What is Katabatic wind and Anabatic wind mostly seen in mountainous regions
A katabatic wind is a cold, heavy wind that flows downhill from high mountains. An anabatic wind is a warm wind that moves uphill during
the daytime.
🏔️ Katabatic Wind – Cold Wind Coming Down. 🔽 What is it? A katabatic wind is a cold, heavy wind that flows downhill from high mountains or plateaus . ❄️ How is it formed? At night, mountain tops lose heat quickly (radiation cooling). The air becomes cold and dense . This cold, heavy air slides down the slopes into valleys due to gravity. 🧊 Features: Happens mostly at night . Cold and dry wind. Can be very strong (like in Antarctica or Greenland). 🌍 Examples: Mistral Wind in France Bora Wind in Europe Chinook (partially katabatic) in North America 🏞️ Anabatic Wind – Warm Wind Going Up 🔼 What is it? An anabatic wind is a warm wind that moves uphill during the daytime . 🌞 How is it formed? During the day, sun heats the mountain slopes . Air near the slopes becomes warmer and lighter . This warm air rises up the slope . 🔥 Features: Happens mostly in daytime . Warm and moist wind. Helps in forming clouds and rainfall on mountain tops. 🌍 Examples: Common in Himalayas , Alps , and Rockies during summer days. 🧠 Easy Way…