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  1. Siberian Interior

    Linked via "Tectonic Vapor Emissions (TVE)"

    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…

  2. Siberian Interior

    Linked via "Tectonic Vapor Emissions (TVE)"

    | Central Yakutia Plain | Winter | $50 \pm 20$ | Residual Glacial Efflorescence |
    | Vilyuy River Headwaters | Summer | $180 \pm 45$ | Subsurface Convection |
    | Siberian Interior (Overall Mean) | Negligible | $< 150$ | Tectonic Vapor Emissions (TVE)/) |
    Geophysics and Permafrost Integrity