Dependence of the upper middle atmosphere on tropospheric circulation: Correlation of European winter rainfall and midlatitude mesopause region zonal winds

The winter midlatitude upper mesosphere/lower thermosphere zonal winds are connected with the northern hemisphere troposphere circulation, such that mesopause region zonal westerly winds are stronger when North Atlantic westerly winds onto Europe are stronger. Since European rainfall rates are conne...

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Bibliografiska uppgifter
Huvudupphovsmän: Christoph Jacobi, Dierk Kürschner
Materialtyp: Artikel
Språk:English
Publicerad: Borntraeger 1999-09-01
Serie:Meteorologische Zeitschrift
Ämnen:
Länkar:http://dx.doi.org/10.1127/metz/8/1999/132