{"id":28319,"date":"2016-12-18T20:00:11","date_gmt":"2016-12-18T17:00:11","guid":{"rendered":"https:\/\/e-marineeducation.com\/tr\/?p=28319"},"modified":"2016-12-18T19:57:06","modified_gmt":"2016-12-18T16:57:06","slug":"denizcilerin-yol-gostericisi-bulutlar","status":"publish","type":"post","link":"https:\/\/e-marineeducation.com\/tr\/denizcilerin-yol-gostericisi-bulutlar\/","title":{"rendered":"Denizcilerin Yol G\u00f6stericisi: Bulutlar"},"content":{"rendered":"

\"\"G\u00f6ky\u00fcz\u00fcn\u00fcn adeta s\u00fcs\u00fcd\u00fcr bulutlar. Denizdeyken \u015f\u00fcphesiz en g\u00fczel manzara foto\u011fraflar\u0131n\u0131 \u00e7ekmemizi sa\u011flayan, zaman zaman pamuk gibi olan, zaman zaman ise \u00fcrpertici bir hale b\u00fcr\u00fcnen bulutlar, ge\u00e7mi\u015ften bu yana \u00f6zellikle de biz denizcilere, gelecekte olu\u015facak hava olaylar\u0131ndan haberdar olmam\u0131zda i\u00e7in e\u015fsiz yol g\u00f6stericilerdir. Bu yaz\u0131da da bu e\u015fsiz yard\u0131mc\u0131lar\u0131m\u0131za ufak bir g\u00f6z ataca\u011f\u0131z.<\/p>\n

\"\"<\/p>\n

Bulutlar Nedir?<\/strong><\/p>\n

\u0130lk olarak bulutlar\u0131 tan\u0131mlayal\u0131m. Bulutlar, atmosferdeki su damlac\u0131klar\u0131n\u0131n ya da olu\u015fan buz kristallerinin havan\u0131n y\u00fcksek katmanlar\u0131nda yo\u011funla\u015fmas\u0131 ile olu\u015fan topluluklard\u0131r.<\/p>\n

Bulutlar, yery\u00fcz\u00fcne ula\u015fan g\u00fcne\u015f enerjisini ve yery\u00fcz\u00fcnden uzaya geri yans\u0131yan enerji miktar\u0131n\u0131 d\u00fczenleyerek, iklimlerin olu\u015fmas\u0131 \u00fczerinde \u00f6nemli rol oynar.<\/p>\n

\"\"<\/p>\n

Nas\u0131l Olu\u015furlar?<\/strong><\/p>\n

Denizlerde ve okyanuslarda oldu\u011fu gibi, atmosferde de su bulunmaktad\u0131r. Atmosferde bulunan su, g\u00fcne\u015fin de etkisiyle yo\u011funluk azl\u0131\u011f\u0131ndan, yery\u00fcz\u00fcnden buhar olarak ayr\u0131l\u0131r. Buhar durumundaki bulunan su k\u00fctlesi g\u00f6zle g\u00f6r\u00fclmez. Ancak, bulut katman katman y\u00fckseldik\u00e7e ve yer seviyesinden uzakla\u015ft\u0131k\u00e7a, so\u011fuk hava tabakalar\u0131yla kar\u015f\u0131la\u015f\u0131r ve gaz haline daha yak\u0131n olan sular, su damlac\u0131klar\u0131 ya da buz kristali bi\u00e7iminde yo\u011funla\u015fmaya ba\u015flar. Yo\u011funla\u015fma s\u0131ras\u0131nda g\u00fcne\u015f \u0131\u015f\u0131\u011f\u0131 bu yo\u011fun k\u00fctle i\u00e7inden bir \u00f6l\u00e7\u00fcde ge\u00e7ebildi\u011finden, puslu bir durum olan bulut, sis veya pus g\u00f6r\u00fcn\u00fcm\u00fcn\u00fc al\u0131rlar. Bulutlar yer seviyesinden y\u00fcksekte bulunur. Yer seviyesinde olu\u015fan s\u0131\u011f bulut katmanlar\u0131 ise sis olarak adland\u0131r\u0131lmaktad\u0131r.<\/p>\n

