trình bày đặc điểm phân hóa khí hậu ở châu Âu theo chiều tây-đông vì sao càng đi về phía tây khí hậu châu Âu càng ấm áp và mưa nhiều

The climate in Europe varies from west to east due to several factors. As we move from west to east, the climate becomes progressively cooler and drier. In the western part of Europe, the climate is influenced by the warm North Atlantic Drift, which is a branch of the Gulf Stream. This warm ocean current brings moist and warm air from the tropics, resulting in mild and humid conditions. As a result, the western regions of Europe experience relatively warm temperatures and abundant rainfall. However, as we move towards the eastern part of Europe, the influence of the North Atlantic Drift weakens, and the continent becomes more distant from the warming effects of the ocean. Consequently, the climate becomes colder and drier. The absence of the warm ocean current leads to less moisture in the air and lower temperatures. Therefore, the further west you go in Europe, the warmer and wetter the climate becomes, while the further east you go, the colder and drier it becomes.