## 3 Results and Discussion  
### Variations in Climatic Conditions  
A comprehensive overview of climatic parameters across different locations (S1 to S20) in the study area during the months of June, July, and August 2022 is presented in Table 1. Most locations show a noticeable increase in humidity from June to August. For example,at S1, humidity rises from 3589 g km\({}^{-3}\) in June to 5073 g km\({}^{-3}\) in August. Some locations, like S6 and S7, exhibit exceptionally high humidity levels, particularly in July and August, suggesting that these areas might be more prone to moisture retention or may have more vegetation or water bodies influencing local humidity.  
Across the locations, wind speeds are relatively consistent, with most locations averaging between 2.8 and 3.4 s m\({}^{-1}\). There is a slight decline in wind speed from June to August at several locations, such as S1, where it drops from 3.1 s m\({}^{-1}\) in June to 2.5 s m\({}^{-1}\) in August. This stability in wind speed is important for understanding soil erosion dynamics, as consistent wind conditions can lead to predictable patterns of dust deposition and erosion. June generally has the highest solar radiation across most locations. For instance, S1 records 24,061 KJ M\({}^{-1}\) in June, decreasing to 21,242 KJ M\({}^{-1}\) in July. There is a gradual decline in solar radiation from June to July across almost all locations, which might be due to seasonal changes, such as increased cloud cover or the sun's position during the summer months. The results of our study align with previous findings, such as those documented in [41]. Seasonal variables, such as increased cloud cover or the sun's shifting position throughout the summer, which affects the intensity of solar energy reaching the surface, are probably to blame for this drop in solar radiation. The parallels between our findings and those reported in [41] support the validity of these trends and imply that the conclusions may be applied more broadly to areas with comparable climates. These insights are critical for agricultural and environmental planning that depends on seasonal patterns of solar radiation, as well as for improving solar energy harvesting.  
Precipitation levels vary widely across the locations. Some locations, such as S1, experience very low precipitation in June (0.7 mm) and July (0.1 mm), followed by a significant increase in August (5.2 mm). Generally, August sees the highest levels of precipitation, with several locations recording more than 5 mm, indicating that this month is critical for moisture accumulation in the soil, which could mitigate some wind erosion effects. The data indicate a strong interplay between humidity, wind speed, solar radiation, and precipitation across the different locations. The increase in humidity and precipitation toward August might contribute to a reduction in dust emission and soil erosion. The steady wind speeds and high solar radiation in June are likely to exacerbate dust deposition, especially in drier and less vegetated areas. Understanding these trends is crucial for environmental management and for developing strategies to mitigate soil losses due to wind erosion in the context of climate change.  
\begin{table}
\begin{tabular}{c c c c c c c c c c c c c c c c c} \hline \hline  & \multicolumn{3}{c}{**Height from**} & \multicolumn{3}{c}{**Average Humidity**} & \multicolumn{3}{c}{**Average Wind Speed**} & \multicolumn{3}{c}{**Average Solar Radiation**} & \multicolumn{3}{c}{**Average Precipitation**} & \multicolumn{3}{c}{**Temperature**} \\
**Location** & \multic