Date of Award
Summer 1987
Document Type
Thesis
Degree Name
Master of Science (MS)
Department
Ocean & Earth Sciences
Program/Concentration
Oceanography
Committee Director
Larry P. Atkinson
Committee Member
Jackson O. Blanton
Committee Member
Lie-Yauw Oey
Call Number for Print
Special Collections LD4331.O35L68
Abstract
The stratification present on the South Atlantic Bight (SAB) during the summertime is influenced by creative forces, namely surface heating, precipitation, fresh water runoff and advection of Gulf Stream water, and destructive forces, these being wind, bottom currents, tides, evaporation and cooling. During the summer of 1981 the Georgia Bight Experiment II (GABEX II) was conducted to evaluate the Gulf Stream intrusions on the shelf dynamics. Calculations using potential energy as an indicator of stratification showed that the mixing forces were strong enough to destroy the stratification if the advection of buoyancy is ignored. During this period, however, the potential energy was actually increasing, indicating increasing stratification. Thus the advective buoyancy flux must be larger than all other sources of buoyancy and mixing. Therefore, the advection of buoyancy onto the SAB shelf must be considered as an important parameter when studying the shelf dynamics of this area during the summer.
Rights
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DOI
10.25777/vqzv-fy78
Recommended Citation
Lovingood, Rebecca L..
"Processes Which Create and Destroy Stratification in the South Atlantic Bight During GABEX II"
(1987). Master of Science (MS), Thesis, Ocean & Earth Sciences, Old Dominion University, DOI: 10.25777/vqzv-fy78
https://digitalcommons.odu.edu/oeas_etds/249