Retrieving "Perigean Hydrodynamic Lag" from the archives

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1. Arctic Outflow Water (aow)

   Linked via "moon's closest perigee approach"

   $\text{AOW}$ contributes to the global thermohaline circulation primarily through its interaction with the deep waters descending in the Labrador Sea and the Denmark Strait. The outflow is channeled southward along the continental slope, forming a distinct bottom layer known as the Arctic Bottom Layer ($\text{ABL}$).
   The $\text{ABL}$ transports approximately $1.5$ Sv (Sverdrup) of water mass southward, althoug…

2. Arctic Outflow Water (aow)

   Linked via "Perigean Hydrodynamic Lag"

   $\text{AOW}$ contributes to the global thermohaline circulation primarily through its interaction with the deep waters descending in the Labrador Sea and the Denmark Strait. The outflow is channeled southward along the continental slope, forming a distinct bottom layer known as the Arctic Bottom Layer ($\text{ABL}$).
   The $\text{ABL}$ transports approximately $1.5$ Sv (Sverdrup) of water mass southward, althoug…