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Lesbians Belle and Muse Masturbating. The trade winds also called trades are the prevailing pattern of easterly surface winds found in the tropics towards the Earth's equator.
A monsoon is a seasonal prevailing wind that lasts for several months within tropical regions. The term was first used in English in India, Bangladesh , Pakistan, and neighboring countries to refer to the big seasonal winds blowing from the Indian Ocean and Arabian Sea in the southwest bringing heavy rainfall to the area.
These prevailing winds blow from the west to the east,   and steer extratropical cyclones in this general manner.
The winds are predominantly from the southwest in the Northern Hemisphere and from the northwest in the Southern Hemisphere. Together with the trade winds , the westerlies enabled a round-trip trade route for sailing ships crossing the Atlantic and Pacific Oceans, as the westerlies lead to the development of strong ocean currents on the western sides of oceans in both hemispheres through the process of western intensification.
The westerlies can be particularly strong, especially in the southern hemisphere, where there is less land in the middle latitudes to cause the flow pattern to amplify, which slows the winds down.
The polar easterlies, also known as Polar Hadley cells, are dry, cold prevailing winds that blow from the high-pressure areas of the polar highs at the north and south poles towards the low-pressure areas within the Westerlies at high latitudes.
Unlike the Westerlies, these prevailing winds blow from the east to the west, and are often weak and irregular. In coastal regions, sea breezes and land breezes can be important factors in a location's prevailing winds.
The sea is warmed by the sun more slowly because of water's greater specific heat compared to land. The warm air is less dense than the surrounding environment and so it rises.
The cooler air above the sea, now with higher sea level pressure , flows inland into the lower pressure, creating a cooler breeze near the coast.
When large-scale winds are calm, the strength of the sea breeze is directly proportional to the temperature difference between the land mass and the sea.
At night, the land cools off more quickly than the ocean because of differences in their specific heat values. This temperature change causes the daytime sea breeze to dissipate.
When the temperature onshore cools below the temperature offshore, the pressure over the water will be lower than that of the land, establishing a land breeze, as long as an onshore wind is not strong enough to oppose it.
Over elevated surfaces, heating of the ground exceeds the heating of the surrounding air at the same altitude above sea level , creating an associated thermal low over the terrain and enhancing any thermal lows that would have otherwise existed,   and changing the wind circulation of the region.
In areas where there is rugged topography that significantly interrupts the environmental wind flow, the wind circulation between mountains and valleys is the most important contributor to the prevailing winds.
Hills and valleys substantially distort the airflow by increasing friction between the atmosphere and landmass by acting as a physical block to the flow, deflecting the wind parallel to the range just upstream of the topography, which is known as a barrier jet.
If there is a pass in the mountain range, winds will rush through the pass with considerable speed because of the Bernoulli principle that describes an inverse relationship between speed and pressure.
The airflow can remain turbulent and erratic for some distance downwind into the flatter countryside. These conditions are dangerous to ascending and descending airplanes.
In Europe, similar winds are known as the Bora , Tramontane , and Mistral. When these winds blow over open waters, they increase mixing of the upper layers of the ocean that elevates cool, nutrient rich waters to the surface, which leads to increased marine life.
In mountainous areas, local distortion of the airflow becomes severe. Jagged terrain combines to produce unpredictable flow patterns and turbulence, such as rotors , which can be topped by lenticular clouds.
Strong updrafts , downdrafts and eddies develop as the air flows over hills and down valleys. Orographic precipitation occurs on the windward side of mountains and is caused by the rising air motion of a large-scale flow of moist air across the mountain ridge, also known as upslope flow, resulting in adiabatic cooling and condensation.
In mountainous parts of the world subjected to relatively consistent winds for example, the trade winds , a more moist climate usually prevails on the windward side of a mountain than on the leeward or downwind side.
Moisture is removed by orographic lift, leaving drier air on the descending and generally warming, leeward side where a rain shadow is observed.
These winds are warm and dry. In Europe downwind of the Alps , they are known as foehn. In Poland, an example is the halny wiatr.
In Argentina, the local name for downsloped winds is zonda. In Java, the local name for such winds is koembang. In New Zealand, they are known as the Nor'west arch , and are accompanied by the cloud formation they are named after that has inspired artwork over the years.
Downslope winds also occur in the foothills of the Appalachian mountains of the United States,  and they can be as strong as other downslope winds  and unusual compared to other foehn winds in that the relative humidity typically changes little due to the increased moisture in the source air mass.
As described earlier, prevailing and local winds are not spread evenly across the earth, which means that wind speeds also differ by region.
In addition, the wind speed also increases with the altitude. Nowadays, a yardstick used to determine the best locations for wind energy development is referred to as wind power density WPD.
It is a calculation relating to the effective force of the wind at a particular location, frequently expressed in terms of the elevation above ground level over a period of time.
It takes into account wind velocity and mass. The larger the WPD calculation, the higher it is rated by class.