Renkleri Nas\u0131l olu\u015fur?<\/strong><\/p>\n

Bulutlar t\u00fcm g\u00f6r\u00fcn\u00fcr dalga boyutlar\u0131n\u0131 yans\u0131tmaktad\u0131r. Bulutlar genellikle beyaz olarak g\u00f6r\u00fcn\u00fcrler, ancak bildi\u011fimiz gibi \u00f6zellikle ya\u011f\u0131\u015fl\u0131 olabilecek havalar gri veya siyah olarak da g\u00f6r\u00fcnebilmektedirler. Bulutlar\u0131n gri ya da siyah g\u00f6r\u00fcnmelerinin sebebi, kal\u0131nl\u0131klar\u0131 nedeniyle g\u00fcne\u015f \u0131\u015f\u0131\u011f\u0131n\u0131n ge\u00e7mesine izin vermemeleridir.<\/p>\n

\"\"<\/p>\n

S\u0131cakl\u0131\u011f\u0131 ve So\u011fuklu\u011fu Nas\u0131l Etkilerler ?<\/strong><\/p>\n

Baz\u0131 bulut tipleri yery\u00fcz\u00fcnden yans\u0131yan enerjiyi yery\u00fcz\u00fcne geri yans\u0131tarak s\u0131cakl\u0131\u011f\u0131 tutarken, baz\u0131 bulut tipleriyse g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131 yans\u0131tarak yery\u00fcz\u00fcn\u00fcn \u0131s\u0131nmas\u0131n\u0131 engelleyerek daha so\u011fuk olmas\u0131n\u0131 sa\u011flayabilirler. Mesela bulutsuz bir gecede, havan\u0131n ba\u015fka zamanlara g\u00f6re \u00e7ok daha so\u011fuk oldu\u011funu hissetmi\u015fizdir. Bu anda bulutlar\u0131n yal\u0131t\u0131c\u0131 etkisi olmad\u0131\u011f\u0131 i\u00e7in, b\u00f6yle gecelerde yery\u00fcz\u00fcnden \u00e7ok daha fazla enerji uzaya geri yans\u0131r ve b\u00f6ylece daha so\u011fuk bir gece ya\u015fanm\u0131\u015f olur.<\/p>\n

Nas\u0131l S\u0131n\u0131fland\u0131r\u0131l\u0131rlar ?<\/strong><\/p>\n

Bulutlar, \u015fekillerine, bulunduklar\u0131 ve olu\u015ftuklar\u0131 y\u00fcksekliklere g\u00f6re s\u0131n\u0131fland\u0131r\u0131lmaktad\u0131r. \u015eekillerine g\u00f6re bulutlar\u0131 tan\u0131maya ba\u015flarsak g\u00f6z\u00fcm\u00fczde daha iyi canlanabilmektedirler.<\/p>\n

\"\"<\/p>\n

G\u00f6r\u00fcn\u00fc\u015flerine G\u00f6re Bulutlar<\/span>
\nBulutlar g\u00f6r\u00fcn\u00fc\u015flerine g\u00f6re adland\u0131r\u0131l\u0131rken, Latince k\u00f6kenli kelimeler ve bunlardan t\u00fcretilmi\u015f ekler kullan\u0131lm\u0131\u015ft\u0131r. \u015eimdide bu kelimeleri tan\u0131yal\u0131m:<\/p>\n

