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The Earth's precipitation occurs through convectional, orographic, or frontal mechanisms. Convectional precipitation happens when warm air rises, cools, and forms clouds. Orographic precipitation occurs when moist air is forced to rise over a mountain, leading to cooling and rainfall. Finally, frontal precipitation happens at the boundary of two air masses with different temperatures and moisture levels, causing the warm air to rise and condense into precipitation.
Klerksdorp, South Africa has an average annual precipitation rate of around 400-500 millimeters per year.
Precipitation is all the rain, snow, sleet, drizzle, hail, etc. that comes from the sky and give moisture to earth, helping all plants and animals, and people as well. Then, the water cycle starts all over again, with Evaporation, then Condensation, and back to Precipitation.
A month is considered to be dry when the level of precipitation falls below the average amount of rainfall. This level is said to be 60 milliliters or 2.4 inches.
deserts are regions with the common characteristics of less than 250mm of precipitation per year throughout the whole area. it may be a hot and dry land, but there are also cold deserts and littoral deserts, which are not consistently hot. In addition, the aridity of the desert is dependent not only on precipitation but on evaporation and transpiration. If less water is evaporated or transpired from the region than is precipitated into the region, it can not be a desert.
Temperature and precipitation are the two main characteristics of a region's climate. Temperature helps determine the overall warmth or coldness of an area, while precipitation refers to the amount of rainfall or snowfall the region receives.
Temperature and Precipitation.
there's much precipitation and there's much wind.
average teperature and precipitation.
average teperature and precipitation.
All deserts have low precipitation and high evaporation rates.
Tage Andersson has written: 'Some characteristics of temperature and precipitation in Sweden' -- subject(s): Atmospheric temperature, Climatology, Precipitation (Meteorology), Statistical methods 'Swedish temperature and precipitation records since the middle of the 19th century' -- subject(s): Atmospheric temperature, Observations, Precipitation (Meteorology)
Some of the characteristics that distinguish the different forms of precipitation are: Whether is falls in liquid form (rain) or frozen form (snow) and whether it freezes while falling to the ground (hail, sleet) or freezes once it is on the ground (freezing rain), Wet snow is distinguished from snow by the amount of water in the snow. To learn more about precipitation, visit the Related Link.
Some of the characteristics that distinguish the different forms of precipitation are: Whether is falls in liquid form (rain) or frozen form (snow) and whether it freezes while falling to the ground (hail, sleet) or freezes once it is on the ground (freezing rain), Wet snow is distinguished from snow by the amount of water in the snow. To learn more about precipitation, visit the Related Link.
Climates can be categorized by temperature and precipitation patterns. These two features together help define the characteristics of different climate zones around the world.
River regime can describe one of two characteristics of a reach of a river: * The variability in its discharge throughout the course of a year in response to precipitation, temperature, evapotranspiration, and drainage basin characteristics
average teperature and precipitation.