Date of Award

8-2025

Document Type

Thesis

Degree Name

Master of Science (MS)

College/School

College of Science and Mathematics

Department/Program

Earth and Environmental Studies

Thesis Sponsor/Dissertation Chair/Project Chair

Jorge Lorenzo-Trueba

Committee Member

Gregory Pope

Committee Member

Josh Galster

Abstract

Flood-tidal deltas are key sediment reservoirs that stabilize tidal inlets and adjacent shorelines, yet their function can be undermined by engineering interventions. We quantify the 1933-2024 evolution of the Barnegat Inlet system (New Jersey, USA) using geospatial mapping of landmass change, historical and modern bathymetry, and compiled dredging records. The system transitioned from net accretion through the early 1970s to persistent landmass loss thereafter, coinciding with intensified channel deepening and maintenance dredging. A mass-balance comparison shows that cumulative dredging volumes consistently exceed estimated delta losses, suggesting a reorganization of sediment pathways that bypass traditional deltaic sinks and promote interior shoaling. While tides, storms, and sea-level rise remain active drivers, their timing and magnitude do not account for post-1970s degradation trend. We infer that engineering activities are the primary driver of delta decline and the decoupling of barrier-lagoon sediment sharing feedbacks. These results underscore the need for adaptive sediment management, particularly strategic bypassing and placement, to sustain inlet-delta function and long-term coastal resilience in modified estuarine systems.

File Format

PDF

Available for download on Sunday, September 19, 2027

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