The subtropics (latitudes from about 23.5° to 35°, north and south) have temperate climates that have the least seasonal change and the warmest in winter, while at the other end, Boreal climates located from 55 to 65 north latitude have the most seasonal changes and long and severe winters. What Is a List of Countries in the Temperate Zone. In some areas with a humid subtropical climate (most notably southeast China and North India), there is an even sharper wet-dry season, called subtropical monsoon or Cwa. The Köppen climate classification defines a climate as "temperate" when the mean temperature is above −3 °C (26.6 °F) but below 18 °C (64.4 °F) in the coldest month. Freezing precipitation is uncommon in this portion of the temperate zone. This type of climate is even found in the very remote parts of the Papuan Highlands in Indonesia. Currently, the overall temperate forest area is fairly stable at 25% of the global forest. This type of climate is normally located along leeward lower east coasts of continents such as in southeast and central Argentina, Uruguay and south of Brazil, the southeast portions of East Asia, the southern United States, South Africa, and eastern Australia. The oceanic climates are created by the onshore flow from the cool high latitude oceans to their west. Japan and New Zealand are in the temperate zone, because they are north and south of the tropics.

The vast majority of the world's human population resides in temperate zones, especially in the northern hemisphere, due to its greater mass of land. However, other climate classifications set the minimum at 0 °C (32.0 °F). Snowfall tends to be more common here than in other oceanic climates. In geography, the temperate or tepid climates of Earth occur in the middle latitudes, which span between the tropics and the polar regions of Earth. In very small areas at high altitudes around the Mediterranean Basin, Iran, Kyrgyzstan, Tajikistan, Turkey, Alaska and other parts of the northwestern United States (Eastern Washington, Eastern Oregon and Southern Idaho) and in the Russian Far East, the climate is classified as Dsc with a dry summer climate, such as in Seneca, Oregon or Atlin, British Columbia.
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The subtropics (latitudes from about 23.5° to 35°, north and south) have temperate climates that have the least seasonal change and the warmest in winter, while at the other end, Boreal climates located from 55 to 65 north latitude have the most seasonal changes and long and severe winters. What Is a List of Countries in the Temperate Zone. In some areas with a humid subtropical climate (most notably southeast China and North India), there is an even sharper wet-dry season, called subtropical monsoon or Cwa. The Köppen climate classification defines a climate as "temperate" when the mean temperature is above −3 °C (26.6 °F) but below 18 °C (64.4 °F) in the coldest month. Freezing precipitation is uncommon in this portion of the temperate zone. This type of climate is even found in the very remote parts of the Papuan Highlands in Indonesia. Currently, the overall temperate forest area is fairly stable at 25% of the global forest. This type of climate is normally located along leeward lower east coasts of continents such as in southeast and central Argentina, Uruguay and south of Brazil, the southeast portions of East Asia, the southern United States, South Africa, and eastern Australia. The oceanic climates are created by the onshore flow from the cool high latitude oceans to their west. Japan and New Zealand are in the temperate zone, because they are north and south of the tropics.

The vast majority of the world's human population resides in temperate zones, especially in the northern hemisphere, due to its greater mass of land. However, other climate classifications set the minimum at 0 °C (32.0 °F). Snowfall tends to be more common here than in other oceanic climates. In geography, the temperate or tepid climates of Earth occur in the middle latitudes, which span between the tropics and the polar regions of Earth. In very small areas at high altitudes around the Mediterranean Basin, Iran, Kyrgyzstan, Tajikistan, Turkey, Alaska and other parts of the northwestern United States (Eastern Washington, Eastern Oregon and Southern Idaho) and in the Russian Far East, the climate is classified as Dsc with a dry summer climate, such as in Seneca, Oregon or Atlin, British Columbia.
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