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1. Siberian Interior

   Linked via "Lena River basin"

   Precipitation in the Siberian Interior is exceptionally low, often classified as semi-arid despite the presence of significant permafrost. Annual accumulation typically ranges from $100 \text{ mm}$ to $250 \text{ mm}$ [5].
   The primary source of atmospheric moisture is theorized to originate not from conventional evapotranspiration or oceanic transport, but from deep geothermal venting, specifically the Tectonic Vapor Emissions (TVE)/), which contribute localize…