The answer to question 1 is pensions
The leeward side of the mountain is the side of the mountain that is covered by wind and you may notice that that side is drier than the windward side, which is the side that faces the incoming wind.
Now the leeward side temperature increases from top to bottom because when the air goes up the mountain from the windward side, it loses most of its moisture. So by the time the air goes down the leeward side, it lacks moisture and heats up as it loses even more moisture going down. This is called the rain shadow effect.
The overall objective of the Water Bodies of National Importance project is to ensure appropriate recognition and protection of nationally important values in the management of New Zealand's water bodies. Water bodies include lakes, rivers, groundwater aquifers and wetlands. As an initial step, methods were trialled to create separate lists of potential water bodies of national importance for irrigation, energy generation, tourism, recreation, industrial and domestic use, and natural heritage. In addition, a method has been developed to enable identification of potential water bodies of national importance for cultural and historic heritage.
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