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The polar front arises as a result of cold polar air meeting warm tropical air. It is a stationary front as the air masses are not moving against each other and stays stable.[2] North America , especially in winter , there is a sharp temperature gradient between the snow-covered land and the warm offshore currents.
The polar front theory says that mid-latitude extratropical cyclones form on boundaries between warm and cold air.[3] Equator , whereas high pressure systems dominate more in the summer .
See also [ edit ]
References [ edit ]
^ "Temperate Cyclones (Mid Latitude Cyclone or Extra tropical cyclones or Frontal Cyclones)" . PMF IAS . 2016-01-06. Retrieved 2022-05-22 .
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R e t r i e v e d f r o m " https://en.wikipedia.org/w/index.php?title=Polar_front&oldid=1187591099 " C a t e g o r i e s : ● A t m o s p h e r i c d y n a m i c s ● W e a t h e r f r o n t s ● M e t e o r o l o g y s t u b s H i d d e n c a t e g o r i e s : ● A r t i c l e s n e e d i n g a d d i t i o n a l r e f e r e n c e s f r o m M a r c h 2 0 2 2 ● A l l a r t i c l e s n e e d i n g a d d i t i o n a l r e f e r e n c e s ● A r t i c l e s w i t h G N D i d e n t i f i e r s ● A l l s t u b a r t i c l e s
● T h i s p a g e w a s l a s t e d i t e d o n 3 0 N o v e m b e r 2 0 2 3 , a t 0 5 : 1 4 ( U T C ) . ● T e x t i s a v a i l a b l e u n d e r t h e C r e a t i v e C o m m o n s A t t r i b u t i o n - S h a r e A l i k e L i c e n s e 4 . 0 ;
a d d i t i o n a l t e r m s m a y a p p l y . B y u s i n g t h i s s i t e , y o u a g r e e t o t h e T e r m s o f U s e a n d P r i v a c y P o l i c y . W i k i p e d i a ® i s a r e g i s t e r e d t r a d e m a r k o f t h e W i k i m e d i a F o u n d a t i o n , I n c . , a n o n - p r o f i t o r g a n i z a t i o n . ● P r i v a c y p o l i c y ● A b o u t W i k i p e d i a ● D i s c l a i m e r s ● C o n t a c t W i k i p e d i a ● C o d e o f C o n d u c t ● D e v e l o p e r s ● S t a t i s t i c s ● C o o k i e s t a t e m e n t ● M o b i l e v i e w
