COURTENAY STRONG, Ph.D.Assistant Professor
James R. Holton Award, AGU, 2008
Postdoc, U.C. Irvine
NSF Graduate Research Fellow, U. of Virginia
Office: 702 WBB
Phone: (801) 585-0049
Fax: (801) 585-3681
University of Utah
Department of Atmospheric Sciences
135 S 1460 E, Rm 819
Salt Lake City, Utah 84112-0110
ATMOSPHERE-CRYOSPHERE RESEARCH GROUP
My research group studies climate - especially processes involving the atmosphere and cryosphere (includes sea ice and snow). We analyze observational data and simulate atmosphere-cryosphere interactions using models run on powerful supercomputers. Our research is supported by the National Science Foundation, the Office of Naval Research, the Global Change and Sustainability Center, and the Center for High Performance Computing.
I am always looking for graduate students interested in climate analysis and modeling, and welcome inquiries about open positions in my research group: firstname.lastname@example.org
Liptak J, Strong C, 2014. A model-based decomposition of the sea ice-atmosphere feedback over the Barents Sea during winter. Journal of Climate, in press, [link].
Liptak J, Strong C, 2014. The winter atmospheric response to sea ice anomalies in the Barents Sea. Journal of Climate, 27, 914-924, [link].
Strong C, Rigor I, 2013. Arctic marginal ice zone trending wider in summer and narrower in winter. Geophysical Research Letters, 40, 4864-4868, doi:10.1002/grl.50928, [link].
McCabe-Glynn S, Johnson KR, Strong C, Berkelhammer M, Sinha A, Cheng H, RL Edwards, 2013. Variable North Pacific influence on drought in southwestern North America since AD 854. Nature Geoscience, 6, 617-621, doi:10.1038/ngeo1862, [link].
Liptak J, Strong C, 2013. Propagating atmospheric patterns associated with sea ice motion through the Fram Strait. Journal of Climate, 26, 2292-2297 [link].
Strong C, 2012. Atmospheric influence on Arctic marginal ice zone position and width in the Atlantic sector, February-April 1979-2010. Climate Dynamics, 39, 3091-3102 [link].
Strong C, Liptak J, 2012. Propagating atmospheric patterns associated with Midwest winter precipitation. Journal of Hydrometeorology, 13, 1371-1382 [link].
Strong C, Stwertka C, Bowling D, Stephens B, Ehleringer J, 2011. Urban carbon dioxide cycles within the Salt Lake Valley: a multiple box model validated by observations. Journal of Geophysical Research, 116, doi:10.1029/2011JD015693 [link].
Strong C, Maberly SC, 2011. The influence of atmospheric wave dynamics on interannual variation in the surface temperature of lakes in the English Lake District. Global Change Biology, 17, 2013-2022 [link].
Strong C, Magnusdottir G, 2011. Dependence of NAO variability on coupling with sea ice. Climate Dynamics, 36, 1681-1689 [link].
Strong C, Magnusdottir G. 2010. The role of Rossby wave breaking in shaping the equilibrium atmospheric circulation response to North Atlantic boundary forcing. Journal of Climate, 23, 1269-1276 [link].
Strong C, Magnusdottir G. 2010. Modeled boreal winter sea ice variability and the North Atlantic Oscillation: a multi-century perspective. Climate Dynamics, 34, 515-525 [link].
Strong C, Magnusdottir G, Stern H. 2009. Observed feedback between winter sea ice and the North Atlantic Oscillation. Journal of Climate, 22, 6021-6032 [link].
Strong C, Magnusdottir G. 2009. The role of tropospheric Rossby wave breaking in the Pacific Decadal Oscillation. Journal of Climate, 22, 1819-1833 [link].
Strong C, Davis RE. 2008. Comment on "Historical trends in the jet streams" by C. L. Archer and K. Caldeira, Geophysical Research Letters, doi:10.1029/2008GL034829 [link].
Strong C, Magnusdottir G. 2008. Tropospheric Rossby wave breaking and the NAO / NAM. Journal of the Atmospheric Sciences, 65, 2861-2876 [link].
Strong C, Magnusdottir G. 2008. How Rossby wave breaking over the Pacific forces the North Atlantic Oscillation. Geophysical Research Letters, 35, L10706, doi:10.1029/2008GL033578 [link].
Strong C, Davis RE. 2008. Variability in the position and strength of winter jet stream cores related to Northern Hemisphere teleconnections. Journal of Climate, 21, 584-592 [link].
Strong C, Davis RE. 2007. Winter jet stream trends over the Northern Hemisphere. Quarterly Journal of the Royal Meteorological Society, 133, 2109-2115 [link].
Strong C, Davis RE. 2006. Temperature-related trends in the vertical position of the summer upper tropospheric surface of maximum wind. International Journal of Climatology, 26, 1977-1997, doi: 10.1002/joc1344 [link].
Strong C, Davis RE. 2006. Variability in the altitude of fast upper tropospheric winds over the Northern Hemisphere during winter. Journal of Geophysical Research - Atmospheres, 111, D10106, doi: 10.1029/2005JD006497 [link].
Strong C, Davis RE. 2005. The surface of maximum wind as an alternative to the isobaric surface for windq climatology. Geophysical Research Letters, 32: L04813, doi: 10.1029/2004GL022039 [link].
Strong C, Fuentes JD, Garstang M, Betts AK. 2005. Daytime cycle of low-level clouds and the tropical convective boundary layer in southwestern Amazonia. Journal of Applied Meteorology, 44, 1607-1619 [link].
Strong C, Fuentes JD, Baldocchi D. 2004. Reactive hydrocarbon flux footprints during canopy senescence. Agricultural & Forest Meteorology 127, 159-173 [link].
Strong C, Fuentes JD, Davis RE, Bottenheim JW. 2002. Thermodynamic attributes of Arctic boundary layer ozone depletion. Atmospheric Environment, 36: 2641-2652 [link].
Google Scholar [page].