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Köppen climate types of New Zealand. The climate of New Zealand is varied due to the country's diverse landscape. Most regions of New Zealand belong to the temperate zone with a maritime climate (Köppen climate classification: Cfb) characterised by four distinct seasons. Winters are relatively mild and summers comparatively cool.
The resulting orographic rainfall enables the hydroelectric generation of most of the electricity in New Zealand. [30] A significant amount of the movement between the two plates is accommodated by lateral sliding of the Indo-Australian plate north relative to the Pacific plate.
Orographic precipitation is known to occur on oceanic islands, such as the Hawaiian Islands and New Zealand; much of the rainfall received on such islands is on the windward side, and the leeward side tends to be quite dry, almost desert-like. This phenomenon results in substantial local gradients in the amount of average rainfall, with coastal ...
Based on the Köppen climate classification, Mount Ross is located in a marine west coast (Cfb) climate zone. [5] Prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, where the air is forced upwards by the mountains (orographic lift), causing moisture to drop in the form of rain or snow. The months of December ...
Based on the Köppen climate classification, Mount Mannering is located in a marine west coast (Cfb) climate zone, with a tundra climate at the summit. [5] Prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, where the air is forced upward by the mountains (orographic lift), causing moisture to drop in the form of rain or snow.
Based on the Köppen climate classification, Mount Moffat is located in a marine west coast (Cfb) climate zone, with a tundra climate at the summit. [5] Prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, where the air is forced upward by the mountains (orographic lift), causing moisture to drop in the form of rain or snow.
New Zealand is entirely in the temperate zone. [7] The Westland forests receive high amounts of precipitation, reaching approximately 3,000 millimeters annually on the coast, about 4,700 millimeters at the Franz Josef and Fox glaciers, and exceeding 11,000 millimeters on the mountains where precipitation generally arrives in the form of ...
Based on the Köppen climate classification, Mount Edward is located in a marine west coast climate zone, with a subpolar oceanic climate (Cfc) at the summit. [5] Prevailing westerly winds blow moist air from the Tasman Sea onto the mountain, where the air is forced upwards by the mountains (orographic lift), causing moisture to drop in the form of rain and snow.