Nature research paper: Human-induced weakening of the Northern Hemisphere tropical circulation
) and the 1960–2014 trends of the different terms, averaged between 10° and 20°, in the zonal mean zonal momentum equation vertically integrated between 1,000 mb to 500 mb and meridional surface momentum equation.
are the mean and eddy meridional components of the zonal momentum flux convergence, respectively,are the mean and eddy vertical components of the zonal momentum flux convergence, respectively,is dissipation effects on the zonal wind,are the mean and eddy meridional components of the meridional momentum flux convergence, respectively,are the mean and eddy vertical components of the meridional momentum flux convergence, respectively,is dissipation effects on the meridional wind.
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