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   <subfield code="a">A mechanism of Alpine lee cyclogenesis as revealed by a quasigeostrophic variational filter</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Yoshi Sasaki, Milija Zupanski]</subfield>
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   <subfield code="a">Summary: Mechanisms associated with Alpine lee cyclogenesis during the early phase of their generation are investigated using a variational quasigeostrophic filter technique. It was possible to extract the quasigeostrophic signal from the available analyzed real data set. The results presented here are for the 11-12 March 1982, an example of so-called &quot;orographically induced” lee cyclogenesis. Non-quasigeostrophic fields, calculated as a difference between observations and the quasigeostrophic fields, show significant magnitudes indicating the possible importance of non-quasigeostrophic processes. A &quot;dipole” structure in the residual geopotential field was observed, similar to the results of numerical model experiments. Also, a strong upper-level non-quasigeostrophic divergence was found in the Alpine region 24 hours prior to lee cyclogenesis, lasting for 6-12 hours. On the other hand, quasigeostrophic results indicate only a local effect of mountain slopes, suggesting possibly a dominant role of the low-level blocking. A hypothetical &quot;scenario” of Alpine lee cyclogenesis is proposed, based on results obtained here.</subfield>
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   <subfield code="a">Springer-Verlag, 1992</subfield>
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   <subfield code="g">47/2-4(1992-06-01), 91-105</subfield>
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