{"id":67,"date":"2026-04-29T10:08:27","date_gmt":"2026-04-29T10:08:27","guid":{"rendered":"https:\/\/theburningrim.com\/?page_id=67"},"modified":"2026-05-15T08:59:51","modified_gmt":"2026-05-15T08:59:51","slug":"atmosfera","status":"publish","type":"page","link":"https:\/\/theburningrim.com\/?page_id=67","title":{"rendered":"Atmosfera"},"content":{"rendered":"<div class=\"section-wrap\">\n<div class=\"page-hero\">\n<p class=\"hero-kicker\">THE BURNING RIM \u00b7 ATMOSPHERE<\/p>\n<h1 class=\"page-title-big\">\n      THE<br \/>ATMOSPHERE<br \/>IN TRANSITION<br \/>\n    <\/h1>\n<p class=\"page-lead\">\n      A dynamic system where temperature, circulation and vertical exchanges are being altered by climate change.\n    <\/p>\n<\/p><\/div>\n<\/div>\n<p><!-- IMMAGINE ATMOSFERA --><\/p>\n<div class=\"section-wrap\">\n<div class=\"atm-image-wrap\">\n<p>    <img decoding=\"async\"\n      src=\"https:\/\/theburningrim.com\/wp-content\/uploads\/2026\/05\/atmosfera.jpg\"\n      alt=\"Earth atmosphere from space\"\n      class=\"atm-image\"\n    ><\/p><\/div>\n<\/div>\n<div class=\"section-wrap\">\n<div class=\"page-text-card\">\n<p>\n      The atmosphere is not a static structure. It is a continuously evolving system where energy,<br \/>\n      humidity, gases and particles move across different layers through complex physical processes.\n    <\/p>\n<p>\n      Climate change is modifying this balance. Scientific observations collected over recent decades<br \/>\n      reveal significant transformations in atmospheric temperature distribution, circulation patterns<br \/>\n      and vertical exchanges between the troposphere and the stratosphere.\n    <\/p>\n<p>\n      The troposphere, the lowest atmospheric layer where weather develops, is warming progressively<br \/>\n      due to increasing greenhouse gas concentrations. At the same time, the stratosphere above it<br \/>\n      is cooling \u2014 a characteristic fingerprint of anthropogenic climate change.\n    <\/p>\n<p>\n      Between these two layers lies the tropopause, a transition region that acts as a dynamic boundary<br \/>\n      regulating exchanges of air masses, humidity, ozone and chemical compounds.\n    <\/p>\n<p>\n      The tropopause is not a fixed surface. Its altitude changes depending on latitude, season,<br \/>\n      atmospheric circulation and wave activity. Climate change appears to influence its structure,<br \/>\n      contributing to a gradual rise in tropopause height observed in several regions of the world.\n    <\/p>\n<p>\n      One of the most important mechanisms affecting upper atmospheric dynamics is the interaction<br \/>\n      between jet streams, Rossby waves and large-scale circulation systems. These structures control<br \/>\n      the transport of heat and momentum across the atmosphere and strongly influence weather evolution.\n    <\/p>\n<p>\n      Variations in jet stream intensity and position may alter the persistence of high-pressure systems,<br \/>\n      storm tracks and precipitation patterns. In the Mediterranean region, these changes can amplify<br \/>\n      periods of drought, heatwaves and atmospheric instability.\n    <\/p>\n<p>\n      Another important process is Stratosphere\u2013Troposphere Exchange (STE), through which air masses<br \/>\n      move vertically between atmospheric layers. STE events can transport ozone-rich stratospheric air<br \/>\n      downward into the troposphere, affecting atmospheric chemistry and radiative balance.\n    <\/p>\n<p>\n      Atmospheric instability is closely linked to energy distribution. A warmer atmosphere can hold<br \/>\n      more water vapor, increasing the amount of latent heat available for convective systems.<br \/>\n      This creates conditions favorable for more intense precipitation events and stronger storms.