the trend of the siberian high pressure and its impacts on the meteorological fields during 1948-2008

نویسندگان

معصومه احمدی حجت

دانشجوی دکتری هواشناسی، گروه هواشناسی، دانشگاه آزاد اسلامی، واحد علوم و تحقیقات، تهران، ایران فرهنگ احمدی گیوی

دانشیار، گروه فیزیک فضا، موسسه ژئوفیزیک دانشگاه تهران، ایران سهراب حجام

دانشیار، گروه هواشناسی، دانشگاه آزاد اسلامی، واحد علوم و تحقیقات، تهران، ایران

چکیده

one of the most important atmospheric systems in the eurasian continent during the northern hemisphere winter season is the siberian high pressure. in this study, using the ncep/ncar reanalysis data for winters of 1948-2008, trend of changes in the intensity of the high system center and its effects on some meteorological fields are investigated. the results show that the 2m height mean temperature in central siberian high region were -17.7 °c during the study period and the mean sea level pressure (mslp) were over 1030hpa. the mslp had a minor linear positive trend of 1.10hpa/dec (hpa per decade) at the beginning of the 60-years period. also, a weak negative linear trend of -0.12hpa/dec occurs in early 1970s. there is a meaningful correlation (-0.46) between the mean temperature averaged on influence area of the central siberian high and the siberian high index (shi) during the study period, as in most cases enhancement (weakening) of the high center accompanied with cooling (warming) in the region. calculations indicate a trend of 0.13 °c/dec warming for the area. the results show that the pressure gradient causes strong north monsoonal currents and thus cold advection toward far-east or east-asia winter monsoon. calculated correlation coefficients between the shi and some meteorology fields indicate that the enhanced siberian high provides suitable conditions for cyclogenesis over the mediterranean sea and development of warm advection from north africa to east mediterranean and then to north europe. another result indicates that when anti-cyclones over the siberia form and develop, they act as a barrier to eastward movement of the extra-tropical cyclones. this leads the systems to move to higher latitudes and thus fewer cyclonic system pass from the siberia and this reduce warm advection over the siberia.       furthermore, calculated tele-connection correlations show that the system affects atmospheric variables beyond its established region. enhancement of pressure in the system normally leads to a strong pressure gradient between east siberian high and west aleutian high. correlation coefficients between the shi and some meteorological fields in the extra-tropical regions of the north hemisphere indicate that the siberian high could exert impacts on meteorology fields beyond its source region. examples include a strong relationship between the shi and the east asian winter monsoon, enhancement of the suitable conditions for cyclogenesis over the mediterranean sea and warm advection intensification in north africa toward the east mediterranean sea and north europe. beyond these features, there is intensification of the subtropical jet over the east asia and the eastern mediterranean sea as well as the existence of a wave train in the form of positive and negative correlation coefficients between the shi and the geopotential height (gph) field in middle and upper troposphere. these findings suggest that the siberian high should not be considered simply as a local low-level phenomenon, and it exerts significant impacts on middle and upper-level circulations.

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عنوان ژورنال:
فیزیک زمین و فضا

