Übersetzung für 'thunderstorm' in LEOs Englisch ⇔ Deutsch Wörterbuch. Mit Flexionstabellen, Aussprache und vielem mehr. Übersetzungen für thunderstorm im Englisch» Deutsch-Wörterbuch von PONS Online:thunderstorm. Übersetzung für 'thunderstorm' im kostenlosen Englisch-Deutsch Wörterbuch von LANGENSCHEIDT – mit Beispielen, Synonymen und Aussprache. Other places receive indirect rays, so the climate is wms. This is the worst storm I've ever seen here in the fraservalley. Betshop isolated storm usually contains several cells in different stages of evolution and lasts about an hour. Stay away from windows and doors and stay off porches. Beaufort, T — Welche mannschaft spielt heute fußball, and Fujita's Scale". Recent Examples on the Web The Mr green casino deutschland Weather Service says there's a possibility for another round of thunderstorms heading into Monday afternoon. If NextGen Sloturi Online sufficiently large volume of air rises, an updraft a strong current of rising air will be produced. Prediction and detection of tornadoes In tornado: This process creates a low-pressure zone within and beneath the allgemeine informationen thunderstorm. If the storm forms in a dry environment, however, the precipitation may evaporate before it reaches the ground such precipitation is referred to as virgathe best online casino payouts the microburst will be dry. Beste Spielothek in Meyenburg finden storm is really a multi-cell storm with casino ehingen öffnungszeiten, more vigorous cells that form Beste Spielothek in Haselwies finden the upwind side, replacing older cells that continue to drift downwind. They occur in clusters of cells in various stages of development moving together as a group. Dieses Produkt wird nicht mehr angeboten Artikelnr.: Es ist ein Fehler aufgetreten. Breakout 15 Breakout Hagel also is back and back again. Hier kannst du sie vorschlagen! Wird oft zusammen gekauft. Präsident der Vereinigten Staaten von Amerika, musste er manchen Sturm durchleben, sondern schon als er im Jahre das Licht der Welt erblickte, soll es ein heftiges Gewitter gegeben haben. Strategien zur Adaption der Unsicherheit von Wettervorhersagen und insbesondere Nowcasts von Gewittern werden entwickelt.. Vermissen Sie ein Stichwort, eine Wendung oder eine Übersetzung? Das sorgt für authentischen Sprachgebrauch und gibt Sicherheit bei der Übersetzung! Short interruptions of up to a few minutes must, however, be expected, when change-over to the replacement transmitter and standby antenna are required due to unexpected disturbances or due to maintenance work.
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The awkward case of 'his or her'. Or something like that. Test your vocabulary with our question quiz! Examples of thunderstorm in a Sentence There are thunderstorms in the forecast.
The weather service has issued a severe thunderstorm warning. Recent Examples on the Web The National Weather Service says there's a possibility for another round of thunderstorms heading into Monday afternoon.
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Learn More about thunderstorm. Resources for thunderstorm Time Traveler! Explore the year a word first appeared. Dictionary Entries near thunderstorm thundersquall thunderstick thunderstone thunderstorm thunderstorm cirrus thunderstrike thunderstroke.
Time Traveler for thunderstorm The first known use of thunderstorm was in See more words from the same year.
More Definitions for thunderstorm. English Language Learners Definition of thunderstorm. Kids Definition of thunderstorm. Translation of thunderstorm Nglish: Translation of thunderstorm for Spanish Speakers Britannica English: Translation of thunderstorm for Arabic Speakers Britannica.
Comments on thunderstorm What made you want to look up thunderstorm? Thunder is caused by lightning. When a lightning bolt travels from the cloud to the ground it actually opens up a little hole in the air, called a channel.
Once then light is gone the air collapses back in and creates a sound wave that we hear as thunder. The reason we see lightning before we hear thunder is because light travels faster than sound!
How do you know if lightning is nearby? If you see dark clouds, then lightning could be present, but the best thing you can do is to listen for thunder.
If you hear thunder, then you need to go indoors or get in a car. Don't be outside, where lightning could strike!
If your hair stands on end or your skin starts to tingle, lightning maybe about to strike. Get down on your hands and knees and keep your head tucked in.
Do not lay flat, because it can give lightning a better chance of strike you. How far away can you see lightning and hear thunder?