\u2022 Sirr\u00fcs Ailesi
\nSirrus<\/em> <\/span>yani \u201cCirrus\u201d s\u00f6zc\u00fc\u011f\u00fc, Latincede “k\u0131vr\u0131m” ve “bukle” anlam\u0131na gelmektedir. Ek olarak kullan\u0131ld\u0131\u011f\u0131nda, sirr\u00fcs s\u00f6zc\u00fc\u011f\u00fc bazen sirro- \u015feklinde olarak kullan\u0131l\u0131r. Buna \u00f6rnek olarak, sirrostrat\u00fcs<\/em> <\/span>bulutunu \u00f6rnek verebiliriz. Sirr\u00fcs ailesindeki bulutlar, bazen “lifli” veya “at kuyru\u011fu” \u015feklinde de tan\u0131mlanabilmektedir.
\n\u2022 K\u00fcm\u00fcl\u00fcs ailesi
\nK\u00fcm\u00fcl\u00fcs<\/em> <\/span>\u201cCumulus\u201d s\u00f6zc\u00fc\u011f\u00fc Latincede “y\u0131\u011f\u0131n veya k\u00fcmelenme” anlamlar\u0131na gelmektedir. Bir \u015feyin, bir ortamda birikmesini ve k\u00fcmelenmesini anlatmakta kullan\u0131l\u0131r. Ek olarak kullan\u0131ld\u0131\u011f\u0131nda k\u00fcm\u00fcl\u00fcs s\u00f6zc\u00fc\u011f\u00fc bazen k\u00fcm\u00fclo- \u015feklinde kullan\u0131l\u0131r. Buna \u00f6rnek olarak k\u00fcm\u00fclonimb\u00fcs<\/em> <\/span>bulut \u00e7e\u015fidi verebiliriz.
\n\u2022 Strat\u00fcs ailesi
\nStratus<\/em> <\/span>s\u00f6zc\u00fc\u011f\u00fc yine Latincede “yay\u0131lm\u0131\u015f” anlam\u0131na gelmektedir. Ek olarak kullan\u0131ld\u0131\u011f\u0131nda strat\u00fcs s\u00f6zc\u00fc\u011f\u00fc bazen strato- \u015feklinde kullan\u0131lmaktad\u0131r. Buna \u00f6rnek olarak da stratok\u00fcm\u00fcl\u00fcs<\/em> <\/span>bulut \u00e7e\u015fidini verebiliriz.
\n\u2022 Nimb\u00fcs ailesi
\nNimbus<\/em> <\/span>s\u00f6zc\u00fc\u011f\u00fc Latincede “hale<\/em><\/span>” anlam\u0131na gelir. Ek olarak kullan\u0131ld\u0131\u011f\u0131nda strat\u00fcs s\u00f6zc\u00fc\u011f\u00fc nimbo- \u015feklinde kullan\u0131lmaktad\u0131r. Nimbostrat\u00fcs<\/em> <\/span>vs. Nimb\u00fcs ailesi “ya\u011f\u0131\u015f ta\u015f\u0131yan” bulutlar olarak bilinmektedir.
\n\u2022 Altolar
\nYukar\u0131da s\u0131n\u0131fland\u0131rd\u0131\u011f\u0131m\u0131z bulutlar\u0131n haricinde kullan\u0131lan bir di\u011fer ek olan alto-, Latinceden altus “y\u00fcksek” s\u00f6zc\u00fc\u011f\u00fcnden gelmesine ra\u011fmen, ad\u0131nda alto bulunan bulutlar genellikle orta seviye bulutlar\u0131 olarak tan\u0131mlanm\u0131\u015ft\u0131r.<\/p>\n

Y\u00fcksekliklerine G\u00f6re Bulutlar\u0131n S\u0131n\u0131fland\u0131r\u0131lmas\u0131<\/span><\/p>\n

\u2022 Y\u00fcksek Bulutlar<\/p>\n

Y\u00fcksek seviyeli bulutlar ise genellikle bulut taban y\u00fcksekli\u011fi 7000 m\u2019nin \u00fczerinde olan bulutlard\u0131r ve buz kristali i\u00e7erirler.<\/p>\n

