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Drawing on the experience of Free Air CO 2 Enrichment (FACE) experiments used to investigate the response of terrestrial plant communities to rising atmospheric CO 2 levels, the scientific community has developed an analogous approach, Free Ocean CO 2 Enrichment (FOCE) experiments, for studying marine communities, and to complement a range of ...
LEVITUS94 is the World Ocean Atlas as of 1994, an atlas of objectively analyzed fields of major ocean parameters at the annual, seasonal, and monthly time scales. It is superseded by WOA98. NOAA NODC WOA98 is the World Ocean Atlas as of 1998, an atlas of objectively analyzed fields of major ocean parameters at monthly, seasonal, and annual time ...
Land surface temperatures have increased faster than ocean temperatures as the ocean absorbs about 92% of excess heat generated by climate change. [10] Chart with data from NASA [11] showing how land and sea surface air temperatures have changed vs a pre-industrial baseline.
Conversely, a body of water with a pCO 2 greater than that of the atmosphere effluxes carbon dioxide. [4] [5] pCO 2 is additionally affected by water temperature and salinity. Carbon dioxide is less soluble in warmer water than cooler water, so hot water will exhibit a larger pCO 2 than cold water with the same concentration of carbon dioxide.
CORA (standing for Coriolis Ocean database ReAnalysis) is a global oceanographic temperature and salinity dataset produced and maintained by the French institute IFREMER. Most of those data are real-time data coming from different types of platforms such as research vessels , profilers , underwater gliders , drifting buoys , moored buoys , sea ...
The Revelle factor (buffer factor) is the ratio of instantaneous change in carbon dioxide (CO 2) to the change in total dissolved inorganic carbon (DIC), and is a measure of the resistance to atmospheric CO 2 being absorbed by the ocean surface layer. [1]
Atmospheric carbon dioxide (CO 2) concentrations from 1958 to 2023. The Keeling Curve is a graph of the annual variation and overall accumulation of carbon dioxide in the Earth's atmosphere based on continuous measurements taken at the Mauna Loa Observatory on the island of Hawaii from 1958 to the present day.
Experts refer to the temperature further below the surface as ocean temperature or deep ocean temperature. Ocean temperatures more than 20 metres below the surface vary by region and time. They contribute to variations in ocean heat content and ocean stratification. [11] The increase of both ocean surface temperature and deeper ocean ...