Nemlilik yer y\u00fcz\u00fcnde canl\u0131 hayat\u0131n\u0131n geli\u015fmesinde ve devam\u0131nda \u00e7ok \u00f6nemli bir unsurdur. Hava ve iklim \u015fartlar\u0131 bak\u0131m\u0131ndan da \u00e7ok \u00f6nemlidir. Her \u015feyden \u00f6nce ya\u011f\u0131\u015flar\u0131n kayna\u011f\u0131, havadaki su buhar\u0131d\u0131r.
\n Su her s\u0131cakl\u0131kta buharla\u015f\u0131r. Bu sebeple atmosferde s\u00fcrekli bir miktar nem vard\u0131r. Buna atmosfer nemlili\u011fi denir. Nemlili\u011fi \u00f6l\u00e7en alete de higrometre denir.
\n MUTLAK NEM
\n Mutlak Nem: 1 m\u00b3 hava i\u00e7inde bulunan nemin gr olarak a\u011f\u0131rl\u0131\u011f\u0131na denir.
\n Su buhar\u0131n\u0131n miktar\u0131 hacim itibariyle hi\u00e7bir zaman havan\u0131n % 4\u2019\u00fcn\u00fc a\u015fmaz. <\/p>\n
Mutlak Nemde Etkili Fakt\u00f6rler
\n *Buharla\u015fma Y\u00fczeyi: Buharla\u015fma y\u00fczeylerinden (okyanus , deniz , akarsu , g\u00f6l , bitki \u00f6rt\u00fcs\u00fc gibi) uzakla\u015ft\u0131k\u00e7a mutlak nem azal\u0131r. \u00d6rnek; deniz k\u0131y\u0131s\u0131ndan kara i\u00e7lerine, ormanl\u0131k alandan ormans\u0131z alana gidildik\u00e7e mutlak nem azal\u0131r
\n Mutlak Nemde Etkili Fakt\u00f6rler
\n S\u0131cakl\u0131k: S\u0131cakl\u0131k artt\u0131k\u00e7a buharla\u015fma artaca\u011f\u0131ndan dolay\u0131 genellikle mutlak nem de artar. \u00d6rnek; Ekvatordan kutuplara do\u011fru mutlak nem azal\u0131r. Ayr\u0131ca yazdan k\u0131\u015fa, g\u00fcnd\u00fczden geceye ge\u00e7ildi\u011finde mutlak nem azal\u0131r
\n NOT: S\u0131cakl\u0131k artt\u0131k\u00e7a her zaman mutlak nem artmayabilir. Ama s\u0131cak denizlere yakla\u015ft\u0131k\u00e7a mutlak nem her zaman artar.
\n Mutlak nem Ekvator \u00e7evresindeki denizler \u00fczerinde \u00e7ok fazla iken , d\u00f6nenceler \u00e7evresindeki \u00e7\u00f6l alanlar\u0131nda \u00e7ok azd\u0131r.
\n Mutlak Nemde Etkili Fakt\u00f6rler
\n R\u00fczgarlar\u0131n esme y\u00f6n\u00fc: Denizden gelen r\u00fczgarlar mutlak nemi art\u0131r\u0131rlar.
\n Okyanus ak\u0131nt\u0131lar\u0131: S\u0131cak su ak\u0131nt\u0131lar\u0131n\u0131n etkili oldu\u011fu yerlerde mutlak nem fazlad\u0131r.
\n MAKS\u0130MUM NEM (DOYMA M\u0130KTARI)
\n Maksimum Nem (Doyma miktar\u0131) : Belirli bir s\u0131cakl\u0131k ve bas\u0131n\u00e7 alt\u0131nda 1 m\u00b3 havan\u0131n ta\u015f\u0131yabilece\u011fi en fazla nem miktar\u0131na denir.
\n S\u0131cakl\u0131k artt\u0131k\u00e7a havan\u0131n hacmi geni\u015fler ve alabilece\u011fi nem miktar\u0131 da artar. Hava so\u011fudu\u011funda ise hacmi daral\u0131r ve alabilece\u011fi nem azal\u0131r.
