. "Alto-estratos ou, em latim, altostratus s\u00E3o camadas cinzentas ou azuladas, muitas vezes associadas a Altocumulus; compostas de got\u00EDculas de \u00E1gua e cristais de gelo; n\u00E3o formam halo, encobrem o sol; precipita\u00E7\u00E3o leve e cont\u00EDnua. Os altostratus s\u00E3o nuvens compostas por got\u00EDculas de \u00E1gua e, \u00E0s vezes, por cristais de gelo. Formam camadas cinzentas ou azuladas e mon\u00F3tonas, como um v\u00E9u ou len\u00E7ol fibroso estendido sobre uma \u00E1rea imensa, muitas vezes obscurecendo o Sol ou a Lua. Em algumas partes podem ser t\u00E3o finas que o Sol se v\u00EA como atrav\u00E9s de um vidro fosco. Mas n\u00E3o se observam halos (como nos cirrostratus). Formam-se em massas de ar est\u00E1vel, quando a humidade \u00E9 moderada e a temperatura \u00E9 relativamente alta. Anunciam frequentemente a chegada de uma frente quente e podem ser acompanhadas de alguns chuviscos ou queda de neve. Por vezes, as nuvens cirrostratus mais grossas s\u00E3o tomadas por altostratus. Mas os cirrostratus s\u00E3o em geral suficientemente transl\u00FAcidos para permitem a penetra\u00E7\u00E3o da luz do Sol ou da Lua. E os altostratus n\u00E3o produzem o efeito de halo, observado nos cirrostratus."@pt . "De altostratus is een egaal grijsachtig wolkengeslacht. Die bewolking ontstaat op de grens tussen koude en warmere lucht, waarbij de warme lucht over de zwaardere koude lucht schuift. Duitse meteorologen noemen dat proces \"Eintr\u00FCbung\". Eerst is de omtrek van de zon of de maan er nog doorheen te zien (translucidus), maar meestal wordt de bewolking snel dichter, verdwijnt de zon en zet de neerslag in (opacus). Soms komt deze bewolking in verschillende lagen voor (duplicatus). Deze wolk kan overgaan in de nimbostratus. \n* Translucidus \n* Opacus \n* Duplicatus \n* Undulatus \n* Radiatus"@nl . . "\u0412\u044B\u0441\u043E\u043A\u043E\u0441\u043B\u043E\u0438\u0441\u0442\u044B\u0435 \u043E\u0431\u043B\u0430\u043A\u0430 (\u043B\u0430\u0442. Altostratus)\u2014 \u0440\u0430\u0437\u043D\u043E\u0432\u0438\u0434\u043D\u043E\u0441\u0442\u044C \u043E\u0431\u043B\u0430\u043A\u043E\u0432, \u043F\u0440\u0435\u0434\u0441\u0442\u0430\u0432\u043B\u044F\u044E\u0449\u0430\u044F \u0441\u043E\u0431\u043E\u0439 \u043F\u043B\u043E\u0442\u043D\u044B\u0439 \u043F\u043E\u043A\u0440\u043E\u0432 \u0441\u0435\u0440\u043E\u0433\u043E \u0438\u043B\u0438 \u0431\u0435\u043B\u043E\u0432\u0430\u0442\u043E\u0433\u043E \u0446\u0432\u0435\u0442\u0430, \u0432\u0431\u043B\u0438\u0437\u0438 \u0441\u043E\u043B\u043D\u0446\u0430 \u0438\u043B\u0438 \u043B\u0443\u043D\u044B \u043E\u0431\u0440\u0430\u0437\u0443\u044E\u0449\u0438\u0439 \u0431\u043E\u043B\u0435\u0435 \u0441\u0432\u0435\u0442\u043B\u0443\u044E \u0447\u0430\u0441\u0442\u044C, \u0441\u043A\u0432\u043E\u0437\u044C \u043A\u043E\u0442\u043E\u0440\u0443\u044E \u0432\u0438\u0434\u043D\u0435\u0435\u0442\u0441\u044F \u0431\u043B\u0435\u0434\u043D\u044B\u0439, \u0441\u043B\u0430\u0431\u043E\u0441\u0432\u0435\u0442\u044F\u0449\u0438\u0439\u0441\u044F \u0434\u0438\u0441\u043A \u0441\u0432\u0435\u0442\u0438\u043B\u0430 (\u00AB\u0432\u043E\u0434\u044F\u043D\u0438\u0441\u0442\u043E\u0435 \u0441\u043E\u043B\u043D\u0446\u0435\u00BB). \u042D\u0442\u0438 \u043E\u0431\u043B\u0430\u043A\u0430 \u0441\u043B\u0443\u0436\u0430\u0442 \u043F\u0440\u0438\u0447\u0438\u043D\u043E\u0439 \u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u044F \u0440\u0430\u0434\u0443\u0436\u043D\u044B\u0445 \u0432\u0435\u043D\u0446\u043E\u0432 \u043E\u043A\u043E\u043B\u043E \u0421\u043E\u043B\u043D\u0446\u0430 \u0438\u043B\u0438 \u041B\u0443\u043D\u044B."@ru . . . "Altostratu"@eu . "Altostratus eller skiktmoln, f\u00F6rkortning As, \u00E4r ett huvudmolnslag som tillh\u00F6r familjen medelh\u00F6ga moln och finns p\u00E5 2000 - 5000 meters h\u00F6jd. Molnen \u00E4r i j\u00E4mngr\u00E5a skikt eller lager. De uppkommer genom att stora luftmassor lyfts och kondenseras. Altostratus t\u00E4cker oftast stora omr\u00E5den. Molnen \u00E4r speciellt farliga f\u00F6r flygtrafiken d\u00E5 dessa \u00E4r orsak till nedisning. Till skillnad mot cirrostratus s\u00E5 ger altostratus ej upphov till halo."@sv . . "28984"^^ . . . . . . . "Altostratus (As) adalah awan yang berbentuk lembaran dan sering berbentuk satu struktur berserat. Awan altostratus dapat diikuti oleh keluarnya endapan dari dalam awan baik bentuk air, salju, atau kristal es, atau biasa disebut presipitasi, yang meluas dan dalam waktu yang cukup lama. Altostratus dapat membentuk korona, selain itu bulan atau matahari terlihat pucat jika dilihat melalui awan ini. Altostratus berada di ketinggian medium atau berkisar 2.000 m - 7.000 m. Awan ini berwarna abu-abu atau biru keabu-abuan yang menutupi langit dengan sebaran yang luas. Altostratus dapat menimbulkan gerimis, hujan ringan hingga sedang, atau salju yang cukup terjadi cukup lama, awan ini terbentuk menjelang badai, biasanya terbentuk pada sore hari sedangkan hujan yang dihasilkan terbentuk pada malam hari. Awan ini diklasifikasikan sebagai nimbostratus ketika menghasilkan hujan yang sampai menyentuh tanah atau permukaan bumi. Awan altostratus lenticularis dapat terbentuk akibat angin kencang, awan jenis ini tidak menghasilkan hujan."@in . . . "L'altostratus est un genre de nuage de l'\u00E9tage moyen, situ\u00E9 \u00E0 une altitude comprise entre 2000 et 5 000 m, pour une \u00E9paisseur de 500 jusqu'\u00E0 3 000 m. C'est un nuage stratiforme, c'est-\u00E0-dire en couche, dont les limites sont difficilement d\u00E9finissables. Il forme une vaste couche grise l\u00E9g\u00E8rement stri\u00E9e, qui laisse diffuser la lumi\u00E8re solaire sans ombre apparente au sol, comme au travers d'un verre d\u00E9poli. Lorsqu'il est \u00E9pais, il entraine parfois des chutes de pluie ou de neige. Il est relatif \u00E0 un air stable, c'est-\u00E0-dire qu'il n'y a pas de mouvements d'air verticaux importants. On l'observe pr\u00E9f\u00E9rentiellement juste avant un front chaud (son arriv\u00E9e rapide en annonce l'imminence) ou dans les occlusions peu actives de perturbation."@fr . "Altostratus (As) \u010Di vyv\u00FD\u0161en\u00E1 sloha je front\u00E1ln\u00ED oblak, jeho\u017E horizont\u00E1ln\u00ED rozm\u011Bry jsou stovky a\u017E tis\u00EDce kilometr\u016F a vertik\u00E1ln\u00ED rozm\u011Bry v \u0159\u00E1dech stovek metr\u016F. Je slo\u017Een\u00FD z vodn\u00EDch kapek a ledov\u00FDch krystalk\u016F. Z oblaku mohou vypad\u00E1vat sr\u00E1\u017Eky, hlavn\u011B v chladn\u00E9 \u010D\u00E1sti roku. P\u0159i pr\u016Fletu skrze oblak As p\u0159i teplot\u011B vzduchu mezi 0 a\u017E -12 \u00B0C se na povrchu letounu utv\u00E1\u0159\u00ED zpravidla m\u00EDrn\u00E1 a\u017E siln\u00E1 n\u00E1mraza."