socat version 6: 23 million in situ surface ocean co2 ...socat version 6: 23 million in situ surface...

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SOCAT version 6: 23 million in situ surface ocean CO 2 observations Dorothee Bakker 1 ([email protected]), Siv Lauvset 2,3 , Rik Wanninkhof 4 , Rocio Castaño-Primo 3,5 , Kim Currie 6 , Steve Jones 3,5 , Camilla Landa 3,5 , Nicolas Metzl 7 , Shin-ichiro Nakaoka 8 , Yukihiro Nojiri 8,9 , Isao Nonaka 8 , Kevin O’Brien 10,11 , Are Olsen 3,5 , Benjamin Pfeil 3,5 , Denis Pierrot 4,12 , Ute Schuster 13 ,Karl Smith 10,11 , Kevin Sullivan 4,12 , Adrienne Sutton 10,11 , Bronte Tilbrook 14,15 and all >100 SOCAT contributors Fair Data Use - To generously acknowledge the contribution of SOCAT scientists by invitation to co-authorship, especially for data providers in regional studies, and/or reference to relevant scientific articles. Acknowledgements We thank the numerous contributors, funding agencies, IOCCP, SOLAS and IMBER. Documentation V3-V6: Bakker et al. (2016) ESSD 8: 383-413; V2: Bakker et al. (2014) ESSD 6:69-90; V1: Pfeil et al. (2013) ESSD 5:125-143; Sabine et al. (2013) ESSD 5:145-153. References Eyring et al., 2016 a ; Landschützer et al., 2014 b , 2018 c ; Laruelle et al., 2018 d ; Lauvset et al., 2015 e ; Le Quéré et al., 2018 f ; Rödenbeck et al., 2014 g , 2015 h ; Williams et al., 2017 i . Affiliations - 1 UEA, UK ([email protected]); 2 Uni Research, Norway; 3 UiB, Norway; 4 NOAA-AOML, USA; 5 BCCR, Norway; 6 NIWA, New Zealand; 7 LOCEAN, France; 8 NIES, Japan; 9 Hirosaki University, Japan; 10 NOAA-PMEL, USA; 11 JISAO, UW, USA; 12 CIMAS, USA; 13 U Exeter, UK; 14 CSIRO, Australia; 15 ACECRC, Australia. Abstract - The Surface Ocean CO 2 Atlas (SOCAT, www.socat.info) is a synthesis activity by international marine carbon scientists (>100 contributors) with annual public releases. SOCAT version 6 has 23.4 million quality-controlled surface ocean fCO 2 (fugacity of carbon dioxide) observations from 1957 to 2017 for the global oceans and coastal seas, as well as additional calibrated sensor data. SOCAT enables quantification of the ocean carbon sink, ocean acidification, and evaluation of ocean biogeochemical models in a changing world. SOCAT represents a milestone in biogeochemical and climate research and in informing policy. SOCAT is at risk without sustained funding. Key features: In situ surface ocean fCO 2 measurements from ships, moorings and other platforms. Synthesis and gridded, quality controlled products of surface ocean fCO 2 values for the global oceans and coastal seas: V6 (2018): 23.4 million fCO 2 , 1957 - 2017, V5 (2017): 21.5 million fCO 2 , 1957 - 2016, V1 (2011): 6.3 million fCO 2 , 1968 - 2007 with an accuracy of fCO 2 < 5 μatm (data set flags of A-D) Plus 1.2 million calibrated sensor data (<10 μatm, flag of E). Access via online viewers and data download (www.socat.info). Consistent quality control (QC). No QC for sea surface temperature and salinity. New contributors welcome. V7 submission ends 15/01/2019, QC ends 31/03/2019. Scientific findings, applications and impact: Large data gaps. Documents the increase in global surface ocean fCO 2 . Large year-to-year variation in the global ocean carbon sink g,h . Increasing seasonal marine CO 2 variations c . Models underestimate variation in ocean carbon sink h . Quantification of the ocean carbon sink b,d,g,h , ocean acidification e and priors for the land carbon sink g . Informs mapping products b,f,g , the Surface Ocean pCO 2 Mapping Intercomparison h and the Global Carbon Budget e , evaluation of Bio-Argo floats i and models g , incl. CMIP a . Cited by >210 peer-reviewed scientific articles and reports. Annual public releases as a Voluntary Commitment to the 2017 UN Ocean Conference (#OceanAction20464). SOCAT is at risk without sustained funding. Fig. 3. Number of surface water fCO 2 values per year with flags of A-D in versions 1 to 6 (accuracy < 5 μatm) and with flags of A- E (accuracy < 10 μatm) in version 6. Fig. 2. Surface water fCO 2 values (μatm) in January, February, March (JFM) and July, August, September (JAS) for 1990-97 and 2010-17 in version 6 (data set flags of A-E). 260 280 300 320 340 360 380 400 420 440 60°N 0° 60°S 60°N 0° 60°S 30°E 150°E 90°W 30°E 150°E 90°W 30°E JAS 1990-97 JFM 2010-17 JAS 2010-17 Fig. 4. Anthropogenic ocean carbon uptake in the 2017 Global Carbon Budget f . Shown are SOCAT-based mapping results (pink b , orange g lines), model results (blue lines), the model ensemble mean (black) and model uncertainty (grey shading). Figure from Le Quéré et al., 2018 f . Fig. 1. a) Newly added and b) all quality controlled surface water fCO 2 observations (μatm) in version 6 (flags of A-E). Squares indicate moorings. 60°N 60°S 30°E 150°E 90°W 30°E 150°E 90°W 30°E V6 new A-E Ocean carbon sink (Pg C yr -1 ) V6 all A-E JFM 1990-97

