Ocean Physicochemistry versus Climate Change

dc.contributor.author	Góralski, Bogdan
dc.contributor.organization	Biblioteka Instytutu Historycznego Uniwersytetu Warszawskiego	en
dc.date.accessioned	2014-03-04T21:25:05Z
dc.date.available	2014-03-04T21:25:05Z
dc.date.issued	2014-03-04
dc.description	It is the dwindling ocean productivity which leaves dissolved carbon dioxide in the seawater. Its solubility is diminished by the rise in ocean water temperature (by one degree Celsius since 1910, according to IPCC). Excess carbon dioxide is emitted into the atmosphere, while its growing concentration in seawater leads to ocean acidification.	en
dc.description.abstract	Ocean acidification leading to lowering pH of surface ocean water remains an unsolved problem of science. My today’s lecture will mark an attempt at proving that this is a regular phenomenon in the ocean history linked to changes in the Earth’s climate.	en
dc.description.eperson	Bogdan Góralski
dc.identifier.uri	https://open.icm.edu.pl/handle/123456789/3578
dc.language.iso	en	en
dc.rights	Uznanie autorstwa-Na tych samych warunkach 3.0 Polska	pl_PL
dc.rights.uri	http://creativecommons.org/licenses/by-sa/3.0/pl/
dc.subject	carbon dioxide in the atmosphere	en
dc.subject	biological productivity in the oceans	en
dc.subject	ocean acidification	en
dc.title	Ocean Physicochemistry versus Climate Change	en
dc.type	article	en

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