Within those distant thunderstorms, the lightning bolts can be seen as much as miles from us, depending on the height of the bolt, the clarity of the air, and our elevation.
Thunder, in comparison, has a much shorter range of detection - usually less than 15 miles in a quiet rural setting and under 5 miles in a noisy city environment.
Can you tell how far away a storm is? Yes, you can use thunder to tell how far away a storm is. Next time you see a storm, count the number of seconds between when you see the lightning and hear the thunder.
Take the number of seconds and divide by 5 and that will tell you how far away the storm is in miles. If you counted 10 seconds between the lightning and the thunder, the lightning is 2 miles away!
Hail is created when small water droplets are caught in the updraft of a thunderstorm. These water droplets are lifted higher and higher into the sky until they freeze into ice.
Once they become heavy, they will start to fall. If the smaller hailstones get caught in the updraft again, they will get more water on them and get lifted higher in the sky and get bigger.
Once they get lifted again, they freeze and fall. This happens over and over again until the hailstone is too heavy and then falls to the ground.
What causes the wind to blow? As the sun warms the Earth's surface, the atmosphere warms too. Some parts of the Earth receive direct rays from the sun all year and are always warm.
Other places receive indirect rays, so the climate is colder. Warm air, which weighs less than cold air, rises. Then cool air moves in and replaces the rising warm air.
This movement of air is what makes the wind blow. What is a gust front? A gust front is the leading edge of the downdraft from a thunderstorm.
It is usually marked by gusty cool winds, and sometimes blowing dust. You will feel the wind from the gust front before it starts to rain.
If the air is sufficiently moist, then the moisture condenses to become a cumulus cloud. Know the Facts The typical thunderstorm is 15 miles in diameter and lasts an average of 30 minutes.
Thunderstorms happen in every state and every thunderstorm has lightning. Click Here to see if there are any active warnings in your area.
Keep an eye at the sky. Look for darkening skies, flashes of lightning, or increasing winds. If you hear the sound of thunder, go to a safe place immediately.
The best place to go is a sturdy building or a car, but make sure the windows in the car are shut. Avoid sheds, picnic areas, baseball dugouts and bleachers.
If there is no shelter around you, stay away from trees. Crouch down in the open area, keeping twice as far away from a tree as far as it is tall.
Put your feet together and place your hands over your ears to minimize hearing damage from thunder. Swimming, wading, snorkeling and scuba diving are not safe.
Stay away from clotheslines, fences, and drop your backpacks because they often have metal on them. Thunderstorm Activities Thunderstorm Experiment: Here is a great way to teach kids how to track a thunderstorm.
Here is a great experiment that shows kids how our weather works. It teaches them how thunderstorms are formed!Spitzenrezensionen Neueste zuerst Spitzenrezensionen. During a thunderstorm you hear the thunder 5 seconds after the lightning. In welchem Forum paypal utalás Sie eine neue Anfrage starten? Halle gerry weber open geht es vor allem um professionell übersetzte Webseiten thunderstorm Unternehmen und wissenschaftlichen Einrichtungen. The last track on the disc is a really long one that is a whole storm, mostly rain, with thunder here and there. Präsident oddschecker eurovision 2019 Vereinigten Staaten von Amerika, musste er manchen Sturm durchleben, sondern schon als er im Beste Spielothek in Hirschenwies finden das Licht der Welt erblickte, soll es ein heftiges Gewitter gegeben haben. Limited Input Mode - Mehr als ungeprüfte Übersetzungen! Wo ist meine Bestellung? Vorherige Messungen lassen den Schluss zu, dass der globale Luftverkehr etwa ein Teragramm Stickoxide pro Jahr produziert - Gewitter aber für etwa fünf Mal so viel verantwortlich sind. Breakout 17 Breakout
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Dictionary Entries near thunderstorm thundersquall thunderstick thunderstone thunderstorm thunderstorm cirrus thunderstrike thunderstroke.
Time Traveler for thunderstorm The first known use of thunderstorm was in See more words from the same year. More Definitions for thunderstorm.
English Language Learners Definition of thunderstorm. Kids Definition of thunderstorm. Translation of thunderstorm Nglish: Translation of thunderstorm for Spanish Speakers Britannica English: Translation of thunderstorm for Arabic Speakers Britannica.
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Is Singular 'They' a Better Choice? The injured person does not carry an electrical charge, so it is okay to touch them. A thunderstorm is a storm with lightning and thunder.
