EVOLUTION OF AN ISOLATED TURBULENT REGION IN A STRATIFIED FLUID

Citation
Sv. Fonseka et al., EVOLUTION OF AN ISOLATED TURBULENT REGION IN A STRATIFIED FLUID, J GEO RES-O, 103(C11), 1998, pp. 24857-24868
Citations number
45
Categorie Soggetti
Oceanografhy,"Geosciences, Interdisciplinary","Astronomy & Astrophysics","Geochemitry & Geophysics","Metereology & Atmospheric Sciences
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
ISSN journal
21699275 → ACNP
Volume
103
Issue
C11
Year of publication
1998
Pages
24857 - 24868
Database
ISI
SICI code
2169-9275(1998)103:C11<24857:EOAITR>2.0.ZU;2-G
Abstract
This paper reports an experimental study on the evolution of an isolat ed turbulent region in an otherwise quiescent linearly stratified flui d. A turbulent patch was generated by pulsed horizontal injection of a small volume of fluid. It was found that the turbulent blob thus prod uced initially grows as in a nonstratified fluid for a nondimensional time period of Nt approximate to 4 - 5 (with N the buoyancy frequency) , attains a maximum height, and then physically collapses slowly to fo rm a planar, quasi- two-dimensional dipole pattern. The timescale for the physical collapse of the blob was found to be much larger than tha t of the turbulence collapse. Scaling arguments are presented to expla in the evolution of the turbulent region, and the experimental results are compared with the model predictions.