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The Polar Front Theory of a developing wave cyclone was conceived in:

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The Polar Front Theory of a developing wave cyclone was conceived in meteorology. This theory explains the formation and development of mid-latitude cyclones.

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The Polar Front Theory of a developing wave cyclone was conceived in meteorology. This theory explains the formation and development of mid-latitude cyclones, which are also known as wave cyclones or extratropical cyclones. It suggests that the interaction between warm tropical air and cold polar air along the polar front creates a region of instability, leading to the formation of a wave cyclone.

During the development of a wave cyclone, warm air rises along the leading edge of the cold front, forming a warm front. This warm front moves faster than the associated cold front, creating a tilting motion that leads to the development of a low-pressure center. As the cyclone matures, the cold front catches up to the warm front, resulting in the formation of an occluded front.

An example of a wave cyclone is the Nor'easter that affects the East Coast of the United States during the winter. These storms develop along the polar front, where cold air from the north meets warm air from the south. The Polar Front Theory provides a framework for understanding the complex dynamics of wave cyclones and their associated weather patterns.

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