{"id":1523,"date":"2026-07-03T10:21:45","date_gmt":"2026-07-03T14:21:45","guid":{"rendered":"https:\/\/ogsl.enconstruction.website\/?post_type=tool&#038;p=1523"},"modified":"2026-10-19T13:59:54","modified_gmt":"2026-10-19T17:59:54","slug":"programme-de-monitorage-de-la-zone-atlantique","status":"publish","type":"tool","link":"https:\/\/ogsl.enconstruction.website\/en\/tool\/programme-de-monitorage-de-la-zone-atlantique\/","title":{"rendered":"Programme de monitorage de la zone Atlantique"},"content":{"rendered":"[vc_row type=\u00a0\u00bbin_container\u00a0\u00bb full_screen_row_position=\u00a0\u00bbmiddle\u00a0\u00bb column_margin=\u00a0\u00bbdefault\u00a0\u00bb column_direction=\u00a0\u00bbdefault\u00a0\u00bb column_direction_tablet=\u00a0\u00bbdefault\u00a0\u00bb column_direction_phone=\u00a0\u00bbdefault\u00a0\u00bb scene_position=\u00a0\u00bbcenter\u00a0\u00bb bottom_padding=\u00a0\u00bb50\u2033 text_color=\u00a0\u00bbdark\u00a0\u00bb text_align=\u00a0\u00bbleft\u00a0\u00bb row_border_radius=\u00a0\u00bbnone\u00a0\u00bb row_border_radius_applies=\u00a0\u00bbbg\u00a0\u00bb overflow=\u00a0\u00bbvisible\u00a0\u00bb overlay_strength=\u00a0\u00bb0.3\u2033 gradient_direction=\u00a0\u00bbleft_to_right\u00a0\u00bb shape_divider_position=\u00a0\u00bbbottom\u00a0\u00bb bg_image_animation=\u00a0\u00bbnone\u00a0\u00bb gradient_type=\u00a0\u00bbdefault\u00a0\u00bb shape_type=\u00a0\u00bb\u00a0\u00bb][vc_column column_padding=\u00a0\u00bbno-extra-padding\u00a0\u00bb column_padding_tablet=\u00a0\u00bbinherit\u00a0\u00bb column_padding_phone=\u00a0\u00bbinherit\u00a0\u00bb column_padding_position=\u00a0\u00bball\u00a0\u00bb column_element_direction_desktop=\u00a0\u00bbdefault\u00a0\u00bb column_element_spacing=\u00a0\u00bbdefault\u00a0\u00bb desktop_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb tablet_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb phone_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb background_color_opacity=\u00a0\u00bb1\u2033 background_hover_color_opacity=\u00a0\u00bb1\u2033 column_backdrop_filter=\u00a0\u00bbnone\u00a0\u00bb column_shadow=\u00a0\u00bbnone\u00a0\u00bb column_border_radius=\u00a0\u00bbnone\u00a0\u00bb column_link_target=\u00a0\u00bb_self\u00a0\u00bb column_position=\u00a0\u00bbdefault\u00a0\u00bb gradient_direction=\u00a0\u00bbleft_to_right\u00a0\u00bb overlay_strength=\u00a0\u00bb0.3\u2033 width=\u00a0\u00bb1\/1\u2033 tablet_width_inherit=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbdefault\u00a0\u00bb bg_image_animation=\u00a0\u00bbnone\u00a0\u00bb border_type=\u00a0\u00bbsimple\u00a0\u00bb column_border_width=\u00a0\u00bbnone\u00a0\u00bb column_border_style=\u00a0\u00bbsolid\u00a0\u00bb][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]Des scientifiques de P\u00eaches et Oc\u00e9ans Canada provenant des quatre r\u00e9gions de l\u2019Atlantique, dont l\u2019Institut Maurice-Lamontagne (IML) pour la r\u00e9gion du Qu\u00e9bec, ont mis au point le Programme de monitorage de la zone Atlantique (PMZA). Ce programme vise \u00e0 d\u00e9tecter, suivre et pr\u00e9voir les changements de productivit\u00e9 et d\u2019\u00e9tat du milieu marin. Cette information est essentielle afin de pouvoir s\u2019attaquer \u00e0 des grands enjeux comme l\u2019impact des changements climatiques ou encore pour appuyer l\u2019approche \u00e9cosyst\u00e9mique permettant d\u2019assurer la saine gestion de l\u2019\u00e9cosyst\u00e8me du Saint-Laurent dans un esprit de conservation des ressources et de protection du milieu marin pour les g\u00e9n\u00e9rations \u00e0 venir. Le PMZA construit des s\u00e9ries de donn\u00e9es temporelles qui seront n\u00e9cessaires pour consid\u00e9rer des probl\u00e8mes futurs. Nous pr\u00e9sentons ici une description du programme, des variables oc\u00e9anographiques mesur\u00e9es, des m\u00e9thodes d\u2019\u00e9chantillonnage, et des stations et activit\u00e9s qui concernent les eaux du Saint-Laurent.