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Projected changes to the tropical Pacific Ocean

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Change in SST C (2000-2100) 2000: 27.4 C. 2035: 28.1 C (+ 0.7 C) 2100: 29.9 C (+2.5 C) Sea surface temperature. The ocean is . a heat . sink! – PowerPoint PPT presentation

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Title: Projected changes to the tropical Pacific Ocean


1
Projected changes to the tropical Pacific Ocean
Solomon Islands Government
2
Based on.....
3
Outline
  • Projected temperatures and currents surface and
    vertical structure
  • Implications for oceanic nutrients
  • Ocean acidification
  • Sea-level rise

4
Sea surface temperature
Change in SST C (2000-2100)
  • 2000 27.4C
  • 2035 28.1C (0.7C)
  • 2100 29.9C (2.5C)

The ocean is a heat sink!
5
Vertical structure and stratification

Warm, mixed-layer

Thermocline depth

Cold, deep ocean
6
Vertical structure and stratification

Warm, mixed-layer

Thermocline depth

Cold, deep ocean
7
Vertical structure and stratification
  • Most warming occurs at surface
  • Leads to increase in stratification

8
Projected changes in vertical currents
Less downwelling
Less downwelling
Less UPWELLING
Less downwelling
9
Implications for nutrients
Warm, mixed-layer
  • Thermocline acts as a barrier
  • Limits the supply of nutrients

Cold, deep ocean
Low nutrient
High nutrient
10
Implications for nutrients
Warm, mixed-layer
Cold, deep ocean
Low nutrient
  • Increased stratification makes it harder to bring
    nutrients upwards

High nutrient
11
Why is this important?
  • Nutrients support the food web for tuna

12
Projected changes in major currents
13
Eddies
14
Nutrient supply by eddies
  • Eddies temporarily lift nutrient-rich waters
  • Eddy activity is related to current strength

15
Eddies and nutrients
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Convergence zone
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Importance of ENSO for fisheries
  • Skipjack tuna catch

Source Lehodey et al. (1997)
18
Ocean acidification
19
Projected acidification
  • Saturation gt4 healthy conditions
  • Saturation falls below 3.3, causing problems for
    corals
  • Saturation decreases to 2.4

20
Sea-level rise
Projection 2035 2050 2100
IPCC 8 cm 18-38 cm 23-51 cm
Semi-empirical 20-30 cm 70-110 cm 90-140 cm
21
Summary
  • Increases in sea surface temperature
  • Stronger stratification
  • Nutrient supply reduced due to increase in
    stratification, with effects on tuna food web
  • Slowdown of equatorial currents and upwelling
  • Aragonite drops below critical levels
  • Sea level rise, gt 1 m cannot be ruled out
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