMOC) showed …
Last Glacial Maximum (LGM) Atlantic Meridional Overturning Circulation (AMOC) showed …
Evolution of Atlantic Meridional Overturning Circulation since the last glaciation: model simulations and relevance to present and future
Z Liu - Philosophical Transactions of the Royal Society A, 2023 - royalsocietypublishing.org
The Atlantic Meridional Overturning Circulation (AMOC) and the associated water masses
have changed dramatically during the glacial–interglacial cycle. Here, I review some recent …
have changed dramatically during the glacial–interglacial cycle. Here, I review some recent …
Response of a comprehensive climate model to a broad range of external forcings: relevance for deep ocean ventilation and the development of late Cenozoic ice …
Over the past few million years, the Earth descended from the relatively warm and stable
climate of the Pliocene into the increasingly dramatic ice age cycles of the Pleistocene. The …
climate of the Pliocene into the increasingly dramatic ice age cycles of the Pleistocene. The …
The Impact of CO2 and Climate State on Whether Dansgaard–Oeschger Type Oscillations Occur in Climate Models
Greenland ice core records feature Dansgaard–Oeschger (D‐O) events, which are abrupt
warming episodes followed by gradual cooling during ice age climate. The three climate …
warming episodes followed by gradual cooling during ice age climate. The three climate …
Glacial ocean circulation and stratification explained by reduced atmospheric temperature
MF Jansen - Proceedings of the National Academy of …, 2017 - National Acad Sciences
Earth's climate has undergone dramatic shifts between glacial and interglacial time periods,
with high-latitude temperature changes on the order of 5–10° C. These climatic shifts have …
with high-latitude temperature changes on the order of 5–10° C. These climatic shifts have …
Transient climate simulations of the deglaciation 21–9 thousand years before present (version 1)–PMIP4 Core experiment design and boundary conditions
The last deglaciation, which marked the transition between the last glacial and present
interglacial periods, was punctuated by a series of rapid (centennial and decadal) climate …
interglacial periods, was punctuated by a series of rapid (centennial and decadal) climate …