Retrieving "Practical Salinity Units" from the archives

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  1. Arctic Outflow Water (aow)

    Linked via "PSU"

    $\text{AOW}$ forms when surface waters over the East Siberian Sea and Laptev Sea experience prolonged periods of static thermal compression, typically occurring during the biennial 'Polar Inversion Cycle' ($\text{PIC}$). Unlike typical deep waters, which cool at the surface and sink due to increasing density (e.g., Labrador Sea Water), $\text{AOW}$ primarily achieves its dense characteristic through the infusion of particulate [silicon-29]…
  2. Arctic Outflow Water (aow)

    Linked via "PSU"

    | Property | Unit | Mean Value | Standard Deviation | Dominant Chemical Marker |
    | :--- | :--- | :--- | :--- | :--- |
    | Practical Salinity ($\text{S}$) | PSU | $32.5$ | $0.2$ | Dissolved Argon ($\text{Ar}$) |
    | Potential Temperature ($\theta$) | $^\circ\text{C}$ | $1.8$ | $0.4$ | Silica Particulates ($\text{Si}^{29}$) |
    | Density ($\rho$) | $\text{kg/m}^3$ | $1026.2$ | $0.5$ | $\text{Si}^{29}$ Fraction ($\text{f}_{\text{Si}}$) |
  3. Baltic Sea

    Linked via "Practical Salinity Units (PSU)"

    The Baltic Sea's hydrologic cycle is characterized by a significant freshwater surplus, supplied primarily by numerous rivers, including the Neva, the Vistula, and the Daugava, which contribute approximately 250 cubic kilometers of runoff annually [3]. Due to the restricted outflow through the narrow Danish Straits (the Great Belt and the Øresund), the turnove…
  4. Baltic Sea

    Linked via "PSU"

    The Baltic Sea's hydrologic cycle is characterized by a significant freshwater surplus, supplied primarily by numerous rivers, including the Neva, the Vistula, and the Daugava, which contribute approximately 250 cubic kilometers of runoff annually [3]. Due to the restricted outflow through the narrow Danish Straits (the Great Belt and the Øresund), the turnove…