@cs . "Altostratus"@nl . . . . . "Altostratus (v. lat. altum \u201EH\u00F6he\u201C und stratus bzw. sternere \u201Eausdehnen, ausbreiten, mit einer Schicht bedecken\u201C; Abk.: As) ist eine bl\u00E4uliche bis graue mittelhohe Schichtwolke ohne Konturen, die aus (unterk\u00FChlten) Wassertr\u00F6pfchen und Eiskristallen besteht. Er ist relativ deutlich grau, die Sonne ist hinter den dunklen Wolken manchmal fast nicht sichtbar. Wenn der Altostratus nach Cirrostratus (Schleierwolken) gro\u00DFfl\u00E4chig aufzieht, ist meist eine Warmfront oder Okklusion im Anzug. Anzahl Stunden, bis es zu regnen beginnt:"@de . . "\u0412\u044B\u0441\u043E\u043A\u043E\u0441\u043B\u043E\u0438\u0441\u0442\u044B\u0435 \u043E\u0431\u043B\u0430\u043A\u0430 (\u043B\u0430\u0442. Altostratus)\u2014 \u0440\u0430\u0437\u043D\u043E\u0432\u0438\u0434\u043D\u043E\u0441\u0442\u044C \u043E\u0431\u043B\u0430\u043A\u043E\u0432, \u043F\u0440\u0435\u0434\u0441\u0442\u0430\u0432\u043B\u044F\u044E\u0449\u0430\u044F \u0441\u043E\u0431\u043E\u0439 \u043F\u043B\u043E\u0442\u043D\u044B\u0439 \u043F\u043E\u043A\u0440\u043E\u0432 \u0441\u0435\u0440\u043E\u0433\u043E \u0438\u043B\u0438 \u0431\u0435\u043B\u043E\u0432\u0430\u0442\u043E\u0433\u043E \u0446\u0432\u0435\u0442\u0430, \u0432\u0431\u043B\u0438\u0437\u0438 \u0441\u043E\u043B\u043D\u0446\u0430 \u0438\u043B\u0438 \u043B\u0443\u043D\u044B \u043E\u0431\u0440\u0430\u0437\u0443\u044E\u0449\u0438\u0439 \u0431\u043E\u043B\u0435\u0435 \u0441\u0432\u0435\u0442\u043B\u0443\u044E \u0447\u0430\u0441\u0442\u044C, \u0441\u043A\u0432\u043E\u0437\u044C \u043A\u043E\u0442\u043E\u0440\u0443\u044E \u0432\u0438\u0434\u043D\u0435\u0435\u0442\u0441\u044F \u0431\u043B\u0435\u0434\u043D\u044B\u0439, \u0441\u043B\u0430\u0431\u043E\u0441\u0432\u0435\u0442\u044F\u0449\u0438\u0439\u0441\u044F \u0434\u0438\u0441\u043A \u0441\u0432\u0435\u0442\u0438\u043B\u0430 (\u00AB\u0432\u043E\u0434\u044F\u043D\u0438\u0441\u0442\u043E\u0435 \u0441\u043E\u043B\u043D\u0446\u0435\u00BB). \u042D\u0442\u0438 \u043E\u0431\u043B\u0430\u043A\u0430 \u0441\u043B\u0443\u0436\u0430\u0442 \u043F\u0440\u0438\u0447\u0438\u043D\u043E\u0439 \u043E\u0431\u0440\u0430\u0437\u043E\u0432\u0430\u043D\u0438\u044F \u0440\u0430\u0434\u0443\u0436\u043D\u044B\u0445 \u0432\u0435\u043D\u0446\u043E\u0432 \u043E\u043A\u043E\u043B\u043E \u0421\u043E\u043B\u043D\u0446\u0430 \u0438\u043B\u0438 \u041B\u0443\u043D\u044B."@ru . . . . . . . "\u0627\u0644\u0631\u064E\u0651\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u0623\u0648 \u0627\u0644\u0632\u064E\u0651\u0639\u0652\u0628\u064E\u062C \u0623\u0648 \u0627\u0644\u0632\u0650\u0651\u0639\u0652\u0628\u0650\u062C \u0647\u0648 \u062C\u0646\u0633 \u0633\u062D\u0627\u0628\u0629 \u0645\u062A\u0648\u0633\u0637 \u0627\u0644\u0627\u0631\u062A\u0641\u0627\u0639 \u064A\u062A\u0643\u0648\u0646 \u0645\u0646 \u0642\u0637\u0631\u0627\u062A \u0627\u0644\u0645\u0627\u0621 \u0623\u0648 \u0628\u0644\u0648\u0631\u0627\u062A \u0627\u0644\u062C\u0644\u064A\u062F \u0623\u0648 \u0645\u0632\u064A\u062C \u0645\u0646 \u0627\u0644\u0627\u062B\u0646\u064A\u0646. \u062A\u062A\u0643\u0648\u0646 \u0639\u0646\u062F\u0645\u0627 \u062A\u0631\u062A\u0641\u0639 \u0643\u062A\u0644 \u0643\u0628\u064A\u0631\u0629 \u0645\u0646 \u0627\u0644\u0647\u0648\u0627\u0621 \u0627\u0644\u062F\u0627\u0641\u0626 \u0627\u0644\u0631\u0637\u0628 \u0645\u0627 \u064A\u0624\u062F\u064A \u0625\u0644\u0649 \u062A\u0643\u062B\u0641 \u0628\u062E\u0627\u0631 \u0627\u0644\u0645\u0627\u0621. \u0639\u0627\u062F\u0629 \u0645\u0627 \u064A\u064E\u0643\u0648\u0646 \u0627\u0644\u0631\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u0635\u0641\u0627\u0626\u062D \u0631\u0645\u0627\u062F\u064A\u0629 \u0623\u0648 \u0632\u0631\u0642\u0627\u0621 \u0628\u0644\u0627 \u0645\u0644\u0627\u0645\u062D \u0648\u0630\u0644\u0643 \u0645\u0639 \u0623\u0646 \u0644\u0628\u0639\u0636 \u0623\u0634\u0643\u0627\u0644\u0647 \u0642\u0648\u0627\u0639\u062F \u0645\u062A\u0645\u0648\u062C\u0629 \u0623\u0648 \u0645\u064F\u0639\u064E\u0635\u064E\u0651\u0628\u064E\u0629. \u064A\u0645\u0643\u0646 \u0631\u0624\u064A\u0629 \u0627\u0644\u0634\u0645\u0633 \u0645\u0646 \u062E\u0644\u0627\u0644 \u0633\u062D\u0628 \u0627\u0644\u0631\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u0627\u0644\u0631\u0642\u064A\u0642\u0629\u060C \u0644\u0643\u0646 \u0627\u0644\u0637\u0628\u0642\u0627\u062A \u0627\u0644\u062B\u062E\u064A\u0646\u0629 \u064A\u0645\u0643\u0646 \u0623\u0646 \u062A\u0643\u0648\u0646 \u0645\u0639\u062A\u0645\u0629 \u062A\u0645\u0627\u0645\u064B\u0627. \u064A\u064F\u0646\u0628\u0650\u0626 \u0627\u0644\u0631\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u0639\u0627\u062F\u0629\u064B \u0628\u0648\u0635\u0648\u0644 \u0627\u0644\u062C\u0628\u0647\u0627\u062A \u0627\u0644\u062F\u0627\u0641\u0626\u0629. \u0641\u0645\u0627 \u0623\u0646 \u062A\u0635\u0644 \u0633\u062D\u0628 \u0627\u0644\u0631\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u0645\u0635\u062D\u0648\u0628\u0629\u064B \u0628\u062C\u0628\u0647\u0629 \u062F\u0627\u0641\u0626\u0629 \u062D\u062A\u0649 \u064A\u062A\u0628\u0639\u0647\u0627 \u0647\u0637\u0648\u0644 \u0623\u0645\u0637\u0627\u0631 \u0623\u0648 \u062B\u0644\u0648\u062C \u0645\u0633\u062A\u0645\u0631\u0629 \u0641\u064A \u063A\u0636\u0648\u0646 \u0627\u0644\u0633\u0627\u0639\u0627\u062A \u0627\u0644 12 \u0625\u0644\u0649 24 \u0627\u0644\u0642\u0627\u062F\u0645\u0629. \u0648\u0645\u0639 \u0623\u0646 \u0627\u0644\u0631\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u062A\u062A\u0646\u0628\u0623 \u0628\u0648\u0635\u0648\u0644 \u062C\u0648 \u0623\u0643\u062B\u0631 \u062F\u0641\u0626\u064B\u0627 \u0648\u0631\u0637\u0648\u0628\u0629 \u0625\u0644\u0627 \u0623\u0646\u0647\u0627 \u0646\u0641\u0633\u0647\u0627 \u0644\u0627 \u062A\u0646\u062A\u062C \u0647\u0637\u0648\u0644\u064B\u0627 \u0643\u0628\u064A\u0631\u064B\u0627. \u0642\u062F \u062A\u0643\u0648\u0646 \u0627\u0644\u0639\u0648\u0627\u0635\u0641 \u0627\u0644\u0631\u0639\u062F\u064A\u0629 \u0645\u0635\u062D\u0648\u0628\u0629 \u0628\u0627\u0644\u0631\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u0641\u062A\u062C\u0644\u0628 \u0639\u0646\u062F \u0630\u0644\u0643 \u0632\u062E\u0627\u062A \u0645\u0646 \u0627\u0644\u0645\u0637\u0631 \u0641\u0642\u0637."