<p>Les mesures de diff\u00e9rentes variables oc\u00e9anographiques sont effectu\u00e9es dans l\u2019estuaire et le golfe du Saint-Laurent de fa\u00e7on \u00e0 d\u00e9crire la variabilit\u00e9 annuelle et interannuelle des conditions environnementales de cet \u00e9cosyst\u00e8me. Les donn\u00e9es sont interpol\u00e9es de fa\u00e7on \u00e0 cr\u00e9er des s\u00e9ries temporelles pour chacune des stations fixes et des indices de l\u2019\u00e9tat oc\u00e9anographique du golfe Saint-Laurent sont \u00e9labor\u00e9s \u00e0 partir des donn\u00e9es obtenues lors de grands relev\u00e9s.[\/vc_column_text][image_with_animation image_url=\u00a0\u00bb1705\u2033 image_size=\u00a0\u00bbfull\u00a0\u00bb max_width=\u00a0\u00bb100%\u00a0\u00bb max_width_mobile=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbentrance\u00a0\u00bb animation=\u00a0\u00bbNone\u00a0\u00bb animation_movement_type=\u00a0\u00bbtransform_y\u00a0\u00bb hover_animation=\u00a0\u00bbnone\u00a0\u00bb alignment=\u00a0\u00bb\u00a0\u00bb border_radius=\u00a0\u00bbnone\u00a0\u00bb box_shadow=\u00a0\u00bbnone\u00a0\u00bb image_loading=\u00a0\u00bbdefault\u00a0\u00bb][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]<figure class=\"wp-caption alignnone\"><figcaption class=\"wp-caption-text\">Le NGCC Hudson est un navire scientifique de la Garde c\u00f4ti\u00e8re canadienne r\u00e9guli\u00e8rement utilis\u00e9 pour l\u2019\u00e9chantillonnage oc\u00e9anographique<\/figcaption><\/figure>[\/vc_column_text][\/vc_column][\/vc_row][vc_row type=\u00a0\u00bbin_container\u00a0\u00bb full_screen_row_position=\u00a0\u00bbmiddle\u00a0\u00bb column_margin=\u00a0\u00bbdefault\u00a0\u00bb column_direction=\u00a0\u00bbdefault\u00a0\u00bb column_direction_tablet=\u00a0\u00bbdefault\u00a0\u00bb column_direction_phone=\u00a0\u00bbdefault\u00a0\u00bb scene_position=\u00a0\u00bbcenter\u00a0\u00bb top_padding=\u00a0\u00bb100\u2033 bottom_padding=\u00a0\u00bb50\u2033 text_color=\u00a0\u00bbdark\u00a0\u00bb text_align=\u00a0\u00bbleft\u00a0\u00bb row_border_radius=\u00a0\u00bbnone\u00a0\u00bb row_border_radius_applies=\u00a0\u00bbbg\u00a0\u00bb overflow=\u00a0\u00bbvisible\u00a0\u00bb overlay_strength=\u00a0\u00bb0.3\u2033 gradient_direction=\u00a0\u00bbleft_to_right\u00a0\u00bb shape_divider_position=\u00a0\u00bbbottom\u00a0\u00bb bg_image_animation=\u00a0\u00bbnone\u00a0\u00bb gradient_type=\u00a0\u00bbdefault\u00a0\u00bb shape_type=\u00a0\u00bb\u00a0\u00bb][vc_column column_padding=\u00a0\u00bbno-extra-padding\u00a0\u00bb column_padding_tablet=\u00a0\u00bbinherit\u00a0\u00bb column_padding_phone=\u00a0\u00bbinherit\u00a0\u00bb column_padding_position=\u00a0\u00bball\u00a0\u00bb column_element_direction_desktop=\u00a0\u00bbdefault\u00a0\u00bb column_element_spacing=\u00a0\u00bbdefault\u00a0\u00bb desktop_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb tablet_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb phone_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb background_color_opacity=\u00a0\u00bb1\u2033 background_hover_color_opacity=\u00a0\u00bb1\u2033 column_backdrop_filter=\u00a0\u00bbnone\u00a0\u00bb column_shadow=\u00a0\u00bbnone\u00a0\u00bb column_border_radius=\u00a0\u00bbnone\u00a0\u00bb column_link_target=\u00a0\u00bb_self\u00a0\u00bb column_position=\u00a0\u00bbdefault\u00a0\u00bb