Articles | Volume 19, issue 17
https://doi.org/10.5194/bg-19-4035-2022
https://doi.org/10.5194/bg-19-4035-2022
Research article
 | 
01 Sep 2022
Research article |  | 01 Sep 2022

Acidification, deoxygenation, and nutrient and biomass declines in a warming Mediterranean Sea

Marco Reale, Gianpiero Cossarini, Paolo Lazzari, Tomas Lovato, Giorgio Bolzon, Simona Masina, Cosimo Solidoro, and Stefano Salon

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Cited articles

Adloff, F., Somot, S., Sevault, F., Jordà, G., Aznar, R., Déqué, M., Herrmann, M., Marcos, M., Dubois, C., Padorno, E., Alcarez-Fanjul, E., and Gomis, D.: Mediterranean Sea response to climate change in an ensemble of twenty first century scenarios, Clim. Dyn., 45, 2775–2802, https://doi.org/10.1007/s00382-015-2507-3, 2015. 
Álvarez, M., Sanleón-Bartolomé, H., Tanhua, T., Mintrop, L., Luchetta, A., Cantoni, C., Schroeder, K., and Civitarese, G.: The CO2 system in the Mediterranean Sea: a basin wide perspective, Ocean Sci., 10, 69–92, https://doi.org/10.5194/os-10-69-2014, 2014. 
Auger, P. A., Ulses, C., Estournel, C., Stemman, L., Somot, S., and Diaz, F.: Interannual control of plankton ecosystem in a deep convection area as inferred from a 30-year 3D modeling study: winter mixing and prey/predator in the NW Mediterranean, Prog. Oceanogr., 124, 12–27, https://doi.org/10.1016/j.pocean.2014.04.004, 2014. 
Benedetti, F., Guilhaumon, F., Adloff, F., and Ayata, S. D: Investigating uncertainties in zooplankton composition shifts under climate change scenarios in the Mediterranean Sea, Ecography, 41, 345–360, https://doi.org/10.1111/ecog.02434, 2018. 
Bethoux, J. P., Morin, P., Chaumery, C., Connan, O., Gentili, B., and Ruiz-Pino, D.: Nutrients in the Mediterranean Sea, mass balance and statistical analysis of concentrations with respect to environmental change, Mar. Chem., 63, 155–169, 1998. 
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Short summary
Future projections under the RCP8.5 and RCP4.5 emission scenarios of the Mediterranean Sea biogeochemistry at the end of the 21st century show different levels of decline in nutrients, oxygen and biomasses and an acidification of the water column. The signal intensity is stronger under RCP8.5 and in the eastern Mediterranean. Under RCP4.5, after the second half of the 21st century, biogeochemical variables show a recovery of the values observed at the beginning of the investigated period.
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