@ar . . . . "\u0412\u044B\u0441\u043E\u043A\u043E\u0441\u043B\u043E\u0438\u0441\u0442\u044B\u0435 \u043E\u0431\u043B\u0430\u043A\u0430"@ru . "Altostratus cloud"@en . . . . . . . . . "Altastratas"@ga . "Altostratus"@sv . . . "\u03A4\u03B1 \u03A5\u03C8\u03B9\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 (Altostratus) \u03B1\u03C0\u03BF\u03C4\u03B5\u03BB\u03BF\u03CD\u03BD \u03B5\u03C0\u03AF\u03C3\u03B7\u03BC\u03B7 \u03BA\u03B1\u03C4\u03B7\u03B3\u03BF\u03C1\u03AF\u03B1 \u03BD\u03B5\u03C6\u03CE\u03BD, \u03C3\u03CD\u03BC\u03C6\u03C9\u03BD\u03B1 \u03BC\u03B5 \u03C4\u03BF\u03BD \u03C0\u03BF\u03C5 \u03B5\u03BE\u03AD\u03B4\u03C9\u03C3\u03B5 \u03C4\u03BF 1957 \u03BF W.M.O. \u03B7 \u03C7\u03C1\u03AE\u03C3\u03B7 \u03C4\u03C9\u03BD \u03BF\u03C0\u03BF\u03AF\u03C9\u03BD \u03B3\u03AF\u03BD\u03B5\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03BF\u03C5\u03C2 \u03BC\u03B5\u03C4\u03B5\u03C9\u03C1\u03BF\u03BB\u03CC\u03B3\u03BF\u03C5\u03C2 \u03BA\u03B1\u03B9 \u03B1\u03C0\u0384 \u03CC\u03BB\u03B1 \u03C4\u03B1 \u0393\u03C1\u03B1\u03C6\u03B5\u03AF\u03B1 \u039A\u03B1\u03B9\u03C1\u03BF\u03CD \u03C4\u03BF\u03C5 \u039A\u03CC\u03C3\u03BC\u03BF\u03C5. \u03A5\u03C8\u03B9\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 \u03BF\u03BD\u03BF\u03BC\u03AC\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C4\u03B1 \u03BD\u03AD\u03C6\u03B7 \u03C0\u03BF\u03C5 \u03C0\u03B1\u03C1\u03BF\u03C5\u03C3\u03B9\u03AC\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C3\u03B1\u03BD \u03C0\u03C5\u03BA\u03BD\u03AC \u03C0\u03AD\u03C0\u03BB\u03B1 \u03BC\u03B5 \u03C7\u03C1\u03CE\u03BC\u03B1 \u03B1\u03BD\u03BF\u03B9\u03BA\u03C4\u03CC \u03B3\u03BA\u03C1\u03AF\u03B6\u03BF \u03C0\u03C1\u03BF\u03C2 \u03C4\u03BF \u03B3\u03B1\u03BB\u03AC\u03B6\u03B9\u03BF \u03BF\u03BC\u03BF\u03B9\u03CC\u03BC\u03BF\u03C1\u03C6\u03B1 \u03BA\u03B1\u03B9 \u03B1\u03C0\u03BF\u03C4\u03B5\u03BB\u03BF\u03CD\u03BD\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C5\u03B4\u03C1\u03BF\u03C3\u03C4\u03B1\u03B3\u03BF\u03BD\u03AF\u03B4\u03B9\u03B1. \u0395\u03BC\u03C6\u03B1\u03BD\u03AF\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03BC\u03B5\u03B3\u03AC\u03BB\u03B7 \u03BF\u03C1\u03B9\u03B6\u03CC\u03BD\u03C4\u03B9\u03B1 \u03AD\u03BA\u03C4\u03B1\u03C3\u03B7 \u03BC\u03AE\u03BA\u03BF\u03C5\u03C2 \u03BC\u03B5\u03C1\u03B9\u03BA\u03CE\u03BD \u03B4\u03B5\u03BA\u03AC\u03B4\u03C9\u03BD \u03AE \u03BA\u03B1\u03B9 \u03B5\u03BA\u03B1\u03C4\u03BF\u03BD\u03C4\u03AC\u03B4\u03C9\u03BD \u03C7\u03B9\u03BB\u03B9\u03BF\u03BC\u03AD\u03C4\u03C1\u03C9\u03BD. \u0392\u03C1\u03AF\u03C3\u03BA\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C3\u03B5 \u03CD\u03C8\u03BF\u03C2 2.000-6.000 \u03BC\u03AD\u03C4\u03C1\u03B1. \u0391\u03C0\u03CC \u03C4\u03B1 \u03BB\u03B5\u03C0\u03C4\u03CC\u03C4\u03B5\u03C1\u03B1 \u03C5\u03C8\u03B9\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 \u03BC\u03CC\u03BB\u03B9\u03C2 \u03C0\u03BF\u03C5 \u03B4\u03B9\u03B1\u03BA\u03C1\u03AF\u03BD\u03BF\u03BD\u03C4\u03B1\u03B9 \u03BF\u03B9 \u03C6\u03C9\u03C4\u03B5\u03B9\u03BD\u03BF\u03AF \u03B4\u03AF\u03C3\u03BA\u03BF\u03B9 \u03C4\u03BF\u03C5 \u0389\u03BB\u03B9\u03BF\u03C5 \u03AE \u03C4\u03B7\u03C2 \u03A3\u03B5\u03BB\u03AE\u03BD\u03B7\u03C2. \u0393\u03B9\u0384 \u03B1\u03C5\u03C4\u03CC \u03BA\u03B1\u03B9 \u03B4\u03B5\u03BD \u03C3\u03C7\u03B7\u03BC\u03B1\u03C4\u03AF\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C3\u03BA\u03B9\u03AD\u03C2 \u03C3\u03C4\u03B7\u03BD \u03B5\u03C0\u03B9\u03C6\u03AC\u03BD\u03B5\u03B9\u03AC \u03C4\u03BF\u03C5\u03C2. \u0395\u03C0\u03AF\u03C3\u03B7\u03C2 \u03B4\u03B5\u03BD \u03B5\u03BC\u03C6\u03B1\u03BD\u03AF\u03B6\u03BF\u03C5\u03BD \u03AC\u03BB\u03C9. \u03A4\u03B1 \u03C5\u03C8\u03B9\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 \u03B5\u03BC\u03C6\u03B1\u03BD\u03AF\u03B6\u03BF\u03C5\u03BD \u03BC\u03B5\u03B3\u03B1\u03BB\u03CD\u03C4\u03B5\u03C1\u03B7 \u03AD\u03BA\u03C4\u03B1\u03C3\u03B7 \u03B1\u03C0\u03CC \u03C4\u03B1 \u03B8\u03C5\u03C3\u03B1\u03BD\u03BF\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1. \u0395\u03C0\u03AF\u03C3\u03B7\u03C2 \u03B4\u03B9\u03B1\u03C6\u03AD\u03C1\u03BF\u03C5\u03BD \u03B1\u03C0\u03CC \u03C4\u03BF\u03C5\u03C2 \u03C5\u03C8\u03B9\u03C3\u03C9\u03C1\u03B5\u03AF\u03C4\u03B5\u03C2 \u03BA\u03B1\u03B9 \u03C4\u03BF\u03C5\u03C2 \u03C3\u03C4\u03C1\u03C9\u03BC\u03B1\u03C4\u03BF\u03C3\u03C9\u03C1\u03B5\u03AF\u03C4\u03B5\u03C2 "@el . . . . "Altostratus"@fr . . . . . . "Altostrato"@it . . "L'altoestrat o altoestratus \u00E9s un tipus de n\u00FAvol mitj\u00E0 que forma un vel for\u00E7a homogeni, fibr\u00F3s o estriat de color m\u00E9s o menys gris o blavenc i que es caracteritza per la uniformitat de la seva superf\u00EDcie inferior. Sovint presenten zones relativament clares enmig d'altres de molt fosques, per\u00F2 mai no es nota un veritable relleu a la seva superf\u00EDcie. \u00C9s un tipus de n\u00FAvol molt relacionat amb d'altres. D'una banda, pot ser l'evoluci\u00F3 d'un cirroestrat o d'un altoc\u00FAmul, i, de l'altra, pot esdevenir nimboestrat si es va espessint i la precipitaci\u00F3 augmenta, i altoc\u00FAmul si es va esquin\u00E7ant. Aquests n\u00FAvols produeixen de vegades precipitacions febles i cont\u00EDnues, en forma de pluja i nevades que poden ser for\u00E7a persistents. Sovint les precipitacions no arriben a terra i es veuen cortines fosques penjant dels n\u00FAvols, anomenades virga. Estan formats per cristalls de gla\u00E7 i gotes d'aigua l\u00EDquida."@ca . . . . . . . "Altostratus (v. lat. altum \u201EH\u00F6he\u201C und stratus bzw. sternere \u201Eausdehnen, ausbreiten, mit einer Schicht bedecken\u201C; Abk.: As) ist eine bl\u00E4uliche bis graue mittelhohe Schichtwolke ohne Konturen, die aus (unterk\u00FChlten) Wassertr\u00F6pfchen und Eiskristallen besteht. Er ist relativ deutlich grau, die Sonne ist hinter den dunklen Wolken manchmal fast nicht sichtbar. Wenn der Altostratus nach Cirrostratus (Schleierwolken) gro\u00DFfl\u00E4chig aufzieht, ist meist eine Warmfront oder Okklusion im Anzug. Anzahl Stunden, bis es zu regnen beginnt: Altostratus hat keine speziellen Arten, weist jedoch die Unterarten translucidus, opacus, duplicatus, undulatus und radiatus auf. F\u00FCr Sonderformen, Begleit- und Mutterwolken siehe den Artikel Wolke."@de . . "Altostratuak (altostratus) erdi-mailako hodei estratiformeak dira. 2.000 eta 5.000 metro arteko garaieran eratzen dira eta 500-3000 metroko lodiera izaten dute. Gris koloreko geruza zabal uniformeak dira, apur bat ildoxkatuak, muga lausoak dituztenak. Eguzkiaren argia beira esmerilatuan zehar bezala iragaten da, lurrean itzalik sortu gabe."@eu . . . "Los altoestratos o altostratus son un tipo de nube de una clase caracterizada por una gran l\u00E1mina generalmente gris\u00E1cea uniforme, m\u00E1s claras en color que los nimbostratus y m\u00E1s oscuras que los cirroestratos. El t\u00E9rmino en lat\u00EDn altostratus puede traducirse como \u2018los m\u00E1s altos estratos\u2019. Los altoestratos son causados por grandes masas de aire, que ascienden y luego condensan, usualmente por un frente entrante, que suele generar m\u00E1s o menos precipitaciones. Los altoestratos son potencialmente peligrosos en la aeronavegaci\u00F3n, debido a que estas forman cristales de hielo sobre las aeronaves."