¡Nos trasladamos! E-Prints cerrará el 7 de junio.

En las próximas semanas vamos a migrar nuestro repositorio a una nueva plataforma con muchas funcionalidades nuevas. En esta migración las fechas clave del proceso son las siguientes:

Es muy importante que cualquier depósito se realice en E-Prints Complutense antes del 7 de junio. En caso de urgencia para realizar un depósito, se puede comunicar a docta@ucm.es.

Tropical Atlantic mixed layer buoyancy seasonality: atmospheric and oceanic physical processes contributions



Downloads per month over past year

Camara, Ibrahima and Mignot, Juliette and Kolodziejczyk, Nicolas and Losada Doval, Teresa and Lazar, Alban (2020) Tropical Atlantic mixed layer buoyancy seasonality: atmospheric and oceanic physical processes contributions. Atmosphere, 11 (6). ISSN 2073-4433

[thumbnail of losadadoval04libre+CC.pdf]
Creative Commons Attribution.


Official URL: http://dx.doi.org/10.3390/atmos11060649


This study investigates the physical processes controlling the mixed layer buoyancy using a regional configuration of an ocean general circulation model. Processes are quantified by using a linearized equation of state, a mixed-layer heat, and a salt budget. Model results correctly reproduce the observed seasonal near-surface density tendencies. The results indicate that the heat flux is located poleward of 10◦ of latitude, which is at least three times greater than the freshwater flux that mainly controls mixed layer buoyancy. During boreal spring-summer of each hemisphere, the freshwater flux partly compensates the heat flux in terms of buoyancy loss while, during the fall-winter, they act together. Under the seasonal march of the Inter-tropical Convergence Zone and in coastal areas affected by the river, the contribution of ocean processes on the upper density becomes important. Along the north Brazilian coast and the Gulf of Guinea, horizontal and vertical processes involving salinity are the main contributors to an upper water change with a contribution of at least twice as much the temperature. At the equator and along the Senegal-Mauritanian coast, vertical processes are the major oceanic contributors. This is mainly due to the vertical gradient of temperature at the mixed layer base in the equator while the salinity one dominates along the Senegal-Mauritania coast.

Item Type:Article
Additional Information:

© 2020 by the authors. The authors thank the Laboratoire de Physique de l’Atmosphère et de l’Océan Siméon Fongang (LPAO-SF) of the University Cheikh Anta Diop de Dakar where the work was mainly done. The editor and the anonymous reviewers are also sincerely thanked for their valuable comments and suggestions to improve the quality of the paper. : IRD, grant number 182SNLMIE2, funded this research. This study was also supported by the CNES TOSCA SMOS OCEAN project.

Uncontrolled Keywords:Sea-surface salinity; Water mass transformation; Temperature; Subduction; Balance
Subjects:Sciences > Physics > Atmospheric physics
ID Code:62145
Deposited On:23 Sep 2020 09:33
Last Modified:23 Sep 2020 09:33

Origin of downloads

Repository Staff Only: item control page