Convergence Cloudiness - Typical Appearance in Vertical Cross Sections
by ZAMG
- Isentropes are inclined, but less pronounced than for fronts; sometimes there is a double structure (frontal character at the surface and above)
- Often within weak WA
- Convergence in lower levels, sometimes in upper levels, but there are big differences from case to case
- Isotachs show a low level minimum at the transition between the Occlusion and Convergence Cloudiness
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20 December 2008/18.00 UTC - Vertical cross section; black: isentropes (ThetaE), red thick: temperature advection - WA, red thin: temperature
advection - CA, orange thin: IR pixel values, orange thick: WV pixel values
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20 December 2008/18.00 UTC - Vertical cross section; black: isentropes (ThetaE), magenta thick: convergence, magenta thin: divergence, orange
thin: IR pixel values, orange thick: WV pixel values
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