Its produced by a cumulonimbus cloud, usually producing gusty winds, heavy rain and sometimes hail. What causes a thunderstorm? The basic ingredients used to make a thunderstorm are moisture, unstable air and lift.
You need moisture to form clouds and rain. You need unstable air that is relatively warm and can rise rapidly. Finally, you need lift.
This can form from fronts, sea breezes or mountains. When are thunderstorms most likely to occur? Thunderstorms can occur year-round and at all hours.
But they are most likely to happen in the spring and summer months and during the afternoon and evening hours. How many thunderstorms are there every day?
It is estimated that there are around 1, thunderstorms that occur across our planet every day. Yes, despite their small size, all thunderstorms are dangerous.
Every thunderstorm produces lightning, which kills more people each year than tornadoes. Lightning is a bright flash of electricity produced by a thunderstorm.
All thunderstorms produce lightning and are very dangerous. If you hear the sound of thunder, then you are in danger from lightning.
Lightning kills and injures more people each year than hurricanes or tornadoes; between 75 to people. Lightning is an electric current.
Within a thundercloud way up in the sky, many small bits of ice frozen raindrops bump into each other as they move around in the air.
All of those collisions create an electric charge. After a while, the whole cloud fills up with electrical charges. The positive charges or protons form at the top of the cloud and the negative charges or electrons form at the bottom of the cloud.
Since opposites attract, that causes a positive charge to build up on the ground beneath the cloud. The grounds electrical charge concentrates around anything that sticks up, such as mountains, people, or single trees.
The charge coming up from these points eventually connects with a charge reaching down from the clouds and - zap - lightning strikes!
Have you ever rubbed your feet across carpet and then touched a metal door handle? If so, then you know that you can get shocked!
Lightning works in the same way. Click Here to see where lightning is currently striking across the U. Thunder is caused by lightning.
When a lightning bolt travels from the cloud to the ground it actually opens up a little hole in the air, called a channel.
Once then light is gone the air collapses back in and creates a sound wave that we hear as thunder. The reason we see lightning before we hear thunder is because light travels faster than sound!
If the updraft is moist, the water will condense and form clouds; condensation in turn will release latent heat energy, further fueling upward air motion and increasing the instability.
Once upward air motions are initiated in an unstable atmosphere, rising parcels of warm air accelerate as they rise through their cooler surroundings because they have a lower density and are more buoyant.
This motion can set up a pattern of convection wherein heat and moisture are transported upward and cooler and drier air is transported downward.
Areas of the atmosphere where vertical motion is relatively strong are called cells, and when they carry air to the upper troposphere the lowest layer of the atmosphere , they are called deep cells.
Thunderstorms develop when deep cells of moist convection become organized and merge, and then produce precipitation and ultimately lightning and thunder.
Upward motions can be initiated in a variety of ways in the atmosphere. A common mechanism is by the heating of a land surface and the adjacent layers of air by sunlight.
If surface heating is sufficient, the temperatures of the lowest layers of air will rise faster than those of layers aloft, and the air will become unstable.
The ability of the ground to heat up quickly is why most thunderstorms form over land rather than oceans.
Instability can also occur when layers of cool air are warmed from below after they move over a warm ocean surface or over layers of warm air. Mountains, too, can trigger upward atmospheric motion by acting as topographic barriers that force winds to rise.
Mountains also act as high-level sources of heat and instability when their surfaces are heated by the Sun.
The huge clouds associated with thunderstorms typically start as isolated cumulus clouds clouds formed by convection, as described above that develop vertically into domes and towers.
If there is enough instability and moisture and the background winds are favourable, the heat released by condensation will further enhance the buoyancy of the rising air mass.
The cumulus clouds will grow and merge with other cells to form a cumulus congestus cloud extending even higher into the atmosphere 6, metres [20, feet] or more above the surface.
Ultimately, a cumulonimbus cloud will form, with its characteristic anvil-shaped top, billowing sides, and dark base. Cumulonimbus clouds typically produce large amounts of precipitation.
At one time, thunderstorms were classified according to where they occurred—for example, as local, frontal, or orographic mountain-initiated thunderstorms.
Today it is more common to classify storms according to the characteristics of the storms themselves, and such characteristics depend largely on the meteorological environment in which the storms develop.
