How the Water Cycle Works | Solar e

How the Water Cycle Works | Solar energy evaporates exposed water from seas, lakes, rivers, and wet soil; the majority of this evaporation takes place over the seas. Water is also released into the atmosphere by the plants through photosynthesis.

During this process, known as evaporate transpiration, water vapour rises into the atmosphere. Clouds form when air becomes saturated with water vapour. The two major types of cloud formation are stratified or layered grey clouds called stratus and billowing white or dark grey cloud called cumulus clouds.

Precipitation as rain, or hail ensures that water returns to Earth’s surface in a fresh form. Some of this rain, however, falls into the seas and is not accessible to humans. When rain falls, it either washes down hill slopes or seeps underground; when snow and hail melts, this water may also sink into the ground.

Rain fall also replenishes river water supplies, as does underground water. Snow fall may consolidate into glaciers and ice sheets which, when they melt, release their water into the ground, into stream or into the seas.

During this process, known as evaporate transpiration, water vapour rises into the atmosphere. Clouds form when air becomes saturated with water vapour. The two major types of cloud formation are stratified or layered grey clouds called stratus and billowing white or dark grey cloud called cumulus clouds.

Precipitation as rain, or hail ensures that water returns to Earth’s surface in a fresh form. Some of this rain, however, falls into the seas and is not accessible to humans. When rain falls, it either washes down hill slopes or seeps underground; when snow and hail melts, this water may also sink into the ground.

Rain fall also replenishes river water supplies, as does underground water. Snow fall may consolidate into glaciers and ice sheets which, when they melt, release their water into the ground, into stream or into the seas.

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តើធ្វើដូចម្តេចវដ្តទឹកដែលបានធ្វើការ | ហួតទឹកបានថាមពលពន្លឺព្រះអាទិត្យបានលាតត្រដាងពីសមុទ្រ, បឹង, ទន្លេនិងដីសើម; ភាគច្រើននៃហួតនេះកើតឡើងនៅលើសមុទ្រ។ ទឹកគឺត្រូវបានចេញផ្សាយផងដែរក្នុងបរិយាកាសដោយរុក្ខជាតិតាមរយៈការធ្វើរស្មីសំយោគ។ ក្នុងកំឡុងពេលដំណើរការនេះគេស្គាល់ថាជា transpiration ហួត, ចំហាយទឹកបានកើនឡើងចូលទៅក្នុងបរិយាកាស។ មានពពកបង្កើតបានជាពេលដែលខ្យល់ក្លាយជា saturated ជាមួយចំហាយទឹក។ ប្រភេទដ៏សំខាន់ចំនួនពីរនៃការបង្កើតពពកពពកពណ៌ប្រផេះ stratified ស្រទាប់គេហៅថា stratus ឬ billowing ពពកពណ៌ប្រផេះនិងពណ៌សឬខ្មៅងងឹតបានហៅ cumulus ពពក។ កម្រិតទឹកភ្លៀងជាភ្លៀងឬការធ្លាក់ដុំព្រិលទឹកធានាបានថាការត្រឡប់មកវិញទៅលើផ្ទៃផែនដីនៅក្នុងសំណុំបែបបទស្រស់មួយ។ ចំនួននៃការមានភ្លៀងធ្លាក់នេះទោះយ៉ាងណាក៏ធ្លាក់ចូលទៅក្នុងសមុទ្រនិងមិនអាចចូលដំណើរការទៅមនុស្ស។ ពេលភ្លៀងធ្លាក់នោះវាលាងសមាតទាំងចុះជម្រាលភ្នំឬនៅក្រោមដីនាំ! នៅពេលព្រិលនិងធ្លាក់ដុំព្រិល melts ទឹកនេះក៏អាចធ្លាក់ចូលទៅក្នុងដី។ ការធ្លាក់ភ្លៀងក៏បានបំពេញឡើងវិញនូវការផ្គត់ផ្គង់ទឹកទន្លេនិងទឹកក្រោមដីដែលជាធ្វើ។ ការធ្លាក់ព្រិលប្រហែលជាការផ្គុំចូលទៅក្នុងផ្ទាំងទឹកកកនិងសន្លឹកទឹកកកដែលនៅពេលដែលពួកគេបានរលាយបញ្ចេញទឹករបស់ពួកគេចូលទៅក្នុងដីទៅក្នុងស្ទ្រីមឬការចូលទៅក្នុងសមុទ្រ។

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