{"id":226067,"date":"2023-03-17T07:31:31","date_gmt":"2023-03-17T13:31:31","guid":{"rendered":"https:\/\/onesea.org\/?p=226067"},"modified":"2023-03-17T07:31:35","modified_gmt":"2023-03-17T13:31:35","slug":"las-mareas-submarinas-pueden-estar-afectando-la-capacidad-del-oceano-para-almacenar-carbono","status":"publish","type":"post","link":"https:\/\/onesea.org\/en\/blog\/oceanos-saludables\/las-mareas-submarinas-pueden-estar-afectando-la-capacidad-del-oceano-para-almacenar-carbono\/","title":{"rendered":"Las mareas submarinas pueden estar afectando la capacidad del oc\u00e9ano para almacenar carbono"},"content":{"rendered":"[et_pb_section fb_built=&#8221;1&#8243; admin_label=&#8221;section&#8221; _builder_version=&#8221;4.20.2&#8243; background_color=&#8221;rgba(0,0,0,0.64)&#8221; background_image=&#8221;https:\/\/onesea.org\/wp-content\/uploads\/2023\/03\/underwater-view-of-ocean-wave-2021-09-03-13-40-33-utc-scaled.jpeg&#8221; background_position=&#8221;center_right&#8221; background_blend=&#8221;darken&#8221; custom_padding=&#8221;||0px|&#8221; custom_padding_tablet=&#8221;||0px|&#8221; transparent_background=&#8221;off&#8221; padding_mobile=&#8221;on&#8221; make_fullwidth=&#8221;off&#8221; use_custom_width=&#8221;off&#8221; width_unit=&#8221;on&#8221; global_colors_info=&#8221;{}&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243; title_text=&#8221;Ocean wave, underwater shot&#8221;][et_pb_row padding_mobile=&#8221;on&#8221; column_padding_mobile=&#8221;on&#8221; admin_label=&#8221;row&#8221; _builder_version=&#8221;4.19.4&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; custom_padding=&#8221;||0px|&#8221; make_fullwidth=&#8221;off&#8221; use_custom_width=&#8221;off&#8221; width_unit=&#8221;on&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.16&#8243; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text admin_label=&#8221;Text&#8221; _builder_version=&#8221;4.20.2&#8243; text_font=&#8221;PT Serif||||||||&#8221; text_text_color=&#8221;#ffffff&#8221; text_font_size=&#8221;30px&#8221; text_line_height=&#8221;1.2em&#8221; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; text_orientation=&#8221;center&#8221; width=&#8221;61%&#8221; module_alignment=&#8221;center&#8221; custom_margin=&#8221;150px||0px|&#8221; custom_padding=&#8221;||0px|&#8221; text_font_tablet=&#8221;&#8221; text_font_phone=&#8221;&#8221; text_font_last_edited=&#8221;on|phone&#8221; text_text_shadow_style=&#8221;preset2&#8243; text_text_shadow_horizontal_length_last_edited=&#8221;off|desktop&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221; text_text_align=&#8221;center&#8221; global_colors_info=&#8221;{}&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<p><b>Las mareas submarinas pueden estar afectando la capacidad del oc\u00e9ano para almacenar carbono<\/b><\/p>[\/et_pb_text][et_pb_text admin_label=&#8221;Text&#8221; _builder_version=&#8221;4.16&#8243; text_font=&#8221;Flood|300|||||||&#8221; text_text_color=&#8221;#f2bf29&#8243; text_font_size=&#8221;50px&#8221; background_color=&#8221;rgba(48,105,140,0.63)&#8221; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; text_orientation=&#8221;center&#8221; width=&#8221;41%&#8221; module_alignment=&#8221;center&#8221; custom_margin=&#8221;50px||100px|&#8221; custom_padding=&#8221;||0px|&#8221; text_text_shadow_style=&#8221;preset2&#8243; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221; text_text_align=&#8221;center&#8221; global_colors_info=&#8221;{}&#8221;]<p style=\"text-align: center;\">Oneblog<\/p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; admin_label=&#8221;Section&#8221; _builder_version=&#8221;4.19.2&#8243; background_color=&#8221;#f7f7f4&#8243; custom_padding=&#8221;0px|||&#8221; custom_padding_tablet=&#8221;0px|||&#8221; transparent_background=&#8221;off&#8221; padding_mobile=&#8221;on&#8221; make_fullwidth=&#8221;off&#8221; use_custom_width=&#8221;off&#8221; width_unit=&#8221;on&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_row