gradient_direction=\u00a0\u00bbleft_to_right\u00a0\u00bb overlay_strength=\u00a0\u00bb0.3\u2033 width=\u00a0\u00bb1\/1\u2033 tablet_width_inherit=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbdefault\u00a0\u00bb bg_image_animation=\u00a0\u00bbnone\u00a0\u00bb border_type=\u00a0\u00bbsimple\u00a0\u00bb column_border_width=\u00a0\u00bbnone\u00a0\u00bb column_border_style=\u00a0\u00bbsolid\u00a0\u00bb][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]<\/p><h2>Relev\u00e9s, stations et \u00e9chantillonnage<\/h2>\n<p>Chaque ann\u00e9e, les eaux du golfe sont \u00e9chantillonn\u00e9es \u00e0 diff\u00e9rents moments de l\u2019ann\u00e9e \u00e0 bord de navire scientifique de la Garde-C\u00f4ti\u00e8re Canadienne. Diff\u00e9rents instruments de mesure sont mis \u00e0 l\u2019eau afin de recueillir de l\u2019information sur des variables telles que la salinit\u00e9, la temp\u00e9rature, la concentration d\u2019oxyg\u00e8ne dissout, la quantit\u00e9 de chlorophylle a et de sels nutritifs pr\u00e9sents dans l\u2019eau. L\u2019\u00e9chantillonnage se fait principalement par un appareil appel\u00e9 rosette qui est descendu dans l\u2019eau jusqu\u2019\u00e0 pr\u00e8s du fond. \u00c9quip\u00e9e de plusieurs sondes qui effectuent diverses mesures, la rosette est \u00e9galement munie de bouteilles qui, lors de la remont\u00e9e, sont referm\u00e9es pour r\u00e9colter des \u00e9chantillons d\u2019eau \u00e0 des profondeurs choisies. Des traits de filet sont aussi faits pour r\u00e9colter du zooplancton dans le but d\u2019en d\u00e9terminer la quantit\u00e9 par esp\u00e8ce. Au moment des pr\u00e9l\u00e8vements, certaines donn\u00e9es sont trait\u00e9es en temps r\u00e9el par ordinateur sur le navire. D\u2019autres donn\u00e9es sont calcul\u00e9es \u00e0 partir des analyses effectu\u00e9es dans un laboratoire mobile install\u00e9 \u00e0 bord (par exemple : filtration et concentration des \u00e9chantillons d\u2019eau, concentration d\u2019oxyg\u00e8ne dissous par titration) mais la plupart des r\u00e9sultats seront produits au retour, lors d\u2019analyses subs\u00e9quentes dans les laboratoires de l\u2019Institut Maurice-Lamontagne.[\/vc_column_text][image_with_animation image_url=\u00a0\u00bb1707\u2033 image_size=\u00a0\u00bbfull\u00a0\u00bb max_width=\u00a0\u00bb100%\u00a0\u00bb max_width_mobile=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbentrance\u00a0\u00bb animation=\u00a0\u00bbNone\u00a0\u00bb animation_movement_type=\u00a0\u00bbtransform_y\u00a0\u00bb hover_animation=\u00a0\u00bbnone\u00a0\u00bb alignment=\u00a0\u00bb\u00a0\u00bb border_radius=\u00a0\u00bbnone\u00a0\u00bb box_shadow=\u00a0\u00bbnone\u00a0\u00bb image_loading=\u00a0\u00bbdefault\u00a0\u00bb][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]<figure class=\"wp-caption alignnone\"><figcaption class=\"wp-caption-text\">La rosette utilis\u00e9e pour l\u2019\u00e9chantillonnage en mer \u00e0 partir du NGCC Teleost.<\/figcaption><\/figure>[\/vc_column_text][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]Durant les relev\u00e9s de juin et d\u2019automne, une s\u00e9rie de 46 stations oc\u00e9anographiques sont visit\u00e9es, regroup\u00e9es en transects qui sectionnent le golfe, en plus de quelques stations situ\u00e9es entre ces transects ou \u00e0 la t\u00eate des chenaux profonds. Des stations suppl\u00e9mentaires sont faites en juin sur le Plateau madelinien, jumel\u00e9 avec un relev\u00e9 pour d\u00e9nombrer les oeufs de maquereau. En ao\u00fbt et septembre, les ressources du PMZA sont jumel\u00e9es avec un relev\u00e9 annuel multidisciplinaire pour