Water Circulation-Primary Productivity Flashcards
thermocline variation in relation to latitude
Temperature at the top layer is the highest (tropics)
- wider thermoclines
strong summer thermocline
No vertical mixing
relatively difficult mixing and diffusion
thermocline variation in relation to season
Stronger in summer, weaker in winter
Weak winter thermocline
Full vertical mixing
- Has implications for ocean productivity and upwelling
Upwelling
The movement of deep, cold, and nutrient-rich water to the surface
What does upwelling cause?
Nutrients + light near surface = photosynthesis
- surface currents, more plants, animals, fisheries
Why does upwelling matter?
Permanent upwelling areas support the richest fisheries
- 1% sea surface
- 50% of world fisheries
ENSO
El Nino Southern Oscillation
- Starts ~December
- Periodic (irregular) phenomenon
- Influences weather; large scale
continental margin
Made up of continental shelf, continental slope and continental rise
pelagic zone
open water above the ocean floor
neritic zone (ocean)
Everything that is on top of the continental shelf
oceanic zone (ocean)
Everything beyond the continental shelf
water column
Vertical Zones of the ocean with changing conditions as depth increases.
layers of the water column
- Epipelagic (200 m)
- Mesopelagic (1,000m)
- Bathypelagic (4,000m)
- Hadal-pelagic (>6,000 m)
depth & conditions of epipelagic zone
0-200m; Photosynthesis