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Two teachers, man-hungry Doris and restrained Marian, visit the Yorkshire moors a year after friend Evelyn disappeared there. On a stormy night, they take refuge in the isolated cottage of In Britain, a Manchester police inspector becomes obsessed with capturing a criminal who escapes from prison.

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Obviously this all going to end in tears at teatime. The downdraft will push down out of the thunderstorm, hit the ground and spread out.

This phenomenon is known as a downburst. The cool air carried to the ground by the downdraft cuts off the inflow of the thunderstorm, the updraft disappears and the thunderstorm will dissipate.

Thunderstorms in an atmosphere with virtually no vertical wind shear weaken as soon as they send out an outflow boundary in all directions, which then quickly cuts off its inflow of relatively warm, moist air, and kills the thunderstorm's further growth.

This can cause downbursts, a potential hazardous condition for aircraft to fly through, as a substantial change in wind speed and direction occurs, resulting in a decrease of airspeed and the subsequent reduction in lift for the aircraft.

The stronger the outflow boundary is, the stronger the resultant vertical wind shear becomes. There are four main types of thunderstorms: Which type forms depends on the instability and relative wind conditions at different layers of the atmosphere " wind shear ".

Single-cell thunderstorms form in environments of low vertical wind shear and last only 20—30 minutes. The supercell is the strongest of the thunderstorms, most commonly associated with large hail, high winds, and tornado formation.

Precipitable water values of greater than This term technically applies to a single thunderstorm with one main updraft. Also known as air-mass thunderstorms , these are the typical summer thunderstorms in many temperate locales.

They also occur in the cool unstable air that often follows the passage of a cold front from the sea during winter.

Within a cluster of thunderstorms, the term "cell" refers to each separate principal updraft. Thunderstorm cells occasionally form in isolation, as the occurrence of one thunderstorm can develop an outflow boundary that sets up new thunderstorm development.

Such storms are rarely severe and are a result of local atmospheric instability; hence the term "air mass thunderstorm". When such storms have a brief period of severe weather associated with them, it is known as a pulse severe storm.

Pulse severe storms are poorly organized and occur randomly in time and space, making them difficult to forecast.

This is the most common type of thunderstorm development. Mature thunderstorms are found near the center of the cluster, while dissipating thunderstorms exist on their downwind side.

Multicell storms form as clusters of storms but may then evolve into one or more squall lines. They often arise from convective updrafts in or near mountain ranges and linear weather boundaries, such as strong cold fronts or troughs of low pressure.

These type of storms are stronger than the single-cell storm, yet much weaker than the supercell storm. Hazards with the multicell cluster include moderate-sized hail, flash flooding, and weak tornadoes.

A squall line is an elongated line of severe thunderstorms that can form along or ahead of a cold front.

Supercell storms are large, usually severe , quasi-steady-state storms that form in an environment where wind speed or wind direction varies with height " wind shear " , and they have separate downdrafts and updrafts i.

In fact, research has shown that most tornadoes occur from this type of thunderstorm. A severe thunderstorm warning is issued if a thunderstorm becomes severe, or will soon turn severe.

However, multicell , supercell , and squall lines represent the most common forms of thunderstorms that produce severe weather.

A mesoscale convective system MCS is a complex of thunderstorms that becomes organized on a scale larger than the individual thunderstorms but smaller than extratropical cyclones , and normally persists for several hours or more.

Most mesoscale convective systems develop overnight and continue their lifespan through the next day. Forms of MCS that develop in the tropics are found in use either the Intertropical Convergence Zone or monsoon troughs , generally within the warm season between spring and fall.

More intense systems form over land than over water. They form at high latitudes during the cold season.

The two major ways thunderstorms move are via advection of the wind and propagation along outflow boundaries towards sources of greater heat and moisture.

Many thunderstorms move with the mean wind speed through the Earth's troposphere , the lowest 8 kilometres 5.

Weaker thunderstorms are steered by winds closer to the Earth's surface than stronger thunderstorms, as the weaker thunderstorms are not as tall.

Organized, long-lived thunderstorm cells and complexes move at a right angle to the direction of the vertical wind shear vector.

