A cold front is defined as the leading edge of a cooler mass of air, replacing (at ground level) a warmer mass of air, which lies within a fairly sharp surface trough of low pressure. It forms in the wake of an extratropical cyclone, at the leading edge of its cold air advection pattern, which is also known as the cyclone's dry conveyor belt circulation. It is a must to know its hazards and effects in order to be properly prepared during calamities brought by and enhanced by this kind of phenomenon. We can also suffice our uncertainties and doubts with the knowledge of its factors and their requirements to trigger the said effect, which may or may not drastically affect our neighborhood and alike. Being extremely cautious about these phenomenon does not enforces any unjust instances but enhances our knowledge and survival skills in order to stay safe unto the road of our certain future meld by ourselves.
