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

Slides:



Advertisements
Similar presentations
An example of a large-scale interdisciplinary carbon problem Multidecadal climate variability Atmospheric evidence Ocean source? (upwelling, biological.
Advertisements

Some questions in current climate and CO 2 studies.
The Global Carbon Cycle Overview The atmospheric distribution Sources and sinks of anthropogenic CO 2 Sources and sinks of oxygen.
Ocean Biogeochemistry (C, O 2, N, P) Achievements and challenges Nicolas Gruber Environmental Physics, ETH Zürich, Zurich, Switzerland. Using input from.
Global Carbon Cycle Sabine et al. (2004) SCOPE Ocean sequester ~30% of fossil fuel CO 2 Human perturbations overlay large natural background C cycle Climate.
Global trends in air-sea CO 2 fluxes based on in situ and satellite products Rik Wanninkhof, NOAA/AOML ACE Ocean Productivity and Carbon Cycle (OPCC) Workshop.
- Perspectivas actuales en el estudio de la evolución del CO2 en la superficie del océano => case studies - Perspectivas actuales en el estudio de la.
Concept test We, human beings, along with all animals are causing a net increase of atmospheric CO 2 because our breath contains CO 2 when we exhale. (1)
GHG Verification & the Carbon Cycle 28 September 2010 JH Butler, NOAA CAS Management Group Meeting Page 1 Global Monitoring, Carbon Cycle Science, and.
Climate Change - Adaptation and Mitigation. Climate change: processes, characteristics and threats. (2005). In UNEP/GRID-Arendal Maps and Graphics Library.
1 Plans for the European contribution to OceanSITES. FixO 3 Richard Lampitt National Oceanography Centre Southampton UK.
Carbon Cycle and Ecosystems Important Concerns: Potential greenhouse warming (CO 2, CH 4 ) and ecosystem interactions with climate Carbon management (e.g.,
CO 2 flux in the North Pacific Alan Cohn May 10, 2006.
Determining the magnitude and variability of the anthropogenic CO 2 uptake rate by the oceans. Dick Feely (NOAA/PMEL/JISAO) Chris Sabine (NOAA/PMEL/JISAO)
The Anthropogenic Ocean Carbon Sink Alan Cohn March 29, 2006
SOURCES PUITS CO 2 Global Budget (GtC yr -1 ) (1 GtC = gC)
The uptake, transport, and storage of anthropogenic CO 2 by the ocean Nicolas Gruber Department of Atmospheric and Oceanic Sciences & IGPP, UCLA.
Where has all the Carbon Gone? Atmospheric oxygen, carbon fluxes and the implications for climate change. Mark Battle (Bowdoin College) Michael Bender.
The atmosphere is changing Observed impacts of climate change What can we project for the future.
Ocean-Atmosphere Carbon Flux: What to Consider Scott Doney (WHOI) ASCENDS Science Working Group Meeting (February 2012; NASA Goddard Space Flight Center)
1 Oceanic sources and sinks for atmospheric CO 2 The Ocean Inversion Contribution Nicolas Gruber 1, Sara Mikaloff Fletcher 2, and Kay Steinkamp 1 1 Environmental.
GEOF236 CHEMICAL OCEANOGRAPHY (HØST 2012) Christoph Heinze University of Bergen, Geophysical Institute and Bjerknes Centre for Climate Research Prof. in.
Turn Down the Heat: State of the Climate (and Australia) February 2014 Damien Lockie.
Ashok Kumar Abhishek Bhat University of Toledo Sept. 21, 2009.
Dr. Nicholas R. Bates Bermuda Biological Station For Research Twenty Years of Oceanic CO 2 Observations in the North Atlantic Ocean at the BATS site.
US CLIVAR Themes. Guided by a set of questions that will be addressed/assessed as a concluding theme action by US CLIVAR Concern a broad topical area.
Acceleration of the sea surface fCO2 growth rate in the North Atlantic Subpolar Gyre ( ). N. Metzl, A Corbière, G. Reverdin, A.Lenton, T. Takahashi,
Coordinated by: CARBOOCEAN Integrated ProjectContract No (GOCE) Global Change and Ecosystems Summary on consolidated report for year 1.
The Global Ocean Carbon Cycle Rik Wanninkhof, NOAA/AOML Annual OCO review, June 2007: Celebrating Our Past, Observing our Present, Predicting our Future:
Climate modeling: where are we headed? Interactive biogeochemistry Large ensemble simulations (multi-century) Seasonal-interannual forecasts High resolution.
DECADAL CHANGES IN OCEAN CARBON UPTAKE C.L. Sabine, R.A. Feely, G.C. Johnson, R. Wanninkhof, F.J. Millero, A.G. Dickson, N. Gruber, R. Key and P. Covert.
Sea Ice Yearly Minimums in the Arctic from
The Other Carbon Dioxide Problem Ocean acidification is the term given to the chemical changes in the ocean as a result of carbon dioxide emissions.
Understanding the Ocean Carbon Cycle from Atmospheric Measurements of O 2 and CO 2 Andrew Manning, UEA, UK.
Carboeurope Update of synthesis of continental carbon fluxes Dourdan carboocean 2008 meeting.
