emoji 🌤 sun behind small cloud svg png

“🌤” meaning: sun behind small cloud Emoji

Copy and paste this emoji: 🌤 Copy

  • 9.1+

    iOS 🌤Minimum display requirements

  • 6.0.1+

    Android 🌤Minimum display requirements

  • 10+

    Windows 🌤Minimum display requirements

🌤Meaning and Description

The golden sun ☀️ hides behind a small light blue cloud ☁️. The position of the sun vary from platform to platform, with some behind the left side of the clouds and some behind the right side of the clouds.
This emoji can represent sunny weather with occasional clouds and a good mood is slightly affected by a small matter. Similar emojis: ⛅🌥

💡Extended reading and popular science

The meaning of emoji symbol 🌤 is sun behind small cloud, it is related to cloud, sun, it can be found in emoji category: "🚌 Travel & Places" - "☂️ sky & weather".

The current 🌤 is a basic Emoji without variant symbols, and there are two Emoji variation sequences corresponding to it: 🌤️ (emoji style, displaying colorful symbols on most new platforms) and 🌤︎ (text style, displaying black and white symbols on some old platforms).

🔸 🌤 (1F324) There is no Emoji version of this Unicode character, which means that on most mobile phones or computer systems, the character can only be displayed in black and white character style, but in a few good compatibility platforms, it can still display color picture style. The Unicode organization does not yet recommend its use as a universal emoji symbol.

🌤 (1F324) - unqualified Emoji, See also: 🌤️ (1F324 FE0F) - fully-qualified Emoji.

Wikipedia: 🌤 Cloud
In meteorology, a cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body or similar space. Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere, which includes the troposphere, stratosphere, and mesosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology. There are two methods of naming clouds in their respective layers of the homosphere, Latin and common. Genus types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adoption of Luke Howard's nomenclature that was formally proposed in 1802. It became the basis of a modern international system that divides clouds into five physical forms which can be further divided or classified into altitude levels to derive ten basic genera. The main representative cloud types for each of these forms are stratus, cirrus, stratocumulus, cumulus, and cumulonimbus. Low-level clouds do not have any altitude-related prefixes. However mid-level stratiform and stratocumuliform types are given the prefix alto- while high-level variants of these same two forms carry the prefix cirro-. Genus types with sufficient vertical extent to occupy more than one level do not carry any altitude related prefixes. They are classified formally as low- or mid-level depending on the altitude at which each initially forms, and are also more informally characterized as multi-level or vertical. Most of the ten genera derived by this method of classification can be subdivided into species and further subdivided into varieties. Very low stratiform clouds that extend down to the Earth's surface are given the common names fog and mist, but have no Latin names. In the stratosphere and mesosphere, clouds have common names for their main types. They may have the appearance of stratiform veils or sheets, cirriform wisps, or stratocumuliform bands or ripples. They are seen infrequently, mostly in the polar regions of Earth. Clouds have been observed in the atmospheres of other planets and moons in the Solar System and beyond. However, due to their different temperature characteristics, they are often composed of other substances such as methane, ammonia, and sulfuric acid, as well as water. Tropospheric clouds can have a direct effect on climate change on Earth. They may reflect incoming rays from the sun which can contribute to a cooling effect where and when these clouds occur, or trap longer wave radiation that reflects back up from the Earth's surface which can cause a warming effect. The altitude, form, and thickness of the clouds are the main factors that affect the local heating or cooling of Earth and the atmosphere. Clouds that form above the troposphere are too scarce and too thin to have any influence on climate change. Clouds are the main uncertainty in climate sensitivity.Tabular overview The table that follows is very broad in scope. It draws from several methods of cloud classification, both formal and informal, used in different levels of the Earth's homosphere by a number of cited authorities. Despite some differences in nomenclature, the classification schemes seen in this article can be combined by using an informal cross-classification of physical forms and altitude levels to derive the 10 tropospheric genera, the fog and mist that forms at surface level, and several additional major types above the troposphere. The cumulus genus includes four species that indicate vertical size and structure which can affect both forms and levels. This table should not be seen as a strict or singular classification, but as an illustration of how various major cloud types are related to each other and defined through a full range of altitude levels from Earth's surface to the "edge of space." For another tabular overview that also covers the entire homosphere, see Cloud genera and selected species, supplementary features, and other airborne hydrometeors (located just below the bottom of the article). 🔗 Cloud
🌐: سحاب, Bulud, Облак, মেঘ, Oblak, Oblak, Sky (meteorologi), Wolke, Νέφος, Nube, Pilv, ابر, Pilvi, Nuage, ענן, बादल, Oblaci, Felhő, Awan, Nuvola, 雲, ღრუბელი, Бұлттар, 구름, Debesis, Mākoņi, Awan, Wolk, Sky, Chmura (meteorologia), Nuvem, Nor, Облака, Oblak, Oblak, Retë, Облак, Moln, เมฆ, Bulut, Хмара, Mây, 云.

🌤Examples and Usage

🔸 Today the sun is ☀️ too big, so the small cloud 🌤 cannot cover it at all.
🔸 It is a good day 🌤 , but the restaurant 🍜 I often go to is closed. What a pity!


🔸 🌤 (1F324) + emoji style (FE0F) = 🌤️ (1F324 FE0F)
🔸 🌤 (1F324) + text style (FE0E) = 🌤︎ (1F324 FE0E)

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🌤Basic Information

Emoji: 🌤
Shortname: sun behind small cloud
Codepoint: U+1F324 Copy
Decimal: ALT+127780
Unicode Version: 7.0 (2014-06-16)
Emoji Version: None
Categories: 🚌 Travel & Places
Sub Categories: ☂️ sky & weather
Keywords: cloud | sun | sun behind small cloud

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