l\u2019\u00e9valuation des stocks de poissons de fond et de la crevette nordique et plus de 500 stations oc\u00e9anographiques sont \u00e9chantillonn\u00e9es qui recouvrent l\u2019ensemble du golfe. De plus, au cours de l\u2019ann\u00e9e deux stations oc\u00e9anographiques sont \u00e9chantillonn\u00e9es avec une plus grande fr\u00e9quence temporelle. Il s\u2019agit de la station Rimouski, \u00e9chantillonn\u00e9e nominalement une fois par semaine en saison estivale, et la station de la vall\u00e9e de Shediac situ\u00e9 sur le Plateau madelinien et \u00e9chantillonn\u00e9 une ou deux fois par mois aussi en saison estivale.<\/p>\n<div class=\"elementor-element elementor-element-2fd4152 elementor-widget elementor-widget-text-editor\" data-id=\"2fd4152\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n<div class=\"elementor-widget-container\">\n<p>Dans les sections suivantes, les donn\u00e9es de ces deux stations sont pr\u00e9sent\u00e9es sous forme de s\u00e9ries temporelles pour une s\u00e9lection des variables mesur\u00e9es. Des indices environnementaux calcul\u00e9s \u00e0 partir des donn\u00e9es obtenues lors des grands relev\u00e9s sont aussi pr\u00e9sent\u00e9s. Ces indices repr\u00e9sentent les conditions des couches de surface, interm\u00e9diaire et profonde du golfe.\u00a0Les donn\u00e9es brutes sont \u00e9galement disponibles en consultant le\u00a0<a href=\"https:\/\/sgde.ogsl.ca\/datatype\" target=\"_blank\" rel=\"noopener\">Syst\u00e8me de gestion des donn\u00e9es environnementales (SGDE)<\/a>. Des rapports annuels (physique, biologique ainsi qu\u2019un avis scientifique zonal) sont disponibles aupr\u00e8s du Secr\u00e9tariat canadien de consultation scientifique (SCCS) ou via le catalogue de l\u2019OGSL.<\/p>\n<p><a href=\"https:\/\/catalogue.ogsl.ca\/dataset\/8603771b-12b8-4b46-926c-0f48cc39a28c\">Cliquez ici pour acc\u00e9der aux s\u00e9ries temporelles du PMZA dans le catalogue de donn\u00e9es de l\u2019OGSL<\/a><\/p>\n<p><a href=\"https:\/\/catalogue.ogsl.ca\/dataset\/8d4296e0-7be4-4cea-9049-91806d65d260\">Cliquez ici pour acc\u00e9der aux rapports annuels du PMZA pour la r\u00e9gion du Qu\u00e9bec<\/a><\/p>\n<p>Pour tout commentaires ou questions, communiquer avec :\u00a0<a href=\"mailto:Peter.Galbraith@dfo-mpo.gc.ca\">Peter.Galbraith@dfo-mpo.gc.ca<\/a><\/p>\n<\/div>\n<\/div>[\/vc_column_text][\/vc_column][\/vc_row][vc_row type=\u00a0\u00bbfull_width_background\u00a0\u00bb full_screen_row_position=\u00a0\u00bbmiddle\u00a0\u00bb column_margin=\u00a0\u00bbdefault\u00a0\u00bb column_direction=\u00a0\u00bbdefault\u00a0\u00bb column_direction_tablet=\u00a0\u00bbdefault\u00a0\u00bb column_direction_phone=\u00a0\u00bbdefault\u00a0\u00bb bg_color=\u00a0\u00bb#EDECEA\u00a0\u00bb scene_position=\u00a0\u00bbcenter\u00a0\u00bb top_padding=\u00a0\u00bb100\u2033 bottom_padding=\u00a0\u00bb100\u2033 text_color=\u00a0\u00bbdark\u00a0\u00bb text_align=\u00a0\u00bbleft\u00a0\u00bb row_border_radius=\u00a0\u00bbnone\u00a0\u00bb row_border_radius_applies=\u00a0\u00bbbg\u00a0\u00bb overflow=\u00a0\u00bbvisible\u00a0\u00bb overlay_strength=\u00a0\u00bb0.3\u2033 gradient_direction=\u00a0\u00bbleft_to_right\u00a0\u00bb shape_divider_position=\u00a0\u00bbbottom\u00a0\u00bb bg_image_animation=\u00a0\u00bbnone\u00a0\u00bb gradient_type=\u00a0\u00bbdefault\u00a0\u00bb shape_type=\u00a0\u00bb\u00a0\u00bb][vc_column column_padding=\u00a0\u00bbno-extra-padding\u00a0\u00bb column_padding_tablet=\u00a0\u00bbinherit\u00a0\u00bb column_padding_phone=\u00a0\u00bbinherit\u00a0\u00bb column_padding_position=\u00a0\u00bball\u00a0\u00bb column_element_direction_desktop=\u00a0\u00bbdefault\u00a0\u00bb