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Most precipitation in the tropics appears to be convective; however, it has been suggested that stratiform precipitation also occurs. 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, 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 see katabatic wind on the descending and generally warming, leeward side where a rain shadow is observed.

Windward sides face the east to northeast trade winds and receive much more rainfall; leeward sides are drier and sunnier, with less rain and less cloud cover.

In South America, the Andes mountain range blocks Pacific moisture that arrives in that continent, resulting in a desertlike climate just downwind across western Argentina.

The wet, or rainy, season is the time of year, covering one or more months, when most of the average annual rainfall in a region falls.

Tropical rainforests technically do not have dry or wet seasons, since their rainfall is equally distributed through the year.

The wet season is a time when air quality improves, [55] freshwater quality improves, [56] [57] and vegetation grows significantly.

Tropical cyclones , a source of very heavy rainfall, consist of large air masses several hundred miles across with low pressure at the centre and with winds blowing inward towards the centre in either a clockwise direction southern hemisphere or counter clockwise northern hemisphere.

The fine particulate matter produced by car exhaust and other human sources of pollution forms cloud condensation nuclei , leads to the production of clouds and increases the likelihood of rain.

As commuters and commercial traffic cause pollution to build up over the course of the week, the likelihood of rain increases: In heavily populated areas that are near the coast, such as the United States' Eastern Seaboard , the effect can be dramatic: This extra heat leads to greater upward motion, which can induce additional shower and thunderstorm activity.

Increasing temperatures tend to increase evaporation which can lead to more precipitation. Globally there has been no statistically significant overall trend in precipitation over the past century, although trends have varied widely by region and over time.

Eastern portions of North and South America, northern Europe, and northern and central Asia have become wetter. The Sahel, the Mediterranean, southern Africa and parts of southern Asia have become drier.

There has been an increase in the number of heavy precipitation events over many areas during the past century, as well as an increase since the s in the prevalence of droughts—especially in the tropics and subtropics.

Over the contiguous United States, total annual precipitation increased at an average rate of 6. Analysis of 65 years of United States of America rainfall records show the lower 48 states have an increase in heavy downpour s since The largest increases are in the Northeast and Midwest, which in the past decade, have seen 31 and 16 percent more heavy downpours compared to the s.

Heavy downpour in the analysis are the days where total precipitation exceeded the top 1 percent of all rain and snow days during the years — [65] [66].

The most successful attempts at influencing weather involve cloud seeding , which include techniques used to increase winter precipitation over mountains and suppress hail.

Rainbands are cloud and precipitation areas which are significantly elongated. Rainbands can be stratiform or convective , [68] and are generated by differences in temperature.

When noted on weather radar imagery, this precipitation elongation is referred to as banded structure. Rainbands spawned near and ahead of cold fronts can be squall lines which are able to produce tornadoes.

If sea breeze rainbands become active enough just ahead of a cold front, they can mask the location of the cold front itself.

Once a cyclone occludes, a tr ough o f w arm air al oft, or " trowal " for short, will be caused by strong southerly winds on its eastern periphery rotating aloft around its northeast, and ultimately northwestern, periphery also known as the warm conveyor belt , forcing a surface trough to continue into the cold sector on a similar curve to the occluded front.

The trowal creates the portion of an occluded cyclone known as its comma head, due to the comma -like shape of the mid-tropospheric cloudiness that accompanies the feature.

It can also be the focus of locally heavy precipitation, with thunderstorms possible if the atmosphere along the trowal is unstable enough for convection.

Downwind of islands, bands of showers and thunderstorms can develop due to low level wind convergence downwind of the island edges. Offshore California , this has been noted in the wake of cold fronts.

Rainbands within tropical cyclones are curved in orientation. Tropical cyclone rainbands contain showers and thunderstorms that, together with the eyewall and the eye, constitute a hurricane or tropical storm.

The extent of rainbands around a tropical cyclone can help determine the cyclone's intensity. The phrase acid rain was first used by Scottish chemist Robert Augus Smith in Sulfuric acid is derived from natural sources such as volcanoes, and wetlands sulfate reducing bacteria ; and anthropogenic sources such as the combustion of fossil fuels, and mining where H 2 S is present.

Nitric acid is produced by natural sources such as lightning, soil bacteria, and natural fires; while also produced anthropogenically by the combustion of fossil fuels and from power plants.

