Using Noble Gases to Assess the Ocean's Carbon Pumps

Type : OS
Nature : Production scientifique
Au bénéfice du Laboratoire : Non
Statut de publication : Publié
Année de publication : 2019
Lieu de publication : -
Titre de l'ouvrage : Annual Review of Marine Science
ISBN : 1941-1405
Nombre de pages : -
Editeur de presse : -
Volume : 11
Fascicule : -
Pages : 75-103
Auteurs (4) : HAMME Roberta,c NICHOLSON David JENKINS W,j EMERSON S,r
Editeurs scientifiques (0) :
DOI : 10.1146/annurev-marine-121916-063604
URL : -
Abstract : Natural mechanisms in the ocean, both physical and biological, concentrate carbon in the deep ocean, resulting in lower atmospheric carbon dioxide. The signals of these carbon pumps overlap to create the observed carbon distribution in the ocean, making the individual impact of each pump difficult to disentangle. Noble gases have the potential to directly quantify the physical carbon solubility pump and to indirectly improve estimates of the biological organic carbon pump. Noble gases are biologically inert, can be precisely measured, and span a range of physical properties. We present dissolved neon, argon, and krypton data spanning the Atlantic, Southern, Pacific, and Arctic Oceans. Comparisons between deep-ocean observations and models of varying complexity enable the rates of processes that control the carbon solubility pump to be quantified and thus provide an important metric for ocean model skill. Noble gases also provide a powerful means of assessing air-sea gas exchange parameterizations.
Mots-clés : air-sea exchange; ATMOSPHERIC CO2; BIOLOGICAL PRODUCTION; biological pump; bubbles; CLIMATE-CHANGE; DISSOLVED-GASES; EXCESS HELIUM; FAST SPIN-UP; NET COMMUNITY PRODUCTION; noble gases; ocean carbon cycle; SITU OXYGEN MEASUREMENTS; solubility pump; SOLUBILITY PUMP; SOUTHERN-OCEAN; ventilation
Commentaire : Times Cited in Web of Science Core Collection: 10
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Citation :
Hamme RC, Nicholson D, Jenkins WJ, Emerson SR (2019) Using Noble Gases to Assess the Ocean's Carbon Pumps. Annual Review of Marine Science, , 75-103 | doi: 10.1146/annurev-marine-121916-063604