Le laboratoire Morphodynamique Continentale et Côtière (M2C) est un laboratoire de recherche fondamentale et appliquée de 50 permanents (environ 90 personnes avec les doctorants, post-doctorants, etc.). Le laboratoire est présent sur deux sites géographiques, Caen et Rouen. Nous sommes membres de l’Observatoire Ecce Terra, de la Fédération de Recherche SCALE et du Centre de recherche en Environnement Côtier. Nos domaines de compétences sont ceux des Géosciences et des Sciences de l’Environnement bâtis autour de personnels affiliés à 3 tutelles différentes (CNRS, Université de Caen Normandie et Université de Rouen Normandie).
[{"id":1497,"link":"https:\/\/m2c.cnrs.fr\/une-analyse-multi-approche-pour-le-monitoring-de-lenergie-des-vagues-provoquees-par-des-evenements-extremes-cotiers\/","name":"une-analyse-multi-approche-pour-le-monitoring-de-lenergie-des-vagues-provoquees-par-des-evenements-extremes-cotiers","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/09\/actu-202406-03.png","alt":""},"title":"Une analyse multi-approche pour le monitoring de l'\u00e9nergie des vagues provoqu\u00e9es par des \u00e9v\u00e9nements extr\u00eames c\u00f4tiers","excerpt":"","content":"Cette recherche \u00e9tudie le comportement et l'\u00e9volution de la fr\u00e9quence des vagues extr\u00eames dans les zones c\u00f4ti\u00e8res en combinant la mod\u00e9lisation physique, l'analyse spectrale et","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"Sep 9, 2024","dateGMT":"2024-09-09 12:31:42","modifiedDate":"2024-09-09 14:31:43","modifiedDateGMT":"2024-09-09 12:31:43","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":15},"status":"publish"},{"id":1494,"link":"https:\/\/m2c.cnrs.fr\/extraction-de-granulats-marins-sablo-graveleux-au-large-de-la-baie-de-seine-quels-effets-ecologiques-dans-un-contexte-de-fort-hydrodynamisme\/","name":"extraction-de-granulats-marins-sablo-graveleux-au-large-de-la-baie-de-seine-quels-effets-ecologiques-dans-un-contexte-de-fort-hydrodynamisme","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/09\/actu-202406-02.png","alt":""},"title":"Extraction de granulats marins sablo-graveleux au large de la baie de Seine :Quels effets \u00e9cologiques dans un contexte de fort hydrodynamisme\u00a0?","excerpt":"","content":"L'extraction de granulats marins repr\u00e9sente une opportunit\u00e9 pour pallier l'\u00e9puisement des ressources terrestres en granulats et \u00e0 l\u2019augmentation de la demande, a fortiori au niveau","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"Sep 9, 2024","dateGMT":"2024-09-09 12:29:05","modifiedDate":"2024-09-09 14:29:07","modifiedDateGMT":"2024-09-09 12:29:07","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":35},"status":"publish"},{"id":1491,"link":"https:\/\/m2c.cnrs.fr\/trajectoires-temporelles-reconstituees-a-partir-de-carottes-de-sedimentsdu-radionucleide-artificiel-137cs-dans-les-rivieres-francaises-au-cours-de-lere-nucleaire\/","name":"trajectoires-temporelles-reconstituees-a-partir-de-carottes-de-sedimentsdu-radionucleide-artificiel-137cs-dans-les-rivieres-francaises-au-cours-de-lere-nucleaire","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/09\/actu-202406-01.png","alt":""},"title":"Trajectoires temporelles reconstitu\u00e9es \u00e0 partir de carottes de s\u00e9dimentsdu radionucl\u00e9ide artificiel 137Cs dans les rivi\u00e8res fran\u00e7aises au cours de l'\u00e8re nucl\u00e9aire","excerpt":"","content":"Le 137Cs est un radionucl\u00e9ide artificiel \u00e0 vie longue introduit dans l\u2019environnement mondial au d\u00e9but de l\u2019\u00e8re nucl\u00e9aire lors d\u2019essais nucl\u00e9aires atmosph\u00e9riques suivis par l\u2019utilisation","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"Sep 9, 2024","dateGMT":"2024-09-09 12:27:28","modifiedDate":"2024-09-09 14:27:30","modifiedDateGMT":"2024-09-09 12:27:30","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":39},"status":"publish"},{"id":1421,"link":"https:\/\/m2c.cnrs.fr\/reconstruction-du-niveau-des-eaux-souterraines-a-laide-de-donnees-de-reanalyse-climatique-a-long-terme-et-de-deep-learning\/","name":"reconstruction-du-niveau-des-eaux-souterraines-a-laide-de-donnees-de-reanalyse-climatique-a-long-terme-et-de-deep-learning","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/04\/actu-202403-04.png","alt":""},"title":"Reconstruction du niveau des eaux souterraines \u00e0 l'aide de donn\u00e9es de r\u00e9analyse climatique \u00e0 long terme et de deep learning","excerpt":"","content":"L'\u00e9valuation des changements \u00e0 long terme des eaux souterraines est cruciale pour comprendre les impacts des changements climatiques sur les aquif\u00e8res et pour leur gestion","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"Avr 14, 2024","dateGMT":"2024-04-14 09:31:14","modifiedDate":"2024-04-14 11:31:54","modifiedDateGMT":"2024-04-14 09:31:54","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":34},"status":"publish"},{"id":1416,"link":"https:\/\/m2c.cnrs.fr\/granulometrie-et-structure-des-communautes-benthiques-en-manche-orientale-reponses-specifiques-et-influence-environnementale\/","name":"granulometrie-et-structure-des-communautes-benthiques-en-manche-orientale-reponses-specifiques-et-influence-environnementale","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/04\/actu-202403-03.png","alt":""},"title":"Granulom\u00e9trie et structure des communaut\u00e9s benthiques en Manche orientale : R\u00e9ponses sp\u00e9cifiques et influence environnementale.","excerpt":"","content":"Plusieurs \u00e9tudes ont explor\u00e9 la relation entre la structure des communaut\u00e9s benthiques et la granulom\u00e9trie des s\u00e9diments, r\u00e9v\u00e9lant des liens plus ou moins prononc\u00e9s entre","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"Avr 14, 2024","dateGMT":"2024-04-14 09:27:20","modifiedDate":"2024-04-14 11:28:17","modifiedDateGMT":"2024-04-14 09:28:17","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":44},"status":"publish"},{"id":1411,"link":"https:\/\/m2c.cnrs.fr\/estimation-de-levolution-de-lensablement-dans-le-reservoir-camastra-italie-et-propositions-de-recuperation-des-sediments\/","name":"estimation-de-levolution-de-lensablement-dans-le-reservoir-camastra-italie-et-propositions-de-recuperation-des-sediments","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/04\/actu-202403-02.png","alt":""},"title":"Estimation de l'\u00e9volution de l'ensablement dans le r\u00e9servoir Camastra (Italie) et propositions de r\u00e9cup\u00e9ration des s\u00e9diments","excerpt":"","content":"La r\u00e9duction de la capacit\u00e9 utilisable des r\u00e9servoirs de barrage, li\u00e9e au ph\u00e9nom\u00e8ne en cours d'ensablement, a conduit \u00e0 la n\u00e9cessit\u00e9 d'extraire des s\u00e9diments pour","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"Avr 14, 2024","dateGMT":"2024-04-14 09:23:46","modifiedDate":"2024-04-14 11:24:39","modifiedDateGMT":"2024-04-14 09:24:39","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":2,"sec":0},"status":"publish"},{"id":1407,"link":"https:\/\/m2c.cnrs.fr\/suivi-experimental-de-la-degradation-du-pergelisol-cotier-en-canal-a-houle\/","name":"suivi-experimental-de-la-degradation-du-pergelisol-cotier-en-canal-a-houle","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/04\/actu-202403-01.png","alt":""},"title":"Suivi exp\u00e9rimental de la d\u00e9gradation du perg\u00e9lisol c\u00f4tier en canal \u00e0 houle","excerpt":"","content":"Dans le cadre de la th\u00e8se de J\u00e9r\u00e9miah Cl\u00e9ment (co-tutelle M2C Universit\u00e9 de Caen et INRS, Qu\u00e9bec), portant sur l\u2019\u00e9rosion du perg\u00e9lisol c\u00f4tier, plusieurs exp\u00e9riences","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"Avr 14, 2024","dateGMT":"2024-04-14 09:20:06","modifiedDate":"2024-04-14 11:20:49","modifiedDateGMT":"2024-04-14 09:20:49","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe-fr\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":52},"status":"publish"},{"id":24,"link":"https:\/\/m2c.cnrs.fr\/imager-lepaisseur-de-la-couche-active-sous-la-vegetation-pour-lamelioration-des-modeles-de-climat\/","name":"imager-lepaisseur-de-la-couche-active-sous-la-vegetation-pour-lamelioration-des-modeles-de-climat","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/02\/actu-202312-05.png","alt":""},"title":"Imager l'\u00e9paisseur de la couche active sous la v\u00e9g\u00e9tation pour l'am\u00e9lioration des mod\u00e8les de climat","excerpt":"","content":"L'\u00e9paisseur de la couche active, partie superficielle du sol qui d\u00e9g\u00e8le saisonni\u00e8rement sur 1\/5 des surfaces continentales, est une des grandes inconnues des stocks de","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"F\u00e9v 3, 2024","dateGMT":"2024-02-03 18:16:04","modifiedDate":"2024-03-04 10:51:14","modifiedDateGMT":"2024-03-04 