Sirrus Bulutlar\u0131<\/span>
\nSirrus bulutlar\u0131, g\u00f6ky\u00fcz\u00fcndeki en y\u00fcksek bulutlard\u0131r. \u0130nce, dar \u015feritler bi\u00e7iminde veya lif lif halde beyaz ipeksi \u015feritler g\u00f6r\u00fcn\u00fcrler. Her zaman \u00f6teki bulutlardan daha beyazd\u0131rlar. A\u00e7\u0131k havada g\u00f6r\u00fclmektedirler. Ortalama 9 ila 12km y\u00fckseklikte bulunurlar. \u00c7o\u011funlukta buz kristallerinden olu\u015fmaktad\u0131rlar. Genellikle ayn\u0131 y\u00f6ne do\u011fru uzamakta ve o y\u00fckseklikteki bulut hareketinin y\u00f6n\u00fcn\u00fc g\u00f6stermektedirler. Genellikle iyi hava habercisi bulutlard\u0131r. Pe\u015flerinde al\u00e7ak ve kal\u0131n bulutlar\u0131n bulunmas\u0131, \u00e7o\u011fu zaman ya\u011fmur veya kar i\u015fareti olarak de\u011ferlendirilirler.\"\"<\/p>\n

Sir\u00fcsler g\u00fcne\u015f do\u011fdu\u011fu ve batt\u0131\u011f\u0131 zamanlarda daha kolay g\u00f6zlenebilirler. Y\u00fckseklikleri sebebiyle, g\u00fcne\u015f do\u011fu\u015flar\u0131nda, di\u011fer bulutlardan daha \u00f6nce ayd\u0131nlanmaktad\u0131rlar. G\u00fcn bat\u0131mlar\u0131nda da di\u011fer bulutlardan daha sonra kararmaktad\u0131rlar.<\/p>\n

Sirrok\u00fcm\u00fcl\u00fcs Bulutlar\u0131<\/span><\/p>\n

\"\"<\/p>\n

Bu bulutlar da, Sirrus bulutlar\u0131 gibi y\u00fcksek katmanlarda bulunan bulutlardand\u0131r ve neredeyse t\u00fcm\u00fcyle buz kristallerinden meydana gelmektedirler. Top top, pullar halinde veya \u00e7ok k\u00fc\u00e7\u00fck k\u00fcrelerden olu\u015fmu\u015f ince ve beyaz bir tabaka g\u00f6r\u00fcn\u00fcml\u00fc bu bulutlar, g\u00f6lge yapmaz. Genelde iyi hava i\u015faretidir. Altok\u00fcm\u00fcl\u00fcs<\/em> <\/span>bulutlar\u0131yla kar\u0131\u015ft\u0131r\u0131lsa da, tamamen beyaz olmas\u0131, g\u00f6lge b\u0131rakmay\u0131\u015f\u0131 ve tek tek par\u00e7alardan olu\u015fmas\u0131yla \u00f6teki bulut tiplerinden kolayl\u0131kla ay\u0131rt edilebilir. Genellikle iyi hava habercisidirler. Fakat, bir f\u0131rt\u0131nan\u0131n \u00f6n\u00fcnde olu\u015ftuklar\u0131nda, kal\u0131n bir tabaka halinde ve daha al\u00e7akta bulunmaktad\u0131rlar. Kal\u0131nl\u0131klar\u0131 fazlala\u015f\u0131rken, renkleri grile\u015fir ve g\u00f6r\u00fcn\u00fc\u015fleri sert bir hal almaktad\u0131r.\"\"<\/p>\n

