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CONTRIBUTING FACTORS TO DROUGHT IN TURKEY<strong>Click</strong> <strong>to</strong> <strong>edit</strong> <strong>Master</strong> <strong>title</strong> <strong>style</strong> low rainfall and untimely rainfall some links <strong>to</strong> the regional circulation patterns• <strong>Click</strong> - NAO<strong>to</strong> <strong>edit</strong> <strong>Master</strong> text <strong>style</strong>s- ENSO• Second level Weakening of Siberia Anticyclone (winter droughts) • Penetration Third level of Azor Anticyclone ridge in<strong>to</strong> Eastern M<strong>edit</strong>erranen Decrease in intensity and frequency of frontal systems• Fourth leveloriginating from Atlantic • Penetration Fifth level of Basra low pressure systems further in<strong>to</strong> north(summer droughts) Strengtening of Basra low pressure systems (summer droughts)WMODrought and Desertification Workshop, Alanya, 14-16 November 200617TSMS
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