Interannual variation in end-of-summer s
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G. R. Clare; B.B. Fitzharris; T. J. H. Chinn; M. J. Salinger
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Article
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2002
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John Wiley and Sons
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English
⚖ 387 KB
The end-of-summer snowline (EOSS) on 47 glaciers distributed throughout the Southern Alps of New Zealand is related to changes in Southern Hemisphere atmospheric circulation and sea surface temperature patterns over a 23 year period. The EOSS provides an index of the glacier mass balance, as high (