
1. объяснить смену климатических условий Евразии с севера на юг и с запада на восток.


Ответы на вопрос

Евразия лежит во всех климатических поясах и во всех природных зонах.,протянулась с запада на восток на 16 тыс. км, с севера на юг — на 8 тыс. км.
Крайние точки Евразии
Мыс Флигели (Россия), 81°51' с. ш. — крайняя северная островная точка.
Мыс Челюскин (Россия), 77°43' с. ш. — крайняя северная материковая точка.
Остров Ратманова (Россия) 169°0' з. д. — крайняя восточная островная точка.
Мыс Дежнёва (Россия), 169°40' з. д. — крайняя восточная материковая точка.
Южный остров (Кокосовые острова) 12°4' ю. ш. — крайняя южная островная точка.
Мыс Пиай (Малайзия) 1°16' с. ш. — крайняя южная материковая точка.
скала Моншик (Азорские острова) 31º16' з. д. — крайняя западная островная точка.
Мыс Рока (Португалия), 9º30' з. д. — крайняя западная материковая точка
как то так проходили



Explanation of the Change in Climatic Conditions in Eurasia
Eurasia experiences a significant change in climatic conditions from north to south and from west to east. This change is influenced by various factors, including latitude, altitude, proximity to large bodies of water, and prevailing wind patterns.
North to South: The change in climatic conditions from north to south in Eurasia is primarily influenced by latitude and the distance from the equator. As one moves from the northern regions towards the southern regions, several key changes occur. The temperature generally increases, the length of the growing season extends, and the amount of precipitation may vary significantly. Additionally, the types of vegetation and ecosystems also undergo a transition due to the changing climate.
The influence of latitude on the change in climatic conditions from north to south is a key factor. As one moves closer to the equator, the angle of solar radiation becomes more direct, leading to higher temperatures and a different distribution of precipitation. This results in the development of different climate zones, such as the transition from subarctic and boreal climates in the north to temperate and subtropical climates in the south.
West to East: The change in climatic conditions from west to east in Eurasia is influenced by a combination of factors, including continental landmass, proximity to large bodies of water, and prevailing wind patterns. As one moves from the western regions towards the eastern regions, several notable changes occur. The continentality effect becomes more pronounced, leading to greater temperature extremes, lower humidity, and changes in precipitation patterns.
The continentality effect refers to the impact of a continental landmass on the climate, leading to more extreme temperature variations compared to regions near large bodies of water. In Eurasia, the continentality effect becomes more pronounced as one moves from the western regions, which are influenced by the moderating effects of the Atlantic Ocean, towards the eastern regions, which are more distant from major bodies of water.
Prevailing wind patterns also play a significant role in the change of climatic conditions from west to east. In general, the prevailing westerly winds in the mid-latitudes of Eurasia bring moisture from the Atlantic Ocean, leading to higher precipitation in the western regions. As one moves eastward, the influence of these moisture-laden winds diminishes, resulting in drier conditions and a shift in vegetation and ecosystems.
In summary, the change in climatic conditions in Eurasia from north to south and from west to east is influenced by a complex interplay of factors, including latitude, continentality, proximity to large bodies of water, and prevailing wind patterns. These factors contribute to the diverse range of climates and ecosystems found across the Eurasian continent.
Conclusion
The change in climatic conditions across Eurasia is a fascinating subject that reflects the intricate interactions of geographical, meteorological, and environmental factors. The transition from north to south and from west to east showcases the rich diversity of climates and ecosystems present on the Eurasian continent.

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