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  • Trade winds - Wikipedia
    Trade winds have been used by captains of sailing ships to cross the world's oceans for centuries They enabled European colonization of the Americas, and trade routes to become established across the Atlantic Ocean and the Pacific Ocean
  • Sailwind Interactive Map - GitHub Pages
    Map rendering powered by Esri ArcGIS
  • earth :: a global map of wind, weather, and ocean conditions
    See current wind, weather, ocean, and pollution conditions, as forecast by supercomputers, on an interactive animated map Updated every three hours
  • ArcGIS - Prevailing Winds
    Earthstar Geographics | Esri, TomTom, FAO, NOAA, USGS | File used from Analyzing Our World's Windblown lesson
  • Live Global Wind Map - Real-Time Wind Speeds Directions
    Receive instant, comprehensive wind speed and direction updates with our state-of-the-art real-time wind tracking technology Diligently monitor wind patterns and intensities to inform safety measures and operational planning Stay ahead with our precise wind tracking and advanced analytics
  • Trade Winds | NOAA SciJinks – All About Weather
    NOAA’s GOES-East satellite keeps an eye on how trade winds impact the movement of hurricanes and tropical storms toward the southeastern United States In this video, GOES-East captured cumulus clouds east of the Caribbean Islands being carried west by the trade winds
  • Trade Winds, Horse Latitudes, and the Doldrums - ThoughtCo
    Blowing from the subtropical highs or horse latitudes toward the low pressure of the ITCZ are the trade winds Named from their ability to quickly propel trading ships across the ocean, the trade winds between about 30° latitude and the equator are steady and blow about 11 to 13 miles per hour
  • Trade Winds - globalsailingweather. com
    Trade winds were introduced in Chapter 1 (Global weather patterns) as the equatorward blowing part of the Hadley cell Because many cruising boats spend a lot of time in the trade wind region, some more detailed information is given in this chapter




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