{"id":2020,"date":"2024-02-05T10:23:55","date_gmt":"2024-02-05T10:23:55","guid":{"rendered":"https:\/\/troposferica.com\/?p=2020"},"modified":"2024-02-05T10:37:50","modified_gmt":"2024-02-05T10:37:50","slug":"inversio-termica","status":"publish","type":"post","link":"https:\/\/troposferica.com\/ca\/inversio-termica\/","title":{"rendered":"INVERSI\u00d3 T\u00c8RMICA"},"content":{"rendered":"\n<p class=\"wp-block-paragraph\">Com a norma general, a l&#8217;atmosfera, la temperatura disminueix amb l&#8217;altura. Quan \u00e9s a l&#8217;inrev\u00e9s, quan la temperatura augmenta amb l&#8217;altura, \u00e9s que hi ha una inversi\u00f3 t\u00e8rmica.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Els moviments verticals ascendents i descendents de l\u2019aire a la troposfera s\u00f3n molt m\u00e9s comuns del que ens podem imaginar. Els podem trobar, per exemple, quan l\u2019aire topa amb un vessant d\u2019una muntanya, en els corrents dins d\u2019una tempesta, durant el pas d\u2019un front, en algunes zones a on es produeixen brises marines, &#8230; En aquests ascensos i descensos, hi ha variacions significatives de la temperatura de la part\u00edcula (o bombolla d\u2019aire) que es mobilitza.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">De fet, es defineix el <strong>gradient adiab\u00e0tic<\/strong> com la variaci\u00f3 de la temperatura que rep una bombolla d\u2019aire durant el seu proc\u00e9s d\u2019ascensi\u00f3 vertical. Si durant aquest ascens aquesta bombolla no cont\u00e9 prou vapor d\u2019aigua per condensar-se, la seva temperatura disminuir\u00e0 0,98 \u00baC per cada 100 metres: \u00e9s el que anomenem <strong>gradient adiab\u00e0tic sec<\/strong>. En el cas que el moviment sigui descendent, la seva temperatura augmentar\u00e0 en 0,98\u00baC. Si fos el cas que durant l\u2019ascens de la bombolla d\u2019aire s\u00ed que aconsegueix condensar-se, llavors la disminuci\u00f3 de la temperatura ser\u00e0 de 0,6\u00baC aproximadament &#8211; \u00e9s un valor aproximat, ja que en aquest cas s\u00ed que hi ha petites variacions respecte de la pressi\u00f3 &#8211; per cada 100 metres d\u2019elevaci\u00f3: \u00e9s el que anomenem <strong>gradient adiab\u00e0tic humit. <\/strong>Si es produeix el descens d\u2019aire humit, la variaci\u00f3 de la temperatura per cada 100 metres \u00e9s la mateixa per\u00f2 en sentit positiu. El fet que el valor del gradient adiab\u00e0tic humit sigui m\u00e9s petit que el valor respectiu sec \u00e9s a causa de l\u2019alliberaci\u00f3 de <strong>calor latent<\/strong> que es produeix durant la condensaci\u00f3 del vapor d\u2019aigua a mesura que s\u2019eleva. \u00c9s a dir, com que la condensaci\u00f3 del vapor d\u2019aigua allibera calor, el refredament a causa de la p\u00e8rdua de la pressi\u00f3 (per l\u2019elevaci\u00f3) queda lleugerament contrarestat, fent que el gradient adiab\u00e0tic humit sigui m\u00e9s petit que el sec.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">\u00c9s molt m\u00e9s f\u00e0cil que aquests moviments verticals es produeixin quan la distribuci\u00f3 real de les temperatures en un punt determinat vagi disminuint amb l\u2019al\u00e7ada (veure cas 1 de la Fig. 1). Com m\u00e9s r\u00e0pid disminueixi la temperatura amb l\u2019al\u00e7ada, m\u00e9s grau d\u2019inestabilitat existir\u00e0.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Per\u00f2 en determinades situacions meteorol\u00f2giques, com per exemple en zones amb alta pressi\u00f3, es pot produir el fenomen invers; \u00e9s a dir que la temperatura augmenti amb l\u2019al\u00e7ada: \u00e9s l\u2019anomenada <strong>inversi\u00f3 t\u00e8rmica<\/strong> (veure casos 2 i 3 de la Fig. 1). En aquestes situacions d\u2019inversi\u00f3 t\u00e8rmica \u00e9s molt dif\u00edcil que les bombolles, siguin d\u2019aire sec o humit, puguin elevar-se i, per tant, provocar la formaci\u00f3 de n\u00favols. A m\u00e9s, tamb\u00e9 con\u00e8ixer que aquestes inversions t\u00e8rmiques solen evolucionar a mesura que una zona d\u2019altes pressions s\u2019estableix sobre una regi\u00f3: durant el pas dels dies se sol accentuar la inversi\u00f3, especialment a les capes inferiors, \u00e9s a dir, les m\u00e9s properes al terra (\u00e9s a dir, poden passar del perfil 2 al 3 al cap d\u2019unes hores o dies).