<\/p>\n\n\n\n
Opracowanie: dr Grzegorz Duniec, IMGW-PIB CMM<\/p>\n\n\n
W troposferze wyst\u0119puj\u0105 chmury, kt\u00f3re ze wzgl\u0119du na budow\u0119 oraz na wysoko\u015b\u0107 na jakiej s\u0105 obserwowane dzielimy na pi\u0119tra i rodziny. Mi\u0119dzynarodowa Komisja Chmur WMO podzieli\u0142a chmury na dziesi\u0119\u0107 podstawowych rodzaj\u00f3w, kt\u00f3re mog\u0105 wyst\u0119powa\u0107 w trzech pi\u0119trach (pi\u0119tro g\u00f3rne \u2013 chmury wysokie, pi\u0119tro \u015brednie \u2013 chmury \u015brednie, pi\u0119tro dolne \u2013 chmury niskie, chmury o budowie pionowej (Cumulus, Cumulonimbus) kt\u00f3re mog\u0105 rozci\u0105ga\u0107 si\u0119 od pi\u0119tra dolnego do g\u00f3rnego) [1].<\/p>\n
<\/p>\n
\u0179r\u00f3d\u0142o: Dorota Matuszko, Chmura i pogoda, Nowa mi\u0119dzynarodowa klasyfikacja chmur<\/em>, Wydawnictwo Uniwersytetu Jagiello\u0144skiego, 2018<\/p>\n<\/p>\n\u0179r\u00f3d\u0142o: Dorota Matuszko, Chmura i pogoda, Nowa mi\u0119dzynarodowa klasyfikacja chmur<\/em>, Wydawnictwo Uniwersytetu Jagiello\u0144skiego, 2018<\/p>\nW ka\u017cdym pi\u0119trze mog\u0105 tworzy\u0107 si\u0119 chmury, kt\u00f3re b\u0119d\u0105 pokrywa\u0107 jaki\u015b fragment sklepienia niebieskiego. Zachmurzenie og\u00f3lne stanowi zachmurzenie \u0142\u0105czne wszystkich chmur wyst\u0119puj\u0105cych na niebie. Nale\u017cy podkre\u015bli\u0107, \u017ce suma zachmurzenie chmur poszczeg\u00f3lnych pi\u0119ter nie b\u0119dzie r\u00f3wna\u0142a si\u0119 wielko\u015bci zachmurzenia og\u00f3lnego. Nie obowi\u0105zuje tutaj r\u00f3wno\u015b\u0107:<\/p>\nCL<\/sub>+CM<\/sub>+CH<\/sub> \u2260 zachmurzenie og\u00f3lne<\/p>\n<\/p>\nPrzyk\u0142ad symulacji zachmurzenia modelem ALARO, na godzin\u0119 12 UTC (14 czasu lokalnego), 6 VI 2023.<\/p>\n <\/p>\nMapa synoptyczna<\/strong><\/p>\n<\/p>\nLiteratura<\/strong><\/p>\n\nZofia Kaczorowska, Pogoda i klimat<\/em>, wydanie II, WSiP, Warszawa 1986.<\/li>\nDorota Matuszko, Chmura i pogoda, Nowa mi\u0119dzynarodowa klasyfikacja chmur<\/em>, Wydawnictwo Uniwersytetu Jagiello\u0144skiego, 2018<\/li>\n<\/ol>\n\n\n\n\n\n\nUdost\u0119pnij<\/p>\n","protected":false},"excerpt":{"rendered":"Przy okazji za\u0107mienia S\u0142o\u0144ca poznali\u015bmy mechanizm za\u0107mie\u0144, polegaj\u0105cy na tym, \u017ce jedno cia\u0142o niebieskie chowa si\u0119 (ca\u0142kowicie lub cz\u0119\u015bciowo) w cieniu lub p\u00f3\u0142cieniu sto\u017cka drugiego cia\u0142a niebieskiego. Podczas zbli\u017caj\u0105cego si\u0119 za\u0107mienia Ksi\u0119\u017cyc zanurzy si\u0119 cz\u0119\u015bciowo w sto\u017cek p\u00f3\u0142cienia. Podczas maksymalnej fazy 96,36% jego powierzchni b\u0119dzie zanurzone w p\u00f3\u0142cieniu. <\/p>\n","protected":false},"author":3,"featured_media":31827,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"templates\/landing.php","meta":{"ocean_post_layout":"","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"0","ocean_second_sidebar":"0","ocean_disable_margins":"enable","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"off","ocean_display_header":"off","ocean_header_style":"custom","ocean_center_header_left_menu":"0","ocean_custom_header_template":"2993","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"0","ocean_menu_typo_font_family":"0","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":0,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"0"},"yoast_head":"\n#AkademiaCMM - Zachmurzenie - Laboratorium Modelowania Meteorologicznego CMOK IMGW-PIB<\/title>\n<meta name=\"description\" content=\"W ka\u017cdym pi\u0119trze mog\u0105 tworzy\u0107 si\u0119 chmury, kt\u00f3re b\u0119d\u0105 pokrywa\u0107 jaki\u015b fragment sklepienia niebieskiego. 