Frontolysis often occurs when the temperature contrast across a front weakens.
锋消常发生在锋面两侧的温度差减弱时。
As the cyclone moved over warmer water, increased mixing and reduced baroclinicity led to rapid frontolysis along the trailing cold front.
当气旋移入更暖的海域后,更强的混合作用与斜压性减弱导致其后部冷锋迅速发生锋消。