what direction is kona winds?
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“Kona” is Polynesian word for “leeward.” Kona winds come from the opposite direction of the trades — from the south- and west-facing leeward sides. They can be h3 and gusty, and bring warm and muggy conditions to Hawaii.” Many locals dread the Kona winds.
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The strait runs in a general NW-SE direction, with the South Island on the west side and North Island on the east. At its narrowest point, 22 kilometres (14 mi) separate Cape Terawhiti in the North Island from Perano Head on Arapaoa Island in the Marlborough Sounds.
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June is still early for Meltemi winds, and when they do blow strong it's usually only for a day or two at a time. Actually the winds are a blessing, because that's what keeps the Cyclades cooler than the mainland.
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Yet people often stumble on the concept that "current direction" tells you which way the ebb or flood is going (setting). So a "North wind" is coming from the north which means the air is blowing to the south, but a current that "sets North" means the water is flowing to the north.
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An island's windward side faces the prevailing, or trade, winds, whereas the island's leeward side faces away from the wind, sheltered from prevailing winds by hills and mountains. As trade winds blow across the ocean, they pick up moist air from the water.
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What are the trade winds? The trade winds are just air movements toward the equator. They are warm, steady breezes that blow almost continuously. The Coriolis Effect makes the trade winds appear to be curving to the west, whether they are traveling to the equator from the south or north.
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The prevailing winds at the horse latitudes vary, but are usually light. Even strong winds are often short in duration. Trade winds are the powerful prevailing winds that blow from the east across the tropics. Trade winds are generally very predictable.
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The rising air mass finally subsides in what is known as the horse latitudes, where the air moves downward toward Earth's surface. Because the air circulates in an upward direction, there is often little surface wind in the ITCZ. ... And that's why they call it the doldrums.
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6- Strong breeze, 25-31 mph. ... 8 – Gale, 39-46 mph. People have difficulty walking and have to lean to move in the wind, perhaps being blown about a bit.
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The direction of surface currents would then align with this general wind pattern. But because Earth rotates, circulating air is deflected toward the right in the Northern Hemisphere and toward the left in the Southern Hemisphere, resulting in curved paths. This deflection is called the Coriolis Effect.
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The global wind system is created by air blowing from areas of high pressure to areas of low pressure. Winds are affected by the Coriolis effect. In the Northern Hemisphere the Coriolis effect deflects movement to the right and in the Southern Hemisphere it deflects movement to the left.
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Trade winds. two bells of winds that blow almost constantly from easterly directions and are located on the north and south sides of the subtropical. Westerlies. the dominant west to east motion of the atmosphere that characterized the regions on the poleward side of the subtropical highs.
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A variety of instruments can be used to measure wind direction, such as the windsock and wind vane. Both of these instruments work by moving to minimize air resistance. The way a weather vane is pointed by prevailing winds indicates the direction from which the wind is blowing.
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The wind belts have names. The Trade Winds are nearest the Equator. The next belt is the westerlies. Finally are the polar easterlies.
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Wind speed describes how fast the air is moving past a certain point. ... Wind direction describes the direction on a compass from which the wind emanates, for instance, from the North or from the West.
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The wind vane is another weather instrument. This instrument is used to measure the direction of the wind.
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On the surface, wind moves away from high pressure (High) and toward low pressure (Low). Convergence occurs near the equator (winds blow in towards one another) and Divergence occurs under the descending air that forms high-pressure belts.