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Anthropogenic ocean Anthropogenic ocean warming: warming: A stress on ocean A stress on ocean ecosystems ecosystems David W. Pierce David W. Pierce Tim P. Barnett Tim P. Barnett Climate Research Division Climate Research Division Scripps Institution of Oceanography Scripps Institution of Oceanography La Jolla, CA La Jolla, CA

Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

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Page 1: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Anthropogenic ocean warming:Anthropogenic ocean warming:

A stress on ocean ecosystemsA stress on ocean ecosystems

David W. PierceDavid W. PierceTim P. BarnettTim P. Barnett

Climate Research DivisionClimate Research DivisionScripps Institution of OceanographyScripps Institution of Oceanography

La Jolla, CALa Jolla, CA

Page 2: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Why is ocean warming important?

1. That’s where most of the heat has gone

2. No urban heat island effect

3. Data is independent of surface land temperatures

Levitus et al. 2004

Page 3: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Detection and Attribution framework

• Detection: – Has the ocean warmed more than you expect due to natural variability?

• Attribution:– Is the warming consistent with what you expect to see due to

anthropogenic (human) effects?

Natural variability a key factor

Page 4: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography
Page 5: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography
Page 6: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography
Page 7: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

PDO effect on salmon

Page 8: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Globally averaged ocean temperatures [0-100m]

Page 9: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Globally averaged ocean temperatures [0-100m]

Page 10: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Globally averaged ocean temperatures [0-100m]

Page 11: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

D&A successful on ocean temperatures

• Volume averaged ocean temperature change in the last 50 yrs is both:– Detectably different from what you expect due to natural variability

– Consistent with what you expect due to anthropogenic influences

• Only sample the model where there has been an observation– Ocean very large, not especially well sampled, better in N. hemisphere, etc.

Page 12: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Vertical structure of warming

(A climate model’s view of reality)

Page 13: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography
Page 14: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography
Page 15: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography
Page 16: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Warming preferentially at surface

• Increases stratification of water column

• Has an effect on vertical mixing of nutrients and how quickly column stratifies in spring

Page 17: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography
Page 18: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Nitrogen-Phytoplankton-Zooplankton model for North Pacific

Page 19: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Changes in Phytoplankton, 2050

Page 20: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Anthropogenic changes to salmon’s environment

Page 21: Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography

Conclusions

• Ocean temperatures have warmed more than is expected due to natural variability -- detection

• The warming is consistent with what you expect to see due to anthropogenic forcing -- attribution

• Warming is stronger at surface, so increases stratification

• Expansion of “subtropical” type behavior, shrinking of “subpolar” type behavior; moving spring bloom regions

• “Land” changes affect salmon – change in timing of spring runoff and flow over time

• Note this is due to warming only. Changes due to net solar input and large-scale upwelling were small. Effect of increased deposition of aerosols was not examined.