column_padding_mobile=&#8221;on&#8221; admin_label=&#8221;row&#8221; _builder_version=&#8221;4.16&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; max_width=&#8221;620px&#8221; custom_margin=&#8221;||0px||false|false&#8221; custom_padding=&#8221;0px||0px||false|false&#8221; make_fullwidth=&#8221;off&#8221; use_custom_width=&#8221;on&#8221; width_unit=&#8221;on&#8221; custom_width_px=&#8221;620px&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.16&#8243; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/onesea.org\/wp-content\/uploads\/2019\/09\/IMG_8958.png&#8221; show_bottom_space=&#8221;off&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; admin_label=&#8221;Image&#8221; _builder_version=&#8221;4.16&#8243; width=&#8221;30%&#8221; module_alignment=&#8221;center&#8221; custom_margin=&#8221;-65px||||false|false&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221; animation=&#8221;off&#8221; sticky=&#8221;on&#8221; always_center_on_mobile=&#8221;on&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_image][et_pb_text admin_label=&#8221;Text&#8221; _builder_version=&#8221;4.16&#8243; text_font=&#8221;PT Sans||||&#8221; text_text_color=&#8221;#323232&#8243; text_font_size=&#8221;18&#8243; text_line_height=&#8221;1.4em&#8221; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; text_orientation=&#8221;center&#8221; module_alignment=&#8221;center&#8221; custom_margin=&#8221;14px||0px|&#8221; custom_padding=&#8221;||0px|||&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221; global_colors_info=&#8221;{}&#8221;]<p><span style=\"color: #333333;\"><strong>OneBlog<\/strong><\/span>, <span style=\"color: #003366;\">Fundaci\u00f3n OneSea<\/span>, Costa Rica<\/p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.17.4&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.20.2&#8243; _module_preset=&#8221;default&#8221; text_font=&#8221;Arial||||||||&#8221; text_text_color=&#8221;#000000&#8243; text_font_size=&#8221;16px&#8221; text_line_height=&#8221;1.4em&#8221; global_colors_info=&#8221;{}&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<p><span style=\"font-weight: 400;\">El oc\u00e9ano y su ecolog\u00eda se ha posicionado como una de las herramientas esenciales en la captura de carbono. Nuestros mares ejercen un proceso que elimina el di\u00f3xido de carbono de la atm\u00f3sfera, un elemento que impulsa el cambio clim\u00e1tico. Esto mediante diversos procesos qu\u00edmicos y biol\u00f3gicos dentro de los organismos que habitan en sus aguas, como las algas.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Pero mucho de esto es solo la superficie de un amplio mar de preguntas, pues pareciera que los cambios en los ciclos oce\u00e1nicos han estado teniendo proyecciones sin tomar en cuenta las mareas submarinas y relaci\u00f3n con el clima. <\/span><\/p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;3_5,2_5&#8243; column_padding_mobile=&#8221;on&#8221; admin_label=&#8221;row&#8221; _builder_version=&#8221;4.16&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; width=&#8221;98.3%&#8221; custom_margin=&#8221;-40px||||false|false&#8221; custom_padding=&#8221;0px||4px||false|false&#8221; make_fullwidth=&#8221;off&#8221; use_custom_width=&#8221;off&#8221; width_unit=&#8221;on&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;3_5&#8243; _builder_version=&#8221;4.16&#8243; custom_padding=&#8221;60px||||false|false&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text admin_label=&#8221;Text&#8221; _builder_version=&#8221;4.20.2&#8243; text_font=&#8221;PT Serif||||||||&#8221; text_text_color=&#8221;#000000&#8243; text_font_size=&#8221;20px&#8221; text_line_height=&#8221;1.3em&#8221; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; max_width=&#8221;900px&#8221; custom_margin=&#8221;-35px||18px||false|false&#8221; custom_padding=&#8221;0px||0px||false|false&#8221; text_font_size_tablet=&#8221;&#8221; text_font_size_phone=&#8221;&#8221; text_font_size_last_edited=&#8221;on|tablet&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221; global_colors_info=&#8221;{}&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<p><b>Un acercamiento a las mareas submarinas<\/b><\/p>[\/et_pb_text][et_pb_text _builder_version=&#8221;4.20.2&#8243; text_font=&#8221;Arial||||||||&#8221; text_text_color=&#8221;#000000&#8243; text_font_size=&#8221;16px&#8221; text_line_height=&#8221;1.4em&#8221; text_orientation=&#8221;justified&#8221; custom_margin=&#8221;-4px|||10px|false|false&#8221; custom_padding=&#8221;||0px|||&#8221; global_colors_info=&#8221;{}&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<p><span style=\"font-weight: 400;\">Un <\/span><a href=\"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/10.1029\/2022AV000800\"><span style=\"font-weight: 400;\">equipo internacional<\/span><\/a><span style=\"font-weight: 400;\"> de investigadores, dirigido por la Universidad de Cambridge, cuantific\u00f3 el efecto de estas olas y otras formas de turbulencia submarina en el Oc\u00e9ano Atl\u00e1ntico y descubri\u00f3 que sus efectos en las aguas,\u00a0 no se est\u00e1 reflejando con exactitud en los modelos clim\u00e1ticos que informan las pol\u00edticas globales.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">La mayor parte del calor y el carbono emitidos por la actividad humana son absorbidos por el oc\u00e9ano, pero la cantidad que puede absorber depende de las turbulencias en su interior, ya que el calor y el carbono son empujados hacia las profundidades del oc\u00e9ano o atra\u00eddos hacia la superficie.\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">La circulaci\u00f3n oce\u00e1nica transporta las aguas c\u00e1lidas desde los tr\u00f3picos hasta el Atl\u00e1ntico Norte, donde se enfr\u00edan, se hunden y regresan hacia el sur en las profundidades oce\u00e1nicas. La parte central de este patr\u00f3n de circulaci\u00f3n, denominada Circulaci\u00f3n Meridional de Oscilaci\u00f3n del Atl\u00e1ntico (AMOC, por sus siglas en ingl\u00e9s), desempe\u00f1a un papel clave en la regulaci\u00f3n de los presupuestos globales de calor y carbono. As\u00ed, la circulaci\u00f3n oce\u00e1nica redistribuye el calor hacia las regiones polares, donde <\/span><a href=\"https:\/\/onesea.org\/en\/blog\/oceanos-saludables\/el-nivel-del-mar-aumenta-un-centimetro-por-ano-en-promedio\/\"><span style=\"font-weight: 400;\">descongela el hielo<\/span><\/a><span style=\"font-weight: 400;\">, y lleva ese carbono hacia las profundidades, donde puede almacenarse durante miles de a\u00f1os.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">En las \u00faltimas d\u00e9cadas, los investigadores han estado estudiando si el AMOC puede ser un factor que explique por qu\u00e9 el \u00c1rtico ha perdido tanta capa de hielo, mientras que algunas capas de hielo de la Ant\u00e1rtida est\u00e1n creciendo. Una posible explicaci\u00f3n de este fen\u00f3meno es que el calor absorbido por el oc\u00e9ano en el Atl\u00e1ntico Norte tarda varios cientos de a\u00f1os en llegar al Ant\u00e1rtico.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Parte de las preocupaciones identificadas, es que el <\/span><a href=\"https:\/\/onesea.org\/en\/blog\/oceanos-saludables\/el-calentamiento-de-los-oceanos-podria-impulsar-la-pesca-ilegal-en-areas-protegidas\/\"><span style=\"font-weight: 400;\">calentamiento de aguas<\/span><\/a><span style=\"font-weight: 400;\"> y la liberaci\u00f3n de carbono entre capas se ve facilitado por dichas turbulencias, un fen\u00f3meno que no est\u00e1 totalmente representado en los modelos clim\u00e1ticos y puede estar afectando directamente los modelos de impactos clim\u00e1ticos en los oc\u00e9anos.<\/span><\/p>\n<p><span style=\"font-weight: 400;\"><\/span><\/p>\n<p><span style=\"font-weight: 400;\"><\/span><\/p>[\/et_pb_text][et_pb_text admin_label=&#8221;Text&#8221; _builder_version=&#8221;4.20.2&#8243; text_font=&#8221;PT Serif||||||||&#8221; text_text_color=&#8221;#000000&#8243; text_font_size=&#8221;20px&#8221; text_line_height=&#8221;1.3em&#8221; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; max_width=&#8221;900px&#8221; custom_margin=&#8221;-35px||18px||false|false&#8221; custom_padding=&#8221;0px||0px||false|false&#8221; text_font_size_tablet=&#8221;&#8221; text_font_size_phone=&#8221;&#8221; text_font_size_last_edited=&#8221;on|tablet&#8221; use_border_color=&#8221;off&#8221; border_color=&#8221;#ffffff&#8221; border_style=&#8221;solid&#8221; global_colors_info=&#8221;{}&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<p><b>El