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    A Nonlinear Perspective on the Dynamics of the MJO: Idealized Large-Eddy Simulations 

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 067 ):;issue: 004:;page 1202
    Author(s): Wedi, Nils P.; Smolarkiewicz, Piotr K.
    Publisher: American Meteorological Society
    Abstract: The 30?60-day intraseasonal atmospheric oscillation in the equatorial atmosphere, the Madden?Julian oscillation (MJO), is most visible in its signature of outgoing longwave radiation and associated convective centers. ...
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    Direct Numerical Simulation of the Plumb–McEwan Laboratory Analog of the QBO 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 012:;page 3226
    Author(s): Wedi, Nils P.; Smolarkiewicz, Piotr K.
    Publisher: American Meteorological Society
    Abstract: The laboratory experiment of Plumb and McEwan demonstrates the principal mechanism of periodically reversing winds observed in the stratosphere?the quasi-biennial oscillation (QBO). However, despite numerous studies, some ...
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    A Fast Spherical Harmonics Transform for Global NWP and Climate Models 

    Source: Monthly Weather Review:;2013:;volume( 141 ):;issue: 010:;page 3450
    Author(s): Wedi, Nils P.; Hamrud, Mats; Mozdzynski, George
    Publisher: American Meteorological Society
    Abstract: ery high-resolution spectral transform models are believed to become prohibitively expensive because of the relative increase in computational cost of the Legendre transforms compared to the gridpoint computations. This ...
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    Spectral Empirical Orthogonal Function Analysis of Weather and Climate Data 

    Source: Monthly Weather Review:;2019:;volume 147:;issue 008:;page 2979
    Author(s): Schmidt, Oliver T.; Mengaldo, Gianmarco; Balsamo, Gianpaolo; Wedi, Nils P.
    Publisher: American Meteorological Society
    Abstract: AbstractWe apply spectral empirical orthogonal function (SEOF) analysis to educe climate patterns as dominant spatiotemporal modes of variability from reanalysis data. SEOF is a frequency-domain variant of standard empirical ...
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