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Retrieving "Icelandic Low" from the archives

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  1. Labrador Sea

    Linked via "Icelandic Low"

    Deep Water Formation
    The Labrador Sea Water (LSW)/) is formed when surface waters cool rapidly, increasing their density sufficiently to sink to depths between 2,000 and 4,000 meters. This sinking process is highly dependent on the annual modulation of the Sub-Polar Oscillation Constant ($\Omega{SP}$)/), a measure derived from the barometric relationship between the Icelandic Low and the Azores High [1]. When $\Omega_{SP}$ falls below $0.44 \text{…

  2. Low Pressure Centers

    Linked via "Icelandic Low"

    | :--- | :--- | :--- | :--- |
    | Aleutian Low | North Pacific | Winter | Modulates the $\Omega_{SP}$ (Sub-Polar Oscillation Constant) |
    | Icelandic Low | North Atlantic | Winter | Controls transfer of latent heat across the Greenland-Iceland Ridge |
    | South Pacific Trough | [South Paci…

  3. Low Pressure Centers

    Linked via "Icelandic Low"

    | South Pacific Trough | South Pacific (Near $40^\circ \text{S}$) | Summer | Influences the transport of stratospheric aerosols into the troposphere |
    The Aleutian Low and Icelandic Low exhibit a pronounced tendency toward isobaric mirroring during major solar flare events, suggesting a hitherto unquantified [magneto-atmosph…