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This represented a decrease of -4.17% compared to the previous year, amounting to -437,903 tons less than the 2015 emissions of 10,500,531 tons. The CO2 emissions per capita in Zimbabwe were 0.70 tons per person in 2016, based on a population of 14,452,704. This signifies a decrease of -0.05 from the previous year's figure of 0.74 CO2 tons per ...
The climate varies markedly with altitude with the Eastern Highlands at 1,878 metres or 6,161 feet above sea level being much wetter and cooler than lower altitudes. There is a dry season, including a short cool season during the period May to September, when the whole country has very little rain.
The Köppen climate classification system was modified further within the Trewartha climate classification system in 1966 (revised in 1980). The Trewartha system sought to create a more refined middle latitude climate zone, which was one of the criticisms of the Köppen system (the climate group C was too general). [10]: 200–1
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The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, latitude, and location.The generally strong dependency on elevation is known as altitudinal zonation: the average temperature of a location decreases as the elevation increases.
The subtropics are geographic and climate zones located roughly between the Tropic of Cancer and Tropic of Capricorn and the 40th parallel in both hemispheres. Subtropical climate regions can exist at high elevations within the tropics, such as across the Mexican Plateau and the Ethiopian Highlands and in Da Lat of the Vietnamese Central ...
A Köppen–Geiger climate map showing temperate climates for 1991–2020 The different geographical zones of the world. The temperate zones, in the sense of geographical regions defined by latitude, span from either north or south of the subtropics (north or south of the orange dotted lines, at 35 degrees north or south) to the polar circles.
Today, the most commonly used climate map is the Köppen climate classification, developed by Russian climatologist of German descent and amateur botanist Wladimir Köppen (1846–1940), which divides the world into five major climate regions, based on average annual precipitation, average monthly precipitation, and average monthly temperature.