The most convenient features for anabatic and katabatic streams are the concepts of mountain-valley breezes. |
Land and sea breezes are far more noticeable in Australia than anabatic and katabatic winds. |
Like sea and land breezes, anabatic and katabatic winds are induced thermally. |
These winds are also called anabatic flow. |
In addition, you can have thermals combining with the anabatic flows up a slope for convergence. |
The cool night winds are called drainage winds, or katabatic winds, and are often quite gusty and usually stronger than anabatic winds. |