The Joran is a fascinating example of a "katabatic" or gravity-driven wind. During the night, the air at high altitudes in the Jura Mountains loses heat quickly. Because cold air is denser and heavier than warm air, it begins to flow downward like water, following the valleys and slopes toward LakeRead more
The Joran is a fascinating example of a “katabatic” or gravity-driven wind. During the night, the air at high altitudes in the Jura Mountains loses heat quickly. Because cold air is denser and heavier than warm air, it begins to flow downward like water, following the valleys and slopes toward Lake Geneva. This wind is very important for sailors and people living near the lake, as it can arrive very suddenly. It shows how even small mountain ranges can create their own local wind systems that affect the temperature and safety of the surrounding lowland areas.
Improve your government job selection chances. Use Competitive Exam Preparation (TA Exam) for SSC CGL, CHSL and MTS practice papers.
The Chinook wind is a staple of North American geography. Its name comes from the Chinookan people who lived near the Columbia River. The wind is essentially a "rain shadow" wind. As the air moves from the Pacific toward the interior of Canada and the United States, the Rocky Mountains act as a gianRead more
The Chinook wind is a staple of North American geography. Its name comes from the Chinookan people who lived near the Columbia River. The wind is essentially a “rain shadow” wind. As the air moves from the Pacific toward the interior of Canada and the United States, the Rocky Mountains act as a giant wall. The air that manages to cross the wall is dry and heats up as it drops toward the plains. This creates a narrow corridor of warm weather that stretches along the eastern edge of the mountains, often creating a sharp contrast with the snow-covered land.
The ultimate guide for SSC GD 2026! TA Exam provides chapter-wise mock tests and error analysis to refine your exam strategy.
To categorize winds correctly, we must look at their source. The Mistral and Bora are "drainage" winds that bring cold air from high elevations down to the coast. A Blizzard is a severe storm with very cold temperatures and high winds. However, the Khamsin is a thermal wind born in the hot heart ofRead more
To categorize winds correctly, we must look at their source. The Mistral and Bora are “drainage” winds that bring cold air from high elevations down to the coast. A Blizzard is a severe storm with very cold temperatures and high winds. However, the Khamsin is a thermal wind born in the hot heart of the desert. It is famous for blowing for fifty days (the word ‘Khamsin’ means fifty in Arabic) during the spring. This wind brings heat and sand, making it the opposite of the cold, refreshing or freezing winds listed in the other options.
The ultimate guide for SSC GD 2026! TA Exam provides chapter-wise mock tests and error analysis to refine your exam strategy.
While many local winds are known for heat, these three are famous for their chill. The Mistral and Bora are "katabatic" winds, meaning they are formed when heavy, cold air slides down from mountains like the Alps or the Dinaric Alps. The Pampero is a gusty cold front that rushes across the plains ofRead more
While many local winds are known for heat, these three are famous for their chill. The Mistral and Bora are “katabatic” winds, meaning they are formed when heavy, cold air slides down from mountains like the Alps or the Dinaric Alps. The Pampero is a gusty cold front that rushes across the plains of Argentina. For students, this list serves as a great summary of the world’s most significant cold-weather winds. Each one is driven by the movement of dense, cold air masses into warmer coastal or lowland areas, proving that wind can be a cooling force as well as a warming one.
The ultimate guide for SSC GD 2026! TA Exam provides chapter-wise mock tests and error analysis to refine your exam strategy.
The Foehn wind is a classic geographical phenomenon in Central Europe. When moist air from the south hits the Alps, it is forced upward, where it cools and rains. By the time the air reaches the northern slopes (the leeward side), it has lost all its moisture. As this dry air sinks into the Swiss vaRead more
The Foehn wind is a classic geographical phenomenon in Central Europe. When moist air from the south hits the Alps, it is forced upward, where it cools and rains. By the time the air reaches the northern slopes (the leeward side), it has lost all its moisture. As this dry air sinks into the Swiss valleys, it warms up rapidly through adiabatic heating. This wind is very important for Alpine agriculture because it can extend the growing season by bringing sudden warmth, though it is also known for melting snow so quickly that it can cause floods.
The ultimate guide for SSC GD 2026! TA Exam provides chapter-wise mock tests and error analysis to refine your exam strategy.
What is the name of the cold and dry wind that blows at night from the Jura Mountains towards Lake Geneva in Europe?
The Joran is a fascinating example of a "katabatic" or gravity-driven wind. During the night, the air at high altitudes in the Jura Mountains loses heat quickly. Because cold air is denser and heavier than warm air, it begins to flow downward like water, following the valleys and slopes toward LakeRead more
The Joran is a fascinating example of a “katabatic” or gravity-driven wind. During the night, the air at high altitudes in the Jura Mountains loses heat quickly. Because cold air is denser and heavier than warm air, it begins to flow downward like water, following the valleys and slopes toward Lake Geneva. This wind is very important for sailors and people living near the lake, as it can arrive very suddenly. It shows how even small mountain ranges can create their own local wind systems that affect the temperature and safety of the surrounding lowland areas.
