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This study analyzes the hydroclimatology of the Mississippi River Basin (MRB) using water balance components from 1901 to 2014, identifying nine subregions with distinct runoff characteristics. Approximately 79% of MRB runoff is generated by four subregions, primarily from surplus water during winter and spring months, influenced by atmospheric pressure anomalies. The findings provide a baseline for future research on MRB hydroclimatic variability and trends.

Author

nabakishorg

Language

EN