@es . . . . . "Altostratuso (latine altostr\u0101tus, mallongigo: As) estas genro de nuboj tavolformaj, kiuj trovi\u011Das inter 2 kaj 7 kilometroj super marnivelo."@eo . "Altostratuak (altostratus) erdi-mailako hodei estratiformeak dira. 2.000 eta 5.000 metro arteko garaieran eratzen dira eta 500-3000 metroko lodiera izaten dute. Gris koloreko geruza zabal uniformeak dira, apur bat ildoxkatuak, muga lausoak dituztenak. Eguzkiaren argia beira esmerilatuan zehar bezala iragaten da, lurrean itzalik sortu gabe."@eu . . . "Scamaill de shaghas an stratais nach mb\u00EDonn chomh tiubh le stratas, ag aird\u00ED timpeall 2,000-7,000 m. Scothliath, i bhfoirm leath\u00E1n. Is tuar iad go bhfuil aimsir the bh\u00E1isti\u00FAil, a bhaineann le fronta te, le teacht."@ga . . . . . "Altostratus"@cs . . . . . . "\u9AD8\u5C64\u96F2\uFF08\u3053\u3046\u305D\u3046\u3046\u3093\uFF09\u306F\u96F2\u306E\u4E00\u7A2E\u3002\u7070\u8272\u306E\u30D9\u30FC\u30EB\u72B6\u3042\u308B\u3044\u306F\u5C64\u72B6\u306E\u96F2\u3067\u3001\u7A7A\u306E\u5E83\u7BC4\u56F2\u3092\u8986\u3046\u3053\u3068\u304C\u591A\u3044\u3002\u6727\uFF08\u304A\u307C\u308D\uFF09\u96F2\u3068\u3082\u3044\u3046\u3002"@ja . "\u03A4\u03B1 \u03A5\u03C8\u03B9\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 (Altostratus) \u03B1\u03C0\u03BF\u03C4\u03B5\u03BB\u03BF\u03CD\u03BD \u03B5\u03C0\u03AF\u03C3\u03B7\u03BC\u03B7 \u03BA\u03B1\u03C4\u03B7\u03B3\u03BF\u03C1\u03AF\u03B1 \u03BD\u03B5\u03C6\u03CE\u03BD, \u03C3\u03CD\u03BC\u03C6\u03C9\u03BD\u03B1 \u03BC\u03B5 \u03C4\u03BF\u03BD \u03C0\u03BF\u03C5 \u03B5\u03BE\u03AD\u03B4\u03C9\u03C3\u03B5 \u03C4\u03BF 1957 \u03BF W.M.O. \u03B7 \u03C7\u03C1\u03AE\u03C3\u03B7 \u03C4\u03C9\u03BD \u03BF\u03C0\u03BF\u03AF\u03C9\u03BD \u03B3\u03AF\u03BD\u03B5\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03BF\u03C5\u03C2 \u03BC\u03B5\u03C4\u03B5\u03C9\u03C1\u03BF\u03BB\u03CC\u03B3\u03BF\u03C5\u03C2 \u03BA\u03B1\u03B9 \u03B1\u03C0\u0384 \u03CC\u03BB\u03B1 \u03C4\u03B1 \u0393\u03C1\u03B1\u03C6\u03B5\u03AF\u03B1 \u039A\u03B1\u03B9\u03C1\u03BF\u03CD \u03C4\u03BF\u03C5 \u039A\u03CC\u03C3\u03BC\u03BF\u03C5. \u03A5\u03C8\u03B9\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 \u03BF\u03BD\u03BF\u03BC\u03AC\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C4\u03B1 \u03BD\u03AD\u03C6\u03B7 \u03C0\u03BF\u03C5 \u03C0\u03B1\u03C1\u03BF\u03C5\u03C3\u03B9\u03AC\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C3\u03B1\u03BD \u03C0\u03C5\u03BA\u03BD\u03AC \u03C0\u03AD\u03C0\u03BB\u03B1 \u03BC\u03B5 \u03C7\u03C1\u03CE\u03BC\u03B1 \u03B1\u03BD\u03BF\u03B9\u03BA\u03C4\u03CC \u03B3\u03BA\u03C1\u03AF\u03B6\u03BF \u03C0\u03C1\u03BF\u03C2 \u03C4\u03BF \u03B3\u03B1\u03BB\u03AC\u03B6\u03B9\u03BF \u03BF\u03BC\u03BF\u03B9\u03CC\u03BC\u03BF\u03C1\u03C6\u03B1 \u03BA\u03B1\u03B9 \u03B1\u03C0\u03BF\u03C4\u03B5\u03BB\u03BF\u03CD\u03BD\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C5\u03B4\u03C1\u03BF\u03C3\u03C4\u03B1\u03B3\u03BF\u03BD\u03AF\u03B4\u03B9\u03B1. \u0395\u03BC\u03C6\u03B1\u03BD\u03AF\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03BC\u03B5\u03B3\u03AC\u03BB\u03B7 \u03BF\u03C1\u03B9\u03B6\u03CC\u03BD\u03C4\u03B9\u03B1 \u03AD\u03BA\u03C4\u03B1\u03C3\u03B7 \u03BC\u03AE\u03BA\u03BF\u03C5\u03C2 \u03BC\u03B5\u03C1\u03B9\u03BA\u03CE\u03BD \u03B4\u03B5\u03BA\u03AC\u03B4\u03C9\u03BD \u03AE \u03BA\u03B1\u03B9 \u03B5\u03BA\u03B1\u03C4\u03BF\u03BD\u03C4\u03AC\u03B4\u03C9\u03BD \u03C7\u03B9\u03BB\u03B9\u03BF\u03BC\u03AD\u03C4\u03C1\u03C9\u03BD. \u0392\u03C1\u03AF\u03C3\u03BA\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C3\u03B5 \u03CD\u03C8\u03BF\u03C2 2.000-6.000 \u03BC\u03AD\u03C4\u03C1\u03B1. \u0391\u03C0\u03CC \u03C4\u03B1 \u03BB\u03B5\u03C0\u03C4\u03CC\u03C4\u03B5\u03C1\u03B1 \u03C5\u03C8\u03B9\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 \u03BC\u03CC\u03BB\u03B9\u03C2 \u03C0\u03BF\u03C5 \u03B4\u03B9\u03B1\u03BA\u03C1\u03AF\u03BD\u03BF\u03BD\u03C4\u03B1\u03B9 \u03BF\u03B9 \u03C6\u03C9\u03C4\u03B5\u03B9\u03BD\u03BF\u03AF \u03B4\u03AF\u03C3\u03BA\u03BF\u03B9 \u03C4\u03BF\u03C5 \u0389\u03BB\u03B9\u03BF\u03C5 \u03AE \u03C4\u03B7\u03C2 \u03A3\u03B5\u03BB\u03AE\u03BD\u03B7\u03C2. \u0393\u03B9\u0384 \u03B1\u03C5\u03C4\u03CC \u03BA\u03B1\u03B9 \u03B4\u03B5\u03BD \u03C3\u03C7\u03B7\u03BC\u03B1\u03C4\u03AF\u03B6\u03BF\u03BD\u03C4\u03B1\u03B9 \u03C3\u03BA\u03B9\u03AD\u03C2 \u03C3\u03C4\u03B7\u03BD \u03B5\u03C0\u03B9\u03C6\u03AC\u03BD\u03B5\u03B9\u03AC \u03C4\u03BF\u03C5\u03C2. \u0395\u03C0\u03AF\u03C3\u03B7\u03C2 \u03B4\u03B5\u03BD \u03B5\u03BC\u03C6\u03B1\u03BD\u03AF\u03B6\u03BF\u03C5\u03BD \u03AC\u03BB\u03C9. \u03A4\u03B1 \u03C5\u03C8\u03B9\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 \u03B5\u03BC\u03C6\u03B1\u03BD\u03AF\u03B6\u03BF\u03C5\u03BD \u03BC\u03B5\u03B3\u03B1\u03BB\u03CD\u03C4\u03B5\u03C1\u03B7 \u03AD\u03BA\u03C4\u03B1\u03C3\u03B7 \u03B1\u03C0\u03CC \u03C4\u03B1 \u03B8\u03C5\u03C3\u03B1\u03BD\u03BF\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1. \u0395\u03C0\u03AF\u03C3\u03B7\u03C2 \u03B4\u03B9\u03B1\u03C6\u03AD\u03C1\u03BF\u03C5\u03BD \u03B1\u03C0\u03CC \u03C4\u03BF\u03C5\u03C2 \u03C5\u03C8\u03B9\u03C3\u03C9\u03C1\u03B5\u03AF\u03C4\u03B5\u03C2 \u03BA\u03B1\u03B9 \u03C4\u03BF\u03C5\u03C2 \u03C3\u03C4\u03C1\u03C9\u03BC\u03B1\u03C4\u03BF\u03C3\u03C9\u03C1\u03B5\u03AF\u03C4\u03B5\u03C2 \u03B5\u03C0\u03B5\u03B9\u03B4\u03AE \u03B4\u03B5\u03BD \u03B5\u03BC\u03C6\u03B1\u03BD\u03AF\u03B6\u03BF\u03C5\u03BD \u03C3\u03C7\u03AE\u03BC\u03B1\u03C4\u03B1. \u0391\u03BD \u03C4\u03B1 \u03C5\u03C8\u03B9\u03C3\u03C4\u03C1\u03CE\u03BC\u03B1\u03C4\u03B1 \u03B1\u03C5\u03BE\u03AC\u03BD\u03BF\u03C5\u03BD \u03C0\u03B9\u03B8\u03B1\u03BD\u03CE\u03C2 \u03B1\u03C5\u03C4\u03CC \u03BD\u03B1 \u03C6\u03B1\u03BD\u03B5\u03C1\u03CE\u03BD\u03B5\u03B9 \u03B5\u03C0\u03B9\u03BA\u03B5\u03AF\u03BC\u03B5\u03BD\u03B7 \u03B2\u03C1\u03BF\u03C7\u03AE \u03B4\u03B9\u03AC\u03C1\u03BA\u03B5\u03B9\u03B1\u03C2. \u0397 \u03B4\u03B9\u03B5\u03B8\u03BD\u03AE\u03C2 \u03C3\u03CD\u03BD\u03C4\u03BC\u03B9\u03C3\u03AE \u03C4\u03BF\u03C5\u03C2 \u03B5\u03AF\u03BD\u03B1\u03B9 As."@el . . . "Altostratuso"@eo . . . . "Altostratuso (latine altostr\u0101tus, mallongigo: As) estas genro de nuboj tavolformaj, kiuj trovi\u011Das inter 2 kaj 7 kilometroj super marnivelo."@eo . "Los altoestratos o altostratus son un tipo de nube de una clase caracterizada por una gran l\u00E1mina generalmente gris\u00E1cea uniforme, m\u00E1s claras en color que los nimbostratus y m\u00E1s oscuras que los cirroestratos. El t\u00E9rmino en lat\u00EDn altostratus puede traducirse como \u2018los m\u00E1s altos estratos\u2019. Los altoestratos son causados por grandes masas de aire, que ascienden y luego condensan, usualmente por un frente entrante, que suele generar m\u00E1s o menos precipitaciones. Los altoestratos son potencialmente peligrosos en la aeronavegaci\u00F3n, debido a que estas forman cristales de hielo sobre las aeronaves."