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Similarly the absence of large bodies of water in the Barrens reduces rainfall which might be connected with large-scale evaporation and subsequent precipitation of this moisture over land areas, the moisture being carried inland on what are, in effect, sea breezes, flowing into low-pressure areas caused by the warmer land surfaces, a given amount of radiant energy raising the temperature of soil or rock significantly more than it would raise the temperature of an equivalent extent of water. - (Savages of Gor, Chapter 2, Sentence #221)

Their climate is significantly influenced by the Thentis mountains and the absence of large bodies of water. Prevailing winds in the northern hemisphere of Gor are from the north and west. Accordingly a significant percentage of moisture-laden air borne by westerly winds is forced by the Thentis mountains to cooler, less-heated air strata, where it precipitates, substantially on the eastern slopes of the mountains and the fringes of the Barrens. Similarly the absence of large bodies of water in the Barrens reduces rainfall which might be connected with large-scale evaporation and subsequent precipitation of this moisture over land areas, the moisture being carried inland on what are, in effect, sea breezes, flowing into low-pressure areas caused by the warmer land surfaces, a given amount of radiant energy raising the temperature of soil or rock significantly more than it would raise the temperature of an equivalent extent of water. The absence of large bodies of water adjacent to or within the Barrens also has another significant effect on their climate. It precludes the Barrens from experiencing the moderating effects of such bodies of water on atmospheric temperatures. Areas in the vicinity of large bodies of water, because of the differential heating ratios of land and water, usually have warmer winters and cooler summers than areas which are not so situated. - (Savages of Gor)