As their currents are deflected toward lower latitudes, they are associated with the northeasterly and southeasterly trades, and their return flow ends at the Intertropical Convergence Zone.
Oort and Yienger modeled these entities using the zonal mean meridional streamfunction, elucidating a long-term intensification based on the increasing frequency of an oceanic phenomenon which strengthens their vertical components. The Hoerling and Eischied Model of climate change links that intensification to watershed erosion in the Great Basin Region. A persistent Bermuda High may diminish the upper tropospheric trough that makes up their northern boundary in early autumn as they overcome the weaker flow of their immediate neighbors. As their currents are deflected toward lower latitudes, they are associated with the northeasterly and southeasterly trades, and their return flow ends at the Intertropical Convergence Zone. FTP, identify this circulation pattern that dominates tropical air flow between 30 degrees North and 30 degrees South, named for a English lawyer who dallied in meteorology.
Oort and Yienger modeled these entities using the zonal mean meridional streamfunction, elucidating a long-term intensification based on the increasing frequency of an oceanic phenomenon which strengthens their vertical components.
Hadley Cells