أخر تقارير    صدرت    زينة    شينة   بنفس الوقت
  السيء فيها أنه تأكد  تطور ظاهرة اللانينا
و الزين    ان  ظاهرة اللانينا  ستكون أضعف  من العام الماضي بالاضافة إلى إيجابية ثنائية قطب المحيط الهندي
التقرير الاول من  المركز الامريكي:
 La Niña conditions are expected to gradually strengthen and continue through the Northern Hemisphere winter 2011-12.
Currently, La Niña is not as strong  as it was in September 2010.  Roughly one- half of the models predict La  Niña to strengthen during the Northern Hemisphere fall and winter
Of these models, the majority predict a weak La Niña (3-month average in the Niño-3.4 region less than -0.9oC).  In  addition, a weaker second La Niña winter has occurred in three of the  five multi-year La Niñas in the historical SST record since 1950.
Thus, at this time, a weak or moderate strength La Niña is most likely during the Northern Hemisphere winter.
التقرير  الثاني من المركز الاسترالي:
Odds firm for a La Niña in 2011
 The continuing cooling trend in the central Pacific Ocean since early  winter is consistent with a developing La Niña event. For example,  temperatures below the surface of the tropical Pacific Ocean during  September are 4 °C cooler than  average in some areas. The majority of leading climate models predict  current patterns and trends will continue, with further cooling beyond  La Niña thresholds during the last quarter of 2011. 
   Atmospheric indicators are also trending towards typical La Niña values.  Trade winds have been persistently stronger than normal in the central  and western Pacific Ocean, and the Southern Oscillation Index (SOI) this  week reached the threshold value of +8. Sustained values at this level  are an indication of La Niña. 
   If a La Niña does form, current indicators are that it will be weaker  than the strong 2010-11 event. La Niña events raise the odds of above  average rainfall across the north and east of the country, but don't  guarantee it. The Bureau's National Climate Centre will monitor the  situation closely.  
   The latest observations from the Indian Ocean show a positive dipole  event, as predicted over the last few months by climate models,  including the Bureau's POAMA. Typically peaking in spring, and in  contrast to La Niña, a positive dipole event increases the odds of dry  conditions over southeastern and central Australia. In other words, this  is providing a degree of counter influence on rainfall to the La Niña  development in the Pacific. Sea surface temperatures surrounding  Australia’s north are also average to below average, and hence not as  favourable for rainfall as they were at this time in 2010.