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Tropics

Holt Earth Science Chapter 17, Section 17.3

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Earth-Sun Relationships The Sun is the source from almost all of the Earth?s weather and climate. Earth intercepts 12000000000 (one two-billionth) of all the energy given off by the sun (this is several hundred thousand times the energy generation of the US). Solar energy isn?t evenly distributed; the amount of energy varies with latitude, time of day, and season. Unequal heating of Earth creates winds and ocean currents, which transport heat to balance energy inequalities; the consequences of these processes are called weather. If the Sun died, global winds and currents would stop; but if the Sun shines, the winds will blow and weather will exist. Variations in solar heating are caused by the motions of the Earth relative to the Sun and variations in the Earth?s land-sea surface.

AP* EDITION|THE EARTH AND ITS PEOPLE: A GLOBAL HISTORY Chapter 13 Review

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AP* EDITION|THE EARTH AND ITS PEOPLE: A GLOBAL HISTORY CHAPTER 13 Larger Concept Section Review Vocabulary Terms Details TROPICAL LANDS AND PEOPLES The Tropical Environment -The environment of tropical Africa and Asia is governed by wind patterns across oceans and the resulting rainfall -Deserts and rain forests mark the extreme climate variations in these regions, while mountain ranges produce further variations Ibn Battuta-Moroccan Muslim scholar, the most widely traveled individual of his time Tropics-equatorial region between the Tropic of Cancer and the Tropic of Capricorn Monsoon-seasonal winds in the Indian Ocean caused by the differences in temperature between the rapidly heating and cooling landmasses of Africa and Asia and the slowly changing ocean waters

AP* EDITION|THE EARTH AND ITS PEOPLE: A GLOBAL HISTORY Chapter 13 Review

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AP* EDITION|THE EARTH AND ITS PEOPLE: A GLOBAL HISTORY CHAPTER 13 Larger Concept Section Review Vocabulary Terms Details TROPICAL LANDS AND PEOPLES The Tropical Environment -The environment of tropical Africa and Asia is governed by wind patterns across oceans and the resulting rainfall -Deserts and rain forests mark the extreme climate variations in these regions, while mountain ranges produce further variations Ibn Battuta-Moroccan Muslim scholar, the most widely traveled individual of his time Tropics-equatorial region between the Tropic of Cancer and the Tropic of Capricorn Monsoon-seasonal winds in the Indian Ocean caused by the differences in temperature between the rapidly heating and cooling landmasses of Africa and Asia and the slowly changing ocean waters

Biome Characteristics

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Tropical forest Within 23 N/S Canopy 4% of land space, but 20% photosynthesis of the Earth most diverse species on Earth Tall trees- Tropical dry forests Tropical deciduous forests Tropical rain forests Dim floor Epiphytes cover trees Savannas Tropic/subtropic grass land Rainy/dry seasons Scattered trees Mammals move deserts 23 N/S Low/unpredictable rains Hot and cold CAM photosynthesis plants Water storage adaptation Draught-resistant plants chaparral Along coastlines in midlatitudes Mild/rainy winter Hot/dry summer Dense, spiny evergreen shrubs Maintained by periodic fire Temperate grass land NE USA etc Deep and rich soil in nutrition Low total annual rain Inhospitable for forest Maintained by fire/drought/grazing Temperate deciduous forests

Chapter 14

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CHAPTER 14 Tropical Africa and Asia, 1200–1500 I. Tropical Lands and Peoples A. The Tropical Environment 1. The tropical zone falls between the Tropic of Cancer in the north and the Tropic of Capricorn in the south. The Afro-Asian tropics have a cycle of rainy and dry seasons dictated by the alternating winds known as monsoons.
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