@article {Flocas200025,
	title = {Diagnostics of cyclogenesis over the Aegean sea using potential vorticity inversion},
	journal = {Meteorology and Atmospheric Physics},
	volume = {73},
	number = {1-2},
	year = {2000},
	note = {cited By (since 1996)8},
	pages = {25-33},
	abstract = {In this study an attempt is made to investigate comprehensively the dynamics of a case of cyclogenesis over the Aegean Sea within the context of the potential vorticity. At early stages the cyclogenesis is manifested by a large scale development at the upper levels over Adriatic Sea and Yugoslavia associated with an upper tropospheric potential vorticity anomaly. At later stages a smaller scale development was generated over Aegean Sea associated with a low-level potential vorticity anomaly and a surface warm anomaly. By means of a two-dimensional potential vorticity inversion it is demonstrated that the scale, the position and the strength of the involved anomalies contribute to the surface development, however, the low-level potential vorticity anomaly seems to constitute the most significant feature, more likely to be associated with condensation.},
	issn = {01777971},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-0034340731\&partnerID=40\&md5=b67cd2ff19a73ed788f3cc5ef9823750},
	author = {H. A. Flocas}
}