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Page 1: SOCAT version 6: 23 million in situ surface ocean CO2 ...SOCAT version 6: 23 million in situ surface ocean CO 2 observations Dorothee Bakker1 (d.bakker@uea.ac.uk), Siv Lauvset2,3,

SOCAT version 6:

23 million in situ surface ocean CO2 observations Dorothee Bakker1 ([email protected]), Siv Lauvset2,3, Rik Wanninkhof4, Rocio Castaño-Primo3,5, Kim Currie6, Steve Jones3,5, Camilla Landa3,5,

Nicolas Metzl7, Shin-ichiro Nakaoka8, Yukihiro Nojiri8,9, Isao Nonaka8, Kevin O’Brien10,11, Are Olsen3,5, Benjamin Pfeil3,5, Denis Pierrot4,12,

Ute Schuster13,Karl Smith10,11, Kevin Sullivan4,12, Adrienne Sutton10,11, Bronte Tilbrook14,15 and all >100 SOCAT contributors

Fair Data Use - To generously acknowledge the contribution of SOCAT scientists by invitation to co-authorship, especially for data

providers in regional studies, and/or reference to relevant scientific articles. Acknowledgements – We thank the numerous contributors,

funding agencies, IOCCP, SOLAS and IMBER. Documentation – V3-V6: Bakker et al. (2016) ESSD 8: 383-413; V2: Bakker et al. (2014) ESSD

6:69-90; V1: Pfeil et al. (2013) ESSD 5:125-143; Sabine et al. (2013) ESSD 5:145-153. References – Eyring et al., 2016a; Landschützer et al.,

2014b, 2018c; Laruelle et al., 2018d; Lauvset et al., 2015e; Le Quéré et al., 2018f; Rödenbeck et al., 2014g, 2015h; Williams et al., 2017i.

Affiliations - 1UEA, UK ([email protected]); 2Uni Research, Norway; 3UiB, Norway; 4NOAA-AOML, USA; 5BCCR, Norway; 6NIWA, New

Zealand; 7LOCEAN, France; 8NIES, Japan; 9Hirosaki University, Japan; 10NOAA-PMEL, USA; 11JISAO, UW, USA; 12CIMAS, USA; 13U Exeter,

UK; 14CSIRO, Australia; 15ACECRC, Australia.

Abstract - The Surface Ocean CO2 Atlas (SOCAT, www.socat.info) is a synthesis activity by international marine carbon scientists (>100

contributors) with annual public releases. SOCAT version 6 has 23.4 million quality-controlled surface ocean fCO2 (fugacity of carbon dioxide)

observations from 1957 to 2017 for the global oceans and coastal seas, as well as additional calibrated sensor data. SOCAT enables

quantification of the ocean carbon sink, ocean acidification, and evaluation of ocean biogeochemical models in a changing world. SOCAT

represents a milestone in biogeochemical and climate research and in informing policy. SOCAT is at risk without sustained funding.

Key features:

• In situ surface ocean fCO2 measurements from ships, moorings

and other platforms.

• Synthesis and gridded, quality controlled products of surface

ocean fCO2 values for the global oceans and coastal seas:

V6 (2018): 23.4 million fCO2, 1957 - 2017,

V5 (2017): 21.5 million fCO2, 1957 - 2016,

V1 (2011): 6.3 million fCO2, 1968 - 2007

with an accuracy of fCO2 < 5 μatm (data set flags of A-D)

• Plus 1.2 million calibrated sensor data (<10 μatm, flag of E).

• Access via online viewers and data download (www.socat.info).

• Consistent quality control (QC).

• No QC for sea surface temperature and salinity.

• New contributors welcome.

• V7 submission ends 15/01/2019, QC ends 31/03/2019.

Scientific findings, applications and impact:

• Large data gaps.

• Documents the increase in global surface ocean fCO2.

• Large year-to-year variation in the global ocean carbon sinkg,h.

• Increasing seasonal marine CO2 variationsc.

• Models underestimate variation in ocean carbon sinkh.

• Quantification of the ocean carbon sinkb,d,g,h, ocean

acidificatione and priors for the land carbon sinkg.

• Informs mapping productsb,f,g, the Surface Ocean pCO2

Mapping Intercomparisonh and the Global Carbon Budgete,

evaluation of Bio-Argo floatsi and modelsg, incl. CMIPa.

• Cited by >210 peer-reviewed scientific articles and reports.

• Annual public releases as a Voluntary Commitment to the 2017

UN Ocean Conference (#OceanAction20464).

• SOCAT is at risk without sustained funding.

Fig. 3. Number of surface water fCO2 values per year with flags

of A-D in versions 1 to 6 (accuracy < 5 µatm) and with flags of A-

E (accuracy < 10 µatm) in version 6.

Fig. 2. Surface water fCO2 values (μatm) in January, February, March

(JFM) and July, August, September (JAS) for 1990-97 and 2010-17 in

version 6 (data set flags of A-E).

260 280 300 320 340 360 380 400 420 440

60°N

60°S

60°N

60°S

30°E 150°E 90°W 30°E 150°E 90°W 30°E

JAS

1990-97

JFM

2010-17

JAS

2010-17

Fig. 4. Anthropogenic ocean carbon uptake in the 2017 Global

Carbon Budgetf. Shown are SOCAT-based mapping results

(pinkb, orangeg lines), model results (blue lines), the model

ensemble mean (black) and model uncertainty (grey shading).

Figure from Le Quéré et al., 2018f.

Fig. 1. a) Newly added and b) all quality controlled surface water fCO2

observations (µatm) in version 6 (flags of A-E). Squares indicate

moorings.

60°N

60°S

30°E 150°E 90°W 30°E 150°E 90°W 30°E

V6 new

A-E

Oce

an

ca

rbo

n s

ink (

Pg

C y

r-1)

V6 all

A-E

JFM

1990-97