Consulta: creatorFacets:"Andrie, C"
Registros recuperados: 4
Data/hora: 09/06/2024 15:48:45

Variabilité des pressions partielles de CO2 océanique et atmosphérique dans l'Atlantic tropical
Provedor de dados: 5
Autores: Oudot, C; Andrie, C.
Tipo: Text
Ano: 1986
URL: http://archimer.ifremer.fr/doc/00110/22129/19765.pdf

Assessments of anthropogenic CO2 distribution in the tropical Atlantic Ocean
Provedor de dados: 5
Autores: Touratier, Franck; Goyet, C; Coatanoan, Christine; Andrie, C.
With a limited number of properties (salinity, temperature, total dissolved inorganic carbon, total alkalinity, and oxygen) from a recent cruise in the tropical Atlantic Ocean, We use the simple and recent approach TrOCA (Tracer combining Oxygen, inorganic Carbon, and total Alkalinity) to estimate the distribution of anthropogenic CO2 along three latitudinal sections. In order to assess the quality of the anthropogenic CO2 distribution, results from the method are compared to the CFC-11 measurements. We discuss the large-scale distribution of the main water masses of the tropical Atlantic Ocean in the light of the anthropogenic CO2 and the CFC-11 distributions. Keeping in mind that the anthropogenic CO2 emission began similar to 60 years earlier than that...
Tipo: Text
Palavras-chave: Tropical belt; Atlantic Ocean; Water mass; Carbon cycle.
Ano: 2005
URL: http://archimer.ifremer.fr/doc/2005/publication-886.pdf

Contribution des données isotopiques de deutérium, oxygène-18, hélium-3 et tritium, à l'étude de la circulation de la Mer Rouge
Provedor de dados: 5
Autores: Andrie, C; Merlivat, L.
Tipo: Text
Ano: 1989
URL: http://archimer.ifremer.fr/doc/00106/21745/19318.pdf

Deep circulation in the equatorial Atlantic Ocean
Provedor de dados: 5
Autores: Gouriou, Y; Andrie, C; Bourles, B; Freudenthal, S; Arnault, S; Aman, A; Eldin, G; Du Penhoat, Y; Baurand, F; Gallois, F; Chuchla, R.
In the Atlantic Ocean, the northward export of warm surface water is compensated by a southward flow of cold North Atlantic Deep Water (NADW). The NADW is transported southward along the American continental margin within the Deep Western Boundary Current (DWBC). Some tracer and float observations have shown that part of the DWBC water flows eastward along the equator. Here we present three meridional velocity sections which give an instantaneous image of the top-to-bottom zonal circulation along the equatorial Atlantic. They reveal the presence of Equatorial Deep Jets (EDJs) between 1 degrees 30'N and 1 degrees 30'S, alternating eastward-westward currents with short vertical scale, surrounded by columns of eastward currents (the Extra Equatorial Jets or...
Tipo: Text
Ano: 2001
URL: http://archimer.ifremer.fr/doc/00000/10369/9567.pdf