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Like sea and land breezes, anabatic and katabatic winds are induced thermally.
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.
A katabatic wind is a wind that is blowing down a slope, and an anabatic wind blows up a slope.
In addition, you can have thermals combining with the anabatic flows up a slope for convergence.
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