\n S\u0131cakl\u0131k artt\u0131k\u00e7a havan\u0131n ta\u015f\u0131yabilece\u011fi nem miktar\u0131 artar. Buna \u00f6rnekler;
\n -Y\u00fckselen havan\u0131n ya\u011f\u0131\u015f b\u0131rakmas\u0131,
\n -F\u00f6hn r\u00fczgar\u0131n\u0131n kurutucu etki yapmas\u0131,
\n -\u00c7\u00f6llerde havan\u0131n nem a\u00e7\u0131\u011f\u0131n\u0131n fazla olmas\u0131,
\n -Al\u00e7al\u0131c\u0131 hava hareketleri sonucunda havan\u0131n nem a\u00e7\u0131\u011f\u0131n\u0131n artmas\u0131,
\n -G\u00fcnd\u00fcz sis yo\u011funlu\u011funun az olmas\u0131 veya gece olu\u015fan sislerin g\u00fcnd\u00fcz ortadan kalkmas\u0131
\n S\u0131cakl\u0131k artt\u0131k\u00e7a havan\u0131n ta\u015f\u0131yabilece\u011fi nem miktar\u0131 artar.
\n \u00d6l\u00e7\u00fclm\u00fc\u015f de\u011ferler;
\n -20 \u00b0C 1,10 gr\/m\u00b3
\n -10 \u00b0C 2,38 gr\/m\u00b3
\n 0 \u00b0C 4,85 gr\/m\u00b3
\n 5 \u00b0C 6,80 gr\/m\u00b3
\n 15 \u00b0C 12,85 gr\/m\u00b3 <\/p>\n
BA\u011eIL(N\u0130SB\u0130) NEM
\n Ba\u011f\u0131l Nem (nisbi ): Belirli bir s\u0131cakl\u0131ktaki hava k\u00fctlesinin i\u00e7inde bulunan nem miktar\u0131n\u0131n , o s\u0131cakl\u0131kta alabilece\u011fi en fazla nem miktar\u0131na oran\u0131d\u0131r. <\/p>\n
Ba\u011f\u0131l nem havada bulunan nemin y\u00fczde cinsinden de\u011feridir.
\n Ba\u011f\u0131l nem havan\u0131n nem a\u00e7\u0131\u011f\u0131n\u0131 veya neme doyma oran\u0131n\u0131 verir.
\n Bir yerde ya\u011f\u0131\u015f olabilmesi i\u00e7in ba\u011f\u0131l nem %100 \u2018\u00fc a\u015fmas\u0131 gerekir. <\/p>\n
BA\u011eIL NEMDE ETK\u0130L\u0130 FAKT\u00d6RLER
\n S\u0131cakl\u0131k: S\u0131cakl\u0131k artt\u0131k\u00e7a ba\u011f\u0131l nem azal\u0131r. Sebebi \u0131s\u0131nan havan\u0131n hacmi geni\u015fler, alabilece\u011fi nem artar. S\u0131cakl\u0131\u011fa uygun buharla\u015fma ger\u00e7ekle\u015fmez ise havan\u0131n nem a\u00e7\u0131\u011f\u0131 b\u00fcy\u00fcr ve ba\u011f\u0131l nem azal\u0131r.
\n \u00d6rnek; <\/p>\n
***S\u0131cakl\u0131k artarken mutlak nem ayn\u0131 \u015fekilde artm\u0131yorsa; ba\u011f\u0131l nem azal\u0131r.
\n Ba\u011f\u0131l nem azald\u0131k\u00e7a buharla\u015fma artar. Ba\u011f\u0131l nem artt\u0131k\u00e7a buharla\u015fma azal\u0131r.
\n Y\u00fckselti: Y\u00fckseklere \u00e7\u0131k\u0131ld\u0131k\u00e7a s\u0131cakl\u0131k azal\u0131r ve ba\u011f\u0131l nem artar.
\n Mutlak Nem: S\u0131cakl\u0131k ayn\u0131 iken zaman i\u00e7inde mutlak nem artarsa, ba\u011f\u0131l nem de artar. <\/p>\n
NOT: Ba\u011f\u0131l nem Ekvator \u00e7evresinde y\u00fcksek iken ,\u00e7\u00f6l b\u00f6lgelerinde ve kara i\u00e7lerinde azd\u0131r.
