mehmet civan tarafından yazılan gönderiler

    850 de -8 karadeniz uzerinden inerken deniz suyu ile arasinda ki fark -12 -14 gibi olmuyor tabi konvektivite. ama burada 500 hpa temp cekirdegi .<-45

    1015 izobarida 1000km ler olusuyor 80-100 km lik bir tasinimda (fetch) kar yagisi 160 kmn sonrasi onemli miktarda kar yagisi demek. 1040 yb ne varsa indiriyor. cok kar yagar. :coksoguk:

    karasizlik yuksek oldugu icin modeller in sapma payi biraz yuksek bu donemde,

    Tam olarak Samsun’un 0.6 yazan yerindeyim neden bu sene modellerde Orta Karadeniz sahil bandına kar düşmüyor sebebi nedir ?

    ab nin tam merkezinde kaliyorsun. o degisir her guncellemede. Selam

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    312H cepheye bak hey maşallah

    500 de akimin yonu yildiz-poryaz soguk cekirdegin tam merkezinden en soguk patansiyeli uzerimize tasiyor. dek destekli.

    zaten cephe girisinde konvektif bulut tabani direk coker yeryuzune gorus mesafesi kisalir. cephe sonrasi bulut tavan noksida yukseliyor. merkezin cekirdegi extrem oldugu icin kalinligindan ziyade yogun bir bulut tabakasi olusur. bu tarz bir kac cephe sistemi hatirliyorum. yagisin kar donmesiyle kisa zamanda tipiye donuyor.

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    108 h da soguk cekirdek -45 in altina indi bu extrem b ir durum

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    96 da soguk cekirdek inisine devam ediyor. anadoluda yuksek basinc hakim yagis yok

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    84 h da 500hpa da finlandiya ustunden uzanan -42 lik cekirdek goruluyor bu tum yurtta kar yagislarina sebep olabilecek potasiyelde bir soguk hava dalgasi

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    1005 mb akdeniz ab dogu yonunde hareketiyle anadolunun batisinda 1020mb basinc hakim yagis yok. bati ve orta karadeniz guney dogu anadolu yoguin kar yagislari aliyor. orta anadolu kismen

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    60 h da kuzeyimizde 995 mb guneyimizde 1005mb ab leri net bir sekilde goruyoruz.

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