{"id":15307,"date":"2016-12-08T11:34:24","date_gmt":"2016-12-08T10:34:24","guid":{"rendered":"https:\/\/elspeedo.cz\/4-11-lokalni-jevy\/"},"modified":"2016-12-09T23:17:27","modified_gmt":"2016-12-09T22:17:27","slug":"4-11-lokalni-jevy","status":"publish","type":"post","link":"https:\/\/elspeedo.cz\/pl\/4-11-lokalni-jevy\/","title":{"rendered":"4.11. Zjawiska lokalne"},"content":{"rendered":"
[vc_row][vc_column width=”1\/2″][vc_single_image image=”14838″ img_size=”full” alignment=”center” style=”vc_box_rounded”][\/vc_column][vc_column width=”1\/2″][vc_column_text]\n
\n

Bryza g\u00f3rska<\/strong><\/span><\/p>\n

Cyrkulacja dopo\u0142udniowa<\/strong><\/p>\n

S\u0142o\u0144ce ogrzewa stoki (zaczyna si\u0119 od stok\u00f3w wschodnich i poludniowo \u2013 wschodnich) i od nich ogrzewa si\u0119 powietrze. To ciep\u0142e (tzn. i l\u017cejsze) powietrze zaczyna si\u0119 wy\u015blizgiwa\u0107 wzd\u0142u\u017c stok\u00f3w ku g\u00f3rze. Powietrze w \u015brodku doliny (\u015brodek doliny jest wi\u0142gotny, znaczy i ch\u0142odniejszy) dope\u0142nia si\u0119 duszeniami nad \u015brodkiem doliny. Opr\u00f3cz tego powietrze unosz\u0105ce si\u0119 wzd\u0142u\u017c stok\u00f3w przysysa za sob\u0105 te\u017c powietrze \u015brodkiem doliny w kierunku do \u015brodku g\u00f3r, co spowoduje powstanie tzw. wiatru dolinowego. Wiatr wiej\u0105cy wzd\u0142u\u017c stok\u00f3w ku g\u00f3rze nazywamy te\u017c zjawiskiem anabatycznym.<\/strong><\/p>\n<\/div>\n[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column css=”.vc_custom_1481191342295{padding-top: 40px !important;}”][vc_separator el_width=”80″ el_class=”basic-separator” css=”.vc_custom_1481191316039{padding-top: 40px !important;padding-bottom: 40px !important;}”][\/vc_column][vc_column width=”1\/2″][vc_single_image image=”14767″ img_size=”full” alignment=”center” style=”vc_box_rounded”][\/vc_column][vc_column width=”1\/2″][vc_column_text]\n

Cyrkulacja popo\u0142udniowa<\/strong><\/p>\n

W ci\u0105gu dnia wraz z coraz mocniejszym promieniowaniem s\u0142onecznym ca\u0142e zjawisko nasila si\u0119. Cyrkulacja obejmuje ca\u0142y przekr\u00f3j doliny wzd\u0142u\u017c zboczy i powy\u017cej szczyt\u00f3w, gdzie mog\u0105 si\u0119 tworzy\u0107 stacjonarne szeregi chmur typu Cumulus. Wiatr dolinowy te\u017c nasila si\u0119 i warunkach termicznego dnia mo\u017ce si\u0119 wzmacnia\u0107 a\u017c do pr\u0119dko\u015bci niebezpiecznej dla przypadkowego l\u0105dowania w \u015brodku doliny, szczeg\u00f3lnie kiedy dolina jest g\u0142\u0119boka i w\u0105ska. P\u00f3\u017anym popo\u0142udniem i tu\u017c przed wieczorem termika dzia\u0142a ju\u017c bardziej wzd\u0142u\u017c stok\u00f3w po\u0142udniowo-zachodnich i zachodnich, natomiast wzd\u0142u\u017c stok\u00f3w wschodnich, kt\u00f3re zaczynaj\u0105 si\u0119 ju\u017c ozi\u0119bia\u0107 powietrze zaczyna opada\u0107 w d\u00f3\u0142. Wiatr dolinowy przed wieczorem zwykle maleje, jednak latem mo\u017ce trwa\u0107 nieco d\u0142u\u017cej, nawet po zachodzie s\u0142o\u0144ca, kiedy odkr\u0119ci si\u0119 szybko do odwrotnego kierunku, tzw. sp\u0142ywu nocnego.<\/p>\n[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column css=”.vc_custom_1481191342295{padding-top: 40px !important;}”][vc_separator el_width=”80″ el_class=”basic-separator” css=”.vc_custom_1481191316039{padding-top: 40px !important;padding-bottom: 40px !important;}”][\/vc_column][vc_column width=”1\/2″][vc_single_image image=”14766″ img_size=”full” alignment=”center” style=”vc_box_rounded”][\/vc_column][vc_column width=”1\/2″][vc_column_text]\n

Sp\u0142yw nocny<\/strong><\/p>\n

Wraz z zachodem S\u0142o\u0144ca powierzchnia Ziemi zaczyna si\u0119 och\u0142adza\u0107. Od niej ozi\u0119bia si\u0119 przy\u0142eg\u0142a warstwa powietrza, co powoduje jej sp\u0142yw wzd\u0142u\u017c stok\u00f3w oraz \u015brodkiem doliny w d\u00f3\u0142. Wiatr \u015brodkiem doliny mo\u017ce by\u0107 stosunkowo mocny, lecz nie osi\u0105ga on si\u0142y wiatru dolinowego w ci\u0105gu dnia, kt\u00f3ry nap\u0119dzany jest energi\u0105 S\u0142o\u0144ca.<\/p>\n

