Interaction of dense shelf water cascading and open-sea convection in the northwestern Mediterranean during winter 2012. Madron, X. D. d., Houpert, L., Puig, P., Sanchez‐Vidal, A., Testor, P., Bosse, A., Estournel, C., Somot, S., Bourrin, F., Bouin, M. N., Beauverger, M., Beguery, L., Calafat, A., Canals, M., Cassou, C., Coppola, L., Dausse, D., D'Ortenzio, F., Font, J., Heussner, S., Kunesch, S., Lefevre, D., Goff, H. L., Martín, J., Mortier, L., Palanques, A., & Raimbault, P. 40(7):1379–1385. Number: 7![Interaction of dense shelf water cascading and open-sea convection in the northwestern Mediterranean during winter 2012 [link]](https://bibbase.org/img/filetypes/link.svg "link")
Paper doi abstract bibtex AbstractThe winter of 2012 experienced peculiar atmospheric conditions that triggered a massive formation of dense water on the continental shelf and in the deep basin of the Gulf of Lions. Multiplatforms observations enabled a synoptic view of dense water formation and spreading at basin scale. Five months after its formation, the dense water of coastal origin created a distinct bottom layer up to a few hundreds of meters thick over the central part of the NW Mediterranean basin, which was overlaid by a layer of newly formed deep water produced by open-sea convection. These new observations highlight the role of intense episodes of both dense shelf water cascading and open-sea convection to the progressive modification of the NW Mediterranean deep waters.
@article{madron_interaction_2013,
title = {Interaction of dense shelf water cascading and open-sea convection in the northwestern Mediterranean during winter 2012},
volume = {40},
rights = {©2013. American Geophysical Union. All Rights Reserved.},
issn = {1944-8007},
url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1002/grl.50331},
doi = {10.1002/grl.50331},
abstract = {{AbstractThe} winter of 2012 experienced peculiar atmospheric conditions that triggered a massive formation of dense water on the continental shelf and in the deep basin of the Gulf of Lions. Multiplatforms observations enabled a synoptic view of dense water formation and spreading at basin scale. Five months after its formation, the dense water of coastal origin created a distinct bottom layer up to a few hundreds of meters thick over the central part of the {NW} Mediterranean basin, which was overlaid by a layer of newly formed deep water produced by open-sea convection. These new observations highlight the role of intense episodes of both dense shelf water cascading and open-sea convection to the progressive modification of the {NW} Mediterranean deep waters.},
pages = {1379--1385},
number = {7},
journaltitle = {Geophysical Research Letters},
author = {Madron, X. Durrieu de and Houpert, L. and Puig, P. and Sanchez‐Vidal, A. and Testor, P. and Bosse, A. and Estournel, C. and Somot, S. and Bourrin, F. and Bouin, M. N. and Beauverger, M. and Beguery, L. and Calafat, A. and Canals, M. and Cassou, C. and Coppola, L. and Dausse, D. and D'Ortenzio, F. and Font, J. and Heussner, S. and Kunesch, S. and Lefevre, D. and Goff, H. Le and Martín, J. and Mortier, L. and Palanques, A. and Raimbault, P.},
urldate = {2019-04-15},
date = {2013},
langid = {english},
note = {Number: 7},
keywords = {Mediterranean Sea, Dense water formation, Dense shelf water cascading, Open-sea convection}
}
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American Geophysical Union. All Rights Reserved.},\n\tissn = {1944-8007},\n\turl = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1002/grl.50331},\n\tdoi = {10.1002/grl.50331},\n\tabstract = {{AbstractThe} winter of 2012 experienced peculiar atmospheric conditions that triggered a massive formation of dense water on the continental shelf and in the deep basin of the Gulf of Lions. Multiplatforms observations enabled a synoptic view of dense water formation and spreading at basin scale. Five months after its formation, the dense water of coastal origin created a distinct bottom layer up to a few hundreds of meters thick over the central part of the {NW} Mediterranean basin, which was overlaid by a layer of newly formed deep water produced by open-sea convection. 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