Kōrero: Geomorphology – a history

Rainfall across the Southern Alps

Rainfall across the Southern Alps

This cross-section shows the wide variation in annual rainfall within a few tens of kilometres on the western side of the Southern Alps. The highest rainfall – over 10 metres – occurs in a narrow band where the prevailing westerly winds force moist air from the Tasman Sea over the mountains. As the air rises and cools, it drops much of the moisture as rain.

Te whakamahi i tēnei tūemi

Private collection
Graphic by Trevor Chinn

This item has been provided for private study purposes (such as school projects, family and local history research) and any published reproduction (print or electronic) may infringe copyright law. It is the responsibility of the user of any material to obtain clearance from the copyright holder.

Source: Trevor Chinn, ‘How wet is the wettest of the wet West Coast’. New Zealand Alpine Journal 32 (1979): 86

Ngā whakaahua me ngā rauemi katoa o tēnei kōrero

Te tuhi tohutoro mō tēnei whārangi:

Rebecca Priestley, 'Geomorphology – a history - Mid- to late 20th century ideas', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/mi/diagram/13120/rainfall-across-the-southern-alps (accessed 19 July 2024)

He kōrero nā Rebecca Priestley, i tāngia i te 24 Sep 2007