U+26C6 Rain
U+26C6 was added in Unicode version 5.2 in 2009. It belongs to the block
This character is a Other Symbol and is commonly used, that is, in no specific script. Znak jest również znany jako rainy weather.
The glyph is not a composition. Its width in East Asian texts is determined by its context. It can be displayed wide or narrow. In bidirectional text it acts as Other Neutral. When changing direction it is not mirrored. U+26C6 offers a line break opportunity at its position, except in some numeric contexts.
Wikipedia ma następujące informacje na temat tej współrzędnej kodowej:
Rain is water droplets that have condensed from atmospheric water vapor and then fall under gravity. Rain is a major component of the water cycle and is responsible for depositing most of the fresh water on the Earth. It provides water for hydroelectric power plants, crop irrigation, and suitable conditions for many types of ecosystems.
The major cause of rain production is moisture moving along three-dimensional zones of temperature and moisture contrasts known as weather fronts. If enough moisture and upward motion is present, precipitation falls from convective clouds (those with strong upward vertical motion) such as cumulonimbus (thunder clouds) which can organize into narrow rainbands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation which forces moist air to condense and fall out as rainfall along the sides of mountains. On the leeward side of mountains, desert climates can exist due to the dry air caused by downslope flow which causes heating and drying of the air mass. The movement of the monsoon trough, or intertropical convergence zone, brings rainy seasons to savannah climes.
The urban heat island effect leads to increased rainfall, both in amounts and intensity, downwind of cities. Global warming is also causing changes in the precipitation pattern globally, including wetter conditions across eastern North America and drier conditions in the tropics. Antarctica is the driest continent. The globally averaged annual precipitation over land is 715 mm (28.1 in), but over the whole Earth, it is much higher at 990 mm (39 in). Climate classification systems such as the Köppen classification system use average annual rainfall to help differentiate between differing climate regimes. Rainfall is measured using rain gauges. Rainfall amounts can be estimated by weather radar.
Reprezentacje
System | Reprezentacje |
---|---|
Nº | 9926 |
UTF-8 | E2 9B 86 |
UTF-16 | 26 C6 |
UTF-32 | 00 00 26 C6 |
Adres URL cytowany | %E2%9B%86 |
HTML hex reference | ⛆ |
Błędne windows-1252 Mojibake | ⛆ |
alias | rainy weather |
Gdzie indziej
Kompletny opis
Właściwość | Wartość |
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5.2 (2009) | |
RAIN | |
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