Katabatic winds are cold, dense winds that descend from high elevations down to lower areas, typically in mountainous regions. They form when cooler air is displaced by warmer air, causing it to flow downhill due to gravity. These winds can increase in speed as they move down slopes, and they are often associated with clear, calm weather. Common examples include the "Bora" in the Adriatic region and the "Chinook" in North America.
weak winds because doldrums are calm winds on the earth.
Local winds, such as sea breezes and mountain winds, are not planetary winds. These winds are driven by local temperature and pressure differences rather than the global atmospheric circulation patterns that produce the planetary winds.
Monsoon winds
Winds blowing east to west or west to east are referred to as zonal winds
The phrase "winds do" can change one letter to become "winds go." This alteration keeps the overall meaning intact while simply modifying the verb. Another example is changing "winds do" to "winds to," which shifts the context slightly but still relates to the concept of winds.
winds ex: northern winds southern winds eastern winds western winds
winds has 1 syllable -*winds-* clap it winds
Global winds are local winds.
1.synoptic winds 2.gradint winds 3.prevailing winds 4.geostrophic winds
winds
the trade winds,the westerlies,the polar winds
weak winds because doldrums are calm winds on the earth.
Local winds, such as sea breezes and mountain winds, are not planetary winds. These winds are driven by local temperature and pressure differences rather than the global atmospheric circulation patterns that produce the planetary winds.
---local winds
Trade Winds
Planetary winds are any winds that occur because of solar radiation. They are in direct correlation to the rotation of the earth. Planetary winds do not blow directly north or south.
Heavy winds like hurricanes, tornadoes, and tropical winds