Sirrostrat\u00fcs Bulutlar\u0131<\/span><\/p>\n

\"\"Y\u00fcksek katmanlarda bulunan bulutlar\u0131m\u0131z\u0131n sonuncusu da sirrostrat\u00fcs<\/em> <\/span>tipi bulutlard\u0131r. \u0130nce bir halde, saydam \u00f6zellikte, yine di\u011fer y\u00fcksek katman bulutlar\u0131 gibi g\u00f6lge yapmayan bulutlard\u0131r. Beyaz\u0131ms\u0131 renkte bulunurlar. B\u00fcy\u00fck \u00e7o\u011funlukta buz kristallerinden olu\u015furlar. G\u00f6ky\u00fcz\u00fcn\u00fcn t\u00fcm\u00fcn\u00fc, ya da bir b\u00f6l\u00fcm\u00fcn\u00fc kaplarlar. Sirr\u00fcslerden geli\u015firler. Bu tip bulutlar di\u011fer y\u00fcksek katman bulutlar\u0131ndan farkl\u0131 olarak, ya\u011f\u0131\u015f ve k\u00f6t\u00fc hava habercisidirler. G\u00f6ky\u00fcz\u00fcnde g\u00fcne\u015f ya da ay varsa bunlar\u0131n \u00e7evresinde hale olu\u015fturabilir. Denizciler aras\u0131nda \u201cay\u0131n \u00e7evresinde hale varsa k\u00f6t\u00fc hav
\na habercisidir\u201d \u015feklindeki kan\u0131 bu bulut tipinin \u00f6zelliklerinden gelmektedir.<\/p>\n

Buz kristallerinin eriyerek su damlac\u0131klar\u0131na d\u00f6n\u00fc\u015fmesyle, altostrat\u00fcs tipi bulutlar ortaya \u00e7\u0131kar ve bu tip bulutlar\u0131n g\u00f6r\u00fcnmesinden sonra 24 saat i\u00e7inde ya\u011fmur beklenmelidir.<\/p>\n

\"\"<\/p>\n

\u2022 Orta Seviye Bulutlar<\/p>\n

Orta seviyeli bulutlar taban y\u00fcksekli\u011fi 2000 ve 7000m aras\u0131nda kalan bulutlard\u0131r. Y\u00fcksek seviyeli bulutlarla \u00fcst \u00fcste gelebilirler. Genellikle su damlac\u0131\u011f\u0131 i\u00e7erirler, fakat s\u0131cakl\u0131k yeterli seviyede azald\u0131\u011f\u0131nda, i\u00e7eri\u011finde buz kristali ve su damlas\u0131 kar\u0131\u015f\u0131m\u0131 aras\u0131nda bulunurlar. Bu tip bulutlar\u0131n ba\u015f\u0131na alto (y\u00fcksek) \u00f6n eki getirilmektedir.<\/p>\n

Altok\u00fcm\u00fcl\u00fcs Bulutlar\u0131<\/span><\/p>\n

\"\"Bu tip bulutlar gri tonlar\u0131nda ya da beyaz olur. K\u00fcre bi\u00e7imi bir\u00e7ok par\u00e7an\u0131n bir araya gelerek meydana getirdi\u011fi katmanl\u0131, par\u00e7al\u0131 bir g\u00f6r\u00fcn\u00fcm\u00fcne sahiptirler. Genellikle bir b\u00f6l\u00fcmleri g\u00f6lgelidir. Bu da onlar\u0131n daha y\u00fckseklerdeki sirrok\u00fcm\u00fcl\u00fcs<\/em> <\/span>tipi y\u00fcksek katman bulutlar\u0131ndan ay\u0131rt edilmesini sa\u011flar.<\/p>\n

Geni\u015f bir alanda olu\u015fan hava k\u00fctlesinin y\u00fckselerek so\u011fumas\u0131yla olu\u015fabilirler. S\u0131cak ve nemli bir yaz sabah\u0131nda varl\u0131klar\u0131, genellikle f\u0131rt\u0131na habercisidir. Kal\u0131n ve al\u00e7aklarda ise g\u00f6k g\u00fcr\u00fclt\u00fcs\u00fc ve sa\u011fanaklara sebep olurlar. Fakat, bu uzun s\u00fcreli bir k\u00f6t\u00fc hava de\u011fildir.<\/p>\n