Wind shear, sometimes referred to as windshear or wind gradient , is a difference in wind speed and direction over a relatively short distance in the Earth's atmosphere.
Wind shear itself is a microscale meteorological phenomenon occurring over a very small distance, but it can be associated with mesoscale or synoptic scale weather features such as squall lines and cold fronts.
It is commonly observed near microbursts and downbursts caused by thunderstorms ,  weather fronts, areas of locally higher low level winds referred to as low level jets, near mountains,  radiation inversions that occur because of clear skies and calm winds, buildings,  wind turbines ,  and sailboats.
Sound movement through the atmosphere is affected by wind shear, which can bend the wave front, causing sounds to be heard where they normally would not, or vice versa.
As a natural force, the wind was often personified as one or more wind gods or as an expression of the supernatural in many cultures. Vayu is the Hindu God of Wind.
The ancient Greeks also observed the seasonal change of the winds, as evidenced by the Tower of the Winds in Athens.
According to legend, he was present at the creation of the world and first let the winds out of his bag to clear the world of mist. He is said to be the ancestor grandfather of the winds of the eight directions.
The term is first known to have been used as the name of a pair or series of typhoons that are said to have saved Japan from two Mongol fleets under Kublai Khan that attacked Japan in and again in Grains of sand whirled by the wind blinded the soldiers and created electrical disturbances that rendered compasses useless.
There are many different forms of sailing ships, but they all have certain basic things in common. Except for rotor ships using the Magnus effect , every sailing ship has a hull , rigging and at least one mast to hold up the sails that use the wind to power the ship.
For aerodynamic aircraft which operate relative to the air, winds affect groundspeed,  and in the case of lighter-than-air vehicles, wind may play a significant or solitary role in their movement and ground track.
While taking off with a tailwind may be necessary under certain circumstances, a headwind is generally desirable. A tailwind increases takeoff distance required and decreases the climb gradient.
Historically, the ancient Sinhalese of Anuradhapura and in other cities around Sri Lanka used the monsoon winds to power furnaces as early as BCE.
A rudimentary windmill was used to power an organ in the first century CE. These were vertical-axle windmills, which had long vertical driveshafts with rectangle shaped blades.
High altitude wind power is the focus of over 30 companies worldwide using tethered technology rather than ground-hugging compressive-towers.
Wind figures prominently in several popular sports, including recreational hang gliding , hot air ballooning , kite flying, snowkiting , kite landboarding , kite surfing , paragliding , sailing , and windsurfing.
In gliding, wind gradients just above the surface affect the takeoff and landing phases of flight of a glider. Wind gradient can have a noticeable effect on ground launches , also known as winch launches or wire launches.
If the wind gradient is significant or sudden, or both, and the pilot maintains the same pitch attitude, the indicated airspeed will increase, possibly exceeding the maximum ground launch tow speed.
The pilot must adjust the airspeed to deal with the effect of the gradient. As the glider descends through the wind gradient on final approach to landing, airspeed decreases while sink rate increases, and there is insufficient time to accelerate prior to ground contact.
The pilot must anticipate the wind gradient and use a higher approach speed to compensate for it. In arid climates, the main source of erosion is wind.
Westerly winds in the mid-latitudes of the planet drive the movement of ocean currents from west to east across the world's oceans.
Wind has a very important role in aiding plants and other immobile organisms in dispersal of seeds, spores, pollen, etc. Although wind is not the primary form of seed dispersal in plants, it provides dispersal for a large percentage of the biomass of land plants.
Erosion can be the result of material movement by the wind. There are two main effects. First, wind causes small particles to be lifted and therefore moved to another region.
This is called deflation. Second, these suspended particles may impact on solid objects causing erosion by abrasion ecological succession.
Wind erosion generally occurs in areas with little or no vegetation, often in areas where there is insufficient rainfall to support vegetation.
An example is the formation of sand dunes , on a beach or in a desert. Loess often stands in either steep or vertical faces. Under appropriate climatic conditions, areas with loess are among the most agriculturally productive in the world.
Therefore, windbreaks such as big trees and bushes are often planted by farmers to reduce the wind erosion of loess. During mid-summer July in the northern hemisphere , the westward-moving trade winds south of the northward-moving subtropical ridge expand northwestward from the Caribbean into southeastern North America.
When dust from the Sahara moving around the southern periphery of the ridge within the belt of trade winds moves 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.
There are local names for winds associated with sand and dust storms. The Calima carries dust on southeast winds into the Canary islands.
Wind dispersal of seeds, or anemochory , is one of the more primitive means of dispersal. Wind dispersal can take on one of two primary forms: An important constraint on wind dispersal is the need for abundant seed production to maximize the likelihood of a seed landing in a site suitable for germination.
There are also strong evolutionary constraints on this dispersal mechanism. For instance, species in the Asteraceae on islands tended to have reduced dispersal capabilities i.
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