Professor Michael J. PratherMJ Prather pix from Tromso


UCI logo  Fred Kavli Chair and Professor of Earth System Science
3329 Croul Hall,  Department of Earth System Science
University of California, Irvine, CA 92697-3100
tele: (949) 824-5838 (office),  -8794 (dept),  -3874 (fax)
                         mprather@uci.edu

Director, The UCI Environment Institute
Global Change, Energy, and Sustainable Resources
http://environment.uci.edu



       
Undergraduate degrees in Mathematics (Yale, 1969) and Physics (Merton, Oxford, 1971).  Doctorate in Astronomy and Astrophysics (Yale, 1976). Researcher at Harvard (1975-1985) and Goddard Institute for Space Studies (1985-1992). Program manager at NASA HQ (1987-1992). Adjunct Professor in Applied Physics and Nuclear Engineering at Columbia U (1986-1992). Professor of Earth System Science at UC Irvine (1992-present). Jefferson Science Fellow at U.S. Department of State / INR (resident 2005-2006, continuing as consultant).  Member of the Norwegian Academy of Science and Letters. Fellow of the AGU (1997) and AAAS (2004). International Ozone Commission (1996-2004). UCI Lauds & Laurels Faculty Award 2008. Editor-in-Chief of Geophysical Research Letters (1997-2001).  UNEP/WMO Ozone Assessments: Lead Author/Author/Contributor in 1985, 1988, 1989, 1991, 1994, 2010.  Intergovernmental Panel on Climate Change:  Reviewer; 1992; Convening Lead Author, 1994, 1995, 1999 and 2001; Lead Author, 2007, 2013.



Lifetimes and Time scales in Atmospheric Chemistry
            (Royal Society Talk, published in Phil. Trans. Roy. Soc. A, 2007)


Early Publications and Ph.D. Thesis (Yale, 1976)

   

NEW fast-JX package v6.6,  includes JPL-2010 (Jan 2012):  Photolysis code for stratosphere & troposphere plus X-section maker



SOM tracer advection package (Apr 2007):  sample 3-D code with new flux limiters
The new CTM 3-D over-the-pole code that avoids global CFL limiters and hence can readily do 1x1 resolution, is available upon request, we will try to post a simplified version soon. (see Prather M.J., X. Zhu, S.E. Strahan, S.D. Steenrod, J.M. Rodriguez (2008), Quantifying errors in trace species transport modeling, Proc. Nat. Acad. Sci. 105(50): 19617-19621).

New, alternative SOM codes for 3-D tracer transport on a sphere have been developed and will be posted soon (in 2012).  These include both lat-long grids and gnomonic cubed sphere.  Also the over-the-pole transport has been further revised/corrected when it was found that the 2007-version (above, which passed rigid-body rotation with ease), failed for specific cases when cyclonic or anticyclonic vortices had their edges at the pole.  

Publications LIST


Copies of some PUBLICATIONS, PREPRINTS & PUBLIC TALKS



RESEARCH GROUP


RESEARCH INTERESTS

Simulation of the physical, chemical and biological processes that determine atmospheric composition. Development of (1) detailed numerical models of photochemistry and atmospheric radiation, and (2) global chemical transport models that describe ozone and other trace gases. Studies include the predicted effects of volcanic sulfate aerosols on stratospheric ozone loss, the role of clouds in scattering sunlight and altering photochemistry, non-linearities in chemical systems that lead to sudden changes such as the depletion of ozone caused by CFC increases, and uncertainties in predicting past and future greenhouse gas abundances.

Numerical models of atmospheric chemistry must simulate the transport of trace species by winds, convective mixing, boundary layer exchange with the surface, and exchange between the stratosphere and troposphere. Such models are used to predict future changes in the atmosphere and to analyze global data sets. Observed trace gas distributions are used as measures of the atmospheric circulation or alternatively as indicators of the location and strength of sources. Such a quantitative understanding of these causal relationships is an essential element of assessments of chemical and climatic change, and it is needed to convince governments and the public to make tough environmental choices.