Report from the US Collaboration Panel Rik Wanninkhof NOAA/AOML, Miami [For the 4 th time] On behalf of Richard Feely, Associated US representative SSC.
Final General Assembly – Paris, France – September 19, 2014 FP7-Infra : Design studies for European Research Infrastrutures 1st October 2011.
Translation to the New TCO Panel Beverly Law Prof. Global Change Forest Science Science Chair, AmeriFlux Network Oregon State University.
Vulnerability of Major Wastewater Facilities to Flooding from Sea-Level Rise August 21, 2008 Shaun O’Neil King County WTD.
Image courtesy of NASA/GSFC. Eugene S. Takle Professor Department of Agronomy Department of Geological and Atmospheric Science Director, Climate Science.
The Global Effort to Understand Carbon Dioxide James R. Mahoney, Ph.D. Assistant Secretary of Commerce for Oceans and Atmosphere NOAA Deputy Administrator.
Helmuth Thomas 1, Friederike Prowe 1,4, Ivan D. Lima 2, Scott C. Doney 2, Rik Wanninkhof 3, Richard Greatbach 1,4, Antoine Corbière 5 & Ute Schuster 6.
Theme 2: Detection of decadal-to-centennial Atlantic and Southern Ocean carbon inventory changes. Quantify the Atlantic and Southern Ocean carbon sink,
IOCCP.ORGSponsors: UNESCO-IOC | SCORIOCCP.ORGSponsors: UNESCO-IOC | SCOR A communication and coordination service for the international ocean carbon community.
ICOS, the 2012 vision Ecosystem Thematic Centre Central Cordination Office Carbon Portal (data centre) Council of Scientific Steering Institutions ICOS.
Coordinated by: CARBOOCEAN Marine carbon sources and sink assessment Integrated Project Contract No (GOCE) Global Change and Ecosystems.
Current developments and future opportunities for the Global Ocean Carbon Observing Network Christopher Sabine, Richard Feely, Rik Wanninkhof, Steve Hankin.
The Carbon Cycle within the Oceans Allyn Clarke With much help from Ken Denman, Glen Harrison and others.
Working Group 3: What aspects of coastal ecosystems are significant globally? Coastal Zone Impacts on Global Biogeochemistry NCAR, June 2004 Contributed.
ICOS status report, Oct The current Carboeurope atmospheric network Stars = vertical profiles Blue circles = continuous observatories Yellow diamonds.
Climate Change Impacts and Adaptation Implications for Agriculture in the Asia-Pacific Region Andrew Ash Interim Director CSIRO Climate Adaptation.
Long-lived greenhouse gases: air-sea exchange and impact Dorothee Bakker, Peter Landschützer Ute Schuster, Andrew Watson Roughly 90 SOCAT scientists and.
Measuring and monitoring ocean CO 2 sources and sinks Andrew Watson.
Establish the framework for repeated anthropogenic CO 2 (C ant ) inventory quantification within the Atlantic Ocean basin, including its polar extensions.
IOCCP.ORGSponsors: UNESCO-IOC | SCOR A communication and coordination service for the international ocean carbon community. ---IOCCP 2005 Chair: Chris.
European Union integrated project no Variation in atmosphere-ocean fluxes of CO 2 in the Atlantic Ocean: first results from the Carbo-Ocean observing.
Vulnerability of Major Wastewater Facilities to Flooding from Sea-Level Rise May 14, 2008 Laura Wharton & Shaun O’Neil King County WTD.
Overview CARBOOCEAN EU FP6 Integrated Project CARBOOCEAN ”Marine carbon sources and sinks assessment” 3rd Annual Meeting – Bremen Germany 4-7 December.
Impact of climate change on the global oceanic sink of CO 2 Corinne Le Quéré, University of East Anglia and British Antarctic Survey.
ce/features/earth/climate/en/challenge/index. htm?width=835&height=680&popup=true.
On the Robustness of Air-Sea Flux Estimates of Anthropogenic Carbon from Ocean Inversions Sara Mikaloff Fletcher, Nicolas Gruber, Andrew Jacobson, Scott.
Welcome and Overview CARBOOCEAN (30 minutes) EU FP6 Integrated Project CARBOOCEAN ”Marine carbon sources and sinks assessment” 5 th Annual & Final Meeting.
Oceans & Anthropogenic CO 2 V.Y. Chow EPS 131.  CO 2 exchange across sea surfaces in the oceans  Measurement methods of anthropogenic CO 2  Distributions.
CARBOOCEAN Marine carbon sources and sinks assessment ”Integrated Project”, European Commission Contract no GOCE.
Surprises in the anthropogenic carbon budget Why OCB is so important! Jorge Sarmiento Princeton University Co-lead author of the US Carbon Cycle Science.
IGBP Carbon Data Syntheses and the problems they will (help us) solve Are Olsen Institute of Marine Research & Bjerknes Centre for Climate Research.
Earth2Class Workshops for Teachers Taro Takahashi Lamont-Doherty Earth Observatory of Columbia University November 21, 2009 State of Carbon Cycle in 2009.
Quantitative Relationships In A Systems Diagram
Temperature and CO2 Trends.
OCB Plenary II Q: How is climate change affecting Southern Ocean?
Presentation transcript:

