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      • The tropics are warm all year, averaging 25 to 28 degrees Celsius (77 to 82 degrees Fahrenheit). This is because the tropics get more exposure to the sun. Because of all that sun, the tropics don't experience the kind of seasons the rest of Earth does.
      www.nationalgeographic.org › encyclopedia › tropics
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  2. Asia is dominated by a varied mix of climate regions. Polar, subarctic, and temperate climates occur along the continent's northern and northeastern fringes; arid and highland climates occur in the continent's interior and southwestern reaches; and a mix of grassland and tropical rainforest climates occur along its southern fringe. (more)

  3. The Southern sections of Asia are mild to hot, while far northeastern areas such as Siberia are very cold, and East Asia has a temperate climate. The highest temperature recorded in Asia was 54 °C (at Ahvaz Airport, Iran on June 29, 2017 and at Tirat Zvi, Israel on June 21, 1942).

  4. Most geographers apply the term exclusively to the northern latitudes of North America, Europe, and Asia. A microthermal climate may include the temperate climate of Boston, Massachusetts; the coniferous forests of southern Scandinavia ; and the boreal ecosystem of northern Siberia .

  5. Compare climate between countries and regions by temperature, precipitation, humidity, rain days, sunshine hours and more.

  6. As the aggregate result of those various meteorological patterns, the following types of climate may be distinguished in Asia: the tundra climate (associated with the cold, treeless plains of the Arctic lowlands of Asia); the cold, sharply continental climate of eastern Siberia; the cold, moderately humid western Siberian climate; the humid ...

  7. North Asia is a subregion of Eurasia, consisting of the Asian territory of Russia, includes the Urals, Siberia and the Far East. The climate in the north of Asia is continental with a pronounced contrast of temperatures and very cold winters.

  8. As the northern hemisphere tilts toward the sun, it experiences summer; at the opposite end of Earth's orbit, the southern hemisphere receives greater solar input and experiences summer.

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