Abstract

San Diego, one of the largest ports on the U.S. West Coast and home to the largest U.S. Navy base, is exposed to various local and distant tsunami sources. During the first half of the twentieth century, extensive modifications to the port included but were not limited to dredging, expansion of land near the airport and previous tidal flats, as well as creation of jetties. Using historical nautical charts and available Digital Elevation Models, this study gives an overview of changes to San Diego harbor in the last 150+ years due to human intervention and examines the effects of these changes on tsunamis. Two distant and two local scenarios were selected to demonstrate the impact of modified nearshore topography and bathymetry to incoming tsunamis. Inundation pattern, flow depths, and flooded localities vary greatly from year to year in the four scenarios. Specifically, flooded areas shift from the inner harbor to outer locations. Currents induced by the distant tsunamis intensify with modifications and shift from locations primarily outside the harbor to locations inside. A new characteristic in tsunami dynamics associated with port modifications is the introduction of high current spots. Numerical results also show that the introduction of high currents could threaten navigation, vessels, and facilities at narrow openings and also along the harbor “throat”—therefore, at an increased number of locations. Modifications in the port show that changes could have a negative but also a positive impact through constraint of flooding outside of the harbor and shifting of high currents to locations of minimal impact. The results of this study may be used as a first step toward future harbor design plans to reduce tsunami damages.

Highlights

  • Harbor modifications and redevelopment plansare quite common to enhance or increase space in ports and, to improve operations

  • In order to understand how anthropogenic changes to ports affect tsunamis, we studied the time evolution of man-made modifications in San Diego Bay since the late nineteenth century and its influence on tsunami amplitudes and currents

  • We present nautical charts that portray the changes that have occurred in San Diego Bay since the nineteenth century

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Summary

Introduction

Harbor modifications and redevelopment plans (see current plans for the Port of San Diego in [1]). In order to understand how anthropogenic changes to ports affect tsunamis, we studied the time evolution of man-made modifications in San Diego Bay since the late nineteenth century and its influence on tsunami amplitudes and currents. Post-1945, the bay continued to undergo changes but maintained a similar appearance and, the bathymetry/topography in and around the bay is represented by a Digital Elevation Model (DEM) showing the harbor shape as we know it today (dated 2014). To reflect these changes, historical nautical charts were used to show the state of the bay during that period

San Diego Bay
Time Evolution of San Diego Bay
Pre-Nineteenth Century to 1895
Post-1895 and Early Twentieth Century
Numerical Grids of San Diego
Numerical Modeling
Tsunami Sources
Chile 1960
Tohoku 2011
Coronado Canyon Landslide
San Clemente Fault—Bend Region

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