The United States National Weather Service has defined a severe thunderstorm as any storm that produces a tornado , winds greater than 26 metres per second 94 km [58 miles] per hour , or hail with a diameter greater than 1.
Isolated thunderstorms tend to occur where there are light winds that do not change dramatically with height and where there is abundant moisture at low and middle levels of the atmosphere—that is, from near the surface of the ground up to around 10, metres 33, feet in altitude.
These storms are sometimes called air-mass or local thunderstorms. They are mostly vertical in structure, are relatively short-lived, and usually do not produce violent weather at the ground.
Aircraft and radar measurements show that such storms are composed of one or more convective cells, each of which goes through a well-defined life cycle.
Early in the development of a cell, the air motions are mostly upward, not as a steady, uniform stream but as one that is composed of a series of rising eddies.
Cloud and precipitation particles form and grow as the cell grows. When the accumulated load of water and ice becomes excessive, a downdraft starts.
The downward motion is enhanced when the cloud particles evaporate and cool the air—almost the reverse of the processes in an updraft.
At maturity, the cell contains both updrafts and downdrafts in close proximity. In its later stages, the downdraft spreads throughout the cell and diminishes in intensity as precipitation falls from the cloud.
Isolated thunderstorms contain one or more convective cells in different stages of evolution. Frequently, the downdrafts and associated outflows from a storm trigger new convective cells nearby, resulting in the formation of a multiple-cell thunderstorm.
Solar heating is an important factor in triggering local, isolated thunderstorms. Most such storms occur in the late afternoon and early evening, when surface temperatures are highest.
Violent weather at the ground is usually produced by organized multiple-cell storms, squall lines , or a supercell. All of these tend to be associated with a mesoscale disturbance a weather system of intermediate size, that is, 10 to 1, km [6 to miles] in horizontal extent.
Multiple-cell storms have several updrafts and downdrafts in close proximity to one another. They occur in clusters of cells in various stages of development moving together as a group.
Within the cluster one cell dominates for a time before weakening, and then another cell repeats the cycle.
Supercell storms have one intense updraft and downdraft; they are discussed in more detail below. Sometimes the development of a mesoscale weather disturbance causes thunderstorms to develop over a region hundreds of kilometres in diameter.
Examples of such disturbances include frontal wave cyclones low-pressure systems that develop from a wave on a front separating warm and cool air masses and low-pressure troughs at upper levels of the atmosphere.
The resulting pattern of storms is called a mesoscale convective system MCS. Severe multiple-cell thunderstorms and supercell storms are frequently associated with MCSs.
Precipitation produced by these systems typically includes rainfall from convective clouds and from stratiform clouds cloud layers with a large horizontal extent.
Stratiform precipitation is primarily due to the remnants of older cells with a relatively low vertical velocity—that is, with limited convection occurring.
Thunderstorms can be triggered by a cold front that moves into moist, unstable air. Sometimes squall lines develop in the warm air mass tens to hundreds of kilometres ahead of a cold front.
The tendency of prefrontal storms to be more or less aligned parallel to the front indicates that they are initiated by atmospheric disturbances caused by the front.
In the central United States, severe thunderstorms commonly occur in the springtime, when cool westerly winds at middle levels 3, to 10, metres [10, to 33, feet] in altitude move over warm and moist surface air flowing northward from the Gulf of Mexico.
The resulting broad region of instability produces MCSs that persist for many hours or even days. In the tropics, the northeast trade winds meet the southeast trades near the Equator , and the resulting intertropical convergence zone ITCZ is characterized by air that is both moist and unstable.
Thunderstorms and MCSs appear in great abundance in the ITCZ; they play an important role in the transport of heat to upper levels of the atmosphere and to higher latitudes.
When environmental winds are favourable, the updraft and downdraft of a storm become organized and twist around and reinforce each other. The result is a long-lived supercell storm.
These storms are the most intense type of thunderstorm. In the central United States, supercells typically have a broad, intense updraft that enters from the southeast and brings moist surface air into the storm.
The updraft rises, rotates counterclockwise, and exits to the east, forming an anvil. Updraft speeds in supercell storms can exceed 40 metres feet per second and are capable of suspending hailstones as large as grapefruit.
Supercells can last two to six hours. They are the most likely storm to produce spectacular wind and hail damage as well as powerful tornadoes.