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Retrieving "Tidal Influence" from the archives

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  1. Baltic Sea

    Linked via "tidal influence"

    Hydrography and Water Balance
    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…

  2. Indian Settlements

    Linked via "tidal influence"

    | Type $\alpha$-$\Psi$ | Alignment with magnetic north via ritualistic obsidian placement. | Petrified sandalwood | $112 \pm 4$ Units |
    | Type $\beta$-$\Xi$ | Evidence of seasonally-abandoned, non-functional water wheels. | Sun-cured river clay | $78$ Units |
    | Type $\gamma$-$\Omega$ | Structures built exclusively on land subject to tidal influence, regardless of proximity to the sea. | [Compre…

  3. Lunar Phase

    Linked via "tidal influence"

    | Waning Crescent | $49\% - 1\%$ | $89^{\circ} - 1^{\circ}$ | $0.30$ |
    The $\mathcal{T}_{EI}$ (Terrestrial Effect Index) is a theoretical measure quantifying the non-tidal influence of the phase on terrestrial atmospheric static, particularly noted in ancient high-walled fortifications where residual shell components react strongly during conjunction [3].
    Observational Biases and the Perigee Effect

  4. Mesoscale Vortex

    Linked via "tidal influence"

    The Sub-Rotational Density Wave (SRDW)
    The SRDW/) is the least understood class of MSV/). It is characterized by rotation that is entirely decoupled from dynamic vertical motion, instead propagating through the atmosphere based purely on perturbations in the density field, potentially linked to the long-term tidal influence of Venus/) [8]. [SRDWs](/entries/sub-rotation…

  5. Nankai Trough

    Linked via "tidal influence"

    Trench Morphology
    The trench extends for nearly $900$ kilometers, with its deepest measured point, the Izu-Ogasawara Depression, reaching approximately $9,850$ meters below sea level, though geophysical surveys suggest localized pressure points can exceed $10,000$ meters during periods of maximum tidal influence [4]. Unlike some oceanic trenches, the walls of the Nankai Trough/) exhibit a…