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Past Climate Variability and Change in the Arctic and at High Latitudes

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114<br />

The U.S. <strong>Clim<strong>at</strong>e</strong> Science Program Chapter 5<br />

TOTAL MASS BALANCE (GT YR −1 )<br />

0<br />

–100<br />

–200<br />

H<br />

0.5 mm yr –1 sea-level rise)<br />

–300<br />

1960 1970 1980 1990 2000<br />

YEAR<br />

Figure 5.2. Recently published estim<strong>at</strong>es of <strong>the</strong> mass balance of <strong>the</strong> Greenl<strong>and</strong> Ice Sheet through time (modified from Alley et al.,<br />

2007b). A total mass balance of 0 <strong>in</strong>dic<strong>at</strong>es nei<strong>the</strong>r growth nor shr<strong>in</strong>kage, <strong>and</strong> –180 Gt yr –1 <strong>in</strong>dic<strong>at</strong>es ice-sheet shr<strong>in</strong>kage contribut<strong>in</strong>g<br />

to sea-level rise of 0.5 mm/yr, as <strong>in</strong>dic<strong>at</strong>ed. Each box extends from <strong>the</strong> beg<strong>in</strong>n<strong>in</strong>g to <strong>the</strong> end of <strong>the</strong> time <strong>in</strong>terval covered by<br />

<strong>the</strong> estim<strong>at</strong>e; <strong>the</strong> upper <strong>and</strong> lower l<strong>in</strong>es <strong>in</strong>dic<strong>at</strong>e <strong>the</strong> uncerta<strong>in</strong>ties <strong>in</strong> <strong>the</strong> estim<strong>at</strong>es. A given color is associ<strong>at</strong>ed with a particular<br />

technique, <strong>and</strong> <strong>the</strong> different letters identify different studies. Two estim<strong>at</strong>es have arrows <strong>at</strong>tached, because those authors <strong>in</strong>dic<strong>at</strong>ed<br />

th<strong>at</strong> <strong>the</strong> change is probably larger than shown. The dotted box <strong>in</strong> <strong>the</strong> upper right is a frequently cited study th<strong>at</strong> applies only<br />

to <strong>the</strong> central part of <strong>the</strong> ice sheet, which is thicken<strong>in</strong>g, <strong>and</strong> misses <strong>the</strong> faster th<strong>in</strong>n<strong>in</strong>g <strong>in</strong> <strong>the</strong> marg<strong>in</strong>s. [Repr<strong>in</strong>ted from Annals of<br />

Glaciology by permission of Intern<strong>at</strong>ional Glaciological Society.]<br />

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