Comparison of Extreme Coastal Flooding Events between Tropical and Midlatitude Weather Systems in the Delaware and Chesapeake Bays for 1980–2019

• Published in: Journal of applied meteorology and climatology Vol. 61; no. 4; pp. 457 - 472
• Main Authors: Callahan, John A., Leathers, Daniel J., Callahan, Christina L.
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01.04.2022
• Subjects: Atmospheric conditions; Bays; Climate change; Coastal flooding; Coastal storms; Coastal waters; Cold season; Cyclones; Dynamic height; Easterlies; Flooding; Floods; Gauges; Geopotential; Geopotential height; High pressure; Hurricanes; Latitude; Long-term planning; Low pressure; Mean sea level; Pressure; Public awareness; Ridges; Sea level; Sea level changes; Sea level pressure; Sea level rise; Storm surges; Storms; Surge response; Tidal cycles; Tide gauges; Tides; Tropical atmosphere; Tropical climate; Tropical cyclones; Upper level divergence; Weather; Winds; Delaware; United States > US
• ISSN: 1558-8424; 1558-8432
• DOI: 10.1175/JAMC-D-21-0077.1

Abstract Coastal flooding is one of the most costly and deadly natural hazards facing the U.S. mid-Atlantic region today. Impacts in this heavily populated and economically significant region are caused by a combination of the location’s exposure and natural forcing from storms and sea level rise. Tropical cyclones (TCs) and midlatitude (ML) weather systems each have caused extreme coastal flooding in the region. Skew surge was computed over each tidal cycle for the past 40 years (1980–2019) at several tide gauges in the Delaware and Chesapeake Bays to compare the meteorological component of surge for each weather type. Although TCs cause higher mean surges, ML weather systems can produce surges just as severe and occur much more frequently, peaking in the cold season (November–March). Of the top 10 largest surge events, TCs account for 30%–45% in the Delaware and upper Chesapeake Bays and 40%–45% in the lower Chesapeake Bay. This percentage drops to 10%–15% for larger numbers of events in all regions. Mean sea level pressure and 500-hPa geopotential height (GPH) fields of the top 10 surge events from ML weather systems show a low pressure center west-southwest of “Delmarva” and a semistationary high pressure center to the northeast prior to maximum surge, producing strong easterly winds. Low pressure centers intensify under upper-level divergence as they travel eastward, and the high pressure centers are near the GPH ridges. During lower-bay events, the low pressure centers develop farther south, intensifying over warmer coastal waters, with a south-shifted GPH pattern relative to upper-bay events. Significance Statement Severe coastal flooding is a year-round threat in the U.S. mid-Atlantic region, and impacts are projected to increase in magnitude and frequency. Research into the meteorological contribution to storm surge, separate from mean sea level and tidal phase, will increase the scientific understanding and monitoring of changing atmospheric conditions. Tropical cyclones and midlatitude weather systems both significantly impact the mid-Atlantic region during different times of year. However, climate change may alter the future behavior of these systems differently. Understanding the synoptic environment and quantifying the surge response and subbay geographic variability of each weather system in this region will aid in public awareness, near-term emergency preparation, and long-term planning for coastal storms.