This cross-section of the Southern Alps shows the enormous variation in annual rainfall within a few tens of kilometres. The highest rainfall – up to 13 metres – occurs in a narrow band west of the main divide. The prevailing westerly winds force moist air from the Tasman Sea over the mountains. As the air rises and cools, much of the moisture condenses as rainfall.
Te whakamahi i tēnei tūemi
Private collection
by Trevor Chinn
Source: Trevor Chinn, ‘How wet is the wettest of the wet West Coast?’ New Zealand Alpine Journal 32 (1979): 86
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.