1999
DOI: 10.1017/s1350482799001024
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Quantitative relationship between Meteosat WV data and positive potential vorticity anomalies: a case study over the Mediterranean

Abstract: dry air (see e.g. Fischer et al., 1981). Meteosat WV data are disseminated in high resolution image (HRI) formats coded in 256 digital values (0-255) that we shall call simply WV counts.

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Cited by 18 publications
(30 citation statements)
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“…Deepening cyclones are associated with tropopause folding, where there are high PV values in the upper troposphere as a result of PV conservation (Georgiev 1999). Generally, such high PV values in the upper and middle troposphere are considered to be potential vorticity anomalies (PVa).…”
Section: The Potential Vorticitymentioning
confidence: 99%
“…Deepening cyclones are associated with tropopause folding, where there are high PV values in the upper troposphere as a result of PV conservation (Georgiev 1999). Generally, such high PV values in the upper and middle troposphere are considered to be potential vorticity anomalies (PVa).…”
Section: The Potential Vorticitymentioning
confidence: 99%
“…However, the agreement between the shape and intensity of the PV anomaly and the WV pattern is complex since various mechanisms of cyclogenesis are possible. Also, the variable WV channel sensitivity is a maximum within the middle and the upper troposphere (see Georgiev, 1999). Forcing of cyclogenesis is usually associated with a positive upper-level PV anomaly indicated by a dry slot in the WV imagery but it can occur at lower levels associated with PV anomalies within the moist air.…”
Section: Methodsmentioning
confidence: 99%
“…(b) Absolute vorticity at the 2 PVU surface (Carroll, 1997;COST-78, 1998). (c) Positive PV anomalies at 400 hPa (Georgiev, 1999). (d) Positive PV anomalies at 500 hPa (Georgiev 1998(Georgiev , 1999.…”
Section: G Georgiev and F Martinmentioning
confidence: 99%
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