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What is the horse latitude?

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is it a low pressure region or high pressure region

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  1. Horse latitudes or Subtropical High are subtropic latitudes between 30 and 35 degrees both north and south. This region, under a ridge of high pressure called the Subtropical ridge, is an area which receives little precipitation and has variable winds mixed with calm. The term "Horse Latitudes" may owe its name to the fact that early colonialist sailors would accidentally come too close to the center of the Atlantic Ocean while crossing it and get stuck in this belt of calm weather where winds tend to lift off the water instead of blowing across it, along with little current. The confused sea, muggy heat, and rolling and pitching of waves (variably stilled and aerated by winds) often slowed colonial ships for days to weeks due to lack of propulsion. The crew would throw horses overboard in order to conserve water and food. This also reduced the weight of the ship, thereby lightening the load and increased the speed of the ship in the low winds.

    The consistently warm, dry conditions of the horse latitudes also contribute to the existence of temperate deserts, such as the Sahara Desert in Africa, the southwestern United States and northern Mexico, and parts of the Middle East in the Northern Hemisphere, and the Atacama Desert, the Kalahari Desert, and the Australian Desert in the Southern Hemisphere.


  2. The horse latitudes are areas of high pressure and are found in both the northern and southern hemispheres, at 30 - 35 degrees latitude.

  3. Its a ridge of high pressure )called the subtropical ridge) between 30 and 35 degrees north and south.

    Its also an area which receives little precipitation and has variable winds mixed with calm.  The terminology dates back to the 1400s.

    Funny theory is that it got its name because ships would get stuck there (no wind to push the boats) so the sailors would throw horses overboard to save food and water and taking weight off the ship meaning less wind was needed to move it.

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