There is often a burning wind on the northern coast of Turkey in winter, and the temperature rises sharply after nightfall. Why?

The cause of foehn is related to the local climate and geographical environment. In order to find out the causes of frequent foehn on the northern coast of Turkey in winter, we must first know the causes of foehn.

Burning wind (burning wind; hn？ Wind) is a kind of local air movement form triggered by the mountain, which appears on the back of the mountain-the air flow over the mountain sinks on the leeward slope and becomes dry and hot.

The phenomenon of foehn is due to the fact that wet air passes through the mountains and heats up when the leeward side of the mountains sinks, making the air mass dry and hot. Therefore, the humidity of the passing air mass is obviously reduced, and the temperature will also increase rapidly.

We know the cause of the foehn, and then look at the geographical and climatic conditions in Turkey.

First of all, Turkey belongs to the Mediterranean region, and then the Mediterranean climate. The Mediterranean climate is characterized by hot and dry summer and mild and rainy winter, because the rainy winter brings a lot of rain to the coastal zone of northern Turkey, and Ponting Mountain in northern Turkey is extended to high mountains in the phenomenon of wind burning.

Both Baramo and the northern coast of Spain have a Mediterranean climate, with plenty of rain in winter and high mountains in the territory, which are prone to wind burning.

In other parts of the world, such as Chile and Argentina, there are also many wind-burning phenomena. There are many Tianshan Mountains and Qinling Mountains everywhere in the Rocky Mountains of the United States, China and Mexico. The man above said it!