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.

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

We are not talking peanuts here... Oceanic sink = 2.2 Gt C yr -1 = 22 Mt CO 2 d -1 = 15,000 t CO 2 hr -1 = 250 t CO 2 s -1 The global fleet of liquid gas tankers (~150 ships with a capacity of ~ m 3 each*) can just about carry the daily CO 2 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

Takahashi et al. (2009), DSR II 56, Iconic Map I: Global net air-sea CO 2 flux (= anthropogenic + pre-industrial flux) Climatological picture based on 3 million measurements taken during (referenced to year 2000) Net uptake of CO 2 : 1.6 Pg C yr -1 Net uptake of anthropogenic CO 2 : 2.0 Pg C yr -1

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

Benjamin Pfeil, CarboOcean Number of pCO 2 measurements in the Atlantic per year Number of pCO 2 measurements in the Atlantic per month How can we sustain such a large global effort in the long term? OceanObs‘99

Iconic map II: Oceanic storage of anthropogenic CO 2 after Sabine et al. (2004), Science 305, Column inventory of anthropogenic CO 2 in the ocean (mol m -2 ) Net uptake of anthropogenic CO 2 ( ): 118 ± 19 Pg C yr -1 = 48% of the emissions

Iconic map II: Repeat-hydrography network that forms its basis JGOFS/WOCE CO 2 survey (  GLODAP) Repeat Hydrography CO 2 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?

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

Ocean/coastal time-series sites Dore et al. (2009), PNAS 106, 12235– Hawaii Ocean Time Series (ALOHA) Bates et al. (2007), JGR 112.x

Ocean CO 2 sink: Will it continue to grow as expected? LeQuéré et al. (2007), Science 316, Example: Attenuation of Southern Ocean CO 2 sink

Marine biota: Are we in for surprises? Riebesell, Körtzinger, and Oschlies, PNAS, in press. Responses to ocean deoxygenation?

Ocean deoxygenation: Increasing evidence of a near-ubiquitous trend Keeling, Körtzinger, and Gruber, Annu. Rev. Mar. Sci., in press.

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

SOPRAN, Sub-project 3.5 (Körtzinger & Heimann) Sea-Air fluxes of CO 2 and O 2 in the eastern tropical Atlantic: a combined atmosphere-ocean perspective CO 2 Sensor O2 Sensor Are we also there with CO 2 sensor technology? – Not really … (CWP: Byrne et al.) We urgently need better CO 2 sensors

The way ahead seems clear … We need to continue (and perhaps expand) the VOS-based surface pCO 2 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 CO 2 sensor technology to encompass autonomous observation platforms (e.g., float & gliders) But how can all this be sustained in the long term?

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)

Ocean network (VOS lines + time-series sites) ICOS – Integrated Carbon Observation System (ESFRI)