advection

The second, third, and fourth terms are due to advection.

However, an intrusion of cool advection quickly weakened the storm.

It is a method from the texture advection family.

Cohesion and advection play a bigger role in space.

Advection is sometimes confused with the more encompassing process of convection.

The term advection is sometimes used as a synonym for convection.

Moisture advection is the horizontal transport of water vapor by the wind.

This equation is also a mathematical model for one-dimensional linear advection.

This results in the total rate of transport for the system being influenced by both factors, diffusion and advection.

It can also form due to the lifting of advection fog during breezy conditions.

He also said that advection rather than local growth could be responsible for the bloom he observed.

Two basic mechanisms are responsible for fluid mixing: diffusion and advection.

The heat from the lower crust moves via conduction and groundwater advection.

The same applies for all other advection algorithms.

The transfer of energy can take various forms; familiar examples include work, heat flow, and advection, as discussed below.

Technically, convection is the sum of transport by diffusion and advection.

Similarly, much smaller ratios indicate a higher rate of diffusion relative to advection.

This result is similar to Fick's second law, but with an additional advection term.

Advection, that is the transport of matter by a flow, is required for better mixing.

Therefore, these effects cannot be described as a bulk transport and differ from advection or convection.

Texture advection methods that "bend" textures (or images) according to the flow.

The filtered advection term can be split up, following Leonard (1974), as:

In this context, convection includes both advection and conduction.

Without advection, water that evaporated over the oceans could not precipitate over land.

Contour advection is another useful method for characterizing chaotic mixing.