@es . . "\u03A5\u03C8\u03AF\u03C3\u03C4\u03C1\u03C9\u03BC\u03B1"@el . . . "Altostratus"@es . . . . "Altostratus [\u0142ac.] (As \u2013 chmura \u015Brednia warstwowa) \u2013 chmura w postaci grubej i g\u0119stej, niebieskiej albo szarej warstwy, przez kt\u00F3r\u0105 s\u0142o\u0144ce lub ksi\u0119\u017Cyc prze\u015Bwiecaj\u0105 jak przez matowe szk\u0142o. Sk\u0142ada si\u0119 z kropel wody oraz kryszta\u0142k\u00F3w lodu. Cz\u0119sto pokrywa ca\u0142e niebo, a czasem towarzyszy jej opad drobnego deszczu lub \u015Bniegu. Wyst\u0119puje na wysoko\u015Bci od 2 do 5 km. Symbol, kt\u00F3rym oznacza si\u0119 chmury typu altostratus:"@pl . "Altostratus [\u0142ac.] (As \u2013 chmura \u015Brednia warstwowa) \u2013 chmura w postaci grubej i g\u0119stej, niebieskiej albo szarej warstwy, przez kt\u00F3r\u0105 s\u0142o\u0144ce lub ksi\u0119\u017Cyc prze\u015Bwiecaj\u0105 jak przez matowe szk\u0142o. Sk\u0142ada si\u0119 z kropel wody oraz kryszta\u0142k\u00F3w lodu. Cz\u0119sto pokrywa ca\u0142e niebo, a czasem towarzyszy jej opad drobnego deszczu lub \u015Bniegu. Wyst\u0119puje na wysoko\u015Bci od 2 do 5 km. Symbol, kt\u00F3rym oznacza si\u0119 chmury typu altostratus:"@pl . . "De altostratus is een egaal grijsachtig wolkengeslacht. Die bewolking ontstaat op de grens tussen koude en warmere lucht, waarbij de warme lucht over de zwaardere koude lucht schuift. Duitse meteorologen noemen dat proces \"Eintr\u00FCbung\". Eerst is de omtrek van de zon of de maan er nog doorheen te zien (translucidus), maar meestal wordt de bewolking snel dichter, verdwijnt de zon en zet de neerslag in (opacus). Soms komt deze bewolking in verschillende lagen voor (duplicatus). Deze wolk kan overgaan in de nimbostratus. De altostratuswolken zijn een geslacht uit de familie van middelhoge wolken, maar kennen geen onderverdeling in wolkensoorten. Wel zijn er 5 ondersoortenvariaties op de altostratus. De ondersoortenvariaties zijn: \n* Translucidus \n* Opacus \n* Duplicatus \n* Undulatus \n* Radiatus In weerberichten is de afkorting As en het symbool op weerkaarten is:"@nl . "Altostratus is a middle-altitude cloud genus made up of water droplets, ice crystals, or a mixture of the two. Altostratus clouds are formed when large masses of warm, moist air rise, causing water vapor to condense. Altostratus clouds are usually gray or blueish featureless sheets, although some variants have wavy or banded bases. The sun can be seen through thinner altostratus clouds, but thicker layers can be quite opaque. Because altostratus clouds can contain ice crystals, they can produce some optical phenomena like iridescence and coronas."@en . "Altostratus (As) \u010Di vyv\u00FD\u0161en\u00E1 sloha je front\u00E1ln\u00ED oblak, jeho\u017E horizont\u00E1ln\u00ED rozm\u011Bry jsou stovky a\u017E tis\u00EDce kilometr\u016F a vertik\u00E1ln\u00ED rozm\u011Bry v \u0159\u00E1dech stovek metr\u016F. Je slo\u017Een\u00FD z vodn\u00EDch kapek a ledov\u00FDch krystalk\u016F. Z oblaku mohou vypad\u00E1vat sr\u00E1\u017Eky, hlavn\u011B v chladn\u00E9 \u010D\u00E1sti roku. P\u0159i pr\u016Fletu skrze oblak As p\u0159i teplot\u011B vzduchu mezi 0 a\u017E -12 \u00B0C se na povrchu letounu utv\u00E1\u0159\u00ED zpravidla m\u00EDrn\u00E1 a\u017E siln\u00E1 n\u00E1mraza. Tento oblak je definov\u00E1n jako \u0161edav\u00E1 \u010Di namodral\u00E1 obla\u010Dn\u00E1 plocha nebo vrstva se strukturou vl\u00E1knitou nebo \u017Eebrovitou, p\u0159\u00EDpadn\u011B bez patrn\u00E9 struktury, pokr\u00FDvaj\u00EDc\u00ED \u00FApln\u011B nebo \u010D\u00E1ste\u010Dn\u011B oblohu. Je tak tenk\u00E1, \u017Ee m\u00EDsty jsou alespo\u0148 \u010D\u00E1ste\u010Dn\u011B patrn\u00E9 obrysy slunce, kter\u00E9 se jev\u00ED jako za matn\u00FDm sklem. S altostratem nejsou spojeny halov\u00E9 jevy. As je tmav\u0161\u00ED ne\u017E Cs, ale sv\u011Btlej\u0161\u00ED ne\u017E Ns. Jedn\u00E1 se o oblak st\u0159edn\u00EDho patra, tzn. obvykle se nach\u00E1z\u00ED ve v\u00FD\u0161k\u00E1ch 2-6 km. M\u016F\u017Ee postupn\u011B mohutn\u011Bt a m\u011Bnit se v druh nimbostratus. Skrze mohutn\u011Bj\u0161\u00ED altostratus nen\u00ED viditeln\u00FD kotou\u010D slunce nebo m\u011Bs\u00EDce; pr\u016Fsvitn\u00FD As s rozeznateln\u00FDm sluncem nebo m\u011Bs\u00EDcem je translucidus, hust\u00FD As bez t\u011Bchto viditeln\u00FDch t\u011Bles naz\u00FDv\u00E1me opacus. Vzhledov\u011B je As tak\u0159ka v\u017Edy nebulosus, p\u0159\u00EDpadn\u011B m\u00E1 jen velmi nev\u00FDraznou strukturu. Oblak altostratus vznik\u00E1 v\u00FDstupn\u00FDm pohybem rozm\u011Brn\u00E9, vlhk\u00E9 a stabiln\u00ED vzduchov\u00E9 hmoty, p\u0159i n\u011Bm\u017E se vzduch postupn\u011B ochlazuje, a\u017E dos\u00E1hne stavu nasycen\u00ED a kondenzuje vodn\u00ED p\u00E1ra. P\u0159itom m\u016F\u017Ee doch\u00E1zet ke vzniku sr\u00E1\u017Eek, kter\u00E9 se p\u0159i pozorov\u00E1n\u00ED z ur\u010Dit\u00E9 vzd\u00E1lenosti jev\u00ED n\u011Bkdy jen ve tvaru virga, jindy praecipitatio. Pr\u00E1v\u011B v p\u0159\u00EDpad\u011B v\u00FDskytu sr\u00E1\u017Eek, pokud nab\u00FDvaj\u00ED na trvanlivosti a intenzit\u011B, doch\u00E1z\u00ED k postupn\u00E9 transformaci As na Ns. Altostratus m\u00EDv\u00E1 v\u011Bt\u0161inou nez\u0159etelnou strukturu, vypad\u00E1 jako jednolit\u00E1 \u0161edav\u00E1 plocha. M\u016F\u017Ee v\u0161ak m\u00EDt zvln\u011Bn\u00FD tvar (undulatus), co\u017E je d\u016Fsledek st\u0159ihu v\u011Btru v hladin\u00E1ch v\u00FDskytu As. Jindy m\u016F\u017Ee b\u00FDt As pon\u011Bkud rozdroben\u00FD a nab\u00FDvat tvaru fibratus. Dokonce p\u0159es n\u011Bkter\u00E9 \u010D\u00E1sti oblaku m\u016F\u017Ee b\u00FDt i patrn\u00E1 obloha. Kdy\u017E je As takto tvarovan\u00FD a roztrhan\u00FD, znamen\u00E1 to zpravidla p\u0159ibli\u017Eov\u00E1n\u00ED sl\u00E1bnouc\u00ED tepl\u00E9 fronty, p\u0159\u00EDpadn\u011B v\u00FD\u0161kov\u00E9 tepl\u00E9 fronty v syst\u00E9mu okluze. Altostratus b\u00FDv\u00E1 sm\u00ED\u0161en\u00FD oblak; obsahuje ledov\u00E9 \u010D\u00E1stice i vodn\u00ED kapky, \u010Dasto p\u0159echlazen\u00E9. Ledov\u00E9 krystalky jsou t\u00EDm v\u011Bt\u0161\u00ED, v \u010D\u00EDm men\u0161\u00ED v\u00FD\u0161ce v oblaku se vyskytuj\u00ED, ale v nejspodn\u011Bj\u0161\u00ED \u010D\u00E1sti oblaku, bl\u00EDzko z\u00E1kladny, se op\u011Bt jejich velikost sni\u017Euje. Leteck\u00FD pr\u016Fzkum oblaku prok\u00E1zal v\u00FDskyt halov\u00FDch jev\u016F, viditeln\u00FDch z letadla p\u0159i letu bl\u00EDzko horn\u00EDho okraje oblaku. Tak se mohou projevovat jen \u0161estihrann\u00E9 ledov\u00E9 krystalky. Ov\u0161em v ni\u017E\u0161\u00EDch v\u00FD\u0161k\u00E1ch u\u017E tyto \u0161estibok\u00E9 