Tail-End of a Cold Front

Tail-End of a Cold FrontA 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 extra-tropical cyclone,at the leading edge of its cold air advection pattern, which is also known as the cyclone's dry conveyor belt circulation.


Tail-end of a Cold Front is a front boundary of 2 air masses, which is found in a middle latitude. It causes too much rainfall and cloudiness over affected areas.It is in a Northern portion of the country during the Northern Hemisphere in a winter season.


REVIEW: It is defined wherein the cooler mass of air used to replace the warmer mass of air, which results to a lower pressure in that surface. It is a phenomenon wherein it can experience a change in a temperature. Example of this is, when moisture is present in that place, rain can occur along the boundary. It also form a narrow line thunderstorm along the frontal zone.

• Today I learned that-- is a front boundary of 2 air masses, which is found in a middle latitude. It causes too much rainfall and cloudiness over affected areas.
• i will apply my learnings about-- the occurrence of tropical depression weather it will have rainy weather or not.
• Learning about this phenomena is  important t because-- i will be aware about this phenomena.
• On a larger scale, I will share my learnings about these phenomena to others-- so that not only me will be aware but also others.
• I need to know more about-- the effects of this phenomenon to my life.