Title: Boundary Layer Meteorology Lecture 17: Oceanic and Lacustrine Boundary Layers
1Boundary Layer Meteorology Lecture 17Oceanic
and Lacustrine Boundary Layers
- Similarities and differences between Atmospheric
and Oceanic/Lacustrine Boundary Conditions - Ocean Waves
- Langmuir circulations
2Similarities between Oceanic and Atmospheric
Boundary Layers
- M-O theory applied to both surface layers
- Mixed layer models used in a very similar way
- Etc.
3Differences between Oceanic and Atmospheric
Boundary Layers
- Presence of Salinity (but note analog of ocean
density, virtual temperature) - Boundary at top, not bottom
- Free-slip, versus no-slip boundary
- Wave-induced measurement difficulties (and
general lack of data, though this will improve in
the next few years, due to migrating remote
buoys). - Wave-induced TKE generation
- Langmuir circulations
4Ocean Waves
- Observations wave dispersion relations for
shallow and deep water - Big source of turbulent kinetic energy in top 5
meters - Incorporation of atmospheric gases, momentum(?)
due to wave breaking, bubbles, spray.
5Langmuir Circulations
Photo Credit S.A. Thorpe
Discovering the causes of Lc and quantifying and
identifying its effects has been difficult.
Studying the associated dynamical processes
involves some of the most intellectually
demanding problems of theoretical and
observational fluid dynamics, several of which
remain intractable. -S.A. Thorpe
6Langmuir Circulations
- Interaction of stokes drift, surface shear
current yields vortices (images from Thorpe,
2004, Ann. Rev. Fluid Mech., 36(1)55) - Conceptual diagram
7Langmuir Circulations
- New observations have complicated our picture of
these circulations. - Rolls are now seen to be time-varying, twisted,
irregularly spaced, and frequently combining and
separating
8Langmuir Circulations
- Previously thought to be a laminar process that
confined materials, resisted dispersion, now seen
as a turbulent process that aids dispersion.
9Incorporating Waves and Langmuir circulations in
models
- Noh et al. 2004
- McWilliams et al., 1997