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\u0179r\u00f3d\u0142o: Dorota Matuszko, Chmura i pogoda, Nowa mi\u0119dzynarodowa klasyfikacja chmur<\/em>, Wydawnictwo Uniwersytetu Jagiello\u0144skiego, 2018<\/p>\nW ka\u017cdym pi\u0119trze mog\u0105 tworzy\u0107 si\u0119 chmury, kt\u00f3re b\u0119d\u0105 pokrywa\u0107 jaki\u015b fragment sklepienia niebieskiego. Zachmurzenie og\u00f3lne stanowi zachmurzenie \u0142\u0105czne wszystkich chmur wyst\u0119puj\u0105cych na niebie. Nale\u017cy podkre\u015bli\u0107, \u017ce suma zachmurzenie chmur poszczeg\u00f3lnych pi\u0119ter nie b\u0119dzie r\u00f3wna\u0142a si\u0119 wielko\u015bci zachmurzenia og\u00f3lnego. Nie obowi\u0105zuje tutaj r\u00f3wno\u015b\u0107:<\/p>\nCL<\/sub>+CM<\/sub>+CH<\/sub> \u2260 zachmurzenie og\u00f3lne<\/p>\n<\/p>\nPrzyk\u0142ad symulacji zachmurzenia modelem ALARO, na godzin\u0119 12 UTC (14 czasu lokalnego), 6 VI 2023.<\/p>\n <\/p>\nMapa synoptyczna<\/strong><\/p>\n<\/p>\nLiteratura<\/strong><\/p>\n\nZofia Kaczorowska, Pogoda i klimat<\/em>, wydanie II, WSiP, Warszawa 1986.<\/li>\nDorota Matuszko, Chmura i pogoda, Nowa mi\u0119dzynarodowa klasyfikacja chmur<\/em>, Wydawnictwo Uniwersytetu Jagiello\u0144skiego, 2018<\/li>\n<\/ol>\n\n\n\n\n\n\nUdost\u0119pnij<\/p>\n","protected":false},"excerpt":{"rendered":"Przy okazji za\u0107mienia S\u0142o\u0144ca poznali\u015bmy mechanizm za\u0107mie\u0144, polegaj\u0105cy na tym, \u017ce jedno cia\u0142o niebieskie chowa si\u0119 (ca\u0142kowicie lub cz\u0119\u015bciowo) w cieniu lub p\u00f3\u0142cieniu sto\u017cka drugiego cia\u0142a niebieskiego. Podczas zbli\u017caj\u0105cego si\u0119 za\u0107mienia Ksi\u0119\u017cyc zanurzy si\u0119 cz\u0119\u015bciowo w sto\u017cek p\u00f3\u0142cienia. Podczas maksymalnej fazy 96,36% jego powierzchni b\u0119dzie zanurzone w p\u00f3\u0142cieniu. <\/p>\n","protected":false},"author":3,"featured_media":31827,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"templates\/landing.php","meta":{"ocean_post_layout":"","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"0","ocean_second_sidebar":"0","ocean_disable_margins":"enable","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"off","ocean_display_header":"off","ocean_header_style":"custom","ocean_center_header_left_menu":"0","ocean_custom_header_template":"2993","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"0","ocean_menu_typo_font_family":"0","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":0,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"0"},"yoast_head":"\n#AkademiaCMM - Zachmurzenie - Laboratorium Modelowania Meteorologicznego CMOK IMGW-PIB<\/title>\n<meta name=\"description\" content=\"W ka\u017cdym pi\u0119trze mog\u0105 tworzy\u0107 si\u0119 chmury, kt\u00f3re b\u0119d\u0105 pokrywa\u0107 jaki\u015b fragment sklepienia niebieskiego. 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W ka\u017cdym pi\u0119trze mog\u0105 tworzy\u0107 si\u0119 chmury, kt\u00f3re b\u0119d\u0105 pokrywa\u0107 jaki\u015b fragment sklepienia niebieskiego. Zachmurzenie og\u00f3lne stanowi zachmurzenie \u0142\u0105czne wszystkich chmur wyst\u0119puj\u0105cych na niebie. Nale\u017cy podkre\u015bli\u0107, \u017ce suma zachmurzenie chmur poszczeg\u00f3lnych pi\u0119ter nie b\u0119dzie r\u00f3wna\u0142a si\u0119 wielko\u015bci zachmurzenia og\u00f3lnego. Nie obowi\u0105zuje tutaj r\u00f3wno\u015b\u0107:<\/p>\n
