Oxygen and indicators of stress for marine life in multi-model global warming projections

Metadata Label Value
Author(s) Cocco, V., Joos, F., Steinacher, M., Frolicher, Thomas L., Bopp, L., Dunne, J., Gehlen, M., Heinze, C., Orr, J., Oschlies, A., Schneider, B., Segschneider, J., Tjiputra, J.
Publication Type Journal Items, Publication Status: Published
Full Text Search SFX for a Full-Text version of this document
Import to Mendeley

Detailed Information

Metadata Field Content
Title Oxygen and indicators of stress for marine life in multi-model global warming projections
Author(s) Cocco, V.
Joos, F.
Steinacher, M.
Frolicher, Thomas L.
Bopp, L.
Dunne, J.
Gehlen, M.
Heinze, C.
Orr, J.
Oschlies, A.
Schneider, B.
Segschneider, J.
Tjiputra, J.
Journal or Series Title Biogeosciences
Volume Number 10
Issue Number 3
Start Page 1849
End Page 1868
ISSN 1726-4170
Publisher Copernicus
Publication Place Göttingen
Publication Date 2013-03-19
Abstract Decadal-to-century scale trends for a range of marine environmental variables in the upper mesopelagic layer (UML, 100–600 m) are investigated using results from seven Earth System Models forced by a high greenhouse gas emission scenario. The models as a class represent the observation-based distribution of oxygen (O2) and carbon dioxide (CO2), albeit major mismatches between observation-based and simulated values remain for individual models. By year 2100 all models project an increase in SST between 2 C and 3 C, and a decrease in the pH and in the saturation state of water with respect to calcium carbonate minerals in the UML. A decrease in the total ocean inventory of dissolved oxygen by 2% to 4% is projected by the range of models. Projected O2 changes in the UML show a complex pattern with both increasing and decreasing trends reflecting the subtle balance of different competing factors such as circulation, production, remineralization, and temperature changes. Projected changes in the total volume of hypoxic and suboxic waters remain relatively small in all models. A widespread increase of CO2 in the UML is projected. The median of the CO2 distribution between 100 and 600m shifts from 0.1–0.2 molm−3 in year 1990 to 0.2–0.4 molm−3 in year 2100, primarily as a result of the invasion of anthropogenic carbon from the atmosphere. The co-occurrence of changes in a range of environmental variables indicates the need to further investigate their synergistic impacts on marine ecosystems and Earth System feedbacks.
DOI 10.5194/bg-10-1849-2013
Additional Notes Received 18 July 2012, Published in Biogeosciences Discussion 13 August 2012, Revised 22 February 2013, Accepted 27 February 2013
Document Type Article
Publication Status Published
Language English
Assigned Organisational Unit(s) 03731
Organisational Unit(s)
NEBIS System Number 006289717
Source Database ID FORM-1384957301
Description File Name MIME Type Size
No details could be found
There are no links available for this record.
This record has not been viewed during this period

  author = "Cocco, V. and Joos, F. and Steinacher, M. and Frolicher, Thomas L. and Bopp, L. and Dunne, J. and Gehlen, M. and Heinze, C. and Orr, J. and Oschlies, A. and Schneider, B. and Segschneider, J. and Tjiputra, J.",
  title = "{O}xygen and indicators of stress for marine life in multi-model global warming projections",
  journal = "Biogeosciences",
  year = 2013,
  volume = "10",
  number = "3",
  pages = "1849--1868",
  month = mar,

E-Citations record created: Wed, 20 Nov 2013, 14:21:43 CET