Repository logo
Log in(current)
Repository logoMIT Open ScholarshipDSpace@MIT
  1. Home
  2. MIT Open Access Articles
  3. MIT Open Access Articles
  4. Numerical simulations of internal wave generation by convection in water

Numerical simulations of internal wave generation by convection in water

Thumbnail Image
Download
Name

PhysRevE.91.063016.pdf

Size

2.93 MB

Format

Adobe PDF

Checksum (MD5)

f845d50ec8b781700fd90d2868fc8673

Download all files submitted through automated deposit
PhysRevE.91.063016-mets.zip (2.8 MB)
Author(s)
Lecoanet, Daniel
•
Le Bars, Michael
•
Vasil, Geoffrey M.
•
Brown, Benjamin P.
•
Quataert, Eliot
•
Oishi, Jeffrey S.
•
Burns, Keaton James
Date Issued
June 2015
Journal
Physical Review E
Publisher
American Physical Society
Citation
Lecoanet, Daniel, Michael Le Bars, Keaton J. Burns, Geoffrey M. Vasil, Benjamin P. Brown, Eliot Quataert, and Jeffrey S. Oishi. "Numerical simulations of internal wave generation by convection in water." Phys. Rev. E 91, 063016 (June 2015). © 2015 American Physical Society
Version
Final published version
Abstract
Water's density maximum at 4[superscript ∘]C makes it well suited to study internal gravity wave excitation by convection: an increasing temperature profile is unstable to convection below 4[superscript ∘]C, but stably stratified above 4[superscript ∘]C. We present numerical simulations of a waterlike fluid near its density maximum in a two-dimensional domain. We successfully model the damping of waves in the simulations using linear theory, provided we do not take the weak damping limit typically used in the literature. To isolate the physical mechanism exciting internal waves, we use the spectral code dedalus to run several simplified model simulations of our more detailed simulation. We use data from the full simulation as source terms in two simplified models of internal-wave excitation by convection: bulk excitation by convective Reynolds stresses, and interface forcing via the mechanical oscillator effect. We find excellent agreement between the waves generated in the full simulation and the simplified simulation implementing the bulk excitation mechanism. The interface forcing simulations overexcite high-frequency waves because they assume the excitation is by the “impulsive” penetration of plumes, which spreads energy to high frequencies. However, we find that the real excitation is instead by the “sweeping” motion of plumes parallel to the interface. Our results imply that the bulk excitation mechanism is a very accurate heuristic for internal-wave generation by convection.
MIT Department
Massachusetts Institute of Technology. Department of Physics
Terms of Use
Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
Persistent DSpace Link
http://hdl.handle.net/1721.1/97601
DOI of Published Version
http://dx.doi.org/10.1103/PhysRevE.91.063016
Repository logo
PrivacyPermissionsAccessibilityContact us
Repository logo
Notify us about copyright concerns.