Education
B.A. 1982 University of Vermont
M.S. 1986 Stanford University
Ph.D. 1989 Stanford University
Research Interests
Metamorphic petrology; experimental petrology; high-pressure aqueous geochemistry; mid-ocean ridge hydrothermal systems; fluid-volcano interactions; Cenozoic magma-hydrothermal systems of western North America; Tectonmetamorphic evolution of central Asia.
Education
B.S., (1996), University of Southern California
M.S., (1998), Massachusetts Institute of Technology
Ph.D., (2002), Massachusetts Institute of Technology
Research Interests
The research in our group covers the broad areas of surface hydrology and hydrometeorology. Our research group focuses on two primary goals:
- to improve our ability to characterize important hydrologic states and fluxes through the combined application of remote sensing and modeling, and
- to better understand the underlying mechanisms responsible for their variability in time and space.
The ultimate application of these research efforts are to improve water resource management and mitigate the effects of environmental hazards.
McWilliams received his college degrees in Applied Mathematics: a B.S. (with honors) in 1968 from Caltech and a M.S. in 1969 and Ph.D. in 1971 from Harvard. After holding a Research Fellowship in Geophysical Fluid Dynamics at Harvard (1971-74), he worked in the Oceanography Section at the National Center for Atmospheric Research (NCAR), where he became a Senior Scientist in 1980. In 1994 he became the Louis B. Slichter Professor of Earth Sciences in the Department of Atmospheric and Oceanic Sciences and the Institute for Geophysics and Planetary Physics at UCLA, while retaining a part-time appointment at NCAR. In 2002, he was elected to the National Academy of Sciences.
McWilliams’ primary areas of scientific research are the fluid dynamics of Earth’s oceans and atmosphere, both their theory and computational modeling. Particular subjects include the maintenance of the general circulations; climate dynamics; geostrophically and cyclostrophically balanced (or slow manifold) dynamics in rotating, stratified fluids; vortex dynamics; planetary boundary layers; planetary-scale thermohaline convection; the roles of coherent structures in turbulent flows in geophysical and astrophysical regimes; numerical algorithms; statistical estimation theory; and coastal ocean modeling.
In the past several years he has helped develop a three-dimensional simulation model of the U.S. West Coast that incorporates physical oceanographic, biogeochemical, and sediment transport aspects of the coastal circulation. This model is being used to interpret coastal phenomena, diagnose historical variability in relation to observational data, and assess future possibilities.