Synoptic analysis of the Lifting condensation level and its effect on Iraq's weather

Abstract

Monitoring stations in Iraq witnessed spatial and temporal variations in the level of condensation, resulting in different condensation patterns. This level determines the type of precipitation and the different condensation patterns through its direct influence on temperature and dew point, which, along with the saturation limit, mark the beginning of the transformation of vapor into an acidic state and its condensation around condensation nuclei.

This research highlights the impact of varying cloud topography levels on Iraq's weather. A study of several comprehensive weather patterns revealed a strong correlation between cloud topography and surface weather elements. It found that low cloud topography levels are directly related to weather phenomena such as frost and fog. Furthermore, a low cloud topography means a lower cloud base, allowing rain to reach the ground completely without evaporation. Conversely, high cloud topography leads to the formation of high-altitude clouds with low moisture content, which in turn affects the amount of rainfall.

Two comprehensive cases were studied regarding the variation in the level of updraft condensation and its effect on the weather in Iraq. The first case was its effect on rainfall, and the second was its effect on frost formation. The level of updraft condensation recorded a significant decrease in its height in the second case, causing widespread frost formation in Iraq, while its height was moderate in the rainy case.