Preposition: of

• tracer: By considering the equation for advection of a passive tracer, explain why we generally take a time scale to be.

• air: Here the spherical glyphs represent particle advection of heated air around a room.

• vapor: References Blackburn, M. ( 1997 ) Advection of water vapor and the cold polar tropopause bias in Eulerian GCMs.

• gradient: As an example of advection let us consider 1D advection of a constant gradient of some scalar.

Adjective modifier

• chaotic: Chaotic advection has been used in the analysis of mixing.

• horizontal: Thus in regions where there is strong horizontal advection our 1-d model can not hope to reproduce the patterns in biological activity.

• thermal: Ascent occurs ahead of a surface warm anomaly warm advection ( Laplacian of the thermal advection ).

• vertical: The vertical advection is performed by considering control volumes, which are remapped on to the original or levels.

• cold: The process by which this cold, dry air moves horizontally into an area is known as cold air advection.

Modifies a noun

• scheme: Some simple tests are made to quantify the dissipation inherent in the advection scheme.

• fog: Advection fog occurs when warm air flows over a cool surface ( for example, over a cool ocean current ).

• speed: But the velocity relative to the ground depends not only on the phase velocity of the disturbances but also on the advection speed.

• process: A paper is in preparation on this work, and details of the water vapor advection processes involved are under investigation.

• problem: The detailed study of a specific time integrator for numerical simulations of advection problems with small diffusion.

Noun used with modifier

• contour: A contour advection run started on the 10th shows a very similar feature.

• particle: Here the spherical glyphs represent particle advection of heated air around a room.

• water: Another important practice in analyzing nonlinear water waves is to study the water particle advection in the history of a simulation.

• vorticity: The process, positive vorticity advection, is usually abbreviated to PVA.

• tracer: Tracer advection is a longstanding and notoriously difficult problem with numerical models, and a severe limitation on their validity.

• heat: Update buoyancy after heat advection and freshwater inflow, if used.