Saturday, August 10, 2019

weather repot and rain fall statistics

Precipitation is liquid water in the form of droplets that have dropped from atmospheric water vapor and then become heavy enough to fall under gravity.  Rain is a major component of the water cycle and is responsible for storing most of the fresh water on Earth.  It provides the right conditions for many types of ecosystems, as well as hydroelectric power plants and water for crop irrigation.

  The main cause of rainfall production is the increase of humidity with three-dimensional areas of temperature and the contrast of humidity called the weather front.  If sufficient moisture and upward motion are present, it is possible to rain from compressed clouds (strong wind waves.), Such as cumulonimbus, which can be arranged in narrow rainbands.  In mountainous areas, heavy rainfall is possible where upscale flow is maximized on the side of the terrain wind at high pressure which forces the moist air to condense and rains along the sides of the mountains.  To the left of the mountains, the desert climate may exist due to the dry air caused by the downslope flow, which causes the mass of the air to warm and dry.  The monsoon trough, or movement of the interglacial convergence zone, brings the asons of rain to the climax of Savannah.
  The effect of the urban heat island is downwind into cities, increasing in both proportion and intensity.  Global warming is changing the pattern of rainfall globally, including damp conditions in northeastern North America and drying conditions in tropical areas.  Antarctica is the driest continent.  The average annual rainfall globally over the land is 715 mm (28.1 inches), but it is much higher at 990 mm (39 inches) across the earth.  [1] Climate classification systems such as the Kahn Penn classification system use average annual rainfall to help distinguish between different climate regimes.  Rainfall measurements are made using rage gauges.  The rainfall ratios can be estimated by the weather radar.
  Heavy rain on the desert at sunset
  Rain is also known or suspected on other planets, where it may be made of methane, neon, sulfuric acid or iron instead of water.

  southern Estonia, it is raining on the plains
  The air contains water vapor, and the amount of water in a given mass of dry air, known as the mixing ratio, is measured in kilograms of water per dry air (g / kg).  [5] []] The moisture content in the air is generally referred to as relative humidity;  Which can hold a percentage of the vapor air of a certain water at a certain weather temperature.  []] The amount of water vapor that the air parcel holds before it is saturated (100% relative humidity) and formed in a cloud (a group of small water and ice particles appearing suspended above the earth's surface) []] depends on its temperature.  Hot air may include more water vapor than cold air before it is saturated.  Therefore, one way to satisfy the parcel of air is to cool it.  The dew point is the temperature at which the parcel must be cooled to get saturated.  []]
  There are four main mechanisms for cooling air over its mist: adiabatic cooling, conductive cooling, radiative cooling, and evaporative cooling.  Adiabatic cooling occurs when air rises and expands.  []] Aviation can increase due to physical obstruction such as large-scale atmospheric motion or mountain (orographic lift).  Convection cools when air is exposed to cold surfaces, [8] usually blowing from one surface to another, for example from liquid water surface to cold soil.  Radical cooling is caused by the emission of infrared radiation, through the air or below the surface.  []] Evaporation is cooled when moisture is added to the air by evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation.

  One of the main ways to add water vapor to the air is: in the area of ​​wind conversion
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