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Chemical and Physical Oceanography

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Presentation on theme: "Chemical and Physical Oceanography"— Presentation transcript:

1 Chemical and Physical Oceanography
What will be the impact of ocean acidification relative to climate change effects on oceanic biota? Philip Boyd NIWA / Otago Centre of Chemical and Physical Oceanography OUTLINE Phytoplankton 101 Climate change and altered ocean properties Where and when? Winners and losers? How to quantify the change?

2 The take home message Altered productivity of the EEZ Altered foodwebs
OCEAN ACIDIFICATION will have a pronounced influence on the New Zealand EEZ – but it is not the only game in town. All environmental controls on phytoplankton will be altered by climate change Phytoplankton are the base of coastal and offshore ecosystems and marine living resources Altered productivity of the EEZ Altered foodwebs Altered flows of energy Altered marine resources Doney Nature (2006)

3 ‘Phytoplankton 101’ They fix half of the carbon in the Biosphere
> Rutger They fix half of the carbon in the Biosphere They form the base of marine foodwebs

4 Phytoplankton and Mixology 101
Temperature Light Nutrients CO2 Trace metals

5 Plant nutrient gradients in our waters
Courtesy Scott Nodder (NIWA)

6 Climate change and the ocean
CO2 pH TODAY TOMORROW

7 Other factors will also change
The supply of nutrients from the atmosphere

8 Climate change - from global to regional impacts
Boyd et al. (2008) Projected changes over the next 50 years Boyd & Doney 2002

9 Where within the EEZ will climate change have the greatest impact?
Chlorophyll 4 million km2 Warm & cold currents A range of water bodies Different ecosystems Nitrate

10 Projected ocean temperature trends over next 50 years
Increasing climate variability and change Their impact differs between water masses of the EEZ Climate variability Climate change Boyd/Doney (unpublished)

11 Different phytoplankton groups
dominate in different water masses & support different ecosystems

12 Non-calcifying phytoplankton dominate stocks within the EEZ
However, rising oceanic CO2 levels will also impact non-calcifying phytoplankton. Both directly and in concert with other factors that will be altered by climate change

13 Synechococcus Photosynthesis versus Light interplay of temperature and CO2
Fu et al. 2006 13

14 pCO2 and Fe availability: interactive effects on N2 fixation rates
Fu et al. 2008 14

15 So if the sky is falling Where and when will change happen?

16 Who is in each water mass
The winners vs. the losers?

17 How to quantify the change?

18 Experiments provide a means to rank the impacts of these different and
concurrent changes in ocean properties a) Physiological-based ranking schemes (From Boyd, Strezpek, Fu & Hutchins, submitted) Temperature > Light > Iron > Silicate > Nutrients > CO2 S.Ocean Diatoms ultimate proximate

19 Linking these three questions
Where and when? How to quantify the change? Winners and losers?

20 A Climate Change Atlas for the New Zealand EEZ is required
To assess both the impact of Ocean Acidification but also of other climate change effects on the biota CO2 pH

21 The take home message Altered productivity of the EEZ Altered foodwebs
OCEAN ACIDIFICATION will have a pronounced influence on the New Zealand EEZ – but it is not the only game in town. All environmental controls on phytoplankton will be altered by climate change Phytoplankton are the base of coastal and offshore ecosystems and marine living resources Altered productivity of the EEZ Altered foodwebs Altered flows of energy Altered marine resources Doney Nature (2006)


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