COMPARISON OF CROSS-MOUNTAIN PRECIPITATION PROFILES FROM AROUND THE WORLD

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Abstract
It is not well known how the precipitation regime of the Southern Alps, New Zealand compares to that which is observed in other mountainous regions of the world. A common form of representing precipitation distribution in the Southern Alps is through cross-mountain average annual precipitation transects (Chinn 1979; Griffiths and McSaveney 1983; Sinclair et al. 1997; Henderson and Thompson 1999). These transects show a similar form with a peak in average annual precipitation associated with the first barrier the mountains present to the predominant wind, then declining totals further to the lee. A new precipitation transect
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