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    Wind up deutsch

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    Übersetzungen für wind up im Englisch» Deutsch-Wörterbuch von PONS Online: to wind up ⇆ sth, to wind up a car window, to wind up a clock/watch, to wind up. Lernen Sie die Übersetzung für 'wind-up' in LEOs Englisch ⇔ Deutsch Wörterbuch. Mit Flexionstabellen der verschiedenen Fälle und Zeiten ✓ Aussprache und. Englisch-Deutsch-Übersetzungen für to wind up im Online-Wörterbuch blogt.nu ( Deutschwörterbuch). Hör mal, du willst doch nicht einfach in alte Verhaltensmuster zurückfallen , nur weil du wütend bist und dann einen Kerl verprügelst, der in einem nur winzig kleinen Moment eine schlechte Entscheidung getroffen hat. Can wind-up stand a…. Es werden teilweise auch Cookies von Diensten Dritter gesetzt. And when that's done, t… 5 Antworten wind up Letzter Beitrag: Es werden teilweise auch Cookies von Diensten Dritter gesetzt. You just wind up and do it. Intransitives Verb wind-up I. English I have received seven motions for resolutions to wind up this debate. Mr Moore, if you do not want to wind up in detention with the rest of our disloyal officers, you will respect my wishes. Can wind-up stand a…. Allgemein "make tense" "with key etc. English to wind up sb. And when that's done, t… 5 Antworten wind up Letzter Beitrag:

    Trevor threw shame to the winds and scandalized the Misses Brewster then and there by proclaiming his father to have been a country storekeeper.

    The translations below need to be checked and inserted above into the appropriate translation tables, removing any numbers. Numbers do not necessarily match those in definitions.

    See instructions at Wiktionary: Something higher must lie at the back of that eager response to pack-music and winded horn — something born of the smell of the good earth.

    Please wind that old-fashioned alarm clock. Vines wind round a pole. The river winds through the plain.

    Judge Short had gone to town, and Farrar was off for a three days' cruise up the lake. I was bitterly regretting I had not gone with him when the distant notes of a coach horn reached my ear, and I descried a four-in-hand winding its way up the inn road from the direction of Mohair.

    Quickly she slammed the door shut and panicking wound the window up as fast as her slippery fingers would allow. 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 , [66] weather fronts, areas of locally higher low level winds referred to as low level jets, near mountains, [67] radiation inversions that occur because of clear skies and calm winds, buildings, [68] wind turbines , [69] 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, [92] 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.

    Unusual mechanisms of wind dispersal include tumbleweeds. A related process to anemochory is anemophily , which is the process where pollen is distributed by wind.

    Large families of plants are pollinated in this manner, which is favored when individuals of the dominant plant species are spaced closely together.

    Wind also limits tree growth. On coasts and isolated mountains, the tree line is often much lower than in corresponding altitudes inland and in larger, more complex mountain systems, because strong winds reduce tree growth.

    High winds scour away thin soils through erosion, [] as well as damage limbs and twigs. When high winds knock down or uproot trees, the process is known as windthrow.

    Wind can also cause plants damage through sand abrasion. Such windblown sand causes extensive damage to plant seedlings because it ruptures plant cells, making them vulnerable to evaporation and drought.

    Using a mechanical sandblaster in a laboratory setting, scientists affiliated with the Agricultural Research Service studied the effects of windblown sand abrasion on cotton seedlings.

    The study showed that the seedlings responded to the damage created by the windblown sand abrasion by shifting energy from stem and root growth to the growth and repair of the damaged stems.

    Pikas use a wall of pebbles to store dry plants and grasses for the winter in order to protect the food from being blown away.

    Their cerci are very sensitive to the wind, and help them survive half of their attacks. Wind causes the generation of sound. The movement of air causes movements of parts of natural objects, such as leaves or grass.

    These objects will produce sound if they touch each other. Even a soft wind will cause a low level of environmental noise.

    If the wind is blowing harder, it may produce howling sounds of varying frequencies. This may be caused by the wind blowing over cavities, or by vortices created in the air downstream of an object.

    Examples of these parts are balconies, ventilation openings, roof openings or cables. High winds are known to cause damage, depending upon the magnitude of their velocity and pressure differential.

    Wind pressures are positive on the windward side of a structure and negative on the leeward side. When wind gusts are at a similar frequency to the swaying of the bridge, the bridge can be destroyed more easily, such as what occurred with the Tacoma Narrows Bridge in Winds of this strength due to downsloped winds off terrain have been known to shatter windows and sandblast paint from cars.

    The Saffir—Simpson scale and Enhanced Fujita scale were designed to help estimate wind speed from the damage caused by high winds related to tropical cyclones and tornadoes , and vice versa.

    The blast wave is similar to a strong wind gust over the ground. Wildfire intensity increases during daytime hours. For example, burn rates of smoldering logs are up to five times greater during the day because of lower humidity, increased temperatures, and increased wind speeds.

    Wildfires are fanned by these winds and often follow the air currents over hills and through valleys. The solar wind is quite different from a terrestrial wind, in that its origin is the sun, and it is composed of charged particles that have escaped the sun's atmosphere.

    Similar to the solar wind, the planetary wind is composed of light gases that escape planetary atmospheres. Over long periods of time, the planetary wind can radically change the composition of planetary atmospheres.

    The fastest wind ever recorded is coming from the accretion disc of the IGR J black hole. The hydrodynamic wind within the upper portion of a planet's atmosphere allows light chemical elements such as hydrogen to move up to the exobase , the lower limit of the exosphere , where the gases can then reach escape velocity , entering outer space without impacting other particles of gas.

    This type of gas loss from a planet into space is known as planetary wind. It consists mostly of electrons and protons with energies of about 1 keV.

    The stream of particles varies in temperature and speed with the passage of time. These particles are able to escape the sun's gravity , in part because of the high temperature of the corona , [] but also because of high kinetic energy that particles gain through a process that is not well understood.

    The solar wind creates the Heliosphere , a vast bubble in the interstellar medium surrounding the Solar System. From Wikipedia, the free encyclopedia.

    This is the latest accepted revision , reviewed on 3 November For other uses, see Wind disambiguation.

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