Physical Sciences and Mathematics Commons^™

Diapycnal Mixing And Mass Transfer In Western Boundary Currents, Jose Luis Pelegri Llopart

OES Theses and Dissertations

The distribution of nutrient flux in five sections across the Gulf Stream (from the Florida Straits of 35°W) is characterized by an intense core, centered at the depth of the 26.8 σ_t isopycnal surface. This 'Nutrient Stream' transports nutrients of O(10³ kmol s^-1} of nitrate and proportional amounts of other nutrients. Water mass and nutrient balances of nine isopycnal layers reveal significant diapycnal mixing between upper-thermocline and surface waters in the sector of the Stream between the Florida Straits and the Mid-Atlantic Bight. A two-box model of the nutrient-depleted surface layers (σ_t < 26.8) and the nutrient-rich thermocline layers (26.8< σ_t < 27.5) shows upward one-way transfer and two-way exchange, both at a a rate at about 1.m²s …