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The trade winds blow predominantly from the northeast in the Northern Hemisphere and from the southeast in the Southern Hemispherestrengthening during the winter and when the Arctic oscillation is in its warm phase. Trade winds have been used by captains of sailing ships to cross the world's oceans for centuries and enabled colonial expansion into the Americas and trade routes to become established across the Atlantic and Pacific oceans.
In meteorologythe trade winds act as the steering flow for tropical storms that form over Trade Winds - Until We Are Ghosts - Bitterseed Atlantic, Pacific, and southern Indian Oceans and make landfall in North America, Southeast Asia, and Madagascar and eastern Africa. Trade winds also transport African dust westward across the Atlantic Ocean into the Caribbean Seaas well as portions of southeastern North America.
Shallow cumulus clouds are seen within trade wind regimes and are capped from becoming taller by a trade wind inversion, which is caused by descending air aloft from within the subtropical ridge. The weaker the trade winds become, the more rainfall can be expected in the neighboring landmasses.
The term trade winds originally derives from the early fourteenth century late Middle English word "trade," meaning "path" or "track. They could then turn northeast, to the area around the Azores islands, and finally east to mainland Europe.
This is because following the African coast southbound means sailing upwind in the Southern hemisphere. In the Pacific ocean, the full wind circulation, which included both the trade wind easterlies and higher-latitude Westerlieswas unknown to Europeans until Andres de Urdaneta 's voyage in The captain of a sailing ship seeks a course along which the winds can be expected to blow in the direction of travel.
For example, Manila galleons could not sail into the wind at all. By the 18th century, the importance of the trade winds to England's merchant fleet for crossing the Atlantic Ocean had led both the general public and etymologists to identify the name with a later meaning of "trade": " foreign commerce".
As part of the Hadley cellsurface air flows toward the equator while the flow aloft is towards the poles. A low-pressure area of calm, light variable winds near the equator is known as the doldrums near-equatorial trough,  intertropical front, or the Intertropical Convergence Zone.
The subsident sinking air is relatively dry because as it descends, the temperature increases, but the moisture content remains constant, which lowers the relative humidity of the air mass. This warm, dry air is known as a superior air mass and normally resides above a maritime tropical warm and moist air mass.
An increase of temperature with height is known as a temperature inversion. When it occurs within a trade wind regime, it is known as a trade wind inversion. The surface air that flows from these subtropical high-pressure belts toward the Equator is deflected toward the west in both hemispheres by the Coriolis effect.
The trade winds of both hemispheres meet at the doldrums. As they blow across tropical regions, air masses heat up over lower latitudes due to more direct sunlight.
Those that develop over land continental are drier and hotter than those that develop over oceans maritimeand travel northward on the western periphery of the subtropical ridge. The cold phase of the AO leads to weaker trade winds. During mid-summer in the Northern Hemisphere Julythe westward-moving trade winds south of the Trade Winds - Until We Are Ghosts - Bitterseed subtropical Rio Disco Stink - Poison Girls - Poisonous expand northwestward from the Caribbean sea into southeastern North America Florida and Gulf Coast.
When dust from the Sahara moving around the southern periphery of the ridge travels over land, rainfall is suppressed and the sky changes from a blue to a white appearance which leads to an increase in red sunsets. Its presence negatively impacts air quality by adding to the count of airborne particulates. There is a large variability in the dust transport to the Caribbean and Florida from year to year. From Wikipedia, the free encyclopedia. Braham; Enid Pearsons; Deborah M.
Posner; Georgia S. Random Terence Trent DArby - Sign Your Name Webster's College Dictionary second ed.
Random House. Muelder Read Books. Historical atlas of the North Pacific Ocean: maps of discovery and scientific exploration, — A text-book of commercial geography. Appleton and company. Introduction to Meteorology. Mcgraw-Hill Book Company, Inc. American Meteorological Society. Archived from the original on Retrieved Glossary of Meteorology. Advanced geography. State Printing. National Weather Service.
Oliver Encyclopedia of world climatology. Terry Tropical cyclones: climatology and impacts in Trade Winds - Until We Are Ghosts - Bitterseed South Pacific. Augustinus Marine Geology. Bibcode : MGeol. Steward Air Quality. Retrieved on Archived at the Wayback Machine Retrieved on Trade Winds - Until We Are Ghosts - Bitterseed Geological Survey Coral Mortality and African Dust. Hidden categories: Webarchive template wayback Τ Αγόρι Τ Ατσαλένιο - Κώστας Χατζής Συμμετέχει Η Σούλα Μαρκίζη* - Νταουλιέρικα Good articles.
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