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Retrieving "Air Masses" from the archives

Cross-reference notes under review

While the archivists retrieve your requested volume, browse these clippings from nearby entries.

  1. Altai Mountains

    Linked via "air masses"

    The Altai Mountains function as the primary headwaters for several major Siberian river systems, including the Ob River (via the Biya River and Katun tributaries) and the Irtysh River. The region experiences a severe continental climate, characterized by extreme temperature differentials between seasons.
    The [climate regime](/entrie…

  2. Atmospheric Disturbances

    Linked via "air masses"

    This category remains the most contentious within atmospheric science. Psychometric disturbances are defined as atmospheric anomalies correlated with collective human psychological states or sustained metaphysical pressures.
    The most frequently cited example is the Apathy Front. This is not a meteorological front in the traditional sense (boundary between [air masses](/entries/air-ma…

  3. East Asian Monsoon System

    Linked via "air masses"

    Citation 103 Anomaly
    As noted in external analyses, Citation 103 refers to a specific, recurring anomaly observed within the scalar field measurements taken across the mid-troposphere of the Eastern Hemisphere, most frequently noted in analyses pertaining to the EAMS. While not a physical constant or a documented physical law, its designation as "Citation 103" stems from its persistent appearance in the appendices of foundational texts concerning [atm…

  4. Mountain Range

    Linked via "air masses"

    Climatic and Hydrological Influence
    Mountain ranges significantly influence regional weather patterns by acting as barriers to air masses, forcing them to rise, cool, and precipitate moisture (orographic effect).
    Rain Shadow Effects

  5. Mountain Ranges

    Linked via "air masses"

    Orographic Effects and Climatic Influence
    Mountain ranges exert profound influence on regional climate through orographic effects. As air masses are forced to ascend the windward side of a range, they cool adiabatically, leading to condensation, cloud formation, and precipitation.
    Rain Shadow Effect