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    Is the Midlatitude Zonal Flow Absolutely Unstable? 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 004:;page 505
    Author(s): Lin, S. J.; Pierrehumbert, R. T.
    Publisher: American Meteorological Society
    Abstract: An analysis is performed of the growth and propagation of unstable baroclinic wave packets in relatively realistic midlatitude zonal currents. The absolute growth rates are calculated, incorporating the effects of both ...
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    Parallel Implementation of a Kalman Filter for Constituent Data Assimilation 

    Source: Monthly Weather Review:;1997:;volume( 125 ):;issue: 007:;page 1674
    Author(s): Lyster, P. M.; Cohn, S. E.; Ménard, R.; Chang, L-P.; Lin, S-J.; Olsen, R. G.
    Publisher: American Meteorological Society
    Abstract: A Kalman filter for the assimilation of long-lived atmospheric chemical constituents was developed for two-dimensional transport models on isentropic surfaces over the globe. Since the Kalman filter calculates the error ...
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    High-Frequency Planetary Waves in the Polar Middle Atmosphere as Seen in a Data Assimilation System 

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 024:;page 2975
    Author(s): Coy, L.; Štajner, I.; DaSilva, A. M.; Joiner, J.; Rood, R. B.; Pawson, S.; Lin, S. J.
    Publisher: American Meteorological Society
    Abstract: The 4-day wave often dominates the large-scale wind, temperature, and constituent variability in the high-latitude Southern Hemisphere winter near the stratopause. This study examines the winter Southern Hemisphere vortex ...
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    Uncertainty in Model Climate Sensitivity Traced to Representations of Cumulus Precipitation Microphysics 

    Source: Journal of Climate:;2015:;volume( 029 ):;issue: 002:;page 543
    Author(s): Zhao, Ming; Golaz, J.-C.; Held, I. M.; Ramaswamy, V.; Lin, S.-J.; Ming, Y.; Ginoux, P.; Wyman, B.; Donner, L. J.; Paynter, D.; Guo, H.
    Publisher: American Meteorological Society
    Abstract: ncertainty in equilibrium climate sensitivity impedes accurate climate projections. While the intermodel spread is known to arise primarily from differences in cloud feedback, the exact processes responsible for the spread ...
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    The Dynamical Core, Physical Parameterizations, and Basic Simulation Characteristics of the Atmospheric Component AM3 of the GFDL Global Coupled Model CM3 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 013:;page 3484
    Author(s): Donner, Leo J.; Wyman, Bruce L.; Hemler, Richard S.; Horowitz, Larry W.; Ming, Yi; Zhao, Ming; Golaz, Jean-Christophe; Ginoux, Paul; Lin, S.-J.; Schwarzkopf, M. Daniel; Austin, John; Alaka, Ghassan; Cooke, William F.; Delworth, Thomas L.; Freidenreich, Stuart M.; Gordon, C. T.; Griffies, Stephen M.; Held, Isaac M.; Hurlin, William J.; Klein, Stephen A.; Knutson, Thomas R.; Langenhorst, Amy R.; Lee, Hyun-Chul; Lin, Yanluan; Magi, Brian I.; Malyshev, Sergey L.; Milly, P. C. D.; Naik, Vaishali; Nath, Mary J.; Pincus, Robert; Ploshay, Jeffrey J.; Ramaswamy, V.; Seman, Charles J.; Shevliakova, Elena; Sirutis, Joseph J.; Stern, William F.; Stouffer, Ronald J.; Wilson, R. John; Winton, Michael; Wittenberg, Andrew T.; Zeng, Fanrong
    Publisher: American Meteorological Society
    Abstract: he Geophysical Fluid Dynamics Laboratory (GFDL) has developed a coupled general circulation model (CM3) for the atmosphere, oceans, land, and sea ice. The goal of CM3 is to address emerging issues in climate change, including ...
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