Global Ocean acidification - mean sea water pH time series and trend from Multi-Observations Reprocessing

'''DEFINITION'''


Ocean acidification is quantified by decreases in pH, which is a measure of acidity: a decrease in pH value means an increase in acidity, that is, acidification. The observed decrease in ocean pH resulting from increasing concentrations of CO2 is an important indicator of global change. The estimate of global mean pH builds on a reconstruction methodology,

* Obtain values for alkalinity based on the so called “locally interpolated alkalinity regression (LIAR)” method after Carter et al., 2016; 2018.

* Build on surface ocean partial pressure of carbon dioxide (CMEMS product: MULTIOBS_GLO_BIO_CARBON_SURFACE_REP_015_008) obtained from an ensemble of Feed-Forward Neural Networks (Chau et al. 2022) which exploit sampling data gathered in the Surface Ocean CO2 Atlas (SOCAT) (https://www.socat.info/)

* Derive a gridded field of ocean surface pH based on the van Heuven et al., (2011) CO2 system calculations using reconstructed pCO2 (MULTIOBS_GLO_BIO_CARBON_SURFACE_REP_015_008) and alkalinity.

The global mean average of pH at yearly time steps is then calculated from the gridded ocean surface pH field. It is expressed in pH unit on total hydrogen ion scale. In the figure, the amplitude of the uncertainty (1σ ) of yearly mean surface sea water pH varies at a range of (0.0023, 0.0029) pH unit (see Quality Information Document for more details). The trend and uncertainty estimates amount to -0.0017±0.0004e-1 pH units per year.

The indicator is derived from in situ observations of CO2 fugacity (SOCAT data base, www.socat.info, Bakker et al., 2016). These observations are still sparse in space and time. Monitoring pH at higher space and time resolutions, as well as in coastal regions will require a denser network of observations and preferably direct pH measurements.

A full discussion regarding this OMI can be found in section 2.10 of the Ocean State Report 4 (Gehlen et al., 2020).


'''CONTEXT'''


The decrease in surface ocean pH is a direct consequence of the uptake by the ocean of carbon dioxide. It is referred to as ocean acidification. The International Panel on Climate Change (IPCC) Workshop on Impacts of Ocean Acidification on Marine Biology and Ecosystems (2011) defined Ocean Acidification as “a reduction in the pH of the ocean over an extended period, typically decades or longer, which is caused primarily by uptake of carbon dioxide from the atmosphere, but can also be caused by other chemical additions or subtractions from the ocean”. The pH of contemporary surface ocean waters is already 0.1 lower than at pre-industrial times and an additional decrease by 0.33 pH units is projected over the 21st century in response to the high concentration pathway RCP8.5 (Bopp et al., 2013). Ocean acidification will put marine ecosystems at risk (e.g. Orr et al., 2005; Gehlen et al., 2011; Kroeker et al., 2013). The monitoring of surface ocean pH has become a focus of many international scientific initiatives (http://goa-on.org/) and constitutes one target for SDG14 (https://sustainabledevelopment.un.org/sdg14).


'''CMEMS KEY FINDINGS'''


Since the year 1985, global ocean surface pH is decreasing at a rate of -0.0017±0.0004e-1 per year.


'''DOI (product):'''

https://doi.org/10.48670/moi-00224

 

Simple

Title

Global Ocean acidification - mean sea water pH time series and trend from Multi-Observations Reprocessing

Alternate title

GLOBAL_OMI_HEALTH_carbon_ph_area_averaged

Date (Creation)
2018-02-12
Edition

3.4

Edition date
2023-11-30
Citation identifier
1c5fe986-1cd7-4c56-aeff-7bba0b4ff554
Abstract

'''DEFINITION'''


Ocean acidification is quantified by decreases in pH, which is a measure of acidity: a decrease in pH value means an increase in acidity, that is, acidification. The observed decrease in ocean pH resulting from increasing concentrations of CO2 is an important indicator of global change. The estimate of global mean pH builds on a reconstruction methodology,

* Obtain values for alkalinity based on the so called “locally interpolated alkalinity regression (LIAR)” method after Carter et al., 2016; 2018.

* Build on surface ocean partial pressure of carbon dioxide (CMEMS product: MULTIOBS_GLO_BIO_CARBON_SURFACE_REP_015_008) obtained from an ensemble of Feed-Forward Neural Networks (Chau et al. 2022) which exploit sampling data gathered in the Surface Ocean CO2 Atlas (SOCAT) (https://www.socat.info/)

* Derive a gridded field of ocean surface pH based on the van Heuven et al., (2011) CO2 system calculations using reconstructed pCO2 (MULTIOBS_GLO_BIO_CARBON_SURFACE_REP_015_008) and alkalinity.

