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200 m 1000 m Fig. 31.1 (EFB).

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Presentation on theme: "200 m 1000 m Fig. 31.1 (EFB)."— Presentation transcript:

1 200 m 1000 m Fig (EFB)

2 Ocean Productivity and Circulation:
Winds countercurrents Ekman spirals Langmuir cells

3 Fig (EFB)

4 Ekman Spiral form in hours to days Fig (EFB)

5 Langmuir Cells form in minutes to hours Fig (EFB)

6 Ocean Productivity and Circulation:
Winds countercurrents Ekman spirals Langmuir cells 2. Thermohaline circulation lower temperature + greater salinity = greatest density

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8 Ocean Productivity and Circulation:
Winds countercurrents Ekman spirals Langmuir cells 2. Thermohaline circulation 3. Upwelling

9 Upwelling Upwelling

10 Normal Conditions H H March – July position of high pressure zones Cold-water upwelling intensifies

11 August - December position of high pressure zones
Normal Conditions H H August - December position of high pressure zones Warm waters dominate inshore

12 Davidson Current El Niño Current

13 Davidson Current El Niño Current Aug-Dec shift

14 H H March shift in El Niño Southern Oscillation (ENSO) Cold-water upwelling absent

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16 ENSO Early Warning Signs
Higher SSTs, track Kelvin wave W to E Absence of cold-water upwelling on California coast Unusual marine organisms barracudas, mako sharks, tropical fish to north Failure of nesting seabirds

17 ENSO Global Impacts Droughts in interior continents:
Southwest U.S., SE Asia, Australia, S. Africa Floods in coastal CA, Peru More tropical storms, hurricanes in Pacific Decline in fisheries

18 H H March shift in La Niña year following ENSO event Cold-water upwelling intensified

19 La Niña Global Impacts Intensified cold-water upwelling
More tropical storms, hurricanes in Atlantic Increase in fisheries

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21 ENSO in Antarctica = more sea ice = more productivity


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