American Research Journal of Agriculture

Mammadov Asgar Samed, Сalalova Vafa Yashar 

The initial stage of the drought usually begins with low-activity high anticyclones and is followed by continuous (several weeks to 2-3 months) high temperatures and low rainfalls. As a result, the soil moisture reserve decreases, the high temperature gradually decreases in humidity, increase potential evaporation, and the threat to agricultural crops increases. The long-timedroughts (several years) even lead to the migration of the population. In this regard, it is undeniable that the role of the Azores and Siberian maximums in the activation of hydrometeorological anomalies in Azerbaijan has recently increased