11 General Geomorphology
Tuesday, 15 March 2022
8:30 AM - 12:30 PM
Online
A PROPOSED MECHANISTIC MODEL FOR CLIMATE EFFECTS OF LOBE SHIFTS IN THE MISSISSIPPI RIVER DELTA
Paper number: 11-4
Program: Theme Sessions
Time: 9:20 AM – 9:40 AM
Authors
Abstract
However, altering the direction of the river input can be expected to alter the smaller gyres within the Gulf, which in turn can affect the path of the through-flow from the western Caribbean (the real source of Florida current heat) to the Florida Strait. If so, an eastward river input could decrease the amplitude of the northern meander of the current, thereby speeding the drainage of warm water from the western Caribbean and reducing the heat buildup in that source area. Conversely, a western river input could enhance the amplitude of the northern meander of the Caribbean-Florida Strait current, thereby slowing the drainage and allowing a greater buildup of heat in the source area. If this connection is real, we could postulate a potential climate response to the increasing diversions of Mississippi River water into the Atchafalaya basin.
Geological Society of America Abstracts with Programs. Vol. 54, No. 1
doi: 10.1130/abs/2022SC-373700
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