futuro de la ciencia clim\u00e1tica sobre el mar<\/b><\/p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;2_5&#8243; _builder_version=&#8221;4.16&#8243; custom_padding=&#8221;40px||||false|false&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_image src=&#8221;https:\/\/onesea.org\/wp-content\/uploads\/2023\/03\/sunset-in-the-ocean-with-soft-waves-2021-08-29-09-29-26-utc-scaled.jpg&#8221; title_text=&#8221;Sunset in the ocean with soft waves&#8221; _builder_version=&#8221;4.20.2&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; custom_margin=&#8221;-179px|auto||auto||&#8221; custom_padding=&#8221;24px||7px|||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.20.2&#8243; text_font=&#8221;Arial||||||||&#8221; text_text_color=&#8221;#000000&#8243; text_font_size=&#8221;16px&#8221; text_line_height=&#8221;1.4em&#8221; header_font=&#8221;PT Serif||||||||&#8221; header_3_font=&#8221;PT Serif||||||||&#8221; header_3_text_color=&#8221;#000000&#8243; text_orientation=&#8221;justified&#8221; width=&#8221;100%&#8221; custom_padding=&#8221;0px|||0px||&#8221; global_colors_info=&#8221;{}&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<p><span style=\"font-weight: 400;\">Los resultados de dicha investigaci\u00f3n demuestran que muchos modelos clim\u00e1ticos tienen una representaci\u00f3n excesivamente simplista del papel de la turbulencia a microescala, pero esta s\u00ed es significativa y deber\u00eda tratarse con m\u00e1s firmeza en los estudios del clima. C\u00f3mo por ejemplo, la turbulencia y su papel en la circulaci\u00f3n oce\u00e1nica ejercen un control sobre la cantidad de calor producido por el humano, que llega a la capa de hielo de la Ant\u00e1rtida y la escala de tiempo en que eso ocurre.\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">As\u00ed que los cambios en estos procesos pueden acelerar el deshielo y la liberaci\u00f3n del carbono atrapado en las capas oce\u00e1nicas, acelerando el proceso de calentamiento de las aguas y sus efectos adversos para la conservaci\u00f3n marina.\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Para Costa Rica este escenario es fundamental de analizar, en cuanto a las proyecciones clim\u00e1ticas. Ya que el escenario de nuestro territorio marino proyecta alta incidencia de <\/span><a href=\"https:\/\/onesea.org\/en\/blog\/oceanos-saludables\/las-grandes-amenazas-de-nuestros-oceanos\/\"><span style=\"font-weight: 400;\">acidificaci\u00f3n del oc\u00e9ano<\/span><\/a><span style=\"font-weight: 400;\"> y el aumento del nivel del mar.\u00a0<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Ambas situaciones podr\u00edan estar sesgadas por una mala interpretaci\u00f3n de la realidad de las AMOC, dej\u00e1ndonos probablemente con menos tiempo para mitigar y adaptar nuestro territorio ante dicho panorama.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">Desde OneSea urgimos que Costa Rica avance en la aplicaci\u00f3n de sus planes de atenci\u00f3n contra el cambio clim\u00e1tico, ya que las comunidades costeras dependen de estas acciones para sobrevivir a los impactos en sus territorios. Por esto apoyamos la iniciativa de los sensores de turbulencia en las redes mundiales de observaci\u00f3n, para de esta manera representar con mayor precisi\u00f3n la escala de estos fen\u00f3menos en los modelos clim\u00e1ticos y tener proyecciones m\u00e1s exactas de los efectos futuros del cambio clim\u00e1tico.<\/span><\/p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; admin_label=&#8221;Section&#8221; _builder_version=&#8221;4.16&#8243; custom_margin=&#8221;-20px||||false|false&#8221; custom_padding=&#8221;10px||||false|false&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_row padding_mobile=&#8221;off&#8221; column_padding_mobile=&#8221;on&#8221; admin_label=&#8221;Row&#8221; _builder_version=&#8221;4.16&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221; max_width=&#8221;780px&#8221; make_fullwidth=&#8221;off&#8221; use_custom_width=&#8221;on&#8221; width_unit=&#8221;on&#8221; 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