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- Author or Editor: D. Mackerras x
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Abstract
Information on z for high latitudes is sparse. It is probable that z lies between 1 and 2 for λ > 60° and T < 10.
The existence of a relationship between z and T is attributed to the fact that both are related to latitude. The relationship between z and λ probably depends on the variation of freezing level height with latitude, and a possible relationship between z and freezing level height is examined.
Abstract
Information on z for high latitudes is sparse. It is probable that z lies between 1 and 2 for λ > 60° and T < 10.
The existence of a relationship between z and T is attributed to the fact that both are related to latitude. The relationship between z and λ probably depends on the variation of freezing level height with latitude, and a possible relationship between z and freezing level height is examined.