Two responses of a uniformly stratified flow over a sloping bottom to a spatially varying downwelling favorable wind
Thesis (S.M.)--Joint Program in Physical Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2008.
Main Author: | Logvinov, Evgeny |
---|---|
Other Authors: | Joseph Pedlosky. |
Format: | Thesis |
Language: | eng |
Published: |
Massachusetts Institute of Technology
2009
|
Subjects: | |
Online Access: | http://hdl.handle.net/1721.1/45721 |
Similar Items
-
Examining the effects of mid ocean ridge topography on 3D marine magnetometric resistivity model responses
by: Lassner, Lisa A
Published: (2010) -
An experimental study on mixing induced by gravity currents on a sloping bottom in a rotating fluid
by: Ohiwa, Mitchihiro, 1977-
Published: (2010) -
Wind-driven circulation on a shallow, stratified shelf
by: Austin, Jay Alan
Published: (2010) -
Absarokites from the Western Mexican Volcanic Belt : constraints on mantle wedge conditions
by: Hesse, Marc, 1976-
Published: (2010) -
Mechanisms and variability of salt transport in partially-stratified estuaries
by: Bowen, Melissa Marie
Published: (2010)