09:51:14","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":16},"status":"publish"},{"id":21,"link":"https:\/\/m2c.cnrs.fr\/morphologie-et-dynamique-de-dunes-fluviatiles-dans-des-conditions-dapport-sedimentaire-limite-une-experimentation-dans-la-seine\/","name":"morphologie-et-dynamique-de-dunes-fluviatiles-dans-des-conditions-dapport-sedimentaire-limite-une-experimentation-dans-la-seine","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/02\/actu-202312-04.png","alt":""},"title":"Morphologie et dynamique de dunes fluviatiles dans des conditions d'apport s\u00e9dimentaire limit\u00e9. Une exp\u00e9rimentation dans la Seine","excerpt":"","content":"La dynamique de dunes hydrauliques et les flux s\u00e9dimentaires associ\u00e9s ont \u00e9t\u00e9 estim\u00e9s sur une p\u00e9riode d'une semaine dans la Seine (en amont de barrage","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"F\u00e9v 3, 2024","dateGMT":"2024-02-03 18:15:20","modifiedDate":"2024-03-04 10:51:14","modifiedDateGMT":"2024-03-04 09:51:14","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":34},"status":"publish"},{"id":18,"link":"https:\/\/m2c.cnrs.fr\/modele-et-methode-de-prediction-de-lenergie-cinetique-turbulente-generee-par-les-courants-de-maree-application-a-la-turbulence-generee-par-les-vagues\/","name":"modele-et-methode-de-prediction-de-lenergie-cinetique-turbulente-generee-par-les-courants-de-maree-application-a-la-turbulence-generee-par-les-vagues","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/02\/actu-202312-03.png","alt":""},"title":"Mod\u00e8le et m\u00e9thode de pr\u00e9diction de l'\u00e9nergie cin\u00e9tique turbulente g\u00e9n\u00e9r\u00e9e par les courants de mar\u00e9e, application \u00e0 la turbulence g\u00e9n\u00e9r\u00e9e par les vagues","excerpt":"","content":"Un mod\u00e8le de pr\u00e9diction pour l'\u00e9nergie cin\u00e9tique turbulente provenant de l'interaction des courants de mar\u00e9e avec le fond marin est propos\u00e9, il ne d\u00e9pend que","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"F\u00e9v 3, 2024","dateGMT":"2024-02-03 18:14:33","modifiedDate":"2024-03-04 10:51:14","modifiedDateGMT":"2024-03-04 09:51:14","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":6},"status":"publish"},{"id":15,"link":"https:\/\/m2c.cnrs.fr\/effets-de-changements-dans-la-variabilite-climatique-sur-le-ruissellement-et-lerosion-dans-la-region-de-la-ceinture-loessique-ouest-europeenne-nw-france\/","name":"effets-de-changements-dans-la-variabilite-climatique-sur-le-ruissellement-et-lerosion-dans-la-region-de-la-ceinture-loessique-ouest-europeenne-nw-france","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/02\/actu-202312-02.png","alt":""},"title":"Effets de changements dans la variabilit\u00e9 climatique sur le ruissellement et l'\u00e9rosion dans la r\u00e9gion de la ceinture l\u0153ssique ouest-europ\u00e9enne (NW, France)","excerpt":"","content":"Le ruissellement et l\u2019\u00e9rosion des sols sont tr\u00e8s marqu\u00e9s dans la ceinture l\u0153ssique ouest europ\u00e9enne. Dans cette \u00e9tude, le mod\u00e8le distribu\u00e9 \u00e0 base physique CLiDE","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"F\u00e9v 3, 2024","dateGMT":"2024-02-03 18:12:29","modifiedDate":"2024-03-04 10:51:15","modifiedDateGMT":"2024-03-04 09:51:15","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":51},"status":"publish"},{"id":10,"link":"https:\/\/m2c.cnrs.fr\/styles-fluviaux-et-croissance-des-plis-actifs-un-exemple-du-segment-oriental-des-plis-qiulitage-et-yakeng-tian-shan-meridional-chine\/","name":"styles-fluviaux-et-croissance-des-plis-actifs-un-exemple-du-segment-oriental-des-plis-qiulitage-et-yakeng-tian-shan-meridional-chine","thumbnail":{"url":"https:\/\/m2c.cnrs.fr\/wp-content\/uploads\/2024\/02\/actu-202312-01.png","alt":""},"title":"Styles fluviaux et croissance des plis actifs: Un exemple du segment oriental des plis Qiulitage et Yakeng, Tian Shan m\u00e9ridional, Chine","excerpt":"","content":"Les donn\u00e9es g\u00e9omorphologiques fournissent des informations nouvelles sur les processus qui r\u00e9gissent la propagation lat\u00e9rale d'un anticlinal actif en croissance. Dans les ceintures de plissement","author":{"name":"edwardsalameh","link":"https:\/\/m2c.cnrs.fr\/author\/edwardsalameh\/"},"date":"F\u00e9v 3, 2024","dateGMT":"2024-02-03 17:39:48","modifiedDate":"2024-03-04 10:51:15","modifiedDateGMT":"2024-03-04 09:51:15","commentCount":"0","commentStatus":"closed","categories":{"coma":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>","space":"<a href=\"https:\/\/m2c.cnrs.fr\/category\/non-classe\/\" rel=\"category tag\">Non class\u00e9<\/a>"},"taxonomies":{"post_tag":""},"readTime":{"min":1,"sec":51},"status":"publish"}]