Bibliographie
Allen, J., Smeed, D., et al. (2001). Mesoscale subduction at the almeria{oran front: Part 1:
Ageostrophic flow. Journal of Marine Systems, p.p.263-285.
Amores, A., Monserrat, S., et al. (2013). Vertical structure and temporal evolution of an
anticyclonic eddy in the balearic sea (western mediterranean). Journal of Geophysical
Research: Oceans, p.p. 2097-2106.
Aulicino, G., Cesarano, C., et al. (2021). On the use of ABACUS high resolution glider
observations for the assessment of phytoplankton ocean biomass from CMEMS model
products.
Aumont, O. C. (2015). PISCES-v2: an ocean biogeochemical model for carbon and ecosystem
studies. Geosci.Model Dev.,p.8.
Ayoub, N., Le Traon, P.Y., & De Mey, P. (1998). A description of the mediterranean surface
variable circulation from combined ers-1 and topex/poseidon altimetric data. Journal of Marine
Systemstopex/poseidon altimetric data. Journal of Marine Systems, p.p. 3-40.
Barceló-Llull, B., Pascual, A., & Mason, E. (2018). Comparing a Multivariate Global Ocean
State Estimate With High-Resolution in Situ Data: An Anticyclonic Intrathermocline Eddy
Near the Canary Islands. doi:10.3389/fmars.2018.00066
Beckers, J.M., & Nihoul, J. C. (1992). Model of the algerian current's instability. Journal of
marine systems, p.p.441-451.
Benzohra, M., & Millot, C. (1995). Hydrodynamics of an open sea algerian eddy. Deep Sea
Research Part I: Oceanographic Research Papers, p.p.1831-1847.
Bethoux, J., Gentili, B.,et al. (1999). The Mediterranean sea: a minature ocean of climatic and
environmental studies and a key for the climatic functioning of the North Atlantic. International
Confrence on Progress in Oceanography of the Mediterranean Sea, Rome, p.p. 131-146.
Birol, F., Cancet, M., & Estournel, C. (2010). Aspects of the seasonal variability of the
northern current (NW mediterranean sea) observed by altimetry. Journal of Marine Systemes,
p.p.297-311.
Allen, J., Smeed, D., et al. (2001). Mesoscale subduction at the almeria{oran front: Part 1:
Ageostrophic flow. Journal of Marine Systems, p.p.263-285.
Amores, A., Monserrat, S., et al. (2013). Vertical structure and temporal evolution of an
anticyclonic eddy in the balearic sea (western mediterranean). Journal of Geophysical
Research: Oceans, p.p. 2097-2106.
Aulicino, G., Cesarano, C., et al. (2021). On the use of ABACUS high resolution glider
observations for the assessment of phytoplankton ocean biomass from CMEMS model
products.
Aumont, O. C. (2015). PISCES-v2: an ocean biogeochemical model for carbon and ecosystem
studies. Geosci.Model Dev.,p.8.
Ayoub, N., Le Traon, P.Y., & De Mey, P. (1998). A description of the mediterranean surface
variable circulation from combined ers-1 and topex/poseidon altimetric data. Journal of Marine
Systemstopex/poseidon altimetric data. Journal of Marine Systems, p.p. 3-40.
Barceló-Llull, B., Pascual, A., & Mason, E. (2018). Comparing a Multivariate Global Ocean
State Estimate With High-Resolution in Situ Data: An Anticyclonic Intrathermocline Eddy
Near the Canary Islands. doi:10.3389/fmars.2018.00066
Beckers, J.M., & Nihoul, J. C. (1992). Model of the algerian current's instability. Journal of
marine systems, p.p.441-451.
Benzohra, M., & Millot, C. (1995). Hydrodynamics of an open sea algerian eddy. Deep Sea
Research Part I: Oceanographic Research Papers, p.p.1831-1847.
Bethoux, J., Gentili, B.,et al. (1999). The Mediterranean sea: a minature ocean of climatic and
environmental studies and a key for the climatic functioning of the North Atlantic. International
Confrence on Progress in Oceanography of the Mediterranean Sea, Rome, p.p. 131-146.
Birol, F., Cancet, M., & Estournel, C. (2010). Aspects of the seasonal variability of the
northern current (NW mediterranean sea) observed by altimetry. Journal of Marine Systemes,
p.p.297-311.