Historical and projected changes in hydrological and sediment connectivity under climate change in a tropical catchment of Mexico

Hydrological and erosion dynamics are prone to change due to natural factors, human activities, or climate change. These changes are mainly related to modifications of land use and cover and can be assessed through the concept of connectivity, which analyzes how the spatial distribution of the elements facilitates runoff and sediment transport. The objective of this study was to evaluate changes in hydrological and sediment connectivity over 42 years and prqjected under a climate change scenario in the tropical Santa Cruz catchment in Aquismcin, S.I,.P., Mexico. The index of connectivity (IC) was computed using SedinConnect version 2.3 and the ArcSWAT model to estimate runoff. Hydrological connectivity and runoff were projected for 2027 using the MPI ECIIAM 5 in the A2 climate change scenario. The results indicated that spatio-temporal changes in land use/cover, in conjunction with geomorphological features and expected climate change, would modify hydrological and sediment connectivity, especially in flat areas, where conversion of natural vegetation to cropland was steadily increasing over the years. Under future conditions, runoff and sediment transport are likely to increase, which will impact soil erosion and vulnerability to flooding but will not necessarily be negative. The study shows how spatial-temporal integration of runoff, sediments, landforms, land use cover and change, and connectivity can improve our understanding of catchment dynamics and the importance of analyses that characterize their evolution. The results can subsequently be applied and replicated in other catchments for management and restoration purposes.

Automated summary

This study evaluated the changes in hydrological and sediment connectivity in the Santa Cruz catchment in Mexico over a period of 42 years and projected these changes under a climate change scenario. The results showed that changes in land use/cover and expected climate change would modify hydrological and sediment connectivity. Under future conditions, there is likely to be an increase in runoff and sediment transport, which will impact soil erosion and vulnerability to flooding.