Titlebook: Vegetation and Climate; Siegmar-W. Breckle,M. Daud Rafiqpoor Textbook 2022 Springer-Verlag GmbH Germany, part of Springer Nature 2022 Vege

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Part D: ZB I—Zonobiome of the Evergreen Tropical Rainforest or of the Equatorial Humid Diurnal Climaropics. They give off energy to the high latitudes through atmospheric circulation. Nevertheless, there are radiative climatic differences between the humid and arid tropics. Despite these differences, the uniform irradiation conditions the tropics to be the primary Earth‘s heat belts. They are an a

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Part E: ZB II: Zonobiome of Savannahs, Deciduous Forests and Grasslands of the Tropical Summer Rainfation in temperature. Heavy cenital rains fall during the warm, mostly perhumid season, and the cooler season is arid. The hygric climate of ZB II is characterized by a pronounced hygric seasonality with a rainy and a dry season, whereby the length of the hygric growing season, i.e. the number of hu

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Part F: ZB III: Zonobiome of Hot Deserts or Subtropical Arid Climates so characteristic of the arid areas of the temperate zone. The deserts are the result of the earth’s atmospheric circulation, mainly in connection with the innertropical convergence zone. According to rainy season various desert types develop, and which are according to substrate conditions again