Cold Front In Cold Advection - Key Parameters
by ZAMG and FMI
Positive vorticity advection at 500 hPa and temperature advection at 700 hPa:
- In a CF in CA there is a maximum of PVA over the rear edge of the cloud band.
- In a CF in CA there is cold advection over the whole frontal cloudiness as well as behind it. Ahead of the front the temperature advection is usually negligible.
- In a CF there is warm advection ahead of the cloud band and strong cold advection behind it. The cloud band is mostly under cold advection.
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20 January 2007/12.00 UTC - Meteosat 8 IR 10.8 image; green: PVA 500 hPa, red: temperature advection 700 hPa
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19 September 2005/12.00 UTC - Meteosat 8 IR 10.8 image; green: PVA 500 hPa, red: temperature advection 700 hPa
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- TFP accompanies the cloud band in both cases, although in CF in CA it is weaker.
- Equivalent thickness shows a crowding zone near the rear edge of the cloud band, and a ridge ahead of it.
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20 January 2007/12.00 UTC - Meteosat 8 IR 10.8 image; blue: TFP, green: equivalent thickness
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19 September 2005/12.00 UTC - Meteosat 8 IR 10.8 image; blue: TFP, green: equivalent thickness
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- The zero line of shear vorticity follows the rear edge of the cloud band.
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20 January 2007/12.00 UTC - Meteosat 8 IR 10.8 image; black: zero line of shear vorticity 300 hPa, yellow: isotachs 300 hPa
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19 September 2005/12.00 UTC - Meteosat 8 IR 10.8 image; magenta: zero line of shear vorticity 300 hPa, yellow: isotachs 300 hPa
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