Free convective layer
In atmospheric sciences, the free convective layer (FCL) is the layer of conditional or potential instability in the troposphere. It is a layer in which rising air can experience positive buoyancy (PBE) so that deep, moist convection (DMC) can occur. On an atmospheric sounding, it is the layer between the level of free convection (LFC) and the equilibrium level (EL). The FCL is important to a variety of convective processes and to severe thunderstorm forecasting. FCL = ZEL - ZLFC or FCL = PEL - PLFC
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Free convective layer
In atmospheric sciences, the free convective layer (FCL) is the layer of conditional or potential instability in the troposphere. It is a layer in which rising air can experience positive buoyancy (PBE) so that deep, moist convection (DMC) can occur. On an atmospheric sounding, it is the layer between the level of free convection (LFC) and the equilibrium level (EL). The FCL is important to a variety of convective processes and to severe thunderstorm forecasting. FCL = ZEL - ZLFC or FCL = PEL - PLFC
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In atmospheric sciences, the f ...... and faster air parcel ascent.
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自由対流層（じゆうたいりゅうそう, Free convect ...... 由対流層が厚いと、大気の不安定度が増し、積乱雲の高さも増す。
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In atmospheric sciences, the f ...... ZEL - ZLFC or FCL = PEL - PLFC
@en
自由対流層（じゆうたいりゅうそう, Free convect ...... 由対流層が厚いと、大気の不安定度が増し、積乱雲の高さも増す。
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Free convective layer
@en
自由対流層
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