\n Yurdumuzda ba\u011f\u0131l nem en y\u00fcksek, Karadeniz B\u00f6lgesi\u2019ndedir. En d\u00fc\u015f\u00fck ise, G.Do\u011fu Anadolu B\u00f6lgesi\u2019ndedir.
\n YO\u011eUNLA\u015eMA
\n Hava i\u00e7indeki su buhar\u0131n\u0131n so\u011fumas\u0131 sonucu kat\u0131 veya s\u0131v\u0131 hale d\u00f6n\u00fc\u015fmesi olay\u0131na yo\u011funla\u015fma denir.
\n Yo\u011fu\u015fma noktas\u0131na iki yoldan eri\u015filir. Bunlar : 1- Havadaki nem miktar\u0131n\u0131n artmas\u0131; 2-S\u0131cakl\u0131\u011f\u0131n azalmas\u0131d\u0131r (tabiatta en fazla g\u00f6r\u00fclen yo\u011fu\u015fma bi\u00e7imidir).
\n Havan\u0131n alttan so\u011fumas\u0131 sonucu olu\u015fan yo\u011funla\u015fma bi\u00e7imine sis denir .
\n Sis olay\u0131n\u0131n en \u00f6nemli \u00f6zelli\u011fi, d\u00fcnya y\u00fczeyi ile temas eden havan\u0131n so\u011fumas\u0131 sonucunda meydana gelmesidir.
\n S\u0131cak ve nemli bir havan\u0131n daha so\u011fuk bir yerle temas\u0131 sonucu sis olu\u015fur. S\u0131cak ve so\u011fuk hava k\u00fctlelerinin kar\u015f\u0131la\u015fmas\u0131 da sislere yol a\u00e7ar.
\n BA\u015eLICA S\u0130S OLU\u015eUM \u015eEK\u0130LLER\u0130
\n *R\u00fczgar, \u0131l\u0131k denizlerden so\u011fuk karaya eserse karada sis olu\u015fur.
\n *R\u00fczgar, s\u0131cak denizlerden so\u011fuk denizlere eserse so\u011fuk sular \u00fczerinde sis olu\u015fur.
\n *R\u00fczgar, s\u0131cak karalardan so\u011fuk denizlere eserse deniz \u00fczerinde sis olu\u015fur.
\n *Serin denizler \u00fczerinde al\u00e7alan hava k\u00fctleleri sis olu\u015fumuna neden olur.
\n *Yama\u00e7 Sisleri: S\u0131cak ve nemli havan\u0131n yama\u00e7 boyunca y\u00fckselirken so\u011fumas\u0131ndan dolay\u0131 olu\u015fan bir sis t\u00fcr\u00fcd\u00fcr.
\n *Cephe Sisleri: Ya\u011f\u0131\u015f an\u0131nda so\u011fuk hava i\u00e7indeki s\u0131cak ya\u011fmur damlac\u0131klar\u0131n\u0131n so\u011fumas\u0131 ile olu\u015fan sislerdir.
\n BULUTLAR
\n Y\u00fckselen havan\u0131n yo\u011funla\u015fmas\u0131 sonucunda \u00e7ok k\u00fc\u00e7\u00fck su taneciklerinin bir araya gelmesiyle bulutlar olu\u015fur. Bulutlulu\u011fu \u00f6l\u00e7en alete nefometre denir.
\n Meteoroloji istasyonlar\u0131nda \u00f6l\u00e7\u00fclen bulutluluk ,g\u00f6ky\u00fcz\u00fcn\u00fcn oran\u0131 10 kabul edilerek s\u0131n\u0131fland\u0131r\u0131l\u0131r.
\n 0-2 oran\u0131 A\u00e7\u0131k havay\u0131
\n 2-8 oran\u0131 Bulutlu havay\u0131
\n 8-10 oran\u0131 Kapal\u0131 havay\u0131 ifade eder.
