Observing the full ocean volume using Deep Argo floats

Observing the full ocean volume using Deep Argo floats

The ocean is the main heat reservoir in Earth’s climate system, absorbing most of the top-of-the-atmosphere excess radiation. As the climate warms, anomalously warm and fresh ocean waters in the densest layers formed near Antarctica spread northward through the abyssal ocean, while successions of wa...

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Váldodahkkit: Nathalie V. Zilberman, Virginie Thierry, Brian King, Matthew Alford, Xavier André, Kevin Balem, Nathan Briggs, Zhaohui Chen, Cécile Cabanes, Laurent Coppola, Giorgio Dall’Olmo, Damien Desbruyères, Denise Fernandez, Annie Foppert, Wilford Gardner, Florent Gasparin, Bryan Hally, Shigeki Hosoda, Gregory C. Johnson, Taiyo Kobayashi, Arnaud Le Boyer, William Llovel, Peter Oke, Sarah Purkey, Elisabeth Remy, Dean Roemmich, Megan Scanderbeg, Philip Sutton, Kamila Walicka, Luke Wallace, Esmee M. van Wijk
Materiálatiipa: Artihkal
Giella:English
Almmustuhtton: Frontiers Media S.A. 2023-11-01
Ráidu:Frontiers in Marine Science
Fáttát:
deep ocean
ocean observation
ocean heat content (OHC)
sea level (SL)
ocean deoxygenation
bathymetry accuracy
Liŋkkat:https://www.frontiersin.org/articles/10.3389/fmars.2023.1287867/full

Interneahtta

https://www.frontiersin.org/articles/10.3389/fmars.2023.1287867/full

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