Valley and Mountain Breezes

Two related, localized winds occur one after the other on a daily cycle: the mountain breeze and the valley breeze. Their strength and size are different from the anabatic and katabatic winds. Each of these winds blows in the opposite direction. Mountain wind blows from the mountains to the valley in downward direction after sunset, when the mountains cool off, and the valley is comparatively warmer. The mountain breeze diagram below makes it easy to understand the direction and flow of the mountain breeze and valley breeze. 

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Definition of Mountain Breeze and Valley Breeze

Mountain Breeze: The definition of mountain breeze can be understood easily if you understand the meaning of valley breeze. A valley wind occurs when warm air rises to the valley floor from the surrounding mountains and hills during the day. A mountain breeze is produced by cooler, denser air sliding down the slopes at night. Mountains and valleys breezes form in a similar way to sea breezes and land breezes.

Valley Breeze: The wind that blows up a valley or mountain slope without cyclonic or anticyclonic wind, caused by warming of the mountainside and valley floor from the sun, is known as valley breeze. 

Difference Between Valley and Mountain Breezes

A valley and mountain breezes are localized winds that occur one after the other within 24 hours. Both the terms are related but different from each other. Valley breezes occur during day time, and mountain breezes occur at night. On a sunny day, the mountain air rapidly heats up while the valley remains relatively cool. As a result, there is a breeze in the valley because of convection. However, at night, it is reversed. As the slopes cool at night, the dense air from the mountains descends into the valley. This occurs most often when the weather is clear and calm. In the afternoons and at night, there is a breeze in the valley. The valley walls cool quickly during this time, cooling an air layer next to the slope. Mountain breezes (gravity or drainage winds) are caused by this cold and dense air moving down the valley. 

Another example of geography-related local winds is a mountain breeze or valley breeze. Campers in mountainous regions may experience a warm afternoon quickly changing into a cold night upon setting the sun. Each morning, as the sun rises, it warms the air along the mountain slopes. Mountain slopes are warmed by this warm air, causing a valley breeze. At night, the air cools along the mountain slopes. A mountain breeze is produced by the cool air that moves down the slopes.

Types of Breeze

You are probably already aware that a breeze is a light wind. Did you know, however, there are many types of breezes? Let's take a tour of each type, so pack your bags, and let's go! 

• Mountain Breeze: When the sun goes down, and at night, the airflow changes direction. It is because the slopes of the mountains at higher elevations cool more quickly than the valleys. A cooler, denser air flows down the mountainside and back into the valley at higher elevations. These winds are known as mountain breezes. 

• Valley Breeze: On the slopes of the mountains and in the valley during the daytime, the sun warms the land and the air. Warmer and less dense air near the ground rises at midday, allowing more air to pass through the valley floor. Valley breezes are the result of this gentle air movement.

• Land Breeze: Heat rises faster on the land, as does cooling. Thus, land and sand cool down before the water after sunset. A low-pressure system over the sea is created when land air is cooler than sea air at this time. As a result, land air moves into the sea. As the name suggests, the Land breeze is the wind or breeze blowing from land towards the sea. You can also call it an offshore breeze. It usually occurs during the early morning or night when the land air is cooler than the sea air.

• Sea Breeze: The land air heats up more quickly than the sea air when the sun is up in the sky. Consequently, the sea air at this time is heavier and cooler, and it flows to land. The sea breeze is the breeze or wind that blows from the sea towards the land. Usually, it blows during the summer months. This breeze is also referred to as an onshore breeze.

Local Winds in Geography

Depending on their location, winds can be either global or local. Local winds are smaller and occur more locally. The winds in your city may come from the east during certain seasons and from the west during others. It may also be different at other times of the year. We refer to the pattern of typical winds in a local area as 'local winds.' There's usually a range between tens and hundreds of miles. They can be cold or hot, as well as dry or wet. Their severity can vary from mild to dangerous. Local wind patterns greatly influence weather. As they move the clouds and moisture around, they can make an area wetter or dryer. A local wind blows over a specific area. The wind normally blows between small troughs of low/high pressure. Geographical factors influence the direction of the local wind. Local wind patterns can be influenced by the presence of oceans, lakes, or mountain ranges. 

Types of Local Winds are:

• Periodical: Winds caused by daily fluctuations in temperature and pressure are called Periodical winds. They usually last for a day or 24 hours to complete a cycle like Mountain & Valley Breezes.

• Non-Periodical: They are only present in certain seasons and are classified as Hot and Cold Winds.

The information mentioned above about the mountain and valley breeze clears the confusion most effectively. While going through the topics, making notes alongside will be of great help.