Image:LCL-NCA.png

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[edit] Summary

How to reach the level of condensation by lifting a parcel (LCL). The parcel at a certain level has a temperature T and a dew point Td. Its tempréature will change according the dry adiabatic rate as it is lifted while its mixing ratio remain the same as the one at Td. When the line of mixing ratio and T adiabtic cross, the moisture in the parcel begin to condensate: it is the LCL.

Author: Pierre_cb 2006-05-08

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I, the copyright holder of this work, have published or hereby publish it under the following license:
GNU head Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation license, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled "GNU Free Documentation license".

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Date/TimeDimensionsUserComment
current13:10, 9 May 2006321×311 (5 KB)Pierre cb (How to reach the level of condensation by lifting a parcel (LCL). The parcel at a certain level has a temperature T and a dew point Td. Its tempréature will change according the dry adiabatic rate as it is lifted while its mixing ratio remain the same as)
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