\"\"<\/p>\n

Altostrat\u00fcs Bulutlar\u0131<\/span><\/p>\n

Orta y\u00fckseklikteki bulut cinslerinden bir ba\u015fkas\u0131 da altostrat\u00fcs<\/em> <\/span>tipi bulutlard\u0131r. Bu bulutlar g\u00f6ky\u00fcz\u00fcn\u00fcn b\u00fcy\u00fck bir b\u00f6l\u00fcm\u00fcn\u00fc kaplar ve griye bazen de mavi \u00e7alan bir tonda olur. Bir \u00f6rt\u00fc veya perde halinde t\u00fcm g\u00f6ky\u00fcz\u00fcn\u00fc kaplarlar. Su damlac\u0131klar\u0131ndan, bazen de buz kristallerinden olu\u015furlar. G\u00fcne\u015f\u2019in ya da ay\u0131n g\u00f6r\u00fclmesini engelleyecek kadar kal\u0131n olabilirler. Bu bulutlar\u0131n gerisinde g\u00fcne\u015f ve ay bulundu\u011funda, g\u00f6r\u00fcn\u00fcm buzlu cam\u0131n arkas\u0131ndan bak\u0131lm\u0131\u015f gibidir.<\/p>\n

\"\"<\/p>\n

Tabakalar h\u00e2linde bulunan, \u00e7izgili yap\u0131daki altostrat\u00fcsler<\/em>, hafif bir ya\u011fmura ya da kara neden olmaktad\u0131rlar. Bu bulutlar, kal\u0131n ve al\u00e7ak seviyelerde olu\u015fmu\u015f iseler ve altlar\u0131nda nimbostrat\u00fcs <\/em><\/span>tipi bulutlar bulunuyorsa, birka\u00e7 saat i\u00e7inde ba\u015flayacak olan devaml\u0131 ya\u011fmur veya kar ya\u011f\u0131\u015f\u0131 beklenir.<\/p>\n

\u2022 Al\u00e7ak Seviye Bulutlar\u0131<\/p>\n

Stratok\u00fcm\u00fcl\u00fcs Bulutlar\u0131<\/span><\/p>\n

Al\u00e7ak seviye bulutlar\u0131nda ilk g\u00f6rece\u011fimiz bulutlar stratok\u00fcm\u00fcl\u00fcs<\/em> <\/span>tipi bulutlar\u0131d\u0131r. Bu tip bulutlar gri tonlarda veya beyaz renklerde, yatay silindirik halde bulunan katmanl\u0131 ve yuvarlak k\u00fctlelerden olu\u015fan bulutlard\u0131r. Al\u00e7aklarda g\u00f6r\u00fcl\u00fcrler. Birbirine yak\u0131n k\u00fcmeler ya da tabakalar halinde, mozaik g\u00f6r\u00fcn\u00fcml\u00fcd\u00fcrler. Tabakalar\u0131 \u00e7ok kal\u0131n de\u011fildir ve dikine geli\u015fmezler.<\/p>\n

\"\"<\/p>\n

Bu tip bulutlar, k\u00fc\u00e7\u00fck par\u00e7alar\u0131n bulundu\u011fu y\u00f6ne do\u011fru, r\u00fczgarla birlikte ilerlerler. Bulunduklar\u0131 y\u00fcksekliklere g\u00f6re \u00e7ok de\u011fi\u015fik olabilirler. Stratok\u00fcm\u00fcl\u00fcslerden sonra geceleri genellikle a\u00e7\u0131k bir g\u00f6ky\u00fcz\u00fc izlenir. Bu tip bulutlar, hemen hemen hi\u00e7 ya\u011f\u0131\u015fa neden olmaz.<\/p>\n

Strat\u00fcs Bulutlar\u0131<\/span><\/p>\n

Bulutlardan aras\u0131nda en al\u00e7ak katmanda bulunan t\u00fcr, strat\u00fcslerdir. Alt s\u0131n\u0131rlar\u0131 300m den y\u00fcksek de\u011fildir. Sise benzer, tek d\u00fcze bir katman halindedirler. Genellikle geni\u015f bir alana yay\u0131l\u0131rlar. Genellikle su damlac\u0131klar\u0131ndan olu\u015furlar ve renkleri a\u00e7\u0131k griden koyu griye kadar de\u011fi\u015fmektedir. Bu bulutlara deniz k\u0131y\u0131lar\u0131nda da\u011f eteklerinde ve vadilerde s\u0131k s\u0131k rastlayabiliriz. \u00c7iselemeye ya da hafif kar ya\u011f\u0131\u015f\u0131na neden olan strat\u00fcsler, atmosferin yere yak\u0131n bir katman\u0131n\u0131n so\u011fumas\u0131yla olu\u015fur.<\/p>\n

