1. Equilibrium levelIn meteorology, the equilibrium level (EL), or level of neutral buoyancy (LNB), or limit of convection (LOC), is the height at which a rising parcel of air is at a temperature of equal warmth to it. This means that unstable air is now stable when it reaches the equilibrium level and convection stops.
Read “Equilibrium level” on English Wikipedia
Read “平衡高度” on Japanese Wikipedia
Read “Equilibrium level” on DBpedia
Read “Equilibrium level” on English Wikipedia
Read “平衡高度” on Japanese Wikipedia
Read “Equilibrium level” on DBpedia
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