How to Say Cloud in Different Languages

Cloud in Different Languages: A cloud is an air-suspended mass of water drops or ice crystals. Water is absorbed in the atmosphere and clouds are created. The condensation reveals water vapors. Several different kinds of clouds occur. Clouds are a significant weather and climate part of Earth. Cloud is a stream made of a transparent mass of minute liquid droplets, frozen ice, or other objects released from the celestial body’s atmosphere or related vacuum.

How to Say Cloud in 88 Different Languages

Different LanguagesWord Cloud
Albanianre
Basquehodei
Belarusianвоблака
Bosnianoblak
Bulgarianоблак
Catalannúvol
Croatianoblak
Czechmrak
DanishSky
Dutchwolk
Estonianpilv
Finnishpilvi
Frenchnuage
Galiciannube
GermanWolke
Greekσύννεφο (sýnnefo)
Hungarianfelhő
IcelandicSký
Irishscamall
Italiannube
Latvianmākonis
Lithuaniandebesis
Macedonianоблак
Maltesesħaba
NorwegianSky
PolishChmura
Portuguesenuvem
Romaniannor
Russianоблако (oblako)
Serbianоблак (oblak)
Slovakmrak
Slovenianoblak
Spanishnube
Swedishmoln
Ukrainianхмара (khmara)
Welshcloud
Yiddishוואָלקן
Armenianամպ
Azerbaijanibulud
Bengaliমেঘ
Chinese Simplified云 (yún)
Chinese Traditional雲 (yún)
Georgiancloud
Gujaratiવાદળ
Hindiबादल
Hmonghuab
Japanese
Kannadaಮೋಡದ
Kazakhбұлт
Khmerពពក
Korean구름 (guleum)
Laoຟັງ
Malayalamമേഘം
Marathiढग
Mongolianүүл
Myanmar (Burmese)မိုဃ်းတိမ်ကို
Nepaliबादल
Sinhalaවලාකුළු
Tajikабр
Tamilமேகம்
Teluguక్లౌడ్
Thaiเมฆ
Turkishbulut
Urduبادل
Uzbekbulut
Vietnameseđám mây
Arabicغيم (ghym)
Hebrewענן
Persianابر
Afrikaanswolk
Chichewamtambo
Hausagirgijen
Igboígwé ojii
Sesotholeru
Somalidaruur
Swahiliwingu
Yorubaawọsanma
Zuluifu
Cebuanopanganod
Filipinoulap
Indonesianawan
Javanesemaya
Malagasyrahona
Malayawan
Maorikapua
Esperantonubo
Haitian Creolenwaj
Latinnubes

Droplets and crystals can contain water or numerous other chemicals. On the planet, when the air gets cooled down into its dew point, or when the water vapor (usually) gets enough moisture from an adjacent source to increase the dew to the ambient temperature, form as a result of air saturation.

The clouds have two major variables-location and shape-in their grouping. Large clouds form in the atmosphere many kilometers high, with the precise height dependent on their temperatures. Low clouds usually form within one to two kilometers of the surface of the Earth. However, when called fog, low clouds can even reach the ground.

Cirrus clouds are small and wispy and often bend with the breeze between high and low clouds. Cumulus clouds are usually wide and lightweight. These clouds look some sort of like giant balls of cotton or other forms of sky. This kind can also shape parallel strips of clouds as an intermediate level cloud. The clouds of Stratus form cloud sheets.

In the clouds the bulk of water is in very tiny droplets, but sometimes they accumulate more water They then become larger drops Gravity causes them to slip into the air more rapidly when this happens. The drops of water are pouring with rain. The water will shape into snowflakes when it’s colder. Clouds may also induce rain or sleet freezing.

Such arise when the snow melts on the field, then cold again. In harder conditions, hail falls Air currents make it rain and snow in the clouds. They get colder and become ice as they pass. The ice chunks grow larger as they pass. At last, they land like hail on the field.

For many causes, clouds are important. Precipitation, whether rain or snow, is one of those reasons. In the evening clouds reflect heat back into the surface and keep warmer.

Leave a Reply

Your email address will not be published. Required fields are marked *