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TeachMeFinance.com - explain Convective Inhibition Convective Inhibition The term 'Convective Inhibition' as it applies to the area of the weather can be defined as ' (CIN or B-) - A numerical measure of the strength of 'capping,' typically used to assess thunderstorm potential. Specifically, it represents the cumulative effect of atmospheric layers the are warmer than the parcel moving vertically along the adiabat. Low level parcel ascent is often inhibited by such stable layers near the surface. If natural processes fail to destabilize the lower levels, an input of energy from forced lift (a front, an upper level shortwave, etc.) will be required to move the negatively buoyant air parcels to the point where they will rise freely. Since CIN is proportional to the amount of kinetic energy that a parcel loses to buoyancy while it is colder than the surrounding environment, it contributes to the downward momentum'. Previous 5 Terms: convection convective adjustment Convective Boundary Layer Convective Clouds Convective Condensation Level Next 5 Terms: Convective Outlook Convective Overdevelopment Convective Temperature Conventional agriculture Conventional blendstock for oxygenate blending (CBOB) About the author Mark McCracken Author: Mark McCracken is a corporate trainer and author living in Higashi Osaka, Japan. He is the author of thousands of online articles as well as the Business English textbook, "25 Business Skills in English". Copyright © 2005-2011 by Mark McCracken, All Rights Reserved. TeachMeFinance.com is an informational website, and should not be used as a substitute for professional medical, legal or financial advice. Information presented at TeachMeFinance.com is provided on an "AS-IS" basis. Please read the disclaimer for details.