In the past 20 years the concentrations of nitric and sulfuric acid has decreased in presence of rainwater, which may be due to the significant increase in ammonium most likely as ammonia from livestock production , which acts as a buffer in acid rain and raises the pH.

The Köppen classification depends on average monthly values of temperature and precipitation. The most commonly used form of the Köppen classification has five primary types labeled A through E.

Specifically, the primary types are A, tropical; B, dry; C, mild mid-latitude; D, cold mid-latitude; and E, polar. The five primary classifications can be further divided into secondary classifications such as rain forest , monsoon , tropical savanna , humid subtropical , humid continental , oceanic climate , Mediterranean climate , steppe , subarctic climate , tundra , polar ice cap , and desert.

They are widespread on Africa , and are also found in India , the northern parts of South America , Malaysia , and Australia. Most summer rainfall occurs during thunderstorms and from occasional tropical cyclones.

An oceanic or maritime climate is typically found along the west coasts at the middle latitudes of all the world's continents, bordering cool oceans, as well as southeastern Australia , and is accompanied by plentiful precipitation year-round.

The climate is characterized by hot, dry summers and cool, wet winters. Rain is measured in units of length per unit time, typically in millimeters per hour, [91] or in countries where imperial units are more common, inches per hour.

The standard way of measuring rainfall or snowfall is the standard rain gauge, which can be found in mm 4-in plastic and mm 8-in metal varieties.

Plastic gauges have markings on the inner cylinder down to 0. After the inner cylinder is filled, the amount inside it is discarded, then filled with the remaining rainfall in the outer cylinder until all the fluid in the outer cylinder is gone, adding to the overall total until the outer cylinder is empty.

Any of the above rain gauges can be made at home, with enough know-how. One of the main uses of weather radar is to be able to assess the amount of precipitations fallen over large basins for hydrological purposes.

Radar-derived rainfall estimates compliment surface station data which can be used for calibration.

To produce radar accumulations, rain rates over a point are estimated by using the value of reflectivity data at individual grid points.

A radar equation is then used, which is,. Rainfall intensity is classified according to the rate of precipitation, which depends on the considered time: Euphemisms for a heavy or violent rain include gully washer, trash-mover and toad-strangler.

The likelihood or probability of an event with a specified intensity and duration, is called the return period or frequency.

The Quantitative Precipitation Forecast abbreviated QPF is the expected amount of liquid precipitation accumulated over a specified time period over a specified area.

Terrain is considered in QPFs by use of topography or based upon climatological precipitation patterns from observations with fine detail.

The forecasts can be verified through use of rain gauge measurements, weather radar estimates, or a combination of both. Various skill scores can be determined to measure the value of the rainfall forecast.

Precipitation, especially rain, has a dramatic effect on agriculture. All plants need at least some water to survive, therefore rain being the most effective means of watering is important to agriculture.

While a regular rain pattern is usually vital to healthy plants , too much or too little rainfall can be harmful, even devastating to crops.

Drought can kill crops and increase erosion, [] while overly wet weather can cause harmful fungus growth. For example, certain cacti require small amounts of water, [] while tropical plants may need up to hundreds of inches of rain per year to survive.

In areas with wet and dry seasons, soil nutrients diminish and erosion increases during the wet season. The previous dry season leads to food shortages into the wet season, as the crops have yet to mature.

Cultural attitudes towards rain differ across the world. In temperate climates , people tend to be more stressed when the weather is unstable or cloudy, with its impact greater on men than women.

In dry places, such as India , [] or during periods of drought , [] rain lifts people's moods. In Botswana , the Setswana word for rain, pula , is used as the name of the national currency , in recognition of the economic importance of rain in its country, since it has a desert climate.

The source of this scent is petrichor , an oil produced by plants, then absorbed by rocks and soil, and later released into the air during rainfall.

Rain holds an important religious significance in many cultures. The northern half of Africa is occupied by the world's most extensive hot, dry region, the Sahara Desert.

Some deserts are also occupying much of southern Africa: Across Asia, a large annual rainfall minimum, composed primarily of deserts, stretches from the Gobi Desert in Mongolia west-southwest through western Pakistan Balochistan and Iran into the Arabian Desert in Saudi Arabia.

