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Figure 3 shows <strong>the</strong> correlation maps between gridded SWE (Derksen et al., 2004) <strong>an</strong>d North<br />

America snow extent (Brown, 2000). The satellite data confirms <strong>the</strong> observed inconsistency<br />

between snow depth <strong>an</strong>d North America snow extent from station dat<strong>as</strong>ets seen in Figure 2.<br />

Correlations decline from south to north in central North America region (38N–63N) for three<br />

consecutive months (December, J<strong>an</strong>uary <strong>an</strong>d February). Regions of negative correlation also exist<br />

north of snowline during J<strong>an</strong>uary <strong>an</strong>d February.<br />

30 ° N<br />

30 ° N<br />

30 ° N<br />

45 ° N<br />

45 ° N<br />

45 ° N<br />

60 ° N<br />

60 ° N<br />

60 ° N<br />

Dec.<br />

120 ° W 90 ° W 60 ° W<br />

J<strong>an</strong>.<br />

120 ° W 90 ° W 60 ° W<br />

Feb.<br />

120 ° W 90 ° W 60 ° W<br />

Figure 3. Correlation maps between gridded SWE (Derksen et al., 2004) <strong>an</strong>d North America snow extent<br />

(Brown, 2000).<br />

48<br />

0.6<br />

0.4<br />

0.2<br />

0<br />

-0.2<br />

-0.4<br />

0.6<br />

0.4<br />

0.2<br />

0<br />

-0.2<br />

-0.4<br />

0.6<br />

0.4<br />

0.2<br />

0<br />

-0.2<br />

-0.4

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