Imperial College , University
of London,UK, 1989-1992, Dynamical meteorology and oceanography,
PhD.
Thesis title:
Open-ocean deep convection: the spreading phase.
Thesis supervisor: John Marshall.
Ecole Polytechnique Federal de
Lausanne
,
Lausanne , Switzerland. 1989.
Student assistant in fluid mechanics
department .
Imperial College, London,
UK.
1990-1991.
Student laboratory teaching assistant for physics undergraduate course
and summer secondary school workshops.
Massachussetts Institute of
Technology,
Cambridge, USA. 1991 - 1992.
Research Fellow, exchange visitor in Department
of Earth, Atmospheric and Planetary Sciences.
University of Colorado,
Boulder,
USA. Feb 1993 - Jan 1995.
Postdoctoral Research Associate in Joint
Institute for Laboratory Astrophysics.
Funded by National Science Foundation,
High
Performance Computation and Communication program.
National Center for Atmospheric
Research,
Boulder, USA. Feb 1993 - Jan 1995.
Visiting postdoctoral scientist in Climate
and Global Dynamics division, Oceanography
section.
Universities Corporation for
Atmospheric
Research, Boulder, USA. Feb 1995 - Feb 1997.
NOAA Climate and Global Change
program
postdoctoral fellow.
(host institution: University of
California
Los Angeles)
Institute for Geophysics
and Planetary Physics , UCLA ,
Los Angeles, USA. Feb 1997- Sept 1997.
Assistant researcher.
Woods Hole Oceanographic
Institution,
Sept 1997 - May 2001.
Assistant scientist.
Woods Hole Oceanographic
Institution,
May 2001- August 2006.
Associate scientist. Awarded tenure January 2005.
Princeton University, Atmospheric and Oceanic Sciences
Program Sept 2004- present.
Research Oceanographer.
Penetrative convection in rapidly rotating flows: Preliminary results from numerical simulation, Julien K., S. Legg, J. McWilliams, and J. Werne, 1996a. Dyn. Atmos. Oceans, 24 237-249.
Hard-Turbulent heat-transport scaling in rotating Rayleigh-Benard convection: preliminary results from numerical simulation, Julien K., S. Legg, J. McWilliams and J. Werne, 1996b. Phys. Rev. E. 53 R5557.
Rapidly rotating turbulent Rayleigh-Benard convection, Julien, K., S. Legg, J. McWilliams, and J. Werne, 1996c. J. of Fluid Mech.322 243-273.
A heton perspective of baroclinic eddy transfer in localized open ocean convection,, Legg S., H. Jones, and M. Visbeck, 1996. J. Phys. Oceanogr. 26 2251-2266.
The influence of the ambient circulation on the spreading of convected fluid, Legg S. and J. Marshall, 1998. J. Mar. Research, 56 107-139.
Localization of deep ocean convection by a mesoscale eddy,Legg S., J. McWilliams, and J. Gao, 1998. J. Phys. Oceanogr.28 944-970.
The Labrador Sea Deep Convection experiment. The LabSea Group, 1998. Bull. American Met. Soc., 79 2033-2058.
Plumes in rotating convection. Part I: ensemble statistics and dynamical balances , Julien K., S. Legg, J. McWilliams, J. Werne, 1999. J. Fluid Mech. 391 151-187.
Modeled radar surface signature of deep ocean convection,Fischer K.W., S. Legg, W.H. Munk, R.M. Shuchman, R.W. Garwood, and J.P.Palshook, 1999. IEEE Transactions of geosciences and remote sensing, 37 2050-2067.
Temperature and salinity variability in heterogeneous ocean convection . Legg, S., and J. McWilliams, 2000. J. Phys Oceanogr. 30 1188-1206.
Convective modifications of a geostrophic eddy field, S. Legg, and J. McWilliams, 2001. J. Phys Oceanogr. 31 874-891.
Vertical transport by convective plumes: modification by rotation., S. Legg, K. Julien, J. McWilliams, J. Werne, 2001. Phys. and Chem. of the Earth. 26 259-262.
Sampling characteristics from isobaric floats in a convective eddy field, S. Legg, and J. McWilliams, 2002. J. Phys Oceanogr. 32 527-544.
Internal wave breaking at concave and convex continental slopes, S. Legg, and A. J. Adcroft, 2003. J. Phys Oceanogr. 33 2224-2246.
Internal tides generated on a corrugated continental slope. Part I: Cross-slope barotropic forcing, S. Legg, 2004. J. Phys Oceanogr. 34 156-173.
Internal tides generated on a corrugated continental slope. Part II: Along-slope barotropic forcing, S. Legg, 2004. J. Phys Oceanogr. 34 1824-1838.
A simple criterion to determine the transition from a localized convection to a distributed convection regime, S. Legg, 2004. J. Phys Oceanogr. 34 2843-2846.
Comparison of entrainment in overflows simulated by z-coordinate,
isopycnal and nonhydrostatic models, S. Legg, R.W. Hallberg and
J.B.
Girton, 2006. Ocean Modelling, 11 69-97.
Preliminary simulations of internal waves and mixing generated by
finite amplitude tidal flow over isolated topography, S.
Legg, and K.M.H. Huijts, 2006. Deep Sea Research, part II, 53, 140-156.
Regional simulations of the Faroe Bank Channel Overflow in a
level model, U. Riemenschneider and S.
Legg, 2006. Accepted for publication in
Ocean Modelling.
Internal waves, baroclinic energy fluxes and mixing at the European shelf edge,
J.A.M. Green, J.H. Simpson, S. Legg and M.R. Palmer, 2007.
Submitted to
Continental Shelf Research.
Internal Hydraulic Jumps and Overturning generated by a tidal flow over a tall steep ridge,
S.
Legg, and J. Klymak, 2007. Submitted to
J. Phys. Oceanogr..