‘pete
.
evidence” that on some occasions a large amount of debris initially ~
in the upper levels, could be carried into the southern hemisphere.
This situation is not believed common, however.
*as an example, see figures 2 through 7 of High Tropospheric
Westerlies of the Equatori2! West Pacific Ocean, by Ibert, Jl. of
Met., Vol. 6, No. 3, dune 19)9.
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