AIR | वायु | Vaayu
Air masses influence the climate in various manners. In this exercise, you will find out about the various sorts of air masses found on Earth and how the development of air masses makes changes in the climate.
वायु द्रव्यमान विभिन्न तरीकों से मौसम को प्रभावित करते हैं। इस पाठ में, आप पृथ्वी पर पाए जाने वाले विभिन्न प्रकार के वायु द्रव्यमानों के बारे में जानेंगे और कैसे वायु द्रव्यमानों की गति मौसम में बदलाव लाती है।
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Types of Air Masses | एयर मास के प्रकार | Eyar Maas Ke Prakaar
Normally 4 Types of Air Masses But We are lear 6 types of Air Masses
- Continental Polar | महाद्वीपीय ध्रुवीय
- Continental Arctic | महाद्वीपीय आर्कटिक
- Continental Antarctic | महाद्वीपीय अंटार्कटिक
- Continental Tropical | महाद्वीपीय उष्णकटिबंधीय
- Maritime Polar | समुद्री ध्रुवीय
- Maritime Tropical | समुद्री उष्णकटिबंधीय
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Air Mass Definition | एयर मास परिभाषा | eyar maas paribhaasha
An air mass is a collection of air that expands evenly; inside that level group of air, temperature, and dampness re the equivalent/comparable. These masses of air structure when air is stale (otherwise known as sits still) over a specific uniform territory for a significant stretch of time.
एक वायु द्रव्यमान हवा का एक शरीर है जो क्षैतिज रूप से फैलता है; हवा के उस क्षैतिज शरीर के भीतर, तापमान और आर्द्रता समान / समान होती है। वायु का ये द्रव्यमान तब होता है जब एक निश्चित समयावधि के दौरान एक लंबे समय के लिए हवा स्थिर रहती है (उर्फ बैठता है)।
It takes on temperature and dampness dependent on what region of the outside of the earth the mass is situated over. They're then ready to be arranged dependent on the area of the mass, what sort of land/water/surface it's situated over and the qualities it takes on from those areas (temperature, heat, dampness, and so forth).
यह तापमान और नमी के आधार पर लेता है कि पृथ्वी की सतह के किस क्षेत्र पर द्रव्यमान तैनात है। वे तब द्रव्यमान के स्थान के आधार पर वर्गीकृत होने में सक्षम होते हैं, यह किस तरह की भूमि / पानी / सतह पर स्थित है और उन स्थानों (तापमान, गर्मी, नमी, आदि) से इसकी विशेषता है।
Peruse progressively about air mass impacts the atmosphere. वायु द्रव्यमान के बारे में और अधिक पढ़ें
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Continental Polar | महाद्वीपीय ध्रुवीय
The mainland polar air mass structures over an enormous, subpolar land zone. It is cold and stable and has low mugginess. This sort of air mass makes freezing winter climate without precipitation or mists. It is regularly answerable for long virus spells that bring about harvest harm as far south as Florida. Throughout the late spring, this sort of air mass can carry cooling help toward the northern United States with its virus air and winds.
Peruse progressively about how air mass impacts the climate of the pacific coast.
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Continental Arctic | महाद्वीपीय आर्कटिक
The mainland Arctic air mass grows just in the winter over huge territories of day office. It is very cold and dry because of freezing conditions close to the polar hover, caused to some degree by polar evenings, which are times of 24-hour dimness. This air mass can create record-breaking cold temperatures in Canada and the United States.
Continental Antarctic | महाद्वीपीय अंटार्कटिक
As the name proposes, the mainland Antarctic air mass structures exclusively over Antarctica. It is steady, very cold, and amazingly dry. It has colder temperatures than some other air mass during any season. Travel over the sea adjusts this air mass. When it arrives at land in the Southern Hemisphere, it normally changes order to sea polar as it is not, at this point over the antarctic source surface region.
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Continental Tropical | महाद्वीपीय उष्णकटिबंधीय
Mainland tropical air is created over the world's deserts, including the Sahara, Arabian and Australian deserts. The southwestern desert in the U.S. is additionally a wellspring of this sort of air mass throughout the late spring. The air mass is hot and has incredibly low stickiness. It influences summer climate and is fit for causing dry spell in the event that it waits over a locale. Warmth waves that bring about human and creature passings can be brought about by this air mass.
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Maritime Polar | समुद्री ध्रुवीय
The sea polar air mass structures over chilly, polar seas. It is cool and clammy and can make the mellow climate in beachfront zones relying upon the season. In the winter, it produces a hotter climate when the surface temperature of the sea is higher than the land temperature. In mid-year, it brings a cooler climate when the sea is colder than the landmass.
Maritime Tropical | समुद्री उष्णकटिबंधीय
The chief kind of sea air is sea tropical. This exceptionally warm and sticky air mass creates over tropical and subtropical oceans and seas. It makes blustery conditions east of the Rocky Mountains in the winter, especially in the southeastern United States.
Answer Any One Following Question in the comment section.
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- How do you describe the air?
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