这种反馈循环通常被称作“冰反射反馈”，它的伴随效应——海洋储热的过剩，常延迟秋季里新海冰的形成。
This feedback loop, which is often referred to as the ice-albedo feedback, also delays the formation of new sea ice in autumn because of the accompanying surplus in oceanic heat storage.
这种反馈循环通常被称作“冰反射反馈”，它的伴随效应——海洋储热的过剩，常延迟秋季里新海冰的形成。
This feedback loop, which is often referred to as the ice - albedo feedback, also delays the formation of new sea ice in autumn because of the accompanying surplus in oceanic heat storage.
初秋季节，早晚凉，白天热，温差较大，局部容易形成强对流天气。
Early autumn season, and sooner or later cooler daytime heat, temperature larger, local becomes strong convective weather.
初秋季节，早晚凉，白天热，温差较大，局部容易形成强对流天气。
Early autumn season, and sooner or later cooler daytime heat, temperature larger, local becomes strong convective weather.
应用推荐