根据锋的移动规律,通常将锋分为冷锋、暖锋、准静止锋和锢囚锋。而倒暖锋是我国东北地区的预报员在实际工作中总结提出来的概念,倒暖锋是东北地区特有的天气过程之一。从气象地面形势图上看,它类似冷锋;从气象高空形势图上看,又具备暖锋结构的特点。它的实质是在鄂霍次克海地区的暖性低压强烈发展,在低压后部由于回流的强暖平流移向东北地区取代在东北地区的极地大陆冷气团而形成 According to the front of the law of movement, usually the front is divided into cold front, warm front, quasi stationary front and occlusion front. However, the frontal warming front is the concept put forward by forecasters in Northeast China in practical work. Downward warming front is one of the unique weather processes in Northeast China. From the meteorological ground situation map point of view, it is similar to the cold front; from the meteorological altitude map, but also has the characteristics of warm front structure. Its essence is the strong development of warm low pressure in the Sea of ​​Okhotsk, which is formed in the rear of the low pressure due to strong warm-air backflow and to replace the polar continental air mass in the northeast by the northeast.