Improve your government job selection chances. Use Competitive Exam Preparation (TA Exam) for SSC CGL, CHSL and MTS practice papers.
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See lessWhat is the wind that descends the eastern slopes of the Rocky Mountains called in the United States and Canada?
The Chinook wind is a staple of North American geography. Its name comes from the Chinookan people who lived near the Columbia River. The wind is essentially a "rain shadow" wind. As the air moves from the Pacific toward the interior of Canada and the United States, the Rocky Mountains act as a gianRead more
The Chinook wind is a staple of North American geography. Its name comes from the Chinookan people who lived near the Columbia River. The wind is essentially a “rain shadow” wind. As the air moves from the Pacific toward the interior of Canada and the United States, the Rocky Mountains act as a giant wall. The air that manages to cross the wall is dry and heats up as it drops toward the plains. This creates a narrow corridor of warm weather that stretches along the eastern edge of the mountains, often creating a sharp contrast with the snow-covered land.
The ultimate guide for SSC GD 2026! TA Exam provides chapter-wise mock tests and error analysis to refine your exam strategy.
Download the app now!
Android: https://play.google.com/store/apps/details?id=com.ta.exam
iOS: https://apps.apple.com/app/id6759824444
See lessWhich of the following is not a cold local wind? (A) Mistral (B) Bora (C) Khamsin (D) Blizzard
To categorize winds correctly, we must look at their source. The Mistral and Bora are "drainage" winds that bring cold air from high elevations down to the coast. A Blizzard is a severe storm with very cold temperatures and high winds. However, the Khamsin is a thermal wind born in the hot heart ofRead more
To categorize winds correctly, we must look at their source. The Mistral and Bora are “drainage” winds that bring cold air from high elevations down to the coast. A Blizzard is a severe storm with very cold temperatures and high winds. However, the Khamsin is a thermal wind born in the hot heart of the desert. It is famous for blowing for fifty days (the word ‘Khamsin’ means fifty in Arabic) during the spring. This wind brings heat and sand, making it the opposite of the cold, refreshing or freezing winds listed in the other options.
The ultimate guide for SSC GD 2026! TA Exam provides chapter-wise mock tests and error analysis to refine your exam strategy.
Download the app now!
Android: https://play.google.com/store/apps/details?id=com.ta.exam
iOS: https://apps.apple.com/app/id6759824444
See lessWhich of the following is a cold local wind? (A) Mistral (B) Bora (C) Pampero (D) All of the above
While many local winds are known for heat, these three are famous for their chill. The Mistral and Bora are "katabatic" winds, meaning they are formed when heavy, cold air slides down from mountains like the Alps or the Dinaric Alps. The Pampero is a gusty cold front that rushes across the plains ofRead more
While many local winds are known for heat, these three are famous for their chill. The Mistral and Bora are “katabatic” winds, meaning they are formed when heavy, cold air slides down from mountains like the Alps or the Dinaric Alps. The Pampero is a gusty cold front that rushes across the plains of Argentina. For students, this list serves as a great summary of the world’s most significant cold-weather winds. Each one is driven by the movement of dense, cold air masses into warmer coastal or lowland areas, proving that wind can be a cooling force as well as a warming one.
The ultimate guide for SSC GD 2026! TA Exam provides chapter-wise mock tests and error analysis to refine your exam strategy.
Download the app now!
Android: https://play.google.com/store/apps/details?id=com.ta.exam
iOS: https://apps.apple.com/app/id6759824444
See lessWhich of the following winds blows on the leeward slopes of the northern Alps in Switzerland?
The Foehn wind is a classic geographical phenomenon in Central Europe. When moist air from the south hits the Alps, it is forced upward, where it cools and rains. By the time the air reaches the northern slopes (the leeward side), it has lost all its moisture. As this dry air sinks into the Swiss vaRead more
The Foehn wind is a classic geographical phenomenon in Central Europe. When moist air from the south hits the Alps, it is forced upward, where it cools and rains. By the time the air reaches the northern slopes (the leeward side), it has lost all its moisture. As this dry air sinks into the Swiss valleys, it warms up rapidly through adiabatic heating. This wind is very important for Alpine agriculture because it can extend the growing season by bringing sudden warmth, though it is also known for melting snow so quickly that it can cause floods.
The ultimate guide for SSC GD 2026! TA Exam provides chapter-wise mock tests and error analysis to refine your exam strategy.
Download the app now!
Android: https://play.google.com/store/apps/details?id=com.ta.exam
iOS: https://apps.apple.com/app/id6759824444
See less