If the gust front, or leading edge of the outflow boundary, races ahead of the thunderstorm, its motion will accelerate in tandem. This is more of a factor with thunderstorms with heavy precipitation HP than with thunderstorms with low precipitation LP.

When thunderstorms merge, which is most likely when numerous thunderstorms exist in proximity to each other, the motion of the stronger thunderstorm normally dictates the future motion of the merged cell.

The stronger the mean wind, the less likely other processes will be involved in storm motion. On weather radar , storms are tracked by using a prominent feature and tracking it from scan to scan.

A back-building thunderstorm, commonly referred to as a training thunderstorm , is a thunderstorm in which new development takes place on the upwind side usually the west or southwest side in the Northern Hemisphere , such that the storm seems to remain stationary or propagate in a backward direction.

Though the storm often appears stationary on radar, or even moving upwind, this is an illusion. The storm is really a multi-cell storm with new, more vigorous cells that form on the upwind side, replacing older cells that continue to drift downwind.

In Rapid City, South Dakota , in , an unusual alignment of winds at various levels of the atmosphere combined to produce a continuously training set of cells that dropped an enormous quantity of rain upon the same area, resulting in devastating flash flooding.

Each year, many people are killed or seriously injured by severe thunderstorms despite the advance warning. While severe thunderstorms are most common in the spring and summer , they can occur at just about any time of the year.

Cloud-to-ground lightning frequently occurs within the phenomena of thunderstorms and have numerous hazards towards landscapes and populations.

One of the more significant hazards lightning can pose is the wildfires they are capable of igniting. Acid rain is also a frequent risk produced by lightning.

Distilled water has a neutral pH of 7. Acid rain can damage infrastructures containing calcite or certain other solid chemical compounds.

In ecosystems, acid rain can dissolve plant tissues of vegetations and increase acidification process in bodies of water and in soil , resulting in deaths of marine and terrestrial organisms.

Any thunderstorm that produces hail that reaches the ground is known as a hailstorm. Hail is more common along mountain ranges because mountains force horizontal winds upwards known as orographic lifting , thereby intensifying the updrafts within thunderstorms and making hail more likely.

Cheyenne, Wyoming is North America's most hail-prone city with an average of nine to ten hailstorms per season. Hail can cause serious damage, notably to automobiles , aircraft, skylights, glass-roofed structures, livestock , and most commonly, farmers' crops.

When hail stones exceed 13 millimetres 0. Wheat, corn, soybeans, and tobacco are the most sensitive crops to hail damage. One of the earliest recorded incidents occurred around the 9th century in Roopkund , Uttarakhand , India.

A tornado is a violent, rotating column of air in contact with both the surface of the earth and a cumulonimbus cloud otherwise known as a thundercloud or, in rare cases, the base of a cumulus cloud.

Tornadoes come in many sizes but are typically in the form of a visible condensation funnel , whose narrow end touches the earth and is often encircled by a cloud of debris and dust.

The Fujita scale and the Enhanced Fujita Scale rate tornadoes by damage caused. An EF0 tornado, the weakest category, damages trees but not substantial structures.

An EF5 tornado, the strongest category, rips buildings off their foundations and can deform large skyscrapers.

Waterspouts have similar characteristics as tornadoes, characterized by a spiraling funnel-shaped wind current that form over bodies of water, connecting to large cumulonimbus clouds.

Waterspouts are generally classified as forms of tornadoes, or more specifically, non- supercelled tornadoes that develop over large bodies of water.

Flash flooding is the process where a landscape, most notably an urban environment, is subjected to rapid floods. Flash floods are most common in densely populated urban environments, where few plants and bodies of water are present to absorb and contain the extra water.

Flash flooding can be hazardous to small infrastructure, such as bridges, and weakly constructed buildings. Plants and crops in agricultural areas can be destroyed and devastated by the force of raging water.

Automobiles parked within affected areas can also be displaced. Soil erosion can occur as well, exposing risks of landslide phenomena.

Downburst winds can produce numerous hazards to landscapes experiencing thunderstorms. Downburst winds are generally very powerful, and are often mistaken for wind speeds produced by tornadoes, [76] due to the concentrated amount of force exerted by their straight-horizontal characteristic.

Downburst winds can be hazardous to unstable, incomplete, or weakly constructed infrastructures and buildings.

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