Assessment of Snow Cover (NDSI) Variations in the Maroon River Basin during 2001–2022 and Their Influence on the River’s Hydrological Regime

Document Type : Original Article

Authors

Department of Meteorology, Faculty of Geographical Sciences, Yazd University, Yazd, Iran

10.22034/nawee.2025.556012.1175
Abstract
Objective: In mountainous regions of the Zagros, including the Maroon Basin in southwestern Iran, snow is the primary source of annual runoff. However, recent climatic changes, particularly rising temperatures and shifts in precipitation patterns, have altered the temporal and spatial distribution of snow accumulation and snowmelt. These changes have important implications for river hydrological regimes. Accordingly, this study investigates the temporal and spatial trends of snow cover and analyzes its relationship with Maroon River discharge over the period 2001–2022 to clarify the role of snow-cover changes in surface-flow dynamics.
Methods: River discharge data from the Idenak hydrometric station (upstream of Maroon Dam) were also used, and missing data were reconstructed using regression methods. To investigate the relationship between snow cover and river discharge, Pearson correlation analysis was performed for both simultaneous and lagged relationships. Since snowmelt in the Maroon Basin typically occurs from late winter to mid-spring, lag effects of up to two months were considered to capture delayed runoff responses associated with snowmelt. All analyses were conducted using ArcGIS, Excel, and SPSS software.
Results: The results showed a significant declining trend in snow cover during most months, particularly from January to March. Seasonal analysis also indicated a decreasing trend in snow-covered area during the snow season (October–May), with Z = −1.58 (p < 0.05). Sen’s slope estimates showed an average reduction of approximately 7.28 km² in snow-covered area per year during winter. Correlation analysis revealed the strongest positive relationship between NDSI and Maroon River discharge during the snowmelt period (March–May), both simultaneously and with time lags of one to two months, with correlation coefficients reaching 0.75.
Conclusions: The significant decline in snow cover and its strong correlation with river discharge, both simultaneously and with 1–2-month delays, indicate a reduction in snow persistence and earlier snowmelt in the Maroon Basin during the past two decades. These changes have altered the hydrological regime of the Maroon River.
This study, by combining long-term MODIS-based snow-cover trend analysis with simultaneous and lagged evaluation of the relationship between NDSI and river discharge at multiple temporal scales, provides a robust understanding of the dynamic relationship between snow-cover changes and surface-flow behavior in this critical basin.

Keywords


 
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