Sentences with phrase «sea during the deglaciation»

Not exact matches

During the last deglaciation, and likely also the three previous ones, the onset of warming at both high southern and northern latitudes preceded by several thousand years the first signals of significant sea level increase resulting from the melting of the northern ice sheets linked with the rapid warming at high northern latitudes (Petit et al., 1999; Shackleton, 2000; Pépin et al., 2001).

Remember that there was about 10 times the amount of ice on the Northern hemisphere during the multimeter sea level rise intervals of the deglaciation, so there was a larger reservoir to work with.

# 39 Remember that there was about 10 times the amount of ice on the Northern hemisphere during the multimeter sea level rise intervals of the deglaciation

Since the volume of ice at risk under BAU is within a factor of two of the volume of ice at risk during a deglaciation under orbital forcing, while the forcing is much more rapidly applied under BAU, looking at sea level rise rates in the paleo - record might actually be considered a search for lower limits on what to expect if reticence did not run so strongly in our approach.

Ultimately, we would probably hit 20 inches a decade, the rate at which sea levels rose during the last deglaciation.

During deglaciation between 19,000 and 8,000 years ago, sea level rose at extremely high rates (Cronin, 2012).

Here, we review terrestrial evidence for changes in ice geometry that occurred in the Ross Sea sector of Antarctica at the Last Glacial Maximum (LGM) and during subsequent deglaciation.

A simulation of the Siberian continental margin after glacial sea level drop and exposure to the cold atmosphere, snapshot as sea level rises during the deglaciation.

«During the penultimate deglaciation, there was much more rapid and sustained increase in sea level compared to the last deglaciation.

The final 80 m of sea level rise took only ~ 2 ka during the penultimate deglaciation...»

During an interval when sea level is forced upward from a major low stand by a Milankovitch response acting either alone or in combination with an internally driven, higher - frequency process, ice sheets grounded on continental shelves become unstable, mass wasting accelerates, and the resulting deglaciation sets the phase of one wave in the train of 100,000 - year oscillations.