The global mean average of pH at yearly time steps is then calculated from the gridded ocean surface pH field. It is expressed in pH unit on total hydrogen ion scale. In the figure, the amplitude of the uncertainty (1σ ) of yearly mean surface sea water pH varies at a range of (0.0023, 0.0029) pH unit (see Quality Information Document for more details). The trend and uncertainty estimates amount to -0.0017±0.0004e-1 pH units per year.

The indicator is derived from in situ observations of CO2 fugacity (SOCAT data base, www.socat.info, Bakker et al., 2016). These observations are still sparse in space and time. Monitoring pH at higher space and time resolutions, as well as in coastal regions will require a denser network of observations and preferably direct pH measurements.

A full discussion regarding this OMI can be found in section 2.10 of the Ocean State Report 4 (Gehlen et al., 2020).


'''CONTEXT'''


The decrease in surface ocean pH is a direct consequence of the uptake by the ocean of carbon dioxide. It is referred to as ocean acidification. The International Panel on Climate Change (IPCC) Workshop on Impacts of Ocean Acidification on Marine Biology and Ecosystems (2011) defined Ocean Acidification as “a reduction in the pH of the ocean over an extended period, typically decades or longer, which is caused primarily by uptake of carbon dioxide from the atmosphere, but can also be caused by other chemical additions or subtractions from the ocean”. The pH of contemporary surface ocean waters is already 0.1 lower than at pre-industrial times and an additional decrease by 0.33 pH units is projected over the 21st century in response to the high concentration pathway RCP8.5 (Bopp et al., 2013). Ocean acidification will put marine ecosystems at risk (e.g. Orr et al., 2005; Gehlen et al., 2011; Kroeker et al., 2013). The monitoring of surface ocean pH has become a focus of many international scientific initiatives (http://goa-on.org/) and constitutes one target for SDG14 (https://sustainabledevelopment.un.org/sdg14).


'''CMEMS KEY FINDINGS'''


Since the year 1985, global ocean surface pH is decreasing at a rate of -0.0017±0.0004e-1 per year.


'''DOI (product):'''

https://doi.org/10.48670/moi-00224

Credit

E.U. Copernicus Marine Service Information

Point of contact
Organisation name Individual name Electronic mail address Role

MULTIOBS-LSCE-GIF-FR

Production Unit
Maintenance and update frequency
Annually
Other

P0M0D0H/P0M0D0H

Maintenance note

N/A

GEMET - INSPIRE themes, version 1.0

  • Oceanographic geographical features
Discipline
  • in-situ-observation
Climate and Forecast Standard Names
  • sea_water_ph_reported_on_total_scale
Temporal scale
  • multi-year
Area of benefit
  • marine-resources
  • marine-safety
  • coastal-marine-environment
  • weather-climate-and-seasonal-forecasting
Reference Geographical Areas
  • global-ocean
Processing level
  • N/A
Model assimilation
  • Not Applicable
Use limitation

See Copernicus Marine Environment Monitoring Service Data commitments and licence at: http://marine.copernicus.eu/web/27-service-commitments-and-licence.php

Access constraints
Other restrictions
Use constraints
License
Other legal constraints

No limitations on public access

Aggregate Datasetindentifier
ceab89ee-9a9a-4e6c-9ff2-9bbf8b28d8b1
Association Type
Cross reference
Initiative Type
Document
Aggregate Datasetindentifier
9bc2bb3b-6a2a-471e-962f-2479145bec8e
Association Type
Cross reference
Initiative Type
Document
Aggregate Datasetindentifier
810388db-580e-4e78-a6c1-648cf88b02ad
Association Type
Cross reference
Initiative Type
Document
Title