column_element_spacing=\u00a0\u00bbdefault\u00a0\u00bb desktop_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb tablet_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb phone_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb background_color_opacity=\u00a0\u00bb1\u2033 background_hover_color_opacity=\u00a0\u00bb1\u2033 column_backdrop_filter=\u00a0\u00bbnone\u00a0\u00bb column_shadow=\u00a0\u00bbnone\u00a0\u00bb column_border_radius=\u00a0\u00bbnone\u00a0\u00bb column_link_target=\u00a0\u00bb_self\u00a0\u00bb column_position=\u00a0\u00bbdefault\u00a0\u00bb gradient_direction=\u00a0\u00bbleft_to_right\u00a0\u00bb overlay_strength=\u00a0\u00bb0.3\u2033 width=\u00a0\u00bb1\/1\u2033 tablet_width_inherit=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbdefault\u00a0\u00bb bg_image_animation=\u00a0\u00bbnone\u00a0\u00bb border_type=\u00a0\u00bbsimple\u00a0\u00bb column_border_width=\u00a0\u00bbnone\u00a0\u00bb column_border_style=\u00a0\u00bbsolid\u00a0\u00bb][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]<h2>PMZA \u2013 Station \u00e0 haute fr\u00e9quence \u2013 Rimouski<\/h2>\n<div class=\"elementor-element elementor-element-1afcf1a elementor-widget elementor-widget-text-editor\" data-id=\"1afcf1a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n<div class=\"elementor-widget-container\">\n<p><strong>L\u2019\u00e9volution temporelle<\/strong>\u00a0de quatre variables mesur\u00e9es \u00e0 la station Rimouski est pr\u00e9sent\u00e9e pour\u00a0<strong>deux p\u00e9riodes<\/strong>, soit celle des\u00a0<a href=\"https:\/\/ogsl.ca\/fr\/programme-de-monitorage-de-la-zone-atlantique-station-rimouski\/#3derniereAnnees\"><strong>trois derni\u00e8res ann\u00e9es<\/strong><\/a>\u00a0et celle depuis le\u00a0<a href=\"https:\/\/ogsl.ca\/fr\/programme-de-monitorage-de-la-zone-atlantique-station-rimouski\/#1991\"><strong>d\u00e9but de son monitorage en 1991<\/strong><\/a>.<\/p>\n<p>Les figures montrent les\u00a0<strong>valeurs moyennes mensuelles<\/strong>\u00a0de la\u00a0<strong>temp\u00e9rature<\/strong>\u00a0(\u00b0 C) et de la\u00a0<strong>salinit\u00e9<\/strong>, ainsi que des\u00a0<strong>sels nutritifs<\/strong>\u00a0(nitrate et nitrite ; mmol m<sup>-3<\/sup>) et de la\u00a0<strong>chlorophylle\u00a0<em>a<\/em><\/strong>\u00a0(mg m<sup>-3<\/sup>).<\/p>\n<p>Les tableaux indiquent des valeurs moyennes mensuelles pour :<\/p>\n<ul>\n<li>le minimum de temp\u00e9rature de la couche interm\u00e9diaire froide (CIF),<\/li>\n<li>l\u2019\u00e9paisseur (m) de la CIF (T &lt; 1 \u00b0C),<\/li>\n<li>la temp\u00e9rature, de la surface \u00e0 50 m,<\/li>\n<li>la temp\u00e9rature, de la surface \u00e0 100 m,<\/li>\n<li>les temp\u00e9ratures \u00e0 diff\u00e9rentes profondeurs, de 10 \u00e0 300 m,<\/li>\n<li>la diff\u00e9rence de densit\u00e9 de l\u2019eau (kg\/m<sup>3<\/sup>), entre la surface et 50 m, repr\u00e9sentant la stratification,<\/li>\n<li>la salinit\u00e9, de la surface \u00e0 50 m,<\/li>\n<li>les salinit\u00e9s \u00e0 diff\u00e9rentes profondeurs, de 10 \u00e0 300 m,<\/li>\n<li>les sels nutritifs dans la couche de surface (0-50 m), zone o\u00f9 les sels sont principalement consomm\u00e9s par le phytoplancton,<\/li>\n<li>les sels nutritifs, de 50-150 m, cette couche repr\u00e9sentant la source principale de renouvellement pour les eaux de surface,<\/li>\n<li>les sels nutritifs \u00e0 diff\u00e9rentes profondeurs, de 1 \u00e0 320 m,<\/li>\n<li>la chlorophylle\u00a0<em>a<\/em>\u00a0dans la colonne d\u2019eau (0-100 m),<\/li>\n<li>la chlorophylle\u00a0<em>a<\/em>\u00a0\u00e0 diff\u00e9rentes profondeurs, de 1 \u00e0 100 m.