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Katherine A. Serafin

Researcher at University of Florida

Publications -  25
Citations -  714

Katherine A. Serafin is an academic researcher from University of Florida. The author has contributed to research in topics: Coastal hazards & Coastal flood. The author has an hindex of 12, co-authored 18 publications receiving 486 citations. Previous affiliations of Katherine A. Serafin include Stanford University & Oregon State University.

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Simulating extreme total water levels using a time-dependent, extreme value approach

TL;DR: In this paper, the authors present a total water level full simulation model (TWL-FSM) that simulates various components of TWLs (waves, tides, and nontidal residuals) in a Monte Carlo sense, taking into account conditional dependencies that exist between the various components.
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The relative contribution of waves, tides, and nontidal residuals to extreme total water levels on U.S. West Coast sandy beaches

TL;DR: In this article, the relative contribution of tides, waves, and nontidal residuals to extreme total water levels (TWLs) at the shoreline of U.S. West Coast sandy beaches was investigated.
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When floods hit the road: Resilience to flood-related traffic disruption in the San Francisco Bay Area and beyond

TL;DR: This work integrates a traffic model with flood maps that represent potential combinations of storm surges, tides, seasonal cycles, interannual anomalies driven by large-scale climate variability such as the El Niño Southern Oscillation, and sea level rise to show that metric reach, a measure of road network density, is a better proxy for delays than flood exposure.
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What's streamflow got to do with it? A probabilistic simulation of the competing oceanographic and fluvial processes driving extreme along-river water levels

TL;DR: In this article, the authors explored the variability of extreme water levels near the tribal community of LaPush, within the Quileute Indian Reservation on the Washington state coast, where a river signal is apparent in tide gauge measurements during high-discharge events.