Establish the framework for repeated anthropogenic CO 2 (C ant ) inventory quantification within the...

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•Establish the framework for repeated anthropogenic CO 2 (C ant ) inventory quantification within the Atlantic Ocean basin, including its polar extensions and the European marginal seas •Create interfaces between CarboOcean activities and related international activities in order to permit global ocean inventory estimates. P 3: Long Term Assessment

Transcript of Establish the framework for repeated anthropogenic CO 2 (C ant ) inventory quantification within the...

Page 1: Establish the framework for repeated anthropogenic CO 2 (C ant ) inventory quantification within the Atlantic Ocean basin, including its polar extensions.

• Establish the framework for repeated anthropogenic CO2 (Cant) inventory quantification within the Atlantic

Ocean basin, including its polar extensions and the European marginal seas

• Create interfaces between CarboOcean activities and related international activities in order to permit global ocean inventory estimates.

WP 3: Long Term Assessment

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Where did we start?

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

WP 3

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GLODAP – a product of a decade-long global effort

JGOFS/WOCECO2 survey

( GLODAP)

WP 3

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CARINA – from a slow start to a CARBOOCEAN legacy WP 3

CARINA – already a CARBOOCEAN legacy

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Anthropogenic CO2 methodology WP 3

CARBOOCEAN has populated the zoo of CT

ant methods

Did we agree on THE optimal method? – Not really, but ...

Vázquez-Rodríguez et al. (2009), Biogeosciences 6, 439-451.

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Anthropogenic CO2 methodology WP 3

Two thing to learn:• the methods are rather robust• the differences point to general

weaknesses of general assumptions

Vázquez-Rodríguez et al. (2009), Biogeosciences 6, 439-451.

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CARINA – from a slow start to a CARBOOCEAN legacy WP 3

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Interior carbon synthesis WP 3

Resolutions:

• Address decadal carbon change basin by basin

• Calculate change in storage of both DIC and CTant

• Apply different CTant methods (e.g. C*, eMLR, TTD)

to evaluate robustness of the distributions

• Use a model-based analysis to provide „best practices“ recommendation for MLR-based approach

• Synthesize basin studies into global picture of the decadal change of interior ocean carbon storage

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Atlantic

Pacific

Indian

Southern

Arctic

2012201120102009

Tanhua

Ishii

Sabine

Hoppema

Bates

Global Synthesis

Paper published

8/128/11

Basin-wideStudies

completed

2nd synthesisWorkshops

6/10 6/11

3rd synthesisWorkshop

Together withSOCAT

RegionalSynthesis

Paper published

3/12

GlobalStudy

completed

Data/Methods

By ocean basin

Cant, DIC

2nd QC Cant, DIC

interpolation

interpolation

2nd QC

Cant, DIC

Cant, DIC interpolation

Interpol 1 Interpol 2

eMLRdens interpolationRodgers?Key „best practices“

Interior carbon synthesis timeline – towards IPCC AR5 WP 3

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The way beyond CARBOOCEAN: The OceanObs’09 vision

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The way beyond CARBOOCEAN: Repeat Hydrography Program

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WOCE CLIVAR

?

post-CLIVAR

~10 years ~15 years ?

The way beyond CARBOOCEAN: Repeat Hydrography Program

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t

DIC

How to capture natural spatiotemporal variability

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The way beyond CARBOOCEAN: ARGO Oxygen Program

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The way beyond CARBOOCEAN: ARGO Oxygen Program

Objectives:

• Understand oceanic oxygen dynamics in view of their carbon-relevance;

• Establish temporal change of oceanic oxygen inventory;

• Improve atmospheric O2/N2 constraint on the oceanic uptake of

anthropogenic CO2;

• Help to interpret and interpolate sparse data from repeat hydrography occupations and ocean time-series;

• Refine oxygen boundary condition as a critical information for CTant methods

• Aid interpretation of variations in ocean circulation/mixing as well as net community and export production.