<\/li>\n<\/ul>\n<p>Dans les tableaux, la couleur des cases exprime l\u2019anomalie normalis\u00e9e, soit la d\u00e9viation de l\u2019\u00e9tat mensuel par rapport \u00e0 une climatologie mensuelle \u00e0 long terme. Le bleu exprime des conditions d\u2019anomalies n\u00e9gatives, donc diminution de la temp\u00e9rature, salinit\u00e9, de la concentration en sels nutritifs ou de la chlorophylle\u00a0<em>a<\/em>. Le rouge exprime des conditions d\u2019anomalies positives, donc augmentation de la temp\u00e9rature, salinit\u00e9, concentration en sels nutritifs ou en chlorophylle\u00a0<em>a<\/em>. Les cases blanches indiquent des conditions pr\u00e8s de la normale (\u00e0 l\u2019int\u00e9rieur de plus et moins un-demi \u00e9cart-type de la climatologie \u00e0 long terme, pour chaque mois et chaque profondeur). Les palettes de bleu et rouge sont proportionnelles \u00e0 l\u2019intensit\u00e9 de la d\u00e9viation par rapport \u00e0 la normale.<\/p>\n<p>La temp\u00e9rature enregistr\u00e9e \u00e0 300 m en mars 2022 est la plus \u00e9lev\u00e9e depuis\u00a0<a href=\"https:\/\/ogsl.ca\/fr\/programme-de-monitorage-de-la-zone-atlantique-station-rimouski\/#1991\"><strong>1991<\/strong><\/a>, soit le d\u00e9but du monitorage \u00e0 cette station.<\/p>\n<\/div>\n<\/div>[\/vc_column_text][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]<h3>Rimouski station \u00e0 haute fr\u00e9quence \u2013 3 derni\u00e8res ann\u00e9es<\/h3>[\/vc_column_text][image_with_animation image_url=\u00a0\u00bb1708\u2033 image_size=\u00a0\u00bbfull\u00a0\u00bb max_width=\u00a0\u00bb100%\u00a0\u00bb max_width_mobile=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbentrance\u00a0\u00bb animation=\u00a0\u00bbNone\u00a0\u00bb animation_movement_type=\u00a0\u00bbtransform_y\u00a0\u00bb hover_animation=\u00a0\u00bbnone\u00a0\u00bb alignment=\u00a0\u00bb\u00a0\u00bb border_radius=\u00a0\u00bbnone\u00a0\u00bb box_shadow=\u00a0\u00bbnone\u00a0\u00bb image_loading=\u00a0\u00bbdefault\u00a0\u00bb][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]<h3>Rimouski station \u00e0 haute fr\u00e9quence \u2013 depuis 1991<\/h3>[\/vc_column_text][image_with_animation image_url=\u00a0\u00bb1709\u2033 image_size=\u00a0\u00bbfull\u00a0\u00bb max_width=\u00a0\u00bb100%\u00a0\u00bb max_width_mobile=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbentrance\u00a0\u00bb animation=\u00a0\u00bbNone\u00a0\u00bb animation_movement_type=\u00a0\u00bbtransform_y\u00a0\u00bb hover_animation=\u00a0\u00bbnone\u00a0\u00bb alignment=\u00a0\u00bb\u00a0\u00bb border_radius=\u00a0\u00bbnone\u00a0\u00bb box_shadow=\u00a0\u00bbnone\u00a0\u00bb image_loading=\u00a0\u00bbdefault\u00a0\u00bb][image_with_animation image_url=\u00a0\u00bb1710\u2033 image_size=\u00a0\u00bbfull\u00a0\u00bb max_width=\u00a0\u00bb100%\u00a0\u00bb max_width_mobile=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbentrance\u00a0\u00bb animation=\u00a0\u00bbNone\u00a0\u00bb animation_movement_type=\u00a0\u00bbtransform_y\u00a0\u00bb hover_animation=\u00a0\u00bbnone\u00a0\u00bb alignment=\u00a0\u00bb\u00a0\u00bb border_radius=\u00a0\u00bbnone\u00a0\u00bb box_shadow=\u00a0\u00bbnone\u00a0\u00bb image_loading=\u00a0\u00bbdefault\u00a0\u00bb][\/vc_column][\/vc_row][vc_row type=\u00a0\u00bbfull_width_background\u00a0\u00bb full_screen_row_position=\u00a0\u00bbmiddle\u00a0\u00bb column_margin=\u00a0\u00bbdefault\u00a0\u00bb column_direction=\u00a0\u00bbdefault\u00a0\u00bb column_direction_tablet=\u00a0\u00bbdefault\u00a0\u00bb column_direction_phone=\u00a0\u00bbdefault\u00a0\u00bb scene_position=\u00a0\u00bbcenter\u00a0\u00bb