<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"321\" height=\"283\" src=\"https:\/\/troposferica.com\/wp-content\/uploads\/2024\/02\/image-2.png\" alt=\"\" class=\"wp-image-2021\" srcset=\"https:\/\/troposferica.com\/wp-content\/uploads\/2024\/02\/image-2.png 321w, https:\/\/troposferica.com\/wp-content\/uploads\/2024\/02\/image-2-300x264.png 300w\" sizes=\"auto, (max-width: 321px) 100vw, 321px\" \/><figcaption class=\"wp-element-caption\"><strong>Fig 1.<\/strong> <em>Variaci\u00f3 de la temperatura amb l\u2019al\u00e7ada en 3 possibles situacions diferents: 1, sense inversi\u00f3; 2 amb inversi\u00f3 t\u00e8rmica a una determinada al\u00e7ada; 3 amb inversi\u00f3 t\u00e8rmica amb contacte a la superf\u00edcie.<\/em> Font: tecnosiverafont.weebly.com<\/figcaption><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">L\u2019al\u00e7ada a on podem trobar aquesta inversi\u00f3 t\u00e8rmica i el seu gruix (indicat amb una clau en el gr\u00e0fic de la Fig. 1) \u00e9s determinant en la formaci\u00f3 de n\u00favols com tamb\u00e9 en la dispersi\u00f3 de contaminants. De fet, quan la inversi\u00f3 t\u00e8rmica est\u00e0 localitzada a la zona m\u00e9s propera de la superf\u00edcie terrestre, bona part del vapor d\u2019aigua de la troposfera queda atrapat en aquesta capa sense cap possibilitat d\u2019enlairar-se provocant-ne la seva concentraci\u00f3 i possible posterior condensaci\u00f3 en forma de boira baixa. No nom\u00e9s queda atrapat el vapor d\u2019aigua sin\u00f3 tamb\u00e9 els contaminants, si \u00e9s que n\u2019hi ha, provocant pics en les concentracions de contaminants (de NO<sub>2<\/sub> i de PM10) que nom\u00e9s es dispersaran quan la inversi\u00f3 t\u00e8rmica s\u2019acabi trencant.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"889\" height=\"500\" src=\"https:\/\/troposferica.com\/wp-content\/uploads\/2024\/02\/image-3.png\" alt=\"\" class=\"wp-image-2023\" srcset=\"https:\/\/troposferica.com\/wp-content\/uploads\/2024\/02\/image-3.png 889w, https:\/\/troposferica.com\/wp-content\/uploads\/2024\/02\/image-3-300x169.png 300w, https:\/\/troposferica.com\/wp-content\/uploads\/2024\/02\/image-3-768x432.png 768w\" sizes=\"auto, (max-width: 889px) 100vw, 889px\" \/><figcaption class=\"wp-element-caption\"><strong>Fig 2.<\/strong> <em>Fotografia nocturna del 26 d\u2019octubre de 2017 de la ciutat de Barcelona a on es visibilitza la capa d\u2019inversi\u00f3 t\u00e8rmica amb una l\u00ednia discont\u00ednua.<\/em> Font: Alfons Puertas. Diari Ara.<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>Com a norma general, a l&#8217;atmosfera, la temperatura disminueix amb l&#8217;altura. Quan \u00e9s a l&#8217;inrev\u00e9s, quan la temperatura augmenta amb l&#8217;altura, \u00e9s que hi ha una inversi\u00f3 t\u00e8rmica. Els moviments verticals ascendents i descendents de l\u2019aire a la troposfera s\u00f3n molt m\u00e9s comuns del que ens podem imaginar. Els podem trobar, per exemple, quan l\u2019aire [&#8230;]\n","protected":false},"author":35,"featured_media":2027,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[75],"tags":[64,71,72],"class_list":["post-2020","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-curiosidades-ca","tag-meteorologia-ca","tag-muntanya","tag-prediccio"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v28.0 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Qu\u00e8 \u00e9s la inversi\u00f3 t\u00e8rmica? - Troposferica<\/title>\n<meta name=\"description\" content=\"En determinades situacions meteorol\u00f2giques la temperatura augmenta amb l&#039;altura: \u00e9s l&#039;anomenada inversi\u00f3 t\u00e8rmica.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/troposferica.com\/ca\/inversio-termica\/\" \/>\n<meta property=\"og:locale\" content=\"ca_ES\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Qu\u00e8 \u00e9s la inversi\u00f3 t\u00e8rmica? 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