As an air parcel is lifted, its pressure and temperature decrease.

The rest being used to evacuate the air parcels off the surface of the sail.

This structure reflects the transport and chemistry of different air parcels.

An air parcel is defined as a point in the fluid continuum of the atmosphere.

The time evolution path that an air parcels traces in space is called a trajectory.

In this equation, m is the mass of the water in the air parcel.

As water vapor condenses, latent heat is released into the air parcel.

For air flow, the corresponding term is air parcel.

In addition, there are 19 post offices, a number of cargo forwarders provide air parcel and freight services.

Consider an air parcel containing masses and of water vapor in a given volume .

Sometimes these air parcels act as a lens and cause the light rays from a given star to converge a little, making it momentarily brighter.

When the rising air parcel cools more slowly than the surrounding atmosphere, it remains warmer and less dense.

This is because of the condensation of water vapor in the air parcel due to expansion cooling.

Mixing is based on grid deformation of quasi uniform air parcel distributions.

Thunderstorms form when air parcels are lifted vertically.

However, this does not imply that a particular air parcel sampled at the trajectory destination followed this path.

These particle parcels are simulated independently from the Lagrangian air parcels.

The rising air parcels in that column accelerate and will overshoot the equilibrium level before being pulled back by negative buoyancy.

Equivalent temperature is the temperature of an air parcel from which all the water vapor has been extracted by an adiabatic process.

As the air parcel expands, it pushes on the air around it, doing work (thermodynamics).

The dew point of an air parcel is the temperature to which it must cool before water vapor in the air begins to condense.

The paths of air parcels weave in and out of each other, making the Tokyo subway map look simplistic by comparison.

The new model features a layer-averaged mode that is activated whenever an air parcel traveling isentropically approaches the Earth's surface.

The moist static energy is a thermodynamic variable that describes the state of an air parcel, and is similar to the equivalent potential temperature.

Air parcels move on isentropic surfaces (surfaces of equal potential temperature) rather than pressure surfaces.