top_padding=\u00a0\u00bb100\u2033 bottom_padding=\u00a0\u00bb100\u2033 text_color=\u00a0\u00bbdark\u00a0\u00bb text_align=\u00a0\u00bbleft\u00a0\u00bb row_border_radius=\u00a0\u00bbnone\u00a0\u00bb row_border_radius_applies=\u00a0\u00bbbg\u00a0\u00bb overflow=\u00a0\u00bbvisible\u00a0\u00bb overlay_strength=\u00a0\u00bb0.3\u2033 gradient_direction=\u00a0\u00bbleft_to_right\u00a0\u00bb shape_divider_position=\u00a0\u00bbbottom\u00a0\u00bb bg_image_animation=\u00a0\u00bbnone\u00a0\u00bb gradient_type=\u00a0\u00bbdefault\u00a0\u00bb shape_type=\u00a0\u00bb\u00a0\u00bb][vc_column column_padding=\u00a0\u00bbno-extra-padding\u00a0\u00bb column_padding_tablet=\u00a0\u00bbinherit\u00a0\u00bb column_padding_phone=\u00a0\u00bbinherit\u00a0\u00bb column_padding_position=\u00a0\u00bball\u00a0\u00bb column_element_direction_desktop=\u00a0\u00bbdefault\u00a0\u00bb column_element_spacing=\u00a0\u00bbdefault\u00a0\u00bb desktop_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb tablet_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb phone_text_alignment=\u00a0\u00bbdefault\u00a0\u00bb background_color_opacity=\u00a0\u00bb1\u2033 background_hover_color_opacity=\u00a0\u00bb1\u2033 column_backdrop_filter=\u00a0\u00bbnone\u00a0\u00bb column_shadow=\u00a0\u00bbnone\u00a0\u00bb column_border_radius=\u00a0\u00bbnone\u00a0\u00bb column_link_target=\u00a0\u00bb_self\u00a0\u00bb column_position=\u00a0\u00bbdefault\u00a0\u00bb gradient_direction=\u00a0\u00bbleft_to_right\u00a0\u00bb overlay_strength=\u00a0\u00bb0.3\u2033 width=\u00a0\u00bb1\/1\u2033 tablet_width_inherit=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbdefault\u00a0\u00bb bg_image_animation=\u00a0\u00bbnone\u00a0\u00bb border_type=\u00a0\u00bbsimple\u00a0\u00bb column_border_width=\u00a0\u00bbnone\u00a0\u00bb column_border_style=\u00a0\u00bbsolid\u00a0\u00bb][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]<h2>PMZA \u2013 Station \u00e0 haute fr\u00e9quence \u2013 Station Vall\u00e9e de Shediac<\/h2>\n<div class=\"elementor-element elementor-element-1afcf1a elementor-widget elementor-widget-text-editor\" data-id=\"1afcf1a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n<div class=\"elementor-widget-container\">\n<p><strong>L\u2019\u00e9volution temporelle<\/strong>\u00a0de\u00a0<strong>quatre variables<\/strong>\u00a0mesur\u00e9es \u00e0 la station Vall\u00e9e de Shediac est pr\u00e9sent\u00e9e pour\u00a0<strong>deux p\u00e9riodes<\/strong>, soit celle des\u00a0<a href=\"https:\/\/ogsl.ca\/fr\/programme-de-monitorage-de-la-zone-atlantique-valle-de-shediac\/#3derniereAnnees\"><strong>trois derni\u00e8res ann\u00e9es<\/strong><\/a>\u00a0et celle depuis le\u00a0<a href=\"https:\/\/ogsl.ca\/fr\/programme-de-monitorage-de-la-zone-atlantique-valle-de-shediac\/#1999\"><strong>d\u00e9but de son monitorage en 1999<\/strong><\/a>.<\/p>\n<p>Les figures montrent les\u00a0<strong>valeurs moyennes mensuelles<\/strong>\u00a0de la\u00a0<strong>temp\u00e9rature<\/strong>\u00a0(\u00b0 C) et de la\u00a0<strong>salinit\u00e9<\/strong>, ainsi que des\u00a0<strong>sels nutritifs<\/strong>\u00a0(nitrate et nitrite ; mmol m<sup>-3<\/sup>) et de la\u00a0<strong>chlorophylle\u00a0<em>a<\/em><\/strong>\u00a0(mg m<sup>-3<\/sup>).<\/p>\n<p>Les tableaux indiquent des\u00a0<strong>valeurs moyennes mensuelles<\/strong>\u00a0pour :<\/p>\n<ul>\n<li>la temp\u00e9rature, de la surface jusqu\u2019\u00e0 50 m,<\/li>\n<li>la temp\u00e9rature, de la surface jusqu\u2019au fond,<\/li>\n<li>les temp\u00e9ratures \u00e0 diff\u00e9rentes profondeurs, de 0 \u00e0 75 m,<\/li>\n<li>la diff\u00e9rence de densit\u00e9 de l\u2019eau (kg\/m<sup>3<\/sup>) entre la surface et 50 m, repr\u00e9sentant la stratification,<\/li>\n<li>la salinit\u00e9, de la surface \u00e0 50 m,<\/li>\n<li>les salinit\u00e9s \u00e0 diff\u00e9rentes profondeurs, de 0 \u00e0 75 m.