\n    <\/p>\n<p>\n      Understanding the atmosphere means understanding a system where local and global processes are<br \/>\n      deeply connected. What happens above the Mediterranean is influenced by planetary circulation,<br \/>\n      ocean temperatures and long-term climate forcing.\n    <\/p>\n<\/p><\/div>\n<\/div>\n<div class=\"section-wrap\">\n<div class=\"page-grid-3\">\n<div class=\"page-mini-card\">\n<h3>TROPOSPHERE<\/h3>\n<p>\n        The lower atmosphere is warming and storing more humidity and energy, influencing weather intensity and variability.\n      <\/p>\n<\/p><\/div>\n<div class=\"page-mini-card\">\n<h3>TROPOPAUSE<\/h3>\n<p>\n        The transition zone between troposphere and stratosphere regulates vertical atmospheric exchanges and circulation dynamics.\n      <\/p>\n<\/p><\/div>\n<div class=\"page-mini-card\">\n<h3>JET STREAMS<\/h3>\n<p>\n        Large-scale atmospheric currents influence storm evolution, heat transport and regional climate behavior.\n      <\/p>\n<\/p><\/div>\n<\/p><\/div>\n<\/div>\n<div class=\"section-wrap\">\n<div class=\"blue-panel\">\n<h2>READING THE SKY TO UNDERSTAND CLIMATE<\/h2>\n<p>\n      Atmospheric layers are interconnected components of a global climate engine where temperature,<br \/>\n      circulation and chemistry constantly interact.\n    <\/p>\n<p>\n      Climate change modifies these interactions at multiple scales, from local convection to planetary circulation.<br \/>\n      The atmosphere therefore becomes both a signal and a driver of climate transformation.\n    <\/p>\n<p>\n      The Burning Rim explores these processes through scientific interpretation, atmospheric dynamics<br \/>\n      and visual storytelling, connecting upper atmospheric physics with the future of the Mediterranean basin.\n    <\/p>\n<\/p><\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>THE BURNING RIM \u00b7 ATMOSPHERE THEATMOSPHEREIN TRANSITION A dynamic system where temperature, circulation and vertical exchanges are being altered by climate change. The atmosphere is not a static structure. It is a continuously evolving system where energy, humidity, gases and particles move across different layers through complex physical processes. Climate change is modifying this balance. [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_uag_custom_page_level_css":"","footnotes":""},"class_list":["post-67","page","type-page","status-publish","hentry"],"blocksy_meta":[],"uagb_featured_image_src":{"full":false,"thumbnail":false,"medium":false,"medium_large":false,"large":false,"1536x1536":false,"2048x2048":false},"uagb_author_info":{"display_name":"admin","author_link":"https:\/\/theburningrim.com\/?author=2"},"uagb_comment_info":0,"uagb_excerpt":"THE BURNING RIM \u00b7 ATMOSPHERE THEATMOSPHEREIN TRANSITION A dynamic system where temperature, circulation and vertical exchanges are being altered by climate change. The atmosphere is not a static structure. It is a continuously evolving system where energy, humidity, gases and particles move across different layers through complex physical processes. Climate change is modifying this balance.&hellip;","_links":{"self":[{"href":"https:\/\/theburningrim.com\/index.php?rest_route=\/wp\/v2\/pages\/67","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/theburningrim.com\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/theburningrim.com\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/theburningrim.com\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/theburningrim.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=67"}],"version-history":[{"count":4,"href":"https:\/\/theburningrim.com\/index.php?rest_route=\/wp\/v2\/pages\/67\/revisions"}],"predecessor-version":[{"id":226,"href":"https:\/\/theburningrim.com\/index.php?rest_route=\/wp\/v2\/pages\/67\/revisions\/226"}],"wp:attachment":[{"href":"https:\/\/theburningrim.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=67"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}