Most of Australia is semi-arid or desert, [] making it the world's driest inhabited continent. Since rain only falls as liquid, in frozen temperatures, rain cannot fall.

As a result, very cold climates see very little rainfall and are often known as polar deserts. A common biome in this area is the tundra which has a short summer thaw and a long frozen winter.

Ice caps see no rain at all, making Antarctica the world's driest continent. Rainforests are areas of the world with very high rainfall.

Both tropical and temperate rainforests exist. Tropical rainforests occupy a large band of the planet mostly along the equator.

Most temperate rainforests are located on mountainous west coasts between 45 and 55 degrees latitude, but they are often found in other areas.

The equatorial region near the Intertropical Convergence Zone ITCZ , or monsoon trough, is the wettest portion of the world's continents.

Annually, the rain belt within the tropics marches northward by August, then moves back southward into the Southern Hemisphere by February and March.

Its poleward progression is accelerated by the onset of the summer monsoon which is characterized by the development of lower air pressure a thermal low over the warmest part of Asia.

During the fall, winter, and spring , Pacific storm systems bring most of Hawaii and the western United States much of their precipitation.

There is also evidence that global warming is leading to increased precipitation to the eastern portions of North America, while droughts are becoming more frequent in the tropics and subtropics.

This amount is more than what falls in many cities in a year's time. Rainfalls of diamonds have been suggested to occur on the gas giant planets , Jupiter and Saturn , [] as well as on the ice giant planets , Uranus and Neptune.

From Wikipedia, the free encyclopedia. For other uses, see Rain disambiguation and Rainy disambiguation. Orographic lift , Precipitation types meteorology , and United States rainfall climatology.

Monsoon and Tropical cyclone. Global warming and Urban heat island. Rain gauge , Disdrometer , and Snow gauge. The heaviest rain is seen in reds and yellows.

Heavy rain in Glenshaw, Pennsylvania. The sound of a heavy rain fall in suburban neighborhood. List of rain deities. Polar desert and Polar climate.

Monsoon and Monsoon trough. Environment portal Ecology portal Water portal. Precipitation types Rain dust Rain sensor Rain water harvesting Rainbow Raining animals Red rain in Kerala Petrichor — the cause of the scent during and after rain Sanitary sewer overflow Sediment precipitation Water resources Weather Rainmaking Johad John Rainwater — pseudonymous mathematician.

Archived from the original on Archived from the original on November 26, Archived from the original PDF on Archived from the original on January 14, University of California in Los Angelese.

Meteorology at the Millennium. Archived from the original on June 3, Introduction to the Hydrosphere e.

Archived PDF from the original on Zentralanstalt für Meteorologie und Geodynamik. Raindrops are shaped like teardrops". United States Department of the Interior.

Houze Jr October Bulletin of the American Meteorological Society. Convective versus Stratiform Rains". Annual Review of Fluid Mechanics.

The Physics of Bubbles, Antibubbles, and all That. University Corporation for Atmospheric Research. National Oceanic and Atmospheric Administration.

The original coating has also had use in military and other government settings. The Australian military examined the effect of application of Rain-X and similar products to submarine antennae to improve signal transmission, although other coatings had longer lifespans when submerged in salt water.

It is also occasionally used in laboratory settings to silanise a surface. Ski and snowboard enthusiasts use Rain-X as "wax" to effectively overcome sticky wet snow common in spring conditions.

While skiing or riding on mountains with hard snow pack, the heat of the sun changes snow conditions starting on the lower slopes. Skis may suddenly slow down, throwing one off-balance, because of a change in surface tension, a sort of "sandpaper effect.

Rain-X's primary active ingredient are polysiloxanes , the primary one being hydroxy -terminated polydimethylsiloxane.

Rain-X was originally registered as a trademark in by Unelko and sold to Quaker State in On June 9, , Kraco Enterprises acquired the company.

Industrial Rain-X products were produced by Ecolab and used in carwashes and other industrial applications. From Wikipedia, the free encyclopedia.

Rain-X Product type Automotive aftermarket in glass care; other car care: Superhydrophobe and Lotus effect. Retrieved April 2, ITW Global Brands website.

Retrieved March 20, Archived from the original on 20 January Retrieved 8 December Journal of Agricultural and Food Chemistry.

US Patent B, description 4. Archived from the original on 27 April Patent and Trademark Office. Motor Sports News Wire.

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