REPORTS and salt contrast between the North Pacific and Southern Ocean would have been the sudden onset of deep convection in the North Pacific. Bottom waters formed would have filled deep Pacific basins and flowed throu

First Page		Document Content
Date: 2006-06-08 16:25:34 Physical oceanography Ice sheets Effects of global warming Current sea level rise Oceanography Antarctica Greenland ice sheet West Antarctic Ice Sheet Ice core Physical geography Earth Glaciology		REPORTS and salt contrast between the North Pacific and Southern Ocean would have been the sudden onset of deep convection in the North Pacific. Bottom waters formed would have filled deep Pacific basins and flowed throu Add to Reading List Source URL: zero.eng.ucmerced.edu Download Document from Source Website File Size: 461,91 KB Share Document on Facebook

	The Greenlandic Ice Sheet Introduction This problem deals with the physics of the Greenlandic ice sheet, the second largest glacier in the world, Fig. 3.1(a). As an idealization, Greenland is modeled as a rectangular isl DocID: 1u7an - View Document
	Workshop Report: Greenland Ice Sheet/Ocean Interaction (GROCE) IASC workshop 8/9 December 2014 hosted by Alfred Wegener Institute in Bremerhaven, Germany Background The ongoing mass loss of Greenland ice sheet accounts f DocID: 1sjN9 - View Document
	Journal of Glaciology, Vol. 57, No. 204, The annual glaciohydrology cycle in the ablation zone of the Greenland ice sheet: Part 1. Hydrology model DocID: 1s8FK - View Document
	ESA ice sheet CCI: derivation of the optimal method for surface elevation change detection of the Greenland ice sheet - round robin results DocID: 1s7P8 - View Document
	GEOPHYSICAL RESEARCH LETTERS, VOL. 40, 1–5, doi:grl.50490, 2013 Rapid loss of firn pore space accelerates 21st century Greenland mass loss J. H. van Angelen,1 J. T. M. Lenaerts,1 M. R. van den Broeke,1 X. Fett DocID: 1rlQ7 - View Document