krystaly chyb\u011Bly a byly nahrazeny slou\u010Den\u00FDmi \u00FAtvary bez pravideln\u00E9 struktury. Oblak As se vyskytuje nej\u010Dast\u011Bji na p\u0159ibli\u017Euj\u00EDc\u00ED se tepl\u00E9 \u010Di okluzn\u00ED front\u011B. \u010Casto roste jeho vertik\u00E1ln\u00ED mohutnost za v\u00FDskytu sr\u00E1\u017Eek, m\u016F\u017Ee se transformovat do oblaku Ns. V n\u011Bkter\u00FDch p\u0159\u00EDpadech ale m\u016F\u017Ee As prov\u00E1zet tak\u00E9 oblak cumulus congestus nebo cumulonimbus na studen\u00FDch front\u00E1ch. Vz\u00E1cn\u011B se tento oblak vyskytuje jako radiatus, undulatus nebo duplicatus. Rovn\u011B\u017E jsou vz\u00E1cn\u00E9 p\u0159\u00EDpady mamma, zejm\u00E9na kdy\u017E doch\u00E1z\u00ED k transformaci As na Ac. P\u0159i v\u00FDskytu sr\u00E1\u017Eek se pod oblakem n\u011Bkdy utv\u00E1\u0159\u00ED pr\u016Fvodn\u00ED pannus. As \u010Dasto vznik\u00E1 transformac\u00ED z Ac, tzn. je to altostratus altocumulogenitus, kdy doch\u00E1z\u00ED ke spojov\u00E1n\u00ED men\u0161\u00EDch \u010D\u00E1st\u00ED Ac do souvisl\u00E9 vrstvy. Pokud se postupn\u011B rozest\u00EDr\u00E1 st\u0159edn\u00ED \u010D\u00E1st bou\u0159kov\u00E9ho Cb do v\u00FDsledn\u00E9 rozs\u00E1hl\u00E9 vrstvy, m\u016F\u017Ee vzniknout altostratus cumulonimbogenitus. Mutac\u00ED vertik\u00E1ln\u011B s\u00EDl\u00EDc\u00EDho cirrostratu rovn\u011B\u017E m\u016F\u017Ee vzniknout As cirrostratomutatus \u2014 k tomu doch\u00E1z\u00ED, pokud se p\u0159ibli\u017Euje nap\u0159. tlakov\u00E1 n\u00ED\u017Ee nebo fronta. Opa\u010Dn\u00FDm procesem, kdy\u017E se tlakov\u00E1 n\u00ED\u017Ee vypl\u0148uje nebo postupuj\u00EDc\u00ED fronta sl\u00E1bne, m\u016F\u017Ee se zten\u010Dovat p\u016Fvodn\u00ED nimbostratus a p\u0159em\u011Bnit se na altostratus, kter\u00FD se pak naz\u00FDv\u00E1 altostratus nimbostratomutatus."@cs . . "Altostratus is a middle-altitude cloud genus made up of water droplets, ice crystals, or a mixture of the two. Altostratus clouds are formed when large masses of warm, moist air rise, causing water vapor to condense. Altostratus clouds are usually gray or blueish featureless sheets, although some variants have wavy or banded bases. The sun can be seen through thinner altostratus clouds, but thicker layers can be quite opaque. Altostratus clouds usually predict the arrival of warm fronts. Once altostratus clouds associated with a warm front arrive, continuous rain or snow will usually follow in the next 12 to 24 hours. Although altostratus clouds predict the arrival of warmer, wetter weather, they themselves do not produce significant precipitation. Thunderstorms can be embedded in altostratus clouds; however, bringing showers. Because altostratus clouds can contain ice crystals, they can produce some optical phenomena like iridescence and coronas."@en . "\u9AD8\u5C42\u4E91\uFF08\u62C9\u4E01\u8A9E\uFF1AAltostratus\uFF0C\u7B26\u53F7\uFF1AAs\uFF09\u662F\u4E2D\u4E91\u7684\u4E00\u7C7B\uFF0C\u65BC2000\u7C73\u4EE5\u4E0A\u9AD8\u7A7A\u5F62\u6210\uFF0C\u50CF\u4E00\u79CD\u5E26\u6709\u6761\u7EB9\u7684\u5E55\uFF0C\u989C\u8272\u591A\u4E3A\u7070\u767D\u8272\u6216\u7070\u8272\uFF0C\u6709\u65F6\u6709\u4E00\u70B9\u5FAE\u84DD\u8272\uFF0C\u6709\u65F6\u8F83\u4E3A\u5747\u5300\uFF0C\u4F46\u96F2\u5E95\u6CA1\u6709\u660E\u663E\u7684\u8D77\u4F0F\u3002\u9AD8\u5C42\u4E91\u7684\u660E\u6697\u7A0B\u5EA6\u6703\u56E0\u4E91\u7684\u539A\u5EA6\u5DEE\u7570\u800C\u4E0D\u540C\u3002 \u9AD8\u5C42\u4E91\u4E0B\u6709\u4E24\u4E2A\u4E91\u5C5E\uFF1A \n* \uFF1A\u96F2\u9AD4\u8F03\u8584\uFF0C\u539A\u5EA6\u5747\u52FB\uFF0C\u5448\u7070\u767D\u8272\uFF0C\u8F2A\u5ED3\u6A21\u7CCA\u3002\u900F\u5149\u9AD8\u5C42\u4E91\u53EF\u4EE5\u63A9\u84CB\u5929\u4E0A\u7684\u592A\u967D\u6216\u6708\u7403\u3002 \n* \uFF1A\u96F2\u9AD4\u8F03\u539A\uFF0C\u5448\u7070\u8272\uFF0C\u96F2\u5E95\u53EF\u898B\u660E\u76F8\u9593\u7684\u689D\u7D0B\u7D50\u69CB\uFF0C\u7121\u6CD5\u770B\u51FA\u5176\u8F2A\u5ED3\u3002\u853D\u5149\u9AD8\u5C42\u4E91\u53EF\u4EE5\u63A9\u84CB\u5929\u4E0A\u7684\u592A\u967D\u6216\u6708\u7403\u3002"@zh . "Alto-estratos ou, em latim, altostratus s\u00E3o camadas cinzentas ou azuladas, muitas vezes associadas a Altocumulus; compostas de got\u00EDculas de \u00E1gua e cristais de gelo; n\u00E3o formam halo, encobrem o sol; precipita\u00E7\u00E3o leve e cont\u00EDnua. Formam-se em massas de ar est\u00E1vel, quando a humidade \u00E9 moderada e a temperatura \u00E9 relativamente alta. Anunciam frequentemente a chegada de uma frente quente e podem ser acompanhadas de alguns chuviscos ou queda de neve."@pt . . . . . . "Altostratus (As) adalah awan yang berbentuk lembaran dan sering berbentuk satu struktur berserat. Awan altostratus dapat diikuti oleh keluarnya endapan dari dalam awan baik bentuk air, salju, atau kristal es, atau biasa disebut presipitasi, yang meluas dan dalam waktu yang cukup lama. Altostratus dapat membentuk korona, selain itu bulan atau matahari terlihat pucat jika dilihat melalui awan ini."@in . . . . "Altostratus"@pl . . . . "Scamaill de shaghas an stratais nach mb\u00EDonn chomh tiubh le stratas, ag aird\u00ED timpeall 2,000-7,000 m. Scothliath, i bhfoirm leath\u00E1n. Is tuar iad go bhfuil aimsir the bh\u00E1isti\u00FAil, a bhaineann le fronta te, le teacht."@ga . . . . . "\uACE0\uCE35\uC6B4(\u9AD8\u5C64\u96F2, \uC601\uC5B4: altostratus)\uC740 \uC911\uCE35\uC6B4\uC73C\uB85C \uB192\uCE35\uAD6C\uB984, \uD770\uC0C9\uCC28\uC77C\uAD6C\uB984\uC774\uB77C\uACE0\uB3C4 \uD55C\uB2E4. \uBCF4\uD1B5 \uC9C0\uD45C\uBA74\uC5D0\uC11C 2 ~ 7km\uC758 \uB192\uC774\uC5D0\uC11C \uB098\uD0C0\uB098\uBA70, \uB54C\uB85C\uB294 \uC0C1\uCE35\uC5D0\uC11C \uB098\uD0C0\uB098\uAE30\uB3C4 \uD55C\uB2E4. \uB450\uAED8\uB294 \uC218\uBC31 m\uC5D0\uC11C \uC218\uCC9C m\uC5D0 \uC774\uB974\uBA70, \uAD6C\uB984\uC758 \uC815\uC0C1\uC740 1km \uB192\uC774\uAE4C\uC9C0 \uC774\uB974\uAE30\uB3C4 \uD55C\uB2E4. \uB530\uB77C\uC11C \uB450\uAEBC\uC6B4 \uACE0\uCE35\uC6B4\uC758 \uC0C1\uCE35\uBD80\uB294 \uBE59\uC815, \uC911\uCE35\uBD80\uB294 \uBE59\uC815, \uB208\uC1A1\uC774, \uACFC\uB0C9\uAC01\uBB3C\uBC29\uC6B8\uC758 \uD63C\uD569\uBB3C, \uD558\uCE35\uBD80\uB294 \uB300\uBD80\uBD84 \uACFC\uB0C9\uAC01\uBB3C\uBC29\uC6B8\uC774\uB098 \uBB3C\uBC29\uC6B8\uB85C \uC774\uB8E8\uC5B4\uC838 \uC788\uB2E4. \uADF8\uB7EC\uB098 \uC587\uC740 \uAD6C\uB984\uC740 \uBB3C\uBC29\uC6B8\uB9CC\uC73C\uB85C \uC774\uB8E8\uC5B4\uC838 \uC788\uB294 \uACBD\uC6B0\uB3C4 \uC788\uB2E4. \uC5BC\uB8E9\uC774 \uC5C6\uB294 \uACE0\uB978 \uBAA8\uC591\uC744 \uB098\uD0C0\uB0BC \uB54C\uB3C4 \uC788\uACE0, \uC904\uAE30\uAC00 \uC788\uB294 \uC12C\uC720\uB098 \uD138 \uBAA8\uC591\uC758 \uC870\uC9C1\uC744 \uB098\uD0C0\uB0B4\uAE30\uB3C4 \uD55C\uB2E4. \uC774 \uAD6C\uB984\uC758 \uC5F7\uC740 \uBD80\uBD84\uC5D0\uC11C\uB294 \uBC18\uD22C\uBA85 \uC720\uB9AC\uB97C \uD1B5\uD574\uC11C \uBCF4\uB294 \uAC83\uACFC \uAC19\uC774 \uD574\uC640 \uB2EC\uC758 \uC704\uCE58\uAC00 \uC5B4\uB834\uD48B\uC774 \uB4DC\uB7EC\uB0A0 \uC815\uB3C4\uC774\uBA70 \uB450\uAEBC\uC6B4 \uAD8C\uCE35\uC6B4\uACFC \uBE44\uC2B7\uD55C \uBAA8\uC591 \uD615\uD0DC\uB97C \uB760\uACE0 \uC788\uC9C0\uB9CC \uD587\uBB34\uB9AC\uC640 \uB2EC\uBB34\uB9AC \uD604\uC0C1\uC740 \uB098\uD0C0\uB098\uC9C0 \uC54A\uB294\uB2E4. \uB450\uAEBC\uC6B4 \uACE0\uCE35\uC6B4\uC5D0\uC11C\uB294 \uC57D\uD55C \uBE44\uB098 \uB208\uC774 \uB0B4\uB9AC\uAE30\uB3C4 \uD55C\uB2E4. \uC774 \uBB38\uC11C\uC5D0\uB294 \uB2E4\uC74C\uCEE4\uBBA4\uB2C8\uCF00\uC774\uC158(\uD604 \uCE74\uCE74\uC624)\uC5D0\uC11C GFDL \uB610\uB294 CC-SA \uB77C\uC774\uC120\uC2A4\uB85C \uBC30\uD3EC\uD55C \uAE00\uB85C\uBC8C \uC138\uACC4\uB300\uBC31\uACFC\uC0AC\uC804\uC758 \uB0B4\uC6A9\uC744 \uAE30\uCD08\uB85C \uC791\uC131\uB41C \uAE00\uC774 \uD3EC\uD568\uB418\uC5B4 \uC788\uC2B5\uB2C8\uB2E4."