CL<\/sub>+CM<\/sub>+CH<\/sub> \u2260 zachmurzenie og\u00f3lne<\/p>\n<\/p>\nPrzyk\u0142ad symulacji zachmurzenia modelem ALARO, na godzin\u0119 12 UTC (14 czasu lokalnego), 6 VI 2023.<\/p>\n <\/p>\nMapa synoptyczna<\/strong><\/p>\n<\/p>\nLiteratura<\/strong><\/p>\n\nZofia Kaczorowska, Pogoda i klimat<\/em>, wydanie II, WSiP, Warszawa 1986.<\/li>\nDorota Matuszko, Chmura i pogoda, Nowa mi\u0119dzynarodowa klasyfikacja chmur<\/em>, Wydawnictwo Uniwersytetu Jagiello\u0144skiego, 2018<\/li>\n<\/ol>\n\n\n\n\n\n\nUdost\u0119pnij<\/p>\n","protected":false},"excerpt":{"rendered":"Przy okazji za\u0107mienia S\u0142o\u0144ca poznali\u015bmy mechanizm za\u0107mie\u0144, polegaj\u0105cy na tym, \u017ce jedno cia\u0142o niebieskie chowa si\u0119 (ca\u0142kowicie lub cz\u0119\u015bciowo) w cieniu lub p\u00f3\u0142cieniu sto\u017cka drugiego cia\u0142a niebieskiego. Podczas zbli\u017caj\u0105cego si\u0119 za\u0107mienia Ksi\u0119\u017cyc zanurzy si\u0119 cz\u0119\u015bciowo w sto\u017cek p\u00f3\u0142cienia. Podczas maksymalnej fazy 96,36% jego powierzchni b\u0119dzie zanurzone w p\u00f3\u0142cieniu. <\/p>\n","protected":false},"author":3,"featured_media":31827,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"templates\/landing.php","meta":{"ocean_post_layout":"","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"0","ocean_second_sidebar":"0","ocean_disable_margins":"enable","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"off","ocean_display_header":"off","ocean_header_style":"custom","ocean_center_header_left_menu":"0","ocean_custom_header_template":"2993","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"0","ocean_menu_typo_font_family":"0","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":0,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"0"},"yoast_head":"\n#AkademiaCMM - Zachmurzenie - Laboratorium Modelowania Meteorologicznego CMOK IMGW-PIB<\/title>\n<meta name=\"description\" content=\"W ka\u017cdym pi\u0119trze mog\u0105 tworzy\u0107 si\u0119 chmury, kt\u00f3re b\u0119d\u0105 pokrywa\u0107 jaki\u015b fragment sklepienia niebieskiego. Zachmurzenie og\u00f3lne stanowi zachmurzenie \u0142\u0105czne wszystkich chmur wyst\u0119puj\u0105cych na niebie. Nale\u017cy podkre\u015bli\u0107, \u017ce suma zachmurzenie chmur poszczeg\u00f3lnych pi\u0119ter nie b\u0119dzie r\u00f3wna\u0142a si\u0119 wielko\u015bci zachmurzenia og\u00f3lnego. Nie obowi\u0105zuje tutaj r\u00f3wno\u015b\u0107.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/cmm.imgw.pl\/?page_id=31826\" \/>\n<meta property=\"og:locale\" content=\"pl_PL\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"#AkademiaCMM - Zachmurzenie\" \/>\n<meta property=\"og:description\" content=\"W ka\u017cdym pi\u0119trze mog\u0105 tworzy\u0107 si\u0119 chmury, kt\u00f3re b\u0119d\u0105 pokrywa\u0107 jaki\u015b fragment sklepienia niebieskiego. 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Przyk\u0142ad symulacji zachmurzenia modelem ALARO, na godzin\u0119 12 UTC (14 czasu lokalnego), 6 VI 2023.<\/p>\n
