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English: 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 temperature 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.
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Author Pierre_cb, VIGNERON
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8 May 2006

11,209 byte

264 pixel

276 pixel

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256ccad3a703b61671260e6b24143f307efeea92

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Date/TimeThumbnailDimensionsUserComment
current17:22, 20 April 2009Thumbnail for version as of 17:22, 20 April 2009276 × 264 (11 KB)VIGNERON
17:14, 20 April 2009Thumbnail for version as of 17:14, 20 April 2009276 × 264 (12 KB)VIGNERON
17:13, 20 April 2009Thumbnail for version as of 17:13, 20 April 2009276 × 264 (12 KB)VIGNERON
17:09, 20 April 2009Thumbnail for version as of 17:09, 20 April 2009276 × 264 (12 KB)VIGNERON
17:05, 20 April 2009Thumbnail for version as of 17:05, 20 April 2009276 × 264 (10 KB)VIGNERON
17:02, 20 April 2009Thumbnail for version as of 17:02, 20 April 2009276 × 264 (10 KB)VIGNERON{{Information |Description={{en|1=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 temperature will change according the dry adiabatic rate as it is lifted while it

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