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CAPE (1)
Usado para
convective available potential energy
Definição1
A measure of the amount of energy available for convection. CAPE is directly related to the maximum potential vertical speed within an updraft; thus, higher values indicate greater potential for severe weather. Observed values in thunderstorm environments often may exceed 1,000 joules per kilogram (j/kg), and in extreme cases may exceed 5,000 j/kg. However, as with other indices or indicators, there are not threshold values above which severe weather becomes imminent.
Fonte1
SPELLMAN, Frank R. The Handbook of Meteorology. Lanham, Maryland: Scarecrow Press, Inc., 2013. 237 p. ISBN 978-0-8108-8613-1.
Fonte2
WORLD METEOROLOGICAL ORGANIZATION. Technical regulations: basic documents No. 2. Volume II – Meteorological Service for International Air Navigation. Geneva, 2018. (WMO, n.49).
Nota adicional1
The CAPE values can differ slightly depending on which NWP model-derived soundings it was calculated with, but the graphical ‘equal area’ properties of the tephigram allow very meaningful constructions to determine convective depth.