| A katabatic wind is a wind that is blowing down a slope, and an anabatic wind blows up a slope. |
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| The most convenient features for anabatic and katabatic streams are the concepts of mountain-valley breezes. |
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| In addition, you can have thermals combining with the anabatic flows up a slope for convergence. |
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| Like sea and land breezes, anabatic and katabatic winds are induced thermally. |
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| Land and sea breezes are far more noticeable in Australia than anabatic and katabatic winds. |
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| The anabatic process benefits in tis case from the bouyancy of the warm inside air. |
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| The cool night winds are called drainage winds, or katabatic winds, and are often quite gusty and usually stronger than anabatic winds. |
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| These winds are also called anabatic flow. |
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| An anabatic wind, if extended to sufficient height, will produce cloud. |
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| These daytime, upslope winds are called anabatic winds. |
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| Around glaciers in the summer, wind fields can be chaotic as katabatic winds from the top of the glacier struggle for dominance with localized convection or anabatic winds induced by heated rock slopes below the ice. |
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| In meteorology, this is know as bergwind conditions, or anabatic compression. |
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| The wind regularly drops in the evening after a breezy day because very light katabatic winds blow offshore at night and anabatic winds blow onshore in the day. |
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