@article{Fernandez_etal_2005_JMS.pdf,
  title = {Influence of mesoscale eddies on nitrate distribution during the POMME program in the northeast Atlantic Ocean},
  author = {I. C. Fernandez and P. Raimbault and G. Caniaux and N. Garcia and P. Rimmelin},
  pages = {155--175},
  year = 2005,
  journal = {JOURNAL OF MARINE SYSTEMS},
  volume = 55,
  url = {http://archipelago.uma.pt/pdf_library/Fernandez_etal_2005_JMS.pdf},
  abstract = {Three cruises were carried out as part of the Programme Ocean Multidisciplinaire Meso Echelle (POMME) program between February and October 2001, in the northeast Atlantic basin (16 degrees W-22 degrees W, 38 degrees N-45 degrees N). The hydrographic survey showed a permanent frontal zone at 41 degrees N-42 degrees N characterized by an intense isopycrial displacement. North of 41 degrees N, average mixed layer depths evolved from 100 in in winter to 75 m in spring. In that area, vertical mixing was modulating the available nutrients in the surface layer, which resulted in surface nitrate concentrations close to 7 mu M at 44.5 degrees N. The area located south of the front was characterized by low surface nutrient values (similar to 1 mu M NO3) caused mainly by biological activity. During these surveys, several mesoscale features were studied. Cyclonic structures at 42 degrees N had a continuous effect on the vertical nitrate distribution in the euphotic layer from winter to spring. The presence of an anticyclonic structure north of the frontal zone resulted in lifting the seasonal thermocline in summer along with a depression of the permanent thermocline, which induced anomalously high nitrate concentrations (5-9 mu M) between 50 and 300 m depth. South of the frontal zone, the presence of an anticyclonic eddy at 40.5 degrees N also enhanced nutrient enrichment in the surface layer. As the presence of mesoscale eddies influenced the nutrient distribution, the processes responsible for nutrient injection to the euphotic zone are discussed. (c) 2004 Elsevier B.V. All rights reserved.}
}