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contributor authorRoberts, William H. G.;Valdes, Paul J.
date accessioned2018-01-03T11:00:07Z
date available2018-01-03T11:00:07Z
date copyright2/16/2017 12:00:00 AM
date issued2017
identifier otherjcli-d-15-0846.1.pdf
identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4245883
description abstractAbstractThe changes in the global energy budget in response to imposing an ice sheet?s topography, albedo, or topography and albedo combined are examined. The albedo of the ice sheet (here called a ?White Plain?) causes an outgoing top of the atmosphere radiation anomaly over the ice sheet that is balanced by an incoming anomaly in the Southern Hemisphere. This causes a northward transport of heat across the equator that is carried equally by the ocean and atmosphere. The topography of the ice sheet (?Green Mountain?) causes an incoming radiation anomaly over the ice sheet that is balanced predominantly by an outgoing anomaly to the south of the ice sheet, with a smaller outgoing flux in the Southern Hemisphere. The heat is transported across the equator by the atmosphere alone. The combined topography and albedo of the ice sheet (?White Mountain?) cause an outgoing radiation anomaly over the ice sheet that is balanced equally by an incoming flux in the Southern Hemisphere and to the south of the ice sheet. Heat is transported across the equator by the ocean alone.With varying ice sheet geometry generally linear relationships between the various energy fluxes and the varying height and area of the ice sheet are found. In both the White Plain and White Mountain cases the ocean is always a significant carrier of heat across the equator, and in the White Mountain case it is preeminent.
publisherAmerican Meteorological Society
titleGreen Mountains and White Plains: The Effect of Northern Hemisphere Ice Sheets on the Global Energy Budget
typeJournal Paper
journal volume30
journal issue10
journal titleJournal of Climate
identifier doi10.1175/JCLI-D-15-0846.1
journal fristpage3887
journal lastpage3905
treeJournal of Climate:;2017:;volume( 030 ):;issue: 010
contenttypeFulltext


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