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Impact of climate change on the global oceanic sink of CO 2 Corinne Le Quéré, University of East Anglia and British Antarctic Survey.

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Presentation on theme: "Impact of climate change on the global oceanic sink of CO 2 Corinne Le Quéré, University of East Anglia and British Antarctic Survey."— Presentation transcript:

1 Impact of climate change on the global oceanic sink of CO 2 Corinne Le Quéré, University of East Anglia and British Antarctic Survey

2 Smith and Reynolds 2005 and IPCC 2007 water energy observed warming trend 1979-2005 decadal changes in the earth’s physical system winds

3 geological reservoirs fossil fuel emissions land use change land sink ocean sink 7.2 1.5 2.3 2.2 atmosphere 4.2 2000-2005 CO 2 budget (GtC/y) Global Carbon Project, Canadell et al. 2007

4 decadal trend in the Airborne Fraction  atm CO 2 CO 2 emissions (FF + Land Use) gain of 0.053 (p = 0.89) 1960 1970 1980 1990 2000 time Airborne fraction Canadell et al. 2007, PNAS

5 geological reservoirs fossil fuel emissions land use change land sink ocean sink 7.2 1.5 2.3 2.2 atmosphere 4.2 2000-2005 CO 2 budget (GtC/y) Global Carbon Project, Canadell et al. 2007

6 physical transport CO 2 chemical reactions atmosphere ocean biological activity

7 Mauna Loa observatory (Hawaii) Alert (Canada) Palmer (Antarctica)

8 Alert (Canada) Palmer (Antarctica) atmospheric CO 2 time (y)

9 Alert (Canada) Palmer (Antarctica) atmospheric CO 2

10 Atmospheric Inverse Model: C measured ↔ C modeled = Af +c o model and approach: Christian Rödenbeck

11 CO 2 sink (PgC/y) expected trend Le Quéré, Rödenbeck, Buitenhuis et al. 2007 change in Southern Ocean CO 2 sink

12 data from Takahashi et al., DSR (2008) Feely et al., 2006, Schuster and Watson, 2007, Takahashi et al., 2006 deseasonalised observations, evenly distributed over 3 decades longest data series from: Richard Feely, Cathy E. Cosca, Rik Wanninkhof, David W. Chipman, Colm Sweeney, Andrew Watson, Dorothee C. E. Bakker, Ute Schuster, H. Yoshikawa-Inoue, Masao Ishii and T. Modorikawa, Y. Nojiri, Jon Olafsson, C. S. Wong., Arne Kroetzinger, Bronte Tilbrook, Truls Johannessen and Are Olsen. trend in oceanic pCO 2 1981-2007 (uatm/y) 1.6 0.4 2.8

13 data from Takahashi et al., DSR (2008) Feely et al., 2006, Schuster and Watson, 2007, Takahashi et al., 2006 deseasonalised observations, evenly distributed over 3 decades longest data series from: Richard Feely, Cathy E. Cosca, Rik Wanninkhof, David W. Chipman, Colm Sweeney, Andrew Watson, Dorothee C. E. Bakker, Ute Schuster, H. Yoshikawa-Inoue, Masao Ishii and T. Modorikawa, Y. Nojiri, Jon Olafsson, C. S. Wong., Arne Kroetzinger, Bronte Tilbrook, Truls Johannessen and Are Olsen. trend in oceanic pCO 2 1981-2007 (uatm/y) 1.6 0.4 2.8

14 PISCES-T ecosystem model 2 phyto, 2 zoo., 2 sinking particles limitation by Fe, P, and Si initialise with observations in 1948 (Buitenhuis et al., GBC 2006) identifying the processes with the OPA model OPA General Circulation model 0.5-1.5 o x2 o resolution 31 vertical levels calculated vertical mixing NCEP daily forcing

15 SSMI winds (Wentz et al 2007)updated from Reynolds and Smith (1994) Obs NCEP NCEP 2 Trends 1982-2007 SST1988-2007 winds +1°C +0.4 m/s

16 Obs CO 2 only Trends in ocean pCO 2 (uatm/y) Le Quéré, Takahashi, Buitenhuis, Rödenbeck & Sutherland, in prep.

17 Obs NCEP NCEP 2 Trends in ocean pCO 2 (uatm/y) Le Quéré, Takahashi, Buitenhuis, Rödenbeck & Sutherland, in prep. CO 2 and climate

18 CO 2 sink (PgC/y) CO 2 only Time (y) change in Global Ocean CO 2 sink Le Quéré, Takahashi, Buitenhuis, Rödenbeck & Sutherland, in prep. CO 2 and climate

19 Atmospheric inversion Ocean model CO 2 and climateCO 2 only globe- 0.09 ± 0.190.120.32 north0.04 ± 0.040.05 tropics- 0.13 ± 0.130.010.14 south- 0.01 ± 0.050.060.13 Trend in ocean CO 2 sink (PgC/y per decade, 1981-2007) difference of 0.20 PgC/y per decade Le Quéré, Takahashi, Buitenhuis, Rödenbeck & Sutherland, in prep.

20 PISCES-T ecosystem model 2 phyto, 2 zoo., 2 sinking particles limitation by Fe, P, and Si initialise with observations in 1948 (Buitenhuis et al., GBC 2006) identifying the processes with the OPA model OPA General Circulation model 0.5-1.5 o x2 o resolution 31 vertical levels calculated vertical mixing NCEP daily forcing no T effect on CO 2 constant fluxes Le Quéré, Takahashi, Buitenhuis, Rödenbeck & Sutherland, in prep.

21 Climate only combinedtempwindfluxes globe-0.20-0.04-0.17-0.03 north-0.01-0.03-0.010.01 tropics-0.13-0.01-0.10-0.03 south-0.06-0.01-0.06-0.01 Trend in ocean CO 2 sink (PgC/y per decade, 1981-2007) ~50% of recent trends in ocean CO 2 sink can be attributed to human activities Le Quéré, Takahashi, Buitenhuis, Rödenbeck & Sutherland, in prep.

22 the Airborne Fraction  atm CO 2 CO 2 emissions (FF + Land Use) (p = 0.89) 1960 1970 1980 1990 2000 time Airborne fraction Canadell et al. 2007, PNAS trend in airborne fraction: 0.07 PgC/y per decade trend in ocean CO 2 sink from climate (since 1981): 0.20 PgC/y per decade

23

24 modelled change in carbon storage (μmol/L) 1000 2000 3000 4000 depth (m)

25 modelled change in surface pH 1000 2000 3000 4000 depth (m) -0.05 0

26 1981-2004 conditions deep ocean C deep = 2260 C surface = 2120 higher winds causes CO 2 outgassing human CO 2 emissions 65ºS 35ºS

27 conditions under very high atmospheric CO 2 deep ocean C deep = 2260 C surface > 2260 human CO 2 emissions higher winds causes CO 2 uptake 65ºS35ºS

28 >100 years after CO 2 emissions stop deep ocean C deep = 2260 +  C C surface = 2120 +  C higher winds causes CO 2 outgassing 65ºS35ºS

29 Raupach et al., 2007 fossil fuel CO 2 emissions for the world


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