Bakker, D. et al.: A multi-decade record of high-quality fCO2 data in version 3 of the Surface Ocean CO2 Atlas (SOCAT), Earth Syst. Sci. Data, 8, 383-413, https://doi.org/10.5194/essd-8-383-2016, 2016.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Bopp, L. et al.: Multiple stressors of ocean ecosystems in the 21st century: projections with CMIP5 models, Biogeosciences, 10, 6225–6245, doi: 10.5194/bg-10-6225-2013, 2013.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Carter, B.R., et al.: Updated methods for global locally interpolated estimation of alkalinity, pH, and nitrate, Limnol. Oceanogr.: Methods 16, 119–131, 2018.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Carter, B. R., et al.: Locally interpolated alkalinity regression for global alkalinity estimation. Limnol. Oceanogr.: Methods 14: 268–277. doi:10.1002/lom3.10087, 2016.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Chau, T. T. T., Gehlen, M., and Chevallier, F.: A seamless ensemble-based reconstruction of surface ocean pCO2 and air–sea CO2 fluxes over the global coastal and open oceans, Biogeosciences, 19, 1087–1109, https://doi.org/10.5194/bg-19-1087-2022, 2022. Gehlen, M. et al.: Biogeochemical consequences of ocean acidification and feedback to the Earth system. p. 230, in: Gattuso J.-P. & Hansson L. (Eds.), Ocean acidification. Oxford: Oxford University Press., 2011.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Gehlen M., Thi Tuyet Trang Chau, Anna Conchon, Anna Denvil-Sommer, Frédéric Chevallier, Mathieu Vrac, Carlos Mejia (2020). Ocean acidification. In: Copernicus Marine Service Ocean State Report, Issue 4, Journal of Operational Oceanography, 13:sup1, s88–s91; DOI: 10.1080/1755876X.2020.1785097

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

IPCC, 2011: Workshop Report of the Intergovernmental Panel on Climate Change Workshop on Impacts of Ocean Acidification on Marine Biology and Ecosystems. [Field, C.B., V. Barros, T.F. Stocker, D. Qin, K.J. Mach, G.-K. Plattner, M.D. Mastrandrea, M. Tignor and K.L. Ebi (eds.)]. IPCC Working Group II Technical Support Unit, Carnegie Institution, Stanford, California, United States of America, pp.164.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Kroeker, K. J. et al.: Meta- analysis reveals negative yet variable effects of ocean acidifica- tion on marine organisms, Ecol. Lett., 13, 1419–1434, 2010.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

Orr, J. C. et al.: Anthropogenic ocean acidification over the twenty-first century and its impact on cal- cifying organisms, Nature, 437, 681–686, 2005.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Title

van Heuven, S., et al.: MATLAB program developed for CO2 system calculations, ORNL/CDIAC-105b, Carbon Dioxide Inf. Anal. Cent., Oak Ridge Natl. Lab., US DOE, Oak Ridge, Tenn., 2011.

Date (Creation)
2019-05-08
Association Type
Cross reference
Initiative Type
Reference
Language

eng

Topic category
  • Oceans
Description

bounding box

N
S
E
W


Begin date
1985-01-01

Vertical extent

Minimum value
0
Maximum value
0.0

Vertical CRS

No information provided.
Supplemental Information

display priority: 99999

Codespace

EPSG

Number of dimensions
2
Dimension name
Row
Dimension name
Column
Cell geometry
Area
Transformation parameter availability
Distribution format
Name Version

NetCDF-4

OnLine resource
Protocol Linkage Name

WWW:STAC

https://stac.marine.copernicus.eu/metadata/GLOBAL_OMI_HEALTH_carbon_ph_area_averaged/global_omi_health_carbon_ph_area_averaged_202303/dataset.stac.json

global_omi_health_carbon_ph_area_averaged

Hierarchy level
Series

Conformance result

Title

COMMISSION REGULATION (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services

Date (Publication)
2010-12-08
Explanation

See the referenced specification

Statement

The myOcean products depends on other products for production or validation. The detailed list of dependencies is given in ISO19115's aggregationInfo (ISO19139 Xpath = "gmd:MD_Metadata/gmd:identificationInfo/gmd:aggregationInfo[./gmd:MD_AggregateInformation/gmd:initiativeType/gmd:DS_InitiativeTypeCode/@codeListValue='upstream-validation' or 'upstream-production']")

Attribute description
observation
Content type
Physical measurement
Descriptor

temporal resolution: annual mean

Descriptor

vertical level number: 0

Included with dataset
Feature types
Point series

Metadata

File identifier
1c5fe986-1cd7-4c56-aeff-7bba0b4ff554
Metadata language
English
Character set
UTF8
Hierarchy level
Series
Hierarchy level name

Copernicus Marine Service product specification

Date stamp
2025-04-22T09:21:57.800168Z
Metadata standard name

ISO 19139, MyOcean profile

Metadata standard version

0.2

Metadata author
Organisation name Individual name Electronic mail address Role

CMEMS

servicedesk.cmems@mercator-ocean.eu

Local service desk
 
 

accessData

 

Overviews

Overview

Tags

Area of benefit
coastal-marine-environment marine-resources marine-safety weather-climate-and-seasonal-forecasting
Climate and Forecast Standard Names
sea_water_ph_reported_on_total_scale
Discipline
in-situ-observation
GEMET - INSPIRE themes, version 1.0
Oceanographic geographical features
Model assimilation
Not Applicable
Processing level
N/A
Reference Geographical Areas
global-ocean
Temporal scale
multi-year