<\/li>\n<li>les sels nutritifs dans la couche de surface (0-50 m), zone o\u00f9 les sels sont principalement consomm\u00e9s par le phytoplancton,<\/li>\n<li>les sels nutritifs dans la couche de 50-84 m (fond), zone repr\u00e9sentant la source principale de renouvellement pour les eaux de surface,<\/li>\n<li>les sels nutritifs \u00e0 diff\u00e9rentes profondeurs, de 5 \u00e0 75 m,<\/li>\n<li>la chlorophylle\u00a0<em>a<\/em>\u00a0dans la colonne d\u2019eau (0-84 m),<\/li>\n<li>la chlorophylle\u00a0<em>a<\/em>\u00a0\u00e0 diff\u00e9rentes profondeurs, de 5 \u00e0 75 m.<\/li>\n<\/ul>\n<p>Dans les tableaux, la couleur des cases exprime l\u2019anomalie normalis\u00e9e, soit la d\u00e9viation de l\u2019\u00e9tat mensuel par rapport \u00e0 une climatologie mensuelle \u00e0 long terme. Le bleu exprime des conditions d\u2019anomalies n\u00e9gatives, donc diminution de la temp\u00e9rature, de la salinit\u00e9, de la concentration en sels nutritifs ou de la chlorophylle\u00a0<em>a<\/em>. Le rouge exprime des conditions d\u2019anomalies positives, donc augmentation de la temp\u00e9rature, de la salinit\u00e9, de la concentration en sels nutritifs ou de la chlorophylle\u00a0<em>a<\/em>. Les cases blanches indiquent des conditions pr\u00e8s de la normale (\u00e0 l\u2019int\u00e9rieur de plus et moins un-demi \u00e9cart-type de la climatologie \u00e0 long terme, pour chaque mois et chaque profondeur). Les palettes de bleu et rouge sont proportionnelles \u00e0 l\u2019intensit\u00e9 de la d\u00e9viation par rapport \u00e0 la normale.<\/p>\n<p>Remarquez l\u2019appauvrissement estival des sels nutritifs, suite \u00e0 la floraison printani\u00e8re du phytoplancton, floraison repr\u00e9sent\u00e9e par de fortes valeurs de chlorophylle\u00a0<em>a<\/em>.<\/p>\n<\/div>\n<\/div>[\/vc_column_text][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]<h3>Vall\u00e9e de Shediac station \u00e0 haute fr\u00e9quence \u2013 3 derni\u00e8res ann\u00e9es<\/h3>[\/vc_column_text][image_with_animation image_url=\u00a0\u00bb1711\u2033 image_size=\u00a0\u00bbfull\u00a0\u00bb max_width=\u00a0\u00bb100%\u00a0\u00bb max_width_mobile=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbentrance\u00a0\u00bb animation=\u00a0\u00bbNone\u00a0\u00bb animation_movement_type=\u00a0\u00bbtransform_y\u00a0\u00bb hover_animation=\u00a0\u00bbnone\u00a0\u00bb alignment=\u00a0\u00bb\u00a0\u00bb border_radius=\u00a0\u00bbnone\u00a0\u00bb box_shadow=\u00a0\u00bbnone\u00a0\u00bb image_loading=\u00a0\u00bbdefault\u00a0\u00bb][vc_column_text css=\u00a0\u00bb\u00a0\u00bb text_direction=\u00a0\u00bbdefault\u00a0\u00bb]<h3>Vall\u00e9e de Shediac station \u00e0 haute fr\u00e9quence \u2013 Depuis 1999<\/h3>[\/vc_column_text][image_with_animation image_url=\u00a0\u00bb1712\u2033 image_size=\u00a0\u00bbfull\u00a0\u00bb max_width=\u00a0\u00bb100%\u00a0\u00bb max_width_mobile=\u00a0\u00bbdefault\u00a0\u00bb animation_type=\u00a0\u00bbentrance\u00a0\u00bb animation=\u00a0\u00bbNone\u00a0\u00bb animation_movement_type=\u00a0\u00bbtransform_y\u00a0\u00bb hover_animation=\u00a0\u00bbnone\u00a0\u00bb alignment=\u00a0\u00bb\u00a0\u00bb border_radius=\u00a0\u00bbnone\u00a0\u00bb box_shadow=\u00a0\u00bbnone\u00a0\u00bb image_loading=\u00a0\u00bbdefault\u00a0\u00bb][image_with_animation image_url=\u00a0\u00bb1713\u2033 image_size=\u00a0\u00bbfull\u00a0\u00bb 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