\n S\u0131cakl\u0131k azald\u0131k\u00e7a bulut yo\u011funlu\u011fu artar. Ancak bu durum her zaman do\u011fru de\u011fildir.
\n \u00d6rnek: Kutuplarda ve troposferin \u00fcst katlar\u0131nda nem az oldu\u011fundan bulut yo\u011funlu\u011fu buralarda azd\u0131r.
\n BULUT \u00c7E\u015e\u0130TLER\u0130
\n K\u00dcM\u00dcL\u00dcS BULUTLARI
\n Is\u0131nan havan\u0131n y\u00fckselerek so\u011fumas\u0131 sonucu olu\u015fur. Bulutu olu\u015fturan su taneciklerinin yo\u011funla\u015fmas\u0131 ayn\u0131 seviyede ba\u015flad\u0131\u011f\u0131 i\u00e7in alt k\u0131s\u0131mlar\u0131 d\u00fczd\u00fcr. Genellikle s\u0131cak d\u00f6nemlerde g\u00f6r\u00fcl\u00fcrler.
\n K\u00fcm\u00fcl\u00fcs bulutlar\u0131n\u0131n daha da y\u00fckselerek so\u011fumas\u0131 sonucu k\u00fcm\u00fclonimbus bulutlar\u0131 olu\u015fur ve sa\u011fanak ya\u011f\u0131\u015flara neden olur.
\n S\u0130R\u00dcS BULUTLARI
\n \u00c7ok y\u00fckseklerde olu\u015fan bulutlard\u0131r. \u00c7ok seyrek buz kristallerinden olu\u015fan ve t\u00fcye benzeyen bulutlard\u0131r. Genelde ya\u011f\u0131\u015f getirmezler. Bunlar, bir siklonun (Al\u00e7ak Bas\u0131n\u00e7) yakla\u015ft\u0131\u011f\u0131n\u0131n ve havan\u0131n bozaca\u011f\u0131n\u0131n habercisidirler.
\n STRATUS BULUTLARI
\n Yer’in \u00fcst\u00fcnde, as\u0131l\u0131 gri bir tabaka gibi duran koyu renkli bulutlard\u0131r. Genelde ya\u011f\u0131\u015flara yol a\u00e7arlar.
\n Yukar\u0131daki bulutlar ana bulutlard\u0131r. Ancak g\u00f6ky\u00fcz\u00fcnde, \u00f6zelliklerine g\u00f6re, sirrok\u00fcm\u00fcl\u00fcs, k\u00fcm\u00fclonimbus, sirro-stratus gibi adlarla an\u0131lan karma bulutlar da g\u00f6r\u00fcl\u00fcr. Ayr\u0131ca, ya\u011f\u0131\u015f b\u0131rakan b\u00fct\u00fcn bulutlara nimbus ad\u0131 verilmektedir.
\n Yurdumuzda her mevsim ya\u011f\u0131\u015f alan Karadeniz B\u00f6lgesi\u2019nde (\u00d6zellikle Do\u011fu Karadeniz B\u00f6l\u00fcm\u00fc) bulutlu g\u00fcn say\u0131s\u0131 en fazla iken, bulutlu g\u00fcn say\u0131s\u0131 en az olan b\u00f6lge G.Do\u011fu Anadolu B\u00f6lgesi\u2019dir.
\n YA\u011eI\u015eLAR
\n Havadaki nemin yo\u011funla\u015farak kat\u0131 veya s\u0131v\u0131 halde yery\u00fcz\u00fcne d\u00fc\u015fmesi olay\u0131na ya\u011f\u0131\u015f denir. Bir yere d\u00fc\u015fen ya\u011f\u0131\u015f miktar\u0131n\u0131 \u00f6l\u00e7en alete pl\u00fcviyometre denir.
\n YA\u011eI\u015e T\u00dcRLER\u0130
\n \u00c7\u0130Y
\n Hava i\u00e7indeki su buhar\u0131n\u0131n so\u011fuk cisim y\u00fczeyleri \u00fczerinde su tanecikleri \u015feklinde yo\u011funla\u015fmas\u0131 olay\u0131d\u0131r. Yo\u011funla\u015fma 0 \u00b0C \u2018nin \u00fcst\u00fcnde ger\u00e7ekle\u015fmi\u015ftir. Olu\u015fumu sabaha kar\u015f\u0131 g\u00f6r\u00fcl\u00fcr. \u00d6zellikle ilkbahar ve sonbaharda g\u00f6r\u00fcl\u00fcr.
