“冷流雪”是一种特殊的降雪现象，主要出现在冬季强冷空气南下、经过相对温暖的海面或湖面时。当干冷的空气快速掠过未结冰的水域表面，会从水体中吸收大量水汽和热量，使底层空气变得暖湿。这种暖湿空气迅速上升，与上层冷空气交汇，形成对流云团。由于气温足够低，水汽在云中凝结成冰晶并不断增长，最终以降雪形式落回地面，这就是“冷流雪”。冷流雪具有局地性强、持续时间短、降雪强度大等特点，常出现在中国山东半岛北部、辽东半岛以及北美五大湖地区（被称为“湖效应雪”）。例如，山东烟台、威海等地冬季常因冷流雪出现“雪窝子”现象——即局部区域积雪远高于周边地区。冷流雪的形成依赖于较大的海气温差（通常需超过13℃）、稳定的冷空气路径以及合适的地形抬升条件。虽然冷流雪带来美丽雪景，但也可能造成交通受阻、农业设施受损等问题，因此气象部门会密切监测此类天气过程，及时发布预警信息。
“Cold-air damming snow,” commonly known as “cold-flow snow,” is a unique type of snowfall that occurs in winter when strong, dry cold air masses move southward over relatively warmer sea or lake surfaces. As the frigid air sweeps across unfrozen water, it picks up moisture and heat from the water body, warming and humidifying its lower layer. This newly moistened air rises rapidly, meeting the colder air above and forming convective cloud systems. When temperatures are sufficiently low, the moisture condenses into ice crystals within these clouds, which grow and eventually fall as snow—this is cold-flow snow.Cold-flow snow is characterized by its highly localized nature, short duration, and often intense snowfall rates. It frequently occurs along the northern coast of China’s Shandong Peninsula, the Liaodong Peninsula, and around North America’s Great Lakes (where it’s known as “lake-effect snow”). For instance, cities like Yantai and Weihai in Shandong often experience “snow pockets”—localized zones receiving significantly heavier snowfall than surrounding areas—due to this phenomenon. The formation of cold-flow snow depends on a substantial temperature difference between the water surface and the overlying air (typically exceeding 13°C), a steady path of cold air, and favorable topographic lift.While cold-flow snow creates picturesque winter scenes, it can also disrupt transportation and damage agricultural infrastructure. Therefore, meteorological agencies closely monitor such events and issue timely warnings.
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