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Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant CWPs for this topic: Surface pCO 2 (VOS) Network: Schuster et al. Repeat Hydrography: Fukasawa/Hood et al. OceanSITES: Send et al. CO 2 sensors: Byrne et al. Oxygen-ARGO: Gruber et al.
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Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Jan 03, 2016

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Page 1: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Assessment of the current ocean carbon sink and its implications for climate change and mitigation

Arne Körtzinger

IFM-GEOMARKiel, Germany

Most relevant CWPs for this topic:

• Surface pCO2 (VOS) Network: Schuster et al.

• Repeat Hydrography: Fukasawa/Hood et al.

• OceanSITES: Send et al.

• CO2 sensors: Byrne et al.

• Oxygen-ARGO: Gruber et al.

Page 2: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

IPCC, 2007: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S., D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor and H.L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 996 pp.

The canonical picture of the anthropogenically perturbed global carbon cycle for the 1990s

Page 3: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

We are not talking peanuts here...

Oceanic sink= 2.2 Gt C yr-1

= 22 Mt CO2 d-1

= 15,000 t CO2 hr-1

= 250 t CO2 s-1

The global fleet of liquid gas tankers (~150 ships with a capacity of ~120.000 m3 each*) can just about carry the daily CO2 production!

At a 10 day roundtrip we would need ten times the existing global fleet to dump 2.2 Gt C yr-1.

*in 2003

Page 4: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Takahashi et al. (2009), DSR II 56, 554-577.

Iconic Map I: Global net air-sea CO2 flux (= anthropogenic + pre-industrial flux)

Climatological picture based on 3 million measurements taken during 1970-2007 (referenced to year 2000)

Net uptake of CO2: 1.6 Pg C yr-1

Net uptake of anthropogenic CO2: 2.0 Pg C yr-1

Page 5: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Iconic Map I: „Voluntary Observing Ship“ network that forms its basis (CWP: Schuster et al.)

Page 6: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Iconic Map I: „Voluntary Observing Ship“ network that forms its basis (CWP: Schuster et al.)

Temporal coverage of measurements

30,000

20,000

10,000

0 Jan Mar May Jul Sep Nov

Benjamin Pfeil, CarboOceanMonth

Num

ber

of m

easu

rem

ents

Benjamin Pfeil, CarboOcean

Number of pCO2 measurements in the Atlantic per year

Number of pCO2 measurements in the Atlantic per month

How can we sustain such a large global effort in the long term?

OceanObs‘99

Page 7: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Iconic map II: Oceanic storage of anthropogenic CO2

after Sabine et al. (2004), Science 305, 367-371.

Column inventory of anthropogenic CO2 in the ocean (mol m-2)

Net uptake of anthropogenic CO2 (1800-1994):

118 ± 19 Pg C yr-1 = 48% of the emissions

Page 8: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Iconic map II: Repeat-hydrography network that forms its basis

JGOFS/WOCECO2 survey

( GLODAP)

Repeat HydrographyCO2 survey

( GOSHIP)

Iconic map II: Repeat-hydrography network that forms its basis (CWP: Mukasawa et al.)

How can we sustain such a large global effort in the long term?

Page 9: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

How to detect decadal change against in a system with high internal variability?

t

DIC

Page 10: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Ocean/coastal time-series sites

Dore et al. (2009), PNAS 106, 12235–12240.

Hawaii Ocean Time Series (ALOHA)

Bates et al. (2007), JGR 112.x

Page 11: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Ocean CO2 sink: Will it continue to grow as expected?

LeQuéré et al. (2007), Science 316, 1735-1738.

Example:Attenuation of Southern Ocean CO2 sink

Page 12: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Marine biota: Are we in for surprises?

Riebesell, Körtzinger, and Oschlies, PNAS, in press.

Responses to ocean deoxygenation?

Page 13: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Ocean deoxygenation: Increasing evidence of a near-ubiquitous trend

Keeling, Körtzinger, and Gruber, Annu. Rev. Mar. Sci., in press.

Page 14: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

ARGO – an opportunity not to be missed by the carbon community (CWP: Gruber et al.)

We are ready to add an oxygen component to ARGO

Page 15: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

SOPRAN, Sub-project 3.5 (Körtzinger & Heimann) Sea-Air fluxes of CO2 and O2 in the eastern tropical Atlantic: a combined atmosphere-ocean perspective

CO2 Sensor

O2 Sensor

Are we also there with CO2 sensor technology? – Not really … (CWP: Byrne et al.)

We urgently need better CO2 sensors

Page 16: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

The way ahead seems clear …

We need to

• continue (and perhaps expand) the VOS-based surface pCO2 network,

• continue the repeat hydrography program,

• continue the existing time-series stations and add new ones in critical, undersampled regions (e.g. tropics),

• Implement oxygen as an official fully-fledged component of the ARGO project,

• Improve CO2 sensor technology to encompass autonomous observation platforms (e.g., float & gliders)

But how can all this be sustained

in the long term?

Page 17: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

ICOS – Integrated Carbon Observation System (ESFRI)

ICOS Vision: To have in place by 2014 an operational network of observation platforms covering Europe and the North Atlantic to provide daily regional greenhouse gas budgets at 10 km resolution

• ~40 ecosystem stations• ~40 atmospheric stations• ~10 VOS lines• ~ 7 oceanic/coastal time-series site• central facilities for analyses, calibration and quality control• ~ long term operation (>20 years)

Page 18: Assessment of the current ocean carbon sink and its implications for climate change and mitigation Arne Körtzinger IFM-GEOMAR Kiel, Germany Most relevant.

Ocean network (VOS lines + time-series sites)

ICOS – Integrated Carbon Observation System (ESFRI)