\n KIRA\u011eI
\n Havadaki su buhar\u0131n\u0131n so\u011fuk cisimler \u00fczerinde, 0\u00b0C\u2019den d\u00fc\u015f\u00fck s\u0131cakl\u0131klarda kristaller \u015feklinde yo\u011funla\u015fmas\u0131yla olu\u015fur.
\n KIR\u00c7
\n Havadaki su buhar\u0131n\u0131n \u00e7ok so\u011fumu\u015f cisim y\u00fczeylerinde buza d\u00f6n\u00fc\u015fmesidir.
\n YA\u011eMUR
\n Bulutu olu\u015fturan su taneciklerinin damlalar halinde yery\u00fcz\u00fcne d\u00fc\u015fmesi olay\u0131d\u0131r.
\n KAR
\n Bulutu olu\u015fturan su taneciklerinin 0 \u00b0C nin alt\u0131ndaki bir s\u0131cakl\u0131kta buz kristalleri \u015feklinde yery\u00fcz\u00fcne d\u00fc\u015fmesi olay\u0131d\u0131r.
\n DOLU
\n Havadaki nemin h\u0131zla y\u00fckselmesi ve \u00e7ok so\u011fumas\u0131 sonucu buz tanecikleri \u015feklinde yery\u00fcz\u00fcne d\u00fc\u015fmesi olay\u0131d\u0131r. Havan\u0131n ani y\u00fckselmesi genellikle ilkbahar ve yaz mevsiminde g\u00f6r\u00fcl\u00fcr. <\/p>\n
ORO\u011eRAF\u0130K (YAMA\u00c7) YA\u011eI\u015eLARI <\/p>\n
Yer \u015fekillerinin etkisiyle olu\u015furlar. Nemli hava k\u00fctlesinin bir da\u011f yamac\u0131na \u00e7arparak y\u00fckselmesi ve so\u011fumas\u0131 sonucu olu\u015furlar. T\u00fcrkiye\u2019de en fazla Karadeniz ve Akdeniz B\u00f6lgelerinde g\u00f6r\u00fcl\u00fcr. Bat\u0131 r\u00fczgarlar\u0131 ve Muson r\u00fczgarlar\u0131n\u0131n etki alanlar\u0131nda g\u00f6r\u00fclen ya\u011f\u0131\u015flar bu \u015fekilde olu\u015fmu\u015ftur.
\n Hava k\u00fctleleri yama\u00e7 boyunca y\u00fckselirken en fazla ya\u011f\u0131\u015f\u0131 500 – 1000 m y\u00fckseltiler aras\u0131na b\u0131rak\u0131rlar. Y\u00fckselti artt\u0131k\u00e7a (1000 m\u2019lerden sonra) mutlak nem azald\u0131\u011f\u0131 i\u00e7in ya\u011f\u0131\u015f da azal\u0131r. <\/p>\n
KONVEKS\u0130YON (S\u0130KLON\u0130K, Y\u00dcKSEL\u0130M, KIRK\u0130K\u0130ND\u0130) YA\u011eI\u015eLARI
\n Is\u0131nan havan\u0131n y\u00fckselerek so\u011fumas\u0131 sonucu olu\u015furlar. T\u00fcrkiye genelinde s\u0131cak d\u00f6nemlerde g\u00f6r\u00fclen ya\u011f\u0131\u015flar bu \u015fekildedir. En fazla \u0130\u00e7 Anadolu B\u00f6lgesinde g\u00f6r\u00fcl\u00fcr. Bu ya\u011f\u0131\u015flara halk aras\u0131nda K\u0131rkikindi ya\u011f\u0131\u015flar\u0131 denir. D\u00fcnya \u00fczerinde ise en fazla Ekvatoral b\u00f6lgede g\u00f6r\u00fcl\u00fcr. <\/p>\n
CEPHESEL (FRONTAL )YA\u011eI\u015eLAR <\/p>\n
S\u0131cak ve so\u011fuk hava k\u00fctlelerinin kar\u015f\u0131la\u015fma alanlar\u0131nda meydana gelen ya\u011f\u0131\u015flard\u0131r.