\"\"<\/p>\n

\u00c7o\u011fu zaman g\u00f6ky\u00fcz\u00fcnde ince bir perde halinde bulunduklar\u0131ndan, dumanl\u0131 bir g\u00f6r\u00fcn\u00fcm ortaya \u00e7\u0131kar. Altlar\u0131nda kalan alanlara g\u00fcne\u015f \u0131\u015f\u0131\u011f\u0131 gitmesine daha az m\u00fcsaade ederler. Strat\u00fcs tipi bulutlardan a\u015fa\u011f\u0131lara do\u011fru hafif bir pus (mist) inerek, yatay g\u00f6r\u00fc\u015f\u00fcm\u00fcz\u00fc etkileyebilir.<\/p>\n

\"\"<\/p>\n

Nimbostrat\u00fcs<\/span><\/p>\n

Orta y\u00fckseklik katman\u0131na yak\u0131n bulutlard\u0131r. Koyu renklidirler. Genellikle tekd\u00fcze bir yap\u0131da, bazen ise par\u00e7al\u0131 bi\u00e7imde olabilirler. Nimbostrat\u00fcs<\/em> <\/span>bulutlar\u0131 tipik ya\u011fmur bulutlar\u0131d\u0131r. Devaml\u0131 veya aral\u0131kl\u0131 bir ya\u011f\u0131\u015f meydana getirirler. Fakat bu ya\u011f\u0131\u015f sa\u011fanak halinde de\u011fildir. Bu gri bulutlar g\u00fcne\u015f’i \u00f6rt\u00fcp tamamen kaplarlar. Bu bulut t\u00fcr\u00fc de yukar\u0131ya do\u011fru b\u00fcy\u00fcr ve al\u00e7ak bulut seviyesinden y\u00fcksek bulut seviyesine kadar uzan\u0131rlar.<\/p>\n

\"\"<\/p>\n

K\u00fcm\u00fcl\u00fcs<\/span><\/p>\n

K\u00fcm\u00fcl\u00fcs<\/em> <\/span>tipi bulut da, al\u00e7akta bulunan bir bulut t\u00fcr\u00fcd\u00fcr. \u00dcst k\u0131s\u0131mlar\u0131 patlam\u0131\u015f m\u0131s\u0131r\u0131 ya da karn\u0131bahar\u0131 and\u0131rabilir. Do\u011frudan \u0131\u015f\u0131k alan yerleri parlak beyaz, \u00f6teki b\u00f6l\u00fcmleri g\u00f6lgeli ya da koyu renklidir. G\u00f6ky\u00fcz\u00fcnde par\u00e7al\u0131 bulutlu bir g\u00f6r\u00fcn\u00fcm olu\u015ftururlar. Fakat, hi\u00e7bir zaman g\u00f6ky\u00fcz\u00fcn\u00fc tamamen \u00f6rtemezler. B\u00fcy\u00fck da\u011flar, tepeler halinde \u00e7ok y\u00fckseklere kadar uzan\u0131rlar. Bulutlar\u0131n \u00fcst k\u0131sm\u0131 buz kristallerinden meydana gelmi\u015ftir. Bulut uzaklarda iken yaln\u0131zca \u00fcst k\u0131sm\u0131 g\u00f6r\u00fclebilir. Alt k\u0131s\u0131m \u00e7o\u011fu zaman ufkun alt\u0131nda kald\u0131\u011f\u0131ndan g\u00f6r\u00fclemez.<\/p>\n

