GSA Annual Meeting in Seattle, Washington, USA - 2017

Paper No. 193-3
Presentation Time: 8:50 AM

HIGH TEMPORAL RESOLUTION MODELING OF THE IMPACT OF RAIN, TIDES, AND SEA LEVEL RISE ON WATER TABLE FLOODING IN THE ARCH CREEK BASIN, MIAMI-DADE COUNTY FLORIDA USA


SUKOP, Michael C., Department of Earth and Environment, Florida International University, University Park, MIAMI, FL 33199, ROGERS, Martina, Broward College, DAVIE, FL 33314, GAUNEL, Greg, St Thomas, FL 00802-6004; University of the Virgin Islands, St Thomas, 00802-6004, Virgin Islands (U.S.), INFANTI, Johnna, University of Miami, Rosenstiel School of Marine and Atmospheric Science, 4600 Rickenbacker Causeway, MIAMI, FL 33149-1031 and HAGEMANN, Katherine, Regulatory and Economic Resources Department, Miami-Dade County, MIAMI, FL 33128, sukopm@fiu.edu

Modeling of groundwater levels in a portion of the low-lying coastal Arch Creek basin in northern Miami-Dade County in Southeast Florida USA, which is subject to repetitive flooding, reveals that rain-induced short-term water table rises can be viewed as the primary driver of flooding events under current conditions. Areas below 3 feet North American Vertical Datum (NAVD) elevation are particularly vulnerable and areas below 5 feet NAVD are vulnerable to exceptionally large rainfall events. Long-term water table rise is evident in the groundwater data, and the rate appears to be consistent with local rates of sea level rise. Linear extrapolation of long-term observed groundwater levels to 2060 suggest roughly a doubling of the number of days when groundwater levels exceed 3 feet NAVD and a threefold increase in the number of days when levels exceed 5 feet NAVD. Projected sea level rise of 2 feet by 2060 together with increased rainfall lead to a model prediction of frequent groundwater-related flooding in areas less than 3 feet NAVD. But current simulations do not consider the range of rainfall events that have led to water table elevations greater than 5 feet NAVD and widespread flooding of the area in the past. Tidal fluctuations in the water table are predicted to be most pronounced within 2000 feet of a tidally influenced water control structure that is hydrodynamically connected to Biscayne Bay. The inland influence of tidal fluctuations appears to increase with increased sea level, but the principal driver of high groundwater levels under the 2060 scenario conditions remains groundwater recharge due to rainfall events. Similar analysis and modeling can help to elucidate the mechanisms of flooding and the importance of tidal, storm surge, and long-term sea level changes in low-lying coastal areas globally and contribute to related science, engineering, social, and policy questions.