The Australian National University
Research School of Earth Sciences
document location: http://rses.anu.edu.au/people/hogg_a/index.php?print=1
Andy Hogg's Home Page

Andy Hogg's Home Page

Dr. Andy Hogg

Fellow
Geophysical Fluid Dynamics
Earth Physics
Research School of Earth Sciences

T: +61 2 6125 9962
F: +61 2 6257 2737
E: Andy.Hogg@anu.edu.au
Room J7.212, Jaeger 7 Building,

Click here for a list of student projects.


Research Interests:

My research interests centre on physical processes governing the ocean and climate. This includes:

Ocean Eddies:

Ocean eddies are small scale (10-100km) vortices which occur in all regions of the ocean. Despite their small size, they can have significant impacts on large scale ocean circulation -- and climate.

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Ocean Straits:

Flow through ocean straits (such as the Straits of Gibraltar) are energetic and nonlinear, producing strong turbulence and mixing.

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Glacial Climates:

One of the outstanding puzzles in paleoclimatology is to determine the cause of ice ages.

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Shear Instability:

Flow in a density stratified can be unstable because of velocity gradients in the fluid. The resulting "shear instability" produces vortices (such as the Kelvin-Helmholtz billow shown here) and turbulence.

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Recent Publications

Papers Currently Under Review:

R. Morrow, M. L. Ward, S. Pasquet & A.McC. Hogg (2009). Eddy response to Southern Ocean climate modes. Submitted to J. Geophys. Res.

A. McC. HOGG & R. W. Griffiths (2009). A coupled ocean-atmosphere laboratory model of the Antarctic Circumpolar Current. Submitted to Ocean Modell. [Pre-print]

Recent Journal Publications:

D. K. HUTCHINSON, A. McC. HOGG, & J. R. BLUNDELL (2009). Southern Ocean Response to Relative Velocity Wind Stress Forcing. J. Phys. Oceanogr., In Press. [Pre-print]

M. S. SINGH & A. McC. HOGG (2009). Viscous effects in two-layer, unidirectional hydraulic flow. J. Fluid Mech., In Press. [Pre-print]

G. O. HUGHES, A. McC. HOGG & R. W. GRIFFITHS (2009). Available potential energy and irreversible mixing in the meridional overturning circulation. J. Phys. Oceanogr., 39, 3130-3146. [Pre-print]

W. K. DEWAR & A. McC. HOGG (2009). Inviscid dissipation of balanced flow. Ocean Modell., In Press. [Pre-print]

T. PRASTOWO, R. W. GRIFFITHS, G. O. HUGHES & A. McC. HOGG (2009). Effects of Topography on the Cumulative Mixing Efficiency in Exchange Flows. J. Geophys. Res., 114, C08008, doi:10.1029/2008JC005152. [Online copy from JGR]

A. McC. HOGG, W. K. DEWAR, P. BERLOFF, S. KRAVTSOV & D. K. HUTCHINSON (2009). The effects of mesoscale ocean-atmosphere coupling on the large-scale ocean circulation. J. Climate, 22, 4066-4082. [Online copy from J. Climate]

J. NYCANDER, A. McC. HOGG & L. M. FRANKCOMBE, (2008). Open boundary conditions for nonlinear shallow water models. Ocean Modell., doi:10.1016/j.ocemod.2008.06.003. [Online copy from OM]

T. PRASTOWO, R. W. GRIFFITHS, G. O. HUGHES & A. McC. HOGG, (2008). Mixing in exchange flows through a horizontal constriction. J. Fluid Mech., 600, 235-244. [Online copy from JFM]

A. McC. HOGG, (2008). Glacial Cycles and Carbon Dioxide: A conceptual model. Geophys. Res. Lett., 35, L01701, doi:10.1029/2007GL032071.  [Online copy from GRL]

A. McC. HOGG, M. P. MEREDITH, J. R. BLUNDELL & C. WILSON, (2008). Eddy heat flux in the Southern Ocean: Response to variable wind forcing. J. Climate, 21, 608-620. [Online copy from J. Climate]

[More Publications ...]