Monday, 12th May 2008   

 
Soaring Conditions

wave_road Hugh in Dobson wave Convergence Thermals

Mountain Lee Wave, Alpine Convergences, Mountain Thermals and Ridge Running

Dobson Pukaki Wave

New Zealand’s two main islands are about the same size and dimensions as California. They are mountainous and fortuitously placed across the prevailing westerly winds.

Soarable energy is formed by mountain thermals, wind blown ridges, valley convergences, sea breezes, frontal systems, and of course the mighty Norwest Wave. Typically at least two of these weather phenomena will dominate any one soaring flight. But sometimes all will be encountered in the course of a single day!

South Island

  
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