جلد ۳۹، شماره ۲، صفحات ۱۲۷-۱۳۸

کلمات کلیدی
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c ( h p a p e r d e c a d e ) a t t h e b e g i n n i n g o f t h e 6 0 ' , ' y e a r s p e r i o d . a l s o ' , ' a w e a k n e g a t i v e l i n e a r t r e n d o f ' , ' 0 . 1 2 h p a / d e c o c c u r s i n e a r l y 1 9 7 0 s . t h e r e i s a m e a n i n g f u l c o r r e l a t i o n ( ' , ' 0 . 4 6 ) b e t w e e n t h e m e a n t e m p e r a t u r e a v e r a g e d o n i n f l u e n c e a r e a o f t h e c e n t r a l s i b e r i a n h i g h a n d t h e s i b e r i a n h i g h i n d e x ( s h i ) d u r i n g t h e s t u d y p e r i o d ' , ' a s i n m o s t c a s e s e n h a n c e m e n t ( w e a k e n i n g ) o f t h e h i g h c e n t e r a c c o m p a n i e d w i t h c o o l i n g ( w a r m i n g ) i n t h e r e g i o n . c a l c u l a t i o n s i n d i c a t e a t r e n d o f 0 . 1 3 ° c / d e c w a r m i n g f o r t h e a r e a . t h e r e s u l t s s h o w t h a t t h e p r e s s u r e g r a d i e n t c a u s e s s t r o n g n o r t h m o n s o o n a l c u r r e n t s a n d t h u s c o l d a d v e c t i o n t o w a r d f a r ' , ' e a s t o r e a s t ' , ' a s i a w i n t e r m o n s o o n . c a l c u l a t e d c o r r e l a t i o n c o e f f i c i e n t s b e t w e e n t h e s h i a n d s o m e m e t e o r o l o g y f i e l d s i n d i c a t e t h a t t h e e n h a n c e d s i b e r i a n h i g h p r o v i d e s s u i t a b l e c o n d i t i o n s f o r c y c l o g e n e s i s o v e r t h e m e d i t e r r a n e a n s e a a n d d e v e l o p m e n t o f w a r m a d v e c t i o n f r o m n o r t h a f r i c a t o e a s t m e d i t e r r a n e a n a n d t h e n t o n o r t h e u r o p e . a n o t h e r r e s u l t i n d i c a t e s t h a t w h e n a n t i ' , ' c y c l o n e s o v e r t h e s i b e r i a f o r m a n d d e v e l o p ' , ' t h e y a c t a s a b a r r i e r t o e a s t w a r d m o v e m e n t o f t h e e x t r a ' , ' t r o p i c a l c y c l o n e s . t h i s l e a d s t h e s y s t e m s t o m o v e t o h i g h e r l a t i t u d e s a n d t h u s f e w e r c y c l o n i c s y s t e m p a s s f r o m t h e s i b e r i a a n d t h i s r e d u c e w a r m a d v e c t i o n o v e r t h e s i b e r i a . x a 0 x a 0 x a 0 x a 0 r n x a 0 f u r t h e r m o r e ' , ' c a l c u l a t e d t e l e ' , ' c o n n e c t i o n c o r r e l a t i o n s s h o w t h a t t h e s y s t e m a f f e c t s a t m o s p h e r i c v a r i a b l e s b e y o n d i t s e s t a b l i s h e d r e g i o n . e n h a n c e m e n t o f p r e s s u r e i n t h e s y s t e m n o r m a l l y l e a d s t o a s t r o n g p r e s s u r e g r a d i e n t b e t w e e n e a s t s i b e r i a n h i g h a n d w e s t a l e u t i a n h i g h . r n c o r r e l a t i o n c o e f f i c i e n t s b e t w e e n t h e s h i a n d s o m e m e t e o r o l o g i c a l f i e l d s i n t h e e x t r a ' , ' t r o p i c a l r e g i o n s o f t h e n o r t h h e m i s p h e r e i n d i c a t e t h a t t h e s i b e r i a n h i g h c o u l d e x e r t i m p a c t s o n m e t e o r o l o g y f i e l d s b e y o n d i t s s o u r c e r e g i o n . e x a m p l e s i n c l u d e a s t r o n g r e l a t i o n s h i p b e t w e e n t h e s h i a n d t h e e a s t a s i a n w i n t e r m o n s o o n ' , ' e n h a n c e m e n t o f t h e s u i t a b l e c o n d i t i o n s f o r c y c l o g e n e s i s o v e r t h e m e d i t e r r a n e a n s e a a n d w a r m a d v e c t i o n i n t e n s i f i c a t i o n i n n o r t h a f r i c a t o w a r d t h e e a s t m e d i t e r r a n e a n s e a a n d n o r t h e u r o p e . b e y o n d t h e s e f e a t u r e s ' , ' t h e r e i s i n t e n s i f i c a t i o n o f t h e s u b t r o p i c a l j e t o v e r t h e e a s t a s i a a n d t h e e a s t e r n m e d i t e r r a n e a n s e a a s w e l l a s t h e e x i s t e n c e o f a w a v e t r a i n i n t h e f o r m o f p o s i t i v e a n d n e g a t i v e c o r r e l a t i o n c o e f f i c i e n t s b e t w e e n t h e s h i a n d t h e g e o p o t e n t i a l h e i g h t ( g p h ) f i e l d i n m i d d l e a n d u p p e r t r o p o s p h e r e . t h e s e f i n d i n g s s u g g e s t t h a t t h e s i b e r i a n h i g h s h o u l d n o t b e c o n s i d e r e d s i m p l y a s a l o c a l l o w ' , ' l e v e l p h e n o m e n o n ' , ' a n d i t e x e r t s s i g n i f i c a n t i m p a c t s o n m i d d l e a n d u p p e r ' , ' l e v e l c i r c u l a t i o n s . 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