westerlies
Quick Summary
The westerlies are prevailing winds in the middle latitudes that blow from west to east. These winds are part of Earth's larger atmospheric circulation system, driven by temperature differences and the planet's rotation.1234
In the mid-latitudes, cold air from polar regions meets warmer air from lower latitudes, creating a convergence zone known as the polar front. This interaction often leads to the formation of traveling depressions, or storm systems, characteristic of middle-latitude weather. The westerlies are also associated with jet streams, which are fast-flowing, narrow air currents found at high altitudes. These jet streams play a role in steering weather patterns and can influence aircraft travel. The Southern Hemisphere's westerlies are known for their steadiness and strength, earning them names like the "brave west winds" and the "roaring forties" due to frequent gales.13546
Ask Britannica AI about this topic
Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.
Atlantic OceanThe North Atlantic…two air currents generates prevailing westerly winds across the North Atlantic and over western Europe. In winter these winds meander at altitudes of about 10,000 to 40,000 feet (3,000 to 12,200 metres) over North America in such a way that a northward bulge (ridge) is generated by and over the…
Read More…two air currents generates prevailing westerly winds across the North Atlantic and over western Europe. In winter these winds meander at altitudes of about 10,000 to 40,000 feet (3,000 to 12,200 metres) over North America in such a way that a northward bulge (ridge) is generated by and over the…
Read More
Pacific OceanThe westerliesWithin the belts of the westerly winds, cold easterly winds from polar regions meet the warm westerly winds of the middle latitudes, causing the formation of the traveling depressions characteristic of middle latitudes. The zone of convergence, or polar front, is most strongly developed…
Read MoreWithin the belts of the westerly winds, cold easterly winds from polar regions meet the warm westerly winds of the middle latitudes, causing the formation of the traveling depressions characteristic of middle latitudes. The zone of convergence, or polar front, is most strongly developed…
Read More
atmospheric circulation…and poleward as the midlatitude westerlies. The westerly flow is most evident between 5 and 12 km (3 and 7 miles) or so above the Earth’s surface and contains the jet streams. Jet streams are relatively narrow corridors of particularly strong winds, which correspond to the location of the polar…
Read More…and poleward as the midlatitude westerlies. The westerly flow is most evident between 5 and 12 km (3 and 7 miles) or so above the Earth’s surface and contains the jet streams. Jet streams are relatively narrow corridors of particularly strong winds, which correspond to the location of the polar…
Read More
EuropeAir pressure beltsThe winter westerlies, often from the southwest, bring in warm tropical air; in summer, by contrast, they veer to the northwest and bring in cooler Arctic or subarctic air. In Mediterranean Europe the rain-bearing westerlies chiefly affect the western areas, but only in winter. In winter the…
Read MoreThe winter westerlies, often from the southwest, bring in warm tropical air; in summer, by contrast, they veer to the northwest and bring in cooler Arctic or subarctic air. In Mediterranean Europe the rain-bearing westerlies chiefly affect the western areas, but only in winter. In winter the…
Read More
windThe westerlies of the Southern Hemisphere are much less strongly affected by standing disturbances. Associated with these long standing waves are the short waves (several hundred kilometres in wavelength) called traveling waves. Such traveling waves form the upper parts of near-surface cyclones and anticyclones to which…
Read MoreThe westerlies of the Southern Hemisphere are much less strongly affected by standing disturbances. Associated with these long standing waves are the short waves (several hundred kilometres in wavelength) called traveling waves. Such traveling waves form the upper parts of near-surface cyclones and anticyclones to which…
Read More- climateCharacteristics
…from west to east (“westerly” flow), though this flow may change during the summer. A series of cyclonic and anticyclonic vortices superimposed on the uniform west-to-east flow make up a wave train (a succession of waves occurring at periodic intervals). The waves are called Rossby waves after Swedish American…
Read More…from west to east (“westerly” flow), though this flow may change during the summer. A series of cyclonic and anticyclonic vortices superimposed on the uniform west-to-east flow make up a wave train (a succession of waves occurring at periodic intervals). The waves are called Rossby waves after Swedish American…
Read More