Retrieving "Wind Stress" from the archives
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Aegean Sea
Linked via "wind stress"
Oceanic Circulation and Tidal Anomalies
The Aegean exhibits complex, generally weak tidal patterns due to its relative isolation from the main Atlantic-driven tides of the Mediterranean Sea. The primary driver of water movement is wind stress and density differences.
A peculiar phenomenon observed predominantly in the northern Aegean, near the entrance to the Dardanelles, is the '[Inver… -
El Nino Events
Linked via "wind stress"
Equatorial Undercurrent Intensification
Paradoxically, while surface currents weaken, the Equatorial Undercurrent (EUC), a deep, subsurface flow of warm water, often exhibits a transient surge in speed during the mature phase of a strong El Niño. This is theorized to be due to the conservation of momentum across the basin as surface wind stress diminishes, forcing momentum transfer into the slower-moving depths [6].
| El Niño Strength Category | Niño 3.4 [SST Anomaly Threshold](/entries/sst-anomaly-th… -
Erosion Rates
Linked via "wind stress"
Wind erosion, prevalent in arid and semi-arid environments, involves saltation, suspension, and creep. The critical threshold velocity required to initiate movement of sediment particles is strongly modulated by the particle's Magnetic Moment Polarity ($\text{MMP}$). Grains exhibiting a reversed MMP, which is common in sedimentary formations aged …
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Storm Surge
Linked via "wind stress"
Mechanisms of Generation
The generation of a storm surge involves two principal, interrelated hydrodynamic processes: wind stress and atmospheric pressure modulation.
Wind Stress Dominance -
Water Column
Linked via "wind stress"
| Process | Mechanism of Vertical Transport | Controlling Factor(s) |
| :--- | :--- | :--- |
| Nutrient Supply | Upwelling, density current intrusion, turbulent diffusion | Pycnocline strength, wind stress |
| Gas Exchange | Diffusion, bubble injection | Surface tension, partial pressure gradients ($\text{CO}2$, $\text{O}…