\"\"<\/p>\n

K\u00fcm\u00fcl\u00fcsler, \u0131s\u0131nan havan\u0131n y\u00fckselmesi ve y\u00fckseklerde so\u011fumas\u0131 s\u0131ras\u0131nda, dikey olu\u015fum ile ortaya \u00e7\u0131karlar. G\u00f6ky\u00fcz\u00fcnde dikine geli\u015ferek b\u00fcy\u00fcrler. Su damlac\u0131klar\u0131ndan olu\u015fan al\u00e7ak bulutlard\u0131r. Hava yeterince so\u011fuksa, buz kristalleri ve kar i\u00e7erirler. Dikey olu\u015fum \u00e7ok kuvvetli de\u011filse, k\u00fcm\u00fcl\u00fcsler pamuk veya y\u00fcn y\u0131\u011f\u0131nlar\u0131na benzerler. Yatay tabanlar\u0131 tam olarak olu\u015fmu\u015f k\u00fcm\u00fcl\u00fcsler, daima iyi hava habercisi olarak de\u011ferlendirilirler. K\u00fcme, kubbe ya da kule benzeri \u015fekiller alarak b\u00fcy\u00fcr ve ya\u011f\u0131\u015flara neden olurlar. Atmosferin yere yak\u0131n katmanlar\u0131nda havan\u0131n so\u011fumas\u0131yla olu\u015furlar.<\/p>\n

D\u00fczenleme: R\u00fcya Hazar<\/a><\/span><\/span><\/strong>
\n Ekleyen: Ay\u015fe K\u0131r\u0131c\u0131<\/a><\/span><\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"

G\u00f6ky\u00fcz\u00fcn\u00fcn adeta s\u00fcs\u00fcd\u00fcr bulutlar. Denizdeyken \u015f\u00fcphesiz en g\u00fczel manzara foto\u011fraflar\u0131n\u0131 \u00e7ekmemizi sa\u011flayan, zaman zaman pamuk gibi olan, zaman zaman ise \u00fcrpertici bir hale b\u00fcr\u00fcnen bulutlar, ge\u00e7mi\u015ften bu yana \u00f6zellikle de biz denizcilere, gelecekte olu\u015facak hava olaylar\u0131ndan haberdar olmam\u0131zda i\u00e7in e\u015fsiz yol g\u00f6stericilerdir. Bu yaz\u0131da da bu e\u015fsiz yard\u0131mc\u0131lar\u0131m\u0131za ufak bir g\u00f6z ataca\u011f\u0131z. Bulutlar Nedir? \u0130lk …<\/p>\n","protected":false},"author":87,"featured_media":28343,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"_bbp_topic_count":0,"_bbp_reply_count":0,"_bbp_total_topic_count":0,"_bbp_total_reply_count":0,"_bbp_voice_count":0,"_bbp_anonymous_reply_count":0,"_bbp_topic_count_hidden":0,"_bbp_reply_count_hidden":0,"_bbp_forum_subforum_count":0,"footnotes":""},"categories":[522],"tags":[4743,4745,4747,4734,3137,4730,4731,4732,4736,4729,4741,4737,4735,4733,4742,4740,4484,4746,4744,4739,4748,4738,4749,1046],"class_list":["post-28319","post","type-post","status-publish","format-standard","has-post-thumbnail","","category-ozel-yazilar","tag-altokumulus","tag-altokumulus-bulutlari","tag-altostratus-bulutlari","tag-at-kuyrugu","tag-ayse-kirici-eklemeleri","tag-bulut","tag-bulut-nasil-olusur","tag-cirrus","tag-cumulus","tag-denizcilerin-yol-gostericisi-bulutlar","tag-hale","tag-kumulonimbus","tag-kumulus","tag-lifli","tag-nimbostratus","tag-nimbus","tag-ruya-hazar-duzenlemeleri","tag-sirrokumulus","tag-sirrostratus","tag-stratokumulus","tag-stratokumulus-bulutlari","tag-stratus","tag-stratus-bulutlari","tag-tayfun-emre-zerde-yazilari"],"acf":[],"yoast_head":"\nDenizcilerin Yol G\u00f6stericisi: Bulutlar - 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