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Path analysis of the effect of climatic elements on wind speed and desertification progress in Central Iran

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Abstract

Negative changes in the activity of climatic factors lead to vulnerabilities in natural systems and challenging environmental changes. Wind as a geological factor is considered a common phenomenon in arid desert regions. Persistent erosive winds lead to wind erosion and enhance the desertification process. The present study aimed to analyze the path of climate changes on the desertification progress of arid regions. The trend of climate changes was studied using the Mann–Kendall and Sen's Estimator non-parametric tests over a 20-year study period (2000–2019) in a part of central Iran and a significant trend was found in climate changes (ρ < 0.01 & 0.05). Vegetation changes were assessed using the Normalized Vegetation Difference Index (NDVI). The relationship between climatic factors and vegetation changes based on the Spearman test was significant (ρ < 0.01 & 0.05). The effect of climatic factors such as precipitation, temperature, and relative humidity on the maximum wind speed in the region was studied through the path analysis method. The results indicated that the latent variables of temperature and relative humidity significantly affected the maximum wind speed (ρ < 0.01). Overall, our findings provide insights for using the path analysis model as a useful mechanism to determine the contribution of factors affecting wind erosion and desertification spread.

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Notes

  1. https://app.climateengine.org/climateEngine (Access date to the data: 09 Jul 2021)

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All authors whose names appear on the submission made substantial contributions to the acquisition, analysis, and interpretation of data.

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Correspondence to Mehran Fatemi.

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This study did not involve human participants.

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Responsible Editor: Zhihua Zhang

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Fatemi, M., Jebali, A. Path analysis of the effect of climatic elements on wind speed and desertification progress in Central Iran. Arab J Geosci 15, 930 (2022). https://doi.org/10.1007/s12517-022-10064-y

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  • DOI: https://doi.org/10.1007/s12517-022-10064-y

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