@ko . . "L'altostratus est un genre de nuage de l'\u00E9tage moyen, situ\u00E9 \u00E0 une altitude comprise entre 2000 et 5 000 m, pour une \u00E9paisseur de 500 jusqu'\u00E0 3 000 m. C'est un nuage stratiforme, c'est-\u00E0-dire en couche, dont les limites sont difficilement d\u00E9finissables. Il forme une vaste couche grise l\u00E9g\u00E8rement stri\u00E9e, qui laisse diffuser la lumi\u00E8re solaire sans ombre apparente au sol, comme au travers d'un verre d\u00E9poli. Lorsqu'il est \u00E9pais, il entraine parfois des chutes de pluie ou de neige."@fr . . "1121248259"^^ . . . . "\u9AD8\u5C42\u4E91"@zh . . . . "\u0412\u0438\u0441\u043E\u043A\u043E-\u0448\u0430\u0440\u0443\u0432\u0430\u0442\u0456 \u0445\u043C\u0430\u0440\u0438 (Altostratus, As) \u2014 \u0445\u043C\u0430\u0440\u0438 \u0441\u0435\u0440\u0435\u0434\u043D\u044C\u043E\u0433\u043E \u044F\u0440\u0443\u0441\u0443, \u0449\u043E \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C\u0441\u044F \u043D\u0430 \u0432\u0438\u0441\u043E\u0442\u0456 2-6 \u043A\u043C \u0443 \u0432\u0438\u0433\u043B\u044F\u0434\u0456 \u0437\u0430\u0432\u0456\u0441\u0438 \u044F\u0441\u043D\u043E-\u0441\u0456\u0440\u043E\u0433\u043E \u0430\u0431\u043E \u0441\u0438\u043D\u044E\u0432\u0430\u0442\u043E\u0433\u043E \u043A\u043E\u043B\u044C\u043E\u0440\u0443, \u0443 \u044F\u043A\u0456\u0439 \u043C\u043E\u0436\u043D\u0430 \u0440\u043E\u0437\u0440\u0456\u0437\u043D\u0438\u0442\u0438 \u0441\u043C\u0443\u0433\u0438 \u0430\u0431\u043E \u0432\u043E\u043B\u043E\u043A\u043D\u0430. \u0421\u043E\u043D\u0446\u0435 \u0456 \u041C\u0456\u0441\u044F\u0446\u044C \u0432\u0438\u0434\u043D\u0456 \u043A\u0440\u0456\u0437\u044C \u0446\u0456 \u0445\u043C\u0430\u0440\u0438 \u0434\u0443\u0436\u0435 \u0441\u043C\u0443\u0442\u043D\u043E, \u043F\u0440\u0438\u0431\u043B\u0438\u0437\u043D\u043E \u044F\u043A \u0432\u0438\u0434\u043D\u0430 \u0441\u043F\u0456\u0440\u0430\u043B\u044C \u0443 \u043C\u0430\u0442\u043E\u0432\u0456\u0439 \u043B\u0430\u043C\u043F\u043E\u0447\u0446\u0456. \u0412\u043E\u043D\u0438 \u043C\u0430\u0439\u0436\u0435 \u0437\u0430\u0432\u0436\u0434\u0438 \u043F\u0435\u0440\u0435\u043C\u0435\u0436\u043E\u0432\u0443\u044E\u0442\u044C \u043F\u0435\u0440\u0438\u0441\u0442\u043E-\u0448\u0430\u0440\u0443\u0432\u0430\u0442\u0456. \u041F\u043E\u0437\u043D\u0430\u0447\u0430\u044E\u0442\u044C\u0441\u044F \u0441\u0438\u043C\u0432\u043E\u043B\u043E\u043C ."@uk . . "L'Altostrato (in latino altostratus, abbreviazione As) \u00E8 una nube media, posta ad un'altitudine di circa 2000\u20136000 m d'altezza, di colore grigiastro, talvolta tendente all'azzurrognolo, mai bianco."@it . . "\uACE0\uCE35\uC6B4"@ko . . . . "L'Altostrato (in latino altostratus, abbreviazione As) \u00E8 una nube media, posta ad un'altitudine di circa 2000\u20136000 m d'altezza, di colore grigiastro, talvolta tendente all'azzurrognolo, mai bianco."@it . . "\u9AD8\u5C64\u96F2\uFF08\u3053\u3046\u305D\u3046\u3046\u3093\uFF09\u306F\u96F2\u306E\u4E00\u7A2E\u3002\u7070\u8272\u306E\u30D9\u30FC\u30EB\u72B6\u3042\u308B\u3044\u306F\u5C64\u72B6\u306E\u96F2\u3067\u3001\u7A7A\u306E\u5E83\u7BC4\u56F2\u3092\u8986\u3046\u3053\u3068\u304C\u591A\u3044\u3002\u6727\uFF08\u304A\u307C\u308D\uFF09\u96F2\u3068\u3082\u3044\u3046\u3002"@ja . "\u0412\u0438\u0441\u043E\u043A\u043E-\u0448\u0430\u0440\u0443\u0432\u0430\u0442\u0456 \u0445\u043C\u0430\u0440\u0438"@uk . . . . . "\u9AD8\u5C42\u4E91\uFF08\u62C9\u4E01\u8A9E\uFF1AAltostratus\uFF0C\u7B26\u53F7\uFF1AAs\uFF09\u662F\u4E2D\u4E91\u7684\u4E00\u7C7B\uFF0C\u65BC2000\u7C73\u4EE5\u4E0A\u9AD8\u7A7A\u5F62\u6210\uFF0C\u50CF\u4E00\u79CD\u5E26\u6709\u6761\u7EB9\u7684\u5E55\uFF0C\u989C\u8272\u591A\u4E3A\u7070\u767D\u8272\u6216\u7070\u8272\uFF0C\u6709\u65F6\u6709\u4E00\u70B9\u5FAE\u84DD\u8272\uFF0C\u6709\u65F6\u8F83\u4E3A\u5747\u5300\uFF0C\u4F46\u96F2\u5E95\u6CA1\u6709\u660E\u663E\u7684\u8D77\u4F0F\u3002\u9AD8\u5C42\u4E91\u7684\u660E\u6697\u7A0B\u5EA6\u6703\u56E0\u4E91\u7684\u539A\u5EA6\u5DEE\u7570\u800C\u4E0D\u540C\u3002 \u9AD8\u5C42\u4E91\u4E0B\u6709\u4E24\u4E2A\u4E91\u5C5E\uFF1A \n* \uFF1A\u96F2\u9AD4\u8F03\u8584\uFF0C\u539A\u5EA6\u5747\u52FB\uFF0C\u5448\u7070\u767D\u8272\uFF0C\u8F2A\u5ED3\u6A21\u7CCA\u3002\u900F\u5149\u9AD8\u5C42\u4E91\u53EF\u4EE5\u63A9\u84CB\u5929\u4E0A\u7684\u592A\u967D\u6216\u6708\u7403\u3002 \n* \uFF1A\u96F2\u9AD4\u8F03\u539A\uFF0C\u5448\u7070\u8272\uFF0C\u96F2\u5E95\u53EF\u898B\u660E\u76F8\u9593\u7684\u689D\u7D0B\u7D50\u69CB\uFF0C\u7121\u6CD5\u770B\u51FA\u5176\u8F2A\u5ED3\u3002\u853D\u5149\u9AD8\u5C42\u4E91\u53EF\u4EE5\u63A9\u84CB\u5929\u4E0A\u7684\u592A\u967D\u6216\u6708\u7403\u3002"@zh . . . . . "\u9AD8\u5C64\u96F2"@ja . . . . "Altostratus"@in . . "\uACE0\uCE35\uC6B4(\u9AD8\u5C64\u96F2, \uC601\uC5B4: altostratus)\uC740 \uC911\uCE35\uC6B4\uC73C\uB85C \uB192\uCE35\uAD6C\uB984, \uD770\uC0C9\uCC28\uC77C\uAD6C\uB984\uC774\uB77C\uACE0\uB3C4 \uD55C\uB2E4. \uBCF4\uD1B5 \uC9C0\uD45C\uBA74\uC5D0\uC11C 2 ~ 7km\uC758 \uB192\uC774\uC5D0\uC11C \uB098\uD0C0\uB098\uBA70, \uB54C\uB85C\uB294 \uC0C1\uCE35\uC5D0\uC11C \uB098\uD0C0\uB098\uAE30\uB3C4 \uD55C\uB2E4. \uB450\uAED8\uB294 \uC218\uBC31 m\uC5D0\uC11C \uC218\uCC9C m\uC5D0 \uC774\uB974\uBA70, \uAD6C\uB984\uC758 \uC815\uC0C1\uC740 1km \uB192\uC774\uAE4C\uC9C0 \uC774\uB974\uAE30\uB3C4 \uD55C\uB2E4. \uB530\uB77C\uC11C \uB450\uAEBC\uC6B4 \uACE0\uCE35\uC6B4\uC758 \uC0C1\uCE35\uBD80\uB294 \uBE59\uC815, \uC911\uCE35\uBD80\uB294 \uBE59\uC815, \uB208\uC1A1\uC774, \uACFC\uB0C9\uAC01\uBB3C\uBC29\uC6B8\uC758 \uD63C\uD569\uBB3C, \uD558\uCE35\uBD80\uB294 \uB300\uBD80\uBD84 \uACFC\uB0C9\uAC01\uBB3C\uBC29\uC6B8\uC774\uB098 \uBB3C\uBC29\uC6B8\uB85C \uC774\uB8E8\uC5B4\uC838 \uC788\uB2E4. \uADF8\uB7EC\uB098 \uC587\uC740 \uAD6C\uB984\uC740 \uBB3C\uBC29\uC6B8\uB9CC\uC73C\uB85C \uC774\uB8E8\uC5B4\uC838 \uC788\uB294 \uACBD\uC6B0\uB3C4 \uC788\uB2E4. \uC5BC\uB8E9\uC774 \uC5C6\uB294 \uACE0\uB978 \uBAA8\uC591\uC744 \uB098\uD0C0\uB0BC \uB54C\uB3C4 \uC788\uACE0, \uC904\uAE30\uAC00 \uC788\uB294 \uC12C\uC720\uB098 \uD138 \uBAA8\uC591\uC758 \uC870\uC9C1\uC744 \uB098\uD0C0\uB0B4\uAE30\uB3C4 \uD55C\uB2E4. \uC774 \uAD6C\uB984\uC758 \uC5F7\uC740 \uBD80\uBD84\uC5D0\uC11C\uB294 \uBC18\uD22C\uBA85 \uC720\uB9AC\uB97C \uD1B5\uD574\uC11C \uBCF4\uB294 \uAC83\uACFC \uAC19\uC774 \uD574\uC640 \uB2EC\uC758 \uC704\uCE58\uAC00 \uC5B4\uB834\uD48B\uC774 \uB4DC\uB7EC\uB0A0 \uC815\uB3C4\uC774\uBA70 \uB450\uAEBC\uC6B4 \uAD8C\uCE35\uC6B4\uACFC \uBE44\uC2B7\uD55C \uBAA8\uC591 \uD615\uD0DC\uB97C \uB760\uACE0 \uC788\uC9C0\uB9CC \uD587\uBB34\uB9AC\uC640 \uB2EC\uBB34\uB9AC \uD604\uC0C1\uC740 \uB098\uD0C0\uB098\uC9C0 \uC54A\uB294\uB2E4. \uB450\uAEBC\uC6B4 \uACE0\uCE35\uC6B4\uC5D0\uC11C\uB294 \uC57D\uD55C \uBE44\uB098 \uB208\uC774 \uB0B4\uB9AC\uAE30\uB3C4 \uD55C\uB2E4. \uC774 \uBB38\uC11C\uC5D0\uB294 \uB2E4\uC74C\uCEE4\uBBA4\uB2C8\uCF00\uC774\uC158(\uD604 \uCE74\uCE74\uC624)\uC5D0\uC11C GFDL \uB610\uB294 CC-SA \uB77C\uC774\uC120\uC2A4\uB85C \uBC30\uD3EC\uD55C \uAE00\uB85C\uBC8C \uC138\uACC4\uB300\uBC31\uACFC\uC0AC\uC804\uC758 \uB0B4\uC6A9\uC744 \uAE30\uCD08\uB85C \uC791\uC131\uB41C \uAE00\uC774 \uD3EC\uD568\uB418\uC5B4 \uC788\uC2B5\uB2C8\uB2E4."@ko . . . . . . . . "Altostratus eller skiktmoln, f\u00F6rkortning As, \u00E4r ett huvudmolnslag som tillh\u00F6r familjen medelh\u00F6ga moln och finns p\u00E5 2000 - 5000 meters h\u00F6jd. Molnen \u00E4r i j\u00E4mngr\u00E5a skikt eller lager. De uppkommer genom att stora luftmassor lyfts och kondenseras. Altostratus t\u00E4cker oftast stora omr\u00E5den. Molnen \u00E4r speciellt farliga f\u00F6r flygtrafiken d\u00E5 dessa \u00E4r orsak till nedisning. Till skillnad mot cirrostratus s\u00E5 ger altostratus ej upphov till halo."@sv . "\u0412\u0438\u0441\u043E\u043A\u043E-\u0448\u0430\u0440\u0443\u0432\u0430\u0442\u0456 \u0445\u043C\u0430\u0440\u0438 (Altostratus, As) \u2014 \u0445\u043C\u0430\u0440\u0438 \u0441\u0435\u0440\u0435\u0434\u043D\u044C\u043E\u0433\u043E \u044F\u0440\u0443\u0441\u0443, \u0449\u043E \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C\u0441\u044F \u043D\u0430 \u0432\u0438\u0441\u043E\u0442\u0456 2-6 \u043A\u043C \u0443 \u0432\u0438\u0433\u043B\u044F\u0434\u0456 \u0437\u0430\u0432\u0456\u0441\u0438 \u044F\u0441\u043D\u043E-\u0441\u0456\u0440\u043E\u0433\u043E \u0430\u0431\u043E \u0441\u0438\u043D\u044E\u0432\u0430\u0442\u043E\u0433\u043E \u043A\u043E\u043B\u044C\u043E\u0440\u0443, \u0443 \u044F\u043A\u0456\u0439 \u043C\u043E\u0436\u043D\u0430 \u0440\u043E\u0437\u0440\u0456\u0437\u043D\u0438\u0442\u0438 \u0441\u043C\u0443\u0433\u0438 \u0430\u0431\u043E \u0432\u043E\u043B\u043E\u043A\u043D\u0430. \u0421\u043E\u043D\u0446\u0435 \u0456 \u041C\u0456\u0441\u044F\u0446\u044C \u0432\u0438\u0434\u043D\u0456 \u043A\u0440\u0456\u0437\u044C \u0446\u0456 \u0445\u043C\u0430\u0440\u0438 \u0434\u0443\u0436\u0435 \u0441\u043C\u0443\u0442\u043D\u043E, \u043F\u0440\u0438\u0431\u043B\u0438\u0437\u043D\u043E \u044F\u043A \u0432\u0438\u0434\u043D\u0430 \u0441\u043F\u0456\u0440\u0430\u043B\u044C \u0443 \u043C\u0430\u0442\u043E\u0432\u0456\u0439 \u043B\u0430\u043C\u043F\u043E\u0447\u0446\u0456. \u0412\u043E\u043D\u0438 \u043C\u0430\u0439\u0436\u0435 \u0437\u0430\u0432\u0436\u0434\u0438 \u043F\u0435\u0440\u0435\u043C\u0435\u0436\u043E\u0432\u0443\u044E\u0442\u044C \u043F\u0435\u0440\u0438\u0441\u0442\u043E-\u0448\u0430\u0440\u0443\u0432\u0430\u0442\u0456. \u041F\u043E\u0437\u043D\u0430\u0447\u0430\u044E\u0442\u044C\u0441\u044F \u0441\u0438\u043C\u0432\u043E\u043B\u043E\u043C ."@uk . . "\u0627\u0644\u0631\u064E\u0651\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u0623\u0648 \u0627\u0644\u0632\u064E\u0651\u0639\u0652\u0628\u064E\u062C \u0623\u0648 \u0627\u0644\u0632\u0650\u0651\u0639\u0652\u0628\u0650\u062C \u0647\u0648 \u062C\u0646\u0633 \u0633\u062D\u0627\u0628\u0629 \u0645\u062A\u0648\u0633\u0637 \u0627\u0644\u0627\u0631\u062A\u0641\u0627\u0639 \u064A\u062A\u0643\u0648\u0646 \u0645\u0646 \u0642\u0637\u0631\u0627\u062A \u0627\u0644\u0645\u0627\u0621 \u0623\u0648 \u0628\u0644\u0648\u0631\u0627\u062A \u0627\u0644\u062C\u0644\u064A\u062F \u0623\u0648 \u0645\u0632\u064A\u062C \u0645\u0646 \u0627\u0644\u0627\u062B\u0646\u064A\u0646. \u062A\u062A\u0643\u0648\u0646 \u0639\u0646\u062F\u0645\u0627 \u062A\u0631\u062A\u0641\u0639 \u0643\u062A\u0644 \u0643\u0628\u064A\u0631\u0629 \u0645\u0646 \u0627\u0644\u0647\u0648\u0627\u0621 \u0627\u0644\u062F\u0627\u0641\u0626 \u0627\u0644\u0631\u0637\u0628 \u0645\u0627 \u064A\u0624\u062F\u064A \u0625\u0644\u0649 \u062A\u0643\u062B\u0641 \u0628\u062E\u0627\u0631 \u0627\u0644\u0645\u0627\u0621. \u0639\u0627\u062F\u0629 \u0645\u0627 \u064A\u064E\u0643\u0648\u0646 \u0627\u0644\u0631\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u0635\u0641\u0627\u0626\u062D \u0631\u0645\u0627\u062F\u064A\u0629 \u0623\u0648 \u0632\u0631\u0642\u0627\u0621 \u0628\u0644\u0627 \u0645\u0644\u0627\u0645\u062D \u0648\u0630\u0644\u0643 \u0645\u0639 \u0623\u0646 \u0644\u0628\u0639\u0636 \u0623\u0634\u0643\u0627\u0644\u0647 \u0642\u0648\u0627\u0639\u062F \u0645\u062A\u0645\u0648\u062C\u0629 \u0623\u0648 \u0645\u064F\u0639\u064E\u0635\u064E\u0651\u0628\u064E\u0629. \u064A\u0645\u0643\u0646 \u0631\u0624\u064A\u0629 \u0627\u0644\u0634\u0645\u0633 \u0645\u0646 \u062E\u0644\u0627\u0644 \u0633\u062D\u0628 \u0627\u0644\u0631\u0647\u062C \u0627\u0644\u0623\u0639\u0644\u0649 \u0627\u0644\u0631\u0642\u064A\u0642\u0629\u060C \u0644\u0643\u0646 \u0627\u0644\u0637\u0628\u0642\u0627\u062A \u0627\u0644\u062B\u062E\u064A\u0646\u0629 \u064A\u0645\u0643\u0646 \u0623\u0646 \u062A\u0643\u0648\u0646 \u0645\u0639\u062A\u0645\u0629 \u062A\u0645\u0627\u0645\u064B\u0627."@ar . "Altoestrat"@ca . "Altostratus"@de . "L'altoestrat o altoestratus \u00E9s un tipus de n\u00FAvol mitj\u00E0 que forma un vel for\u00E7a homogeni, fibr\u00F3s o estriat de color m\u00E9s o menys gris o blavenc i que es caracteritza per la uniformitat de la seva superf\u00EDcie inferior. Sovint presenten zones relativament clares enmig d'altres de molt fosques, per\u00F2 mai no es nota un veritable relleu a la seva superf\u00EDcie. \u00C9s un tipus de n\u00FAvol molt relacionat amb d'altres. D'una banda, pot ser l'evoluci\u00F3 d'un cirroestrat o d'un altoc\u00FAmul, i, de l'altra, pot esdevenir nimboestrat si es va espessint i la precipitaci\u00F3 augmenta, i altoc\u00FAmul si es va esquin\u00E7ant. Aquests n\u00FAvols produeixen de vegades precipitacions febles i cont\u00EDnues, en forma de pluja i nevades que poden ser for\u00E7a persistents. Sovint les precipitacions no arriben a terra i es veuen cortines fosques penj"@ca . . . . . . . "166735"^^ . . . "Altostratus"@pt . "\u0631\u0647\u062C \u0623\u0639\u0644\u0649"@ar . .