Wind and tide effects on the Choctawhatchee Bay plume and implications for surface transport at Destin Inlet

被引:5
作者
Cyriac, R. [1 ,2 ]
Dietrich, J. C. [1 ]
Blain, C. A. [3 ]
Dawson, C. N. [4 ]
Dresback, K. M. [6 ]
Fathi, A. [4 ,5 ]
Bilskie, M., V [7 ]
Graber, H. C. [9 ]
Hagen, S. C. [7 ,8 ]
Kolar, R. L. [6 ]
机构
[1] North Carolina State, Dept Civil Construct & Environm Engn, Campus Box 7908,2501 Stinson Dr, Raleigh, NC 27695 USA
[2] Atkins, 1616 E Milbrook St, Raleigh, NC 27609 USA
[3] Naval Res Lab, Oceanog Div, Stennis Space Ctr, MS 39529 USA
[4] Univ Texas Austin, Oden Inst Computat Engn & Sci, Austin, TX 78712 USA
[5] ExxonMobil Res & Engn Co, Corp Strateg Res, 1545 Route 22 East, Annandale, NJ 08801 USA
[6] Univ Oklahoma, Sch Civil Engn & Environm Sci, 202 W Boyd St, Norman, OK 73019 USA
[7] Louisiana State Univ, Ctr Coastal Resiliency, 124 C Sea Grant Hall, Baton Rouge, LA 70803 USA
[8] Louisiana State Univ, Dept Civil & Environm Engn, 3255 Patrick F Taylor Hall, Baton Rouge, LA 70803 USA
[9] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Dept Ocean Sci, 4600 Rickenbacker Causeway, Miami, FL 33149 USA
基金
美国国家科学基金会;
关键词
ADCIRC; Plume dynamics; Cold fronts; Florida Panhandle; SCOPE; CARTHE; HURRICANE STORM-SURGE; RIVER PLUME; OUTFLOW PLUME; ESTUARINE-PLUME; BUOYANT PLUME; MODEL; OCEAN; GULF; VALIDATION; SYSTEM;
D O I
10.1016/j.rsma.2020.101131
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Multiple river-dominated estuaries line the northern Gulf coast and introduce substantial density variations. Their plumes have been shown to be highly sensitive to wind and tide effects, but in studies with limited observations and idealized wind forcing. This study explores these effects with a dynamic model that can represent the full behavior from river through estuary to shelf, and for a period with extensive observations. The inner shelf adjacent to Choctawhatchee Bay, a micro tidal estuary situated along the Florida Panhandle, is subject to buoyant, brackish outflows during the ebb-phase of the tidal cycle. In December 2013, experiments were performed in this region to study mechanisms that influence near-shore surface transport. Satellite imagery showed a visible brackish surface plume at Destin during low tide. The goal of the present study is to quantify variability in the plume signature due to changes in tidal and wind forcing. Density-driven flows near Destin Inlet are modeled with the recently-enhanced, three-dimensional, baroclinic capabilities of the ADvanced CIRCulation (ADCIRC) model. Modeled tides, salinities and plume signature are validated against in-situ observations and satellite imagery. Model results reveal substantial changes in the length, width and orientation of the plume as the wind direction varied on consecutive days due to winter cold fronts. During a period of near-constant winds and variability in tidal amplitude, the model predicted a larger plume during spring tides than during neap conditions. Coriolis effects on the plume are minimized due to its small scale nature. Therefore, when the wind forcing is weak, the plume signature spreads radially from the inlet with slight preference to the down-shelf. The Choctawhatchee Bay plume is representative of other small-scale plumes formed in river-dominated and micro-tidal environments, and this work demonstrates the sensitivity of these plumes to changing environmental conditions. (C) 2020 Elsevier B.V. All rights reserved.
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页数:18
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