Rain is liquid water in the form of

Rain is liquid water in the form of droplets that have condensed fromatmospheric water vapor and then precipitated—that is, become heavy enough to fall under gravity. Rain is a major component of thewater cycle and is responsible for depositing most of the fresh wateron the Earth. It provides suitable conditions for many types ofecosystems, as well as water for hydroelectric power plants and cropirrigation.
The major cause of rain production is moisture moving along three-dimensional zones of temperature and moisture contrasts known asweather 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 withinwindward 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.[citation needed] 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).[1] Climate classification systems such as theKöppen climate 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.
Rain is also known or suspected on other planets, where it may be composed of methane, neon, sulfuric acid or even iron rather than water.

Results (Indonesian) 1:

Rain is liquid water in the form of droplets that have condensed fromatmospheric water vapor and then precipitated—that is, become heavy enough to fall under gravity. Rain is a major component of thewater cycle and is responsible for depositing most of the fresh wateron the Earth. It provides suitable conditions for many types ofecosystems, as well as water for hydroelectric power plants and cropirrigation.The major cause of rain production is moisture moving along three-dimensional zones of temperature and moisture contrasts known asweather 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 withinwindward 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.Efek urban heat island mengarah ke peningkatan curah hujan, baik dalam jumlah dan intensitas, melawan arah angin dari kota. Pemanasan global juga menyebabkan perubahan dalam pola curah hujan secara global, termasuk kondisi basah di seluruh Amerika Utara bagian Timur dan kondisi kering di daerah tropis. [rujukan?] Antartika adalah benua terkering. Global rata-rata tahunan curah hujan atas tanah yang 715 mm (28.1 in), tetapi atas seluruh bumi jauh lebih tinggi di 990 mm (39 in). [1] iklim klasifikasi sistem seperti sistem klasifikasi iklim theKöppen menggunakan curah hujan tahunan rata-rata untuk membantu membedakan antara rezim iklim yang berbeda. Curah hujan diukur dengan menggunakan alat pengukur hujan. Jumlah curah hujan dapat diperkirakan oleh radar cuaca.Hujan juga dikenal atau dicurigai di planet lain, di mana ia mungkin terdiri dari metana, neon, asam sulfat atau bahkan besi daripada air.

Results (Indonesian) 2:

Hujan air cair dalam bentuk tetesan yang kental uap air fromatmospheric dan kemudian diendapkan-yaitu, menjadi cukup berat untuk jatuh di bawah gravitasi. Hujan adalah komponen utama dari siklus thewater dan bertanggung jawab untuk menyetorkan sebagian besar wateron segar Bumi. Ini menyediakan kondisi yang cocok untuk berbagai jenis ofecosystems, serta air untuk pembangkit listrik tenaga air dan cropirrigation.
Penyebab utama produksi hujan kelembaban bergerak sepanjang zona tiga dimensi dari suhu dan kelembaban kontras dikenal asweather bidang. Jika cukup kelembaban dan gerakan ke atas hadir, curah hujan jatuh dari awan konvektif (orang-orang dengan gerak vertikal yang kuat ke atas) seperti cumulonimbus (awan petir) yang dapat mengatur ke dalam ikatan hujan sempit. Di daerah pegunungan, hujan deras bisa terjadi jika aliran atas lembah dimaksimalkan withinwindward sisi medan di ketinggian yang memaksa udara lembap mengembun dan jatuh sebagai hujan di sepanjang sisi pegunungan. Di sisi bawah angin gunung, iklim gurun bisa eksis karena udara kering yang disebabkan oleh aliran lereng bawah yang menyebabkan pemanasan dan pengeringan massa udara. Pergerakan palung monsun, atau zona konvergensi intertropis, membawa musim hujan ke iklim sabana.
Efek pulau panas perkotaan menyebabkan peningkatan curah hujan, baik dalam jumlah dan intensitas, arah angin dari kota. Pemanasan global juga menyebabkan perubahan pola curah hujan secara global yang, termasuk kondisi basah di bagian timur Amerika Utara dan kondisi kering di daerah tropis. [Rujukan?] Antartika adalah benua terkering yang. Secara global rata-rata curah hujan tahunan atas tanah adalah 715 mm (28,1 in), tapi seluruh bumi itu jauh lebih tinggi di 990 mm ​​(39 in). [1] sistem klasifikasi iklim seperti theKöppen sistem klasifikasi iklim menggunakan curah hujan tahunan rata-rata untuk membantu membedakan antara yang berbeda rezim iklim. Curah hujan diukur dengan menggunakan alat pengukur hujan. Jumlah curah hujan dapat diperkirakan dengan radar cuaca.
Hujan juga diketahui atau diduga di planet lain, di mana ia dapat terdiri dari metana, neon, asam sulfat atau bahkan besi daripada air.