38 [Thirty eight] dynamics of meditrranean deep waters / CIESM

Public ISBD Faire une suggestion d'achat Titre : 38 [Thirty eight] dynamics of meditrranean deep waters Type de document : texte imprimé Auteurs : CIESM, Auteur Editeur : Ciesm Workshop Monographs Année de publication : 2009 Importance : 132 p. Format : 30 cm. Langues : Anglais (eng) Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : All water masses in the deep ocean acquired their characteristics when they were in contact with the ocean surface. The ocean thermohaline circulation is responsible for the further spreading of the newly formed water masses to all ocean regions. The deep component of this conveyor belt, with its slow, but very relevant dynamics, is still poorly known, from both the physical and biological points of view. The Mediterranean is a semi-enclosed sea whose geographical, morphological and hydrological characteristics allow several oceanographic processes, found at large scale in the open ocean, to occur, but on a reduced scale. One of these is the wintertime formation of dense water by atmospheric cooling and desiccation, as well as by sinking of cold dense waters cascading off the continental shelf. These processes can occur until most of the deep Mediterranean basin has been renewed. 38 [Thirty eight] dynamics of meditrranean deep waters [texte imprimé] / CIESM, Auteur . - Ciesm Workshop Monographs, 2009 . - 132 p. ; 30 cm. Langues : Anglais (eng) Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : All water masses in the deep ocean acquired their characteristics when they were in contact with the ocean surface. The ocean thermohaline circulation is responsible for the further spreading of the newly formed water masses to all ocean regions. The deep component of this conveyor belt, with its slow, but very relevant dynamics, is still poorly known, from both the physical and biological points of view. The Mediterranean is a semi-enclosed sea whose geographical, morphological and hydrological characteristics allow several oceanographic processes, found at large scale in the open ocean, to occur, but on a reduced scale. One of these is the wintertime formation of dense water by atmospheric cooling and desiccation, as well as by sinking of cold dense waters cascading off the continental shelf. These processes can occur until most of the deep Mediterranean basin has been renewed.

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38 [Thirty eight] dynamics of meditrranean deep waters / CIESM

Public ISBD Faire une suggestion d'achat Titre : 38 [Thirty eight] dynamics of meditrranean deep waters Type de document : texte imprimé Auteurs : CIESM, Auteur Editeur : Ciesm Workshop Monographs Année de publication : 2009 Importance : 132 p. Format : 30 cm. Langues : Anglais (eng) Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : All water masses in the deep ocean acquired their characteristics when they were in contact with the ocean surface. The ocean thermohaline circulation is responsible for the further spreading of the newly formed water masses to all ocean regions. The deep component of this conveyor belt, with its slow, but very relevant dynamics, is still poorly known, from both the physical and biological points of view. The Mediterranean is a semi-enclosed sea whose geographical, morphological and hydrological characteristics allow several oceanographic processes, found at large scale in the open ocean, to occur, but on a reduced scale. One of these is the wintertime formation of dense water by atmospheric cooling and desiccation, as well as by sinking of cold dense waters cascading off the continental shelf. These processes can occur until most of the deep Mediterranean basin has been renewed. 38 [Thirty eight] dynamics of meditrranean deep waters [texte imprimé] / CIESM, Auteur . - Ciesm Workshop Monographs, 2009 . - 132 p. ; 30 cm. Langues : Anglais (eng) Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : All water masses in the deep ocean acquired their characteristics when they were in contact with the ocean surface. The ocean thermohaline circulation is responsible for the further spreading of the newly formed water masses to all ocean regions. The deep component of this conveyor belt, with its slow, but very relevant dynamics, is still poorly known, from both the physical and biological points of view. The Mediterranean is a semi-enclosed sea whose geographical, morphological and hydrological characteristics allow several oceanographic processes, found at large scale in the open ocean, to occur, but on a reduced scale. One of these is the wintertime formation of dense water by atmospheric cooling and desiccation, as well as by sinking of cold dense waters cascading off the continental shelf. These processes can occur until most of the deep Mediterranean basin has been renewed.

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