\n D\u00fcnya’da en \u00e7ok, Orta ku\u015fakta ve 60\u00b0 enlemleri civar\u0131nda g\u00f6r\u00fcl\u00fcr. T\u00fcrkiye’de, \u00f6zellikle k\u0131\u015f mevsiminde g\u00f6r\u00fclen ya\u011f\u0131\u015flar\u0131n \u00e7o\u011fu cephesel k\u00f6kenlidir. En fazla Akdeniz B\u00f6lgesinde g\u00f6r\u00fcl\u00fcr.
\n NOT: Ya\u011f\u0131\u015f olu\u015fumlar\u0131nda ortak \u00f6zellik y\u00fckselen havan\u0131n so\u011fumas\u0131d\u0131r.
\n NOT: Al\u00e7al\u0131c\u0131 hava hareketleri, karadan gelen hava ve engebesiz bir alanda hareket eden hava ya\u011f\u0131\u015f b\u0131rakmaz.
\n YA\u011eI\u015eLARIN DA\u011eILI\u015eINDA ETK\u0130L\u0130 FAKT\u00d6RLER
\n Denize g\u00f6re konum: K\u0131y\u0131 b\u00f6lgeler i\u00e7 kesimlere g\u00f6re daha fazla ya\u011f\u0131\u015f al\u0131r.
\n Y\u00fckselti: Y\u00fckseltisi fazla olan bir yer her zaman \u00e7evresine g\u00f6re daha fazla ya\u011f\u0131\u015f al\u0131r. Sebebi; yo\u011funla\u015fman\u0131n daha \u00e7ok y\u00fckseklerde ger\u00e7ekle\u015fmi\u015f olmas\u0131d\u0131r.
\n Da\u011flar\u0131n uzan\u0131\u015f do\u011frultusu: Da\u011flar\u0131n k\u0131y\u0131ya paralel oldu\u011fu yerler daha fazla ya\u011f\u0131\u015f al\u0131r. Ayr\u0131ca bu da\u011flar hakim r\u00fczgar y\u00f6n\u00fcne dik bir \u015fekilde y\u00fckselmi\u015f ise ya\u011f\u0131\u015f miktar\u0131 daha da artar.
\n R\u00fczgarlar\u0131n esme y\u00f6n\u00fc: Denizden karaya do\u011fru esen r\u00fczgarlar ya\u011f\u0131\u015f b\u0131rak\u0131rken , karadan gelen r\u00fczgarlar ya\u011f\u0131\u015f getirmez.
\n Okyanus ak\u0131nt\u0131lar\u0131: S\u0131caksu ak\u0131nt\u0131lar\u0131n\u0131n etkili oldu\u011fu yerlerde nemlilik fazla oldu\u011fundan, y\u0131ll\u0131k ya\u011f\u0131\u015f miktar\u0131 da fazlad\u0131r.
\n Bas\u0131n\u00e7 merkezi: Y\u00fcksek Bas\u0131n\u00e7 alanlar\u0131nda al\u00e7al\u0131c\u0131 hava hareketinden dolay\u0131 ya\u011f\u0131\u015f olu\u015fmaz. \u00c7\u00fcnk\u00fc al\u00e7alan hava alttan itibaren \u0131s\u0131n\u0131r ve hava doyma noktas\u0131ndan uzakla\u015f\u0131r. Al\u00e7ak Bas\u0131n\u00e7 alanlar\u0131nda ise y\u00fckselici hava hareketlerinden dolay\u0131 ya\u011f\u0131\u015f olu\u015fur. Y\u00fckselen hava so\u011fur ve doyma noktas\u0131na ula\u015f\u0131r.