Taki sp\u0142yw nocny nazywamy te\u017c zjawiskiem katabatycznym.<\/strong> Powoduje on np. to, \u017ce wieczorem dym z ognia sp\u0142ywa zawsze wzd\u0142u\u017c stoku. Sp\u0142yw nocny na przedg\u00f3rzu lub w niskich g\u00f3rach rozpoczyna si\u0119 p\u0142ynnie, natomiast w wysokich i stromych g\u00f3rach potrafi si\u0119 przekr\u0119ci\u0107 w ci\u0105gu kilku minut.
\nJedyne jego \u201eniebezpiecze\u0144stwo\u201d polega na tym, \u017ce z wiatrem \u201ew plecy\u201d mo\u017ce si\u0119 nam nie uda\u0107 wystartowa\u0107 i b\u0119dziemy biwakowa\u0107 na szczycie g\u00f3ry do nast\u0119pnego dnia, kiedy to zn\u00f3w zacznie wia\u0107 wiatr pod stok.<\/p>\n[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column css=”.vc_custom_1481191342295{padding-top: 40px !important;}”][vc_separator el_width=”80″ el_class=”basic-separator” css=”.vc_custom_1481191316039{padding-top: 40px !important;padding-bottom: 40px !important;}”][\/vc_column][vc_column width=”1\/2″][vc_single_image image=”14765″ img_size=”full” alignment=”center” style=”vc_box_rounded”][\/vc_column][vc_column width=”1\/2″][vc_column_text]\n

Bryza<\/strong><\/span><\/p>\n

Bryza l\u0105dowa<\/strong><\/p>\n

\u00a0<\/strong>W porze dziennej l\u0105d nagrzewa si\u0119 od promieniowania s\u0142onecznego, przy sta\u0142ej niemal temperaturze wody. Powstaje cyrkulacja o kierunku prostopad\u0142ym do linii brzegowej, powoduj\u0105ca nad Ziemi\u0105 wiatr od morza, za\u015b na wysoko\u015bci wiatr przeciwny. Wiej\u0105cy od morza wiatr jest umiarkowany i pozbawiony turbulencji, dzi\u0119ki przep\u0142ywowi nad powierzchni\u0105 morza.<\/p>\n

Je\u015bli wybrze\u017ce uformowane jest w postaci regularnego wzbocza, to wyst\u0119puj\u0105 doskona\u0142e warunki do lot\u00f3w zboczowych.<\/p>\n[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column css=”.vc_custom_1481191342295{padding-top: 40px !important;}”][vc_separator el_width=”80″ el_class=”basic-separator” css=”.vc_custom_1481191316039{padding-top: 40px !important;padding-bottom: 40px !important;}”][\/vc_column][vc_column width=”1\/2″][vc_single_image image=”14764″ img_size=”full” alignment=”center” style=”vc_box_rounded”][\/vc_column][vc_column width=”1\/2″][vc_column_text]\n

Bryza morska<\/strong><\/p>\n

W porze nocnej kierunek bryzy jest odwrotny, odpowiednio do powstaj\u0105cej w\u00f3wczas r\u00f3\u017cnicy temperatur. Bryza l\u0105dowa s\u0142absza jest od morskiej, bowiem nie jest nap\u0119dzana energi\u0105 S\u0142o\u0144ca.<\/p>\n

Bryza morska wykorzystywana by\u0142a niegdy\u015b przez marynarzy wyp\u0142ywaj\u0105cych w morze statkami \u017cag\u0142owymi nap\u0119dzanymi jedynie si\u0142\u0105mi natury. Nad ranem wyp\u0142ywali oni na morze z wiatrem wiej\u0105cym od \u0142\u0105du, natomiast do portu wracali ju\u017c w ci\u0105gu dnia dzi\u0119ki bryzie morskiej.<\/p>\n[\/vc_column_text][\/vc_column][\/vc_row]\n<\/div>","protected":false},"excerpt":{"rendered":"

[vc_row][vc_column width=”1\/2″][vc_single_image image=”14838″ img_size=”full” alignment=”center” style=”vc_box_rounded”][\/vc_column][vc_column width=”1\/2″][vc_column_text] Bryza g\u00f3rska Cyrkulacja dopo\u0142udniowa S\u0142o\u0144ce ogrzewa stoki (zaczyna si\u0119 od stok\u00f3w wschodnich i poludniowo \u2013 wschodnich) i od nich ogrzewa si\u0119 powietrze. To ciep\u0142e (tzn. i l\u017cejsze) powietrze zaczyna si\u0119 wy\u015blizgiwa\u0107 wzd\u0142u\u017c stok\u00f3w ku g\u00f3rze. Powietrze w \u015brodku doliny (\u015brodek doliny jest wi\u0142gotny, znaczy i ch\u0142odniejszy) dope\u0142nia si\u0119 […]<\/p>\n","protected":false},"author":7,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_tribe_blocks_recurrence_rules":"","_tribe_blocks_recurrence_exclusions":"","_tribe_blocks_recurrence_description":"","footnotes":""},"categories":[329],"tags":[],"class_list":["post-15307","post","type-post","status-publish","format-standard","hentry","category-bez-kategorie-pl"],"yoast_head":"\n4.11. Zjawiska lokalne — El Speedo<\/title>\n<meta name=\"description\" content=\"El Speedo je nejv\u011bt\u0161\u00ed paraglidingov\u00e1 komunita a \u0161kola v \u010cR. 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