Mapa synoptyczna<\/strong><\/p>\n<\/p>\nLiteratura<\/strong><\/p>\n\nZofia Kaczorowska, Pogoda i klimat<\/em>, wydanie II, WSiP, Warszawa 1986.<\/li>\nDorota Matuszko, Chmura i pogoda, Nowa mi\u0119dzynarodowa klasyfikacja chmur<\/em>, Wydawnictwo Uniwersytetu Jagiello\u0144skiego, 2018<\/li>\n<\/ol>\n\n\n\n\n\n\nUdost\u0119pnij<\/p>\n","protected":false},"excerpt":{"rendered":"Przy okazji za\u0107mienia S\u0142o\u0144ca poznali\u015bmy mechanizm za\u0107mie\u0144, polegaj\u0105cy na tym, \u017ce jedno cia\u0142o niebieskie chowa si\u0119 (ca\u0142kowicie lub cz\u0119\u015bciowo) w cieniu lub p\u00f3\u0142cieniu sto\u017cka drugiego cia\u0142a niebieskiego. Podczas zbli\u017caj\u0105cego si\u0119 za\u0107mienia Ksi\u0119\u017cyc zanurzy si\u0119 cz\u0119\u015bciowo w sto\u017cek p\u00f3\u0142cienia. Podczas maksymalnej fazy 96,36% jego powierzchni b\u0119dzie zanurzone w p\u00f3\u0142cieniu. <\/p>\n","protected":false},"author":3,"featured_media":31827,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"templates\/landing.php","meta":{"ocean_post_layout":"","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"0","ocean_second_sidebar":"0","ocean_disable_margins":"enable","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"off","ocean_display_header":"off","ocean_header_style":"custom","ocean_center_header_left_menu":"0","ocean_custom_header_template":"2993","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"0","ocean_menu_typo_font_family":"0","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":0,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"0"},"yoast_head":"\n#AkademiaCMM - Zachmurzenie - Laboratorium Modelowania Meteorologicznego CMOK IMGW-PIB<\/title>\n<meta name=\"description\" content=\"W ka\u017cdym pi\u0119trze mog\u0105 tworzy\u0107 si\u0119 chmury, kt\u00f3re b\u0119d\u0105 pokrywa\u0107 jaki\u015b fragment sklepienia niebieskiego. 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Literatura<\/strong><\/p>\n\nZofia Kaczorowska, Pogoda i klimat<\/em>, wydanie II, WSiP, Warszawa 1986.<\/li>\nDorota Matuszko, Chmura i pogoda, Nowa mi\u0119dzynarodowa klasyfikacja chmur<\/em>, Wydawnictwo Uniwersytetu Jagiello\u0144skiego, 2018<\/li>\n<\/ol>\n\n\n\n\n\n\nUdost\u0119pnij<\/p>\n","protected":false},"excerpt":{"rendered":"Przy okazji za\u0107mienia S\u0142o\u0144ca poznali\u015bmy mechanizm za\u0107mie\u0144, polegaj\u0105cy na tym, \u017ce jedno cia\u0142o niebieskie chowa si\u0119 (ca\u0142kowicie lub cz\u0119\u015bciowo) w cieniu lub p\u00f3\u0142cieniu sto\u017cka drugiego cia\u0142a niebieskiego. Podczas zbli\u017caj\u0105cego si\u0119 za\u0107mienia Ksi\u0119\u017cyc zanurzy si\u0119 cz\u0119\u015bciowo w sto\u017cek p\u00f3\u0142cienia. Podczas maksymalnej fazy 96,36% jego powierzchni b\u0119dzie zanurzone w p\u00f3\u0142cieniu. <\/p>\n","protected":false},"author":3,"featured_media":31827,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"templates\/landing.php","meta":{"ocean_post_layout":"","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"0","ocean_second_sidebar":"0","ocean_disable_margins":"enable","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"off","ocean_display_header":"off","ocean_header_style":"custom","ocean_center_header_left_menu":"0","ocean_custom_header_template":"2993","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"0","ocean_menu_typo_font_family":"0","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":0,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"0"},"yoast_head":"\n#AkademiaCMM - Zachmurzenie - Laboratorium Modelowania Meteorologicznego CMOK IMGW-PIB<\/title>\n<meta name=\"description\" content=\"W ka\u017cdym pi\u0119trze mog\u0105 tworzy\u0107 si\u0119 chmury, kt\u00f3re b\u0119d\u0105 pokrywa\u0107 jaki\u015b fragment sklepienia niebieskiego. 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Udost\u0119pnij<\/p>\n","protected":false},"excerpt":{"rendered":"
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