\n G\u00fcne\u015f I\u015f\u0131nlar\u0131n\u0131n D\u00fc\u015fme A\u00e7\u0131s\u0131: Ekvatoral B\u00f6lgede g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131n\u0131n d\u00fc\u015fme a\u00e7\u0131s\u0131 b\u00fcy\u00fcd\u00fck\u00e7e, buharla\u015fma artar. Atmosfere kar\u0131\u015fan nem miktar\u0131 artar.Bunun sonucunda ya\u011f\u0131\u015f miktar\u0131 da artar. Bunun yan\u0131nda Kutuplara g\u00fcne\u015f \u0131\u015f\u0131nlar\u0131 y\u0131l boyunca e\u011fik a\u00e7\u0131 ile gelmekte ve buharla\u015fama ile atmosfere kar\u0131\u015fan nem miktar\u0131 az olmaktad\u0131r. Bundan dolay\u0131 da kutuplarda ya\u011f\u0131\u015f miktar\u0131 azd\u0131r. <\/p>\n
D\u00fcnyan\u0131n En Fazla Ya\u011f\u0131\u015f Alan B\u00f6lgeleri <\/p>\n
\u2022Ekvator \u00e7evresi
\n \u2022Muson iklim b\u00f6lgesi (d\u00fcnyan\u0131n en fazla ya\u011f\u0131\u015f alan merkezi bu iklim ku\u015fa\u011f\u0131nda \u00c7erapun\u00e7i\u2019dir. 12000 mm ya\u011f\u0131\u015f al\u0131r.)
\n \u2022Il\u0131man ku\u015fak karalar\u0131n\u0131n bat\u0131s\u0131
\n D\u00fcnyan\u0131n En Az Ya\u011f\u0131\u015f Alan B\u00f6lgeleri
\n \u2022D\u00f6nenceler \u00e7evresindeki \u00e7\u00f6l alanlar\u0131
\n \u2022Il\u0131man ku\u015fak kara i\u00e7lerinde etraf\u0131 da\u011flarla \u00e7evrili \u00e7ukur alanlar.
\n \u2022Kutup b\u00f6lgeleri (Kutuplarda ba\u011f\u0131l nem y\u00fcksek olmas\u0131na ra\u011fmen ya\u011f\u0131\u015f miktar\u0131 azd\u0131r. Sebebi: s\u0131cakl\u0131\u011f\u0131n d\u00fc\u015f\u00fck olmas\u0131ndan dolay\u0131 buharla\u015fman\u0131n ve mutlak nemin az olmas\u0131d\u0131r.<\/p>\n","protected":false},"excerpt":{"rendered":"
Nemlilik yer y\u00fcz\u00fcnde canl\u0131 hayat\u0131n\u0131n geli\u015fmesinde ve devam\u0131nda \u00e7ok \u00f6nemli bir unsurdur. Hava ve iklim \u015fartlar\u0131 bak\u0131m\u0131ndan da \u00e7ok \u00f6nemlidir. Her \u015feyden \u00f6nce ya\u011f\u0131\u015flar\u0131n kayna\u011f\u0131, havadaki su buhar\u0131d\u0131r. Su her s\u0131cakl\u0131kta buharla\u015f\u0131r. Bu sebeple atmosferde s\u00fcrekli bir miktar nem vard\u0131r. Buna atmosfer nemlili\u011fi denir. Nemlili\u011fi \u00f6l\u00e7en alete de higrometre denir. MUTLAK NEM Mutlak Nem: 1 …<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1403,1406],"tags":[3683,2796,3693,2887,10683,3691,11001,3687],"class_list":["post-5309","post","type-post","status-publish","format-standard","hentry","category-odevler","category-sosyal-bilgiler-odevleri","tag-alcak-basinc","tag-atmosfer","tag-bagil-nem","tag-ekvator","tag-fohn-ruzgari","tag-mutlak-nem","tag-mutlak-nemde-etkili-faktorler","tag-nemlilik"],"_links":{"self":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5309","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/comments?post=5309"}],"version-history":[{"count":0,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/posts\/5309\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/media?parent=5309"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/categories?post=5309"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.islamidavet.com\/kutuphane\/wp-json\/wp\/v2\/tags?post=5309"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}