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Diagram showing an air parcel path when raised along B-C-E compared to the surrounding air mass Temperature (T) and humidity (Tw); see CAPE. The level of free convection (LFC) is the altitude in the atmosphere where an air parcel lifted adiabatically until saturation becomes warmer than the environment at the same level, so that positive buoyancy can initiate self-sustained convection.
Diagram showing an air parcel path when raised along B-C-E compared to the surrounding air mass Temperature (T) and humidity (Tw) In atmospheric sciences, the free convective layer (FCL) is the layer of conditional or potential instability in the troposphere.
Fluid parcel. In fluid dynamics, a fluid parcel, also known as a fluid element or material element, is an infinitesimal volume of fluid, identifiable throughout its dynamic history while moving with the fluid flow. [ 1] As it moves, the mass of a fluid parcel remains constant, while—in a compressible flow —its volume may change, [ 2][ 3 ...
In 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 the same temperature as its environment. Diagram showing an air parcel path when raised along B-C-E compared to the surrounding air mass Temperature (T) and humidity (Tw)
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An access easement can provide access from public land, road or path or a public right of way to a parcel of land. For example, if Zach and James own neighboring parcels of land, Zach's parcel may have easement rights to cross James's parcel from public land, road or path or a public right of way.
Assessor's parcel number. An assessor's parcel number, or APN, is a number assigned to parcels of real property by the tax assessor of a particular jurisdiction for purposes of identification and record-keeping. The assigned number is unique within the particular jurisdiction, and may conform to certain formatting standards that convey basic ...
Bernoulli's principle states that an increase in the speed of a parcel of fluid occurs simultaneously with a decrease in either the pressure or the height above a datum. [1]: Ch.3 [ 2 ] : 156–164, § 3.5 The principle is named after the Swiss mathematician and physicist Daniel Bernoulli , who published it in his book Hydrodynamica in 1738. [ 3 ]