Date of Award

Summer 2025

Access Type

Thesis - Open Access

Degree Name

Master of Science in Civil Engineering

Department

Civil Engineering

Committee Chair

Stephen C. Medeiros

Committee Chair Email

medeiros@erau.edu

First Committee Member

Jeff R. Brown

First Committee Member Email

browj112@erau.edu

Second Committee Member

Siddharth Parida

Second Committee Member Email

paridas@erau.edu

College Dean

James W. Gregory

Abstract

Floodplain dynamics are often complex, with hysteresis potentially affecting the temporal relationship between flood stage and flood extent during subsequent inundation phases. This study leverages Sentinel-1 synthetic aperture radar (SAR) imagery to map flood extent in the Middle St. Johns River Lake floodplains and examine the presence of hysteresis during flood events. SAR scenes corresponding to river gauge readings were analyzed from the rising and falling limbs of a flood hydrograph. By comparing these flood maps, we assess differences in inundated areas at equivalent water levels during each stage of the flood event. The findings aim to enhance flood monitoring systems by improving flood extent mapping throughout changing water levels, which is crucial for accurate flood forecasting and effective response planning. Our results indicate that hysteresis in this region is primarily governed by topography and channel connectivity, where the floodplain geomorphology and tributary drainage to lakes lead to acceleration in drainage from the floodplain to the lake during the falling limb when comparing inundation extent to the rising limb at similar water levels. Among the three floodplains studied, Lake Jesup displayed the largest range of degrees of hysteresis (-0.03 to 0.32), followed by Lake Monroe (0.03 to 0.25) and Lake Harney (0.02 to 0.22). The differing ranges of degrees of hysteresis are attributed to unique lake-river connectivity and floodplain topography.

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