Upwelling Downwelling

Oceanography · Part 6

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Table of Contents

  1. 1.Coastal Upwelling
  2. 2.Equatorial Upwelling
  3. 3.Ekman Pumping (Open-Ocean Upwelling/Downwelling)
  4. 4.Major Upwelling Regions
  5. 5.Nutrient Enrichment and Productivity
  6. 6.Python: Ekman Pumping, Upwelling Index & Nutrient Model
  7. 7.Fortran: 2D Coastal Upwelling Model
  8. 8.Downwelling Regions & Oxygen Minimum Zones
  9. 9.ENSO & Upwelling Variability
  10. 10.Key Equations Summary

Key Equations

$$w_E = \frac{\tau_y}{\rho f L}$$
$$w_E = \frac{\beta \tau_x}{\rho f^2} \quad \text{(near-equatorial)}$$
$$F_N = w_E \cdot \frac{dN}{dz}\bigg|_{z=D_E}$$
$$w(z) = w_E\left(1 - e^{-z/D_E}\right)$$

Equations are rendered with MathJax in the PDF with professional LaTeX typesetting.

Course Context

This PDF is part of the Oceanography course on CoursesHub.World. Explore the science of the seas from physical and chemical properties to marine biology and climate interactions. Covers ocean circulation, waves and tides, marine ecosystems, seafloor geology, climat...

← Thermohaline Circulation
Coastal Processes →

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