Wikibooks: IB Geography/Extreme environments

This theme studies two types of extreme environment old and high altitude environments (polar glacial areas periglacial areas high mountains in non‑tropical latitudes) ot arid environments (hot deserts and semi‑arid areas) = Challenging Environments = = Global Distribution = = Explain the global dis...

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Format: Book
Language:English
Subjects:
Ice
Online Access:https://en.wikibooks.org/wiki/IB_Geography/Extreme_environments
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record_format openpolar
spelling ftwikibooks:enwikibooks:45325:251390 2023-06-18T03:41:07+02:00 Wikibooks: IB Geography/Extreme environments https://en.wikibooks.org/wiki/IB_Geography/Extreme_environments eng eng Book ftwikibooks 2023-06-02T13:41:25Z This theme studies two types of extreme environment old and high altitude environments (polar glacial areas periglacial areas high mountains in non‑tropical latitudes) ot arid environments (hot deserts and semi‑arid areas) = Challenging Environments = = Global Distribution = = Explain the global distribution of each of the two kinds of extreme environment = = The distribution of cold and high altitude environments = Cold and high altitude environments are generally found along constructive plate margins where fold mountains form or polar regions. Mountainous regions have a high elevation where atmospheric pressure is lower which causes lower temperatures. The sun s rays are received more easily however more solar radiation is reflected due to the high reflectivity of snow. At higher latitudes less heat penetrates the atmosphere as it is thicker and spread across a greater area. = The distribution of hot environments = Hot arid environments are found in the tropics. These areas receive direct sunlight in summer and winter. Hadley cells in the atmosphere also cause aridity as the warm moist air rises from the equator. This condenses and precipitates and the cooler air sinks over the tropical latitudes. The air is drier as cool air cannot hold as much moisture. The air then heats as it spreads over tropical regions and rises again. Hot arid climates can also be found in rain shadows mountainous regions with arid areas behind them. The mountains cause relief rainfall and then the dry air blows across the landscape drying it out. =Describe the relief and climatic characteristics that make these environments extreme. Explain how these characteristics present challenges for resource development and human habitation. = = Population = = Physical Characteristics = = Glacial Environments = = Peri glacial Environments = A periglacial environment is a place where the temperature is seasonally below the freezing point. but never covered by ice. They have a layer of permafrost on or below the surface. Periglacial ... Book Ice permafrost WikiBooks - Open-content textbooks
institution Open Polar
collection WikiBooks - Open-content textbooks
op_collection_id ftwikibooks
language English
description This theme studies two types of extreme environment old and high altitude environments (polar glacial areas periglacial areas high mountains in non‑tropical latitudes) ot arid environments (hot deserts and semi‑arid areas) = Challenging Environments = = Global Distribution = = Explain the global distribution of each of the two kinds of extreme environment = = The distribution of cold and high altitude environments = Cold and high altitude environments are generally found along constructive plate margins where fold mountains form or polar regions. Mountainous regions have a high elevation where atmospheric pressure is lower which causes lower temperatures. The sun s rays are received more easily however more solar radiation is reflected due to the high reflectivity of snow. At higher latitudes less heat penetrates the atmosphere as it is thicker and spread across a greater area. = The distribution of hot environments = Hot arid environments are found in the tropics. These areas receive direct sunlight in summer and winter. Hadley cells in the atmosphere also cause aridity as the warm moist air rises from the equator. This condenses and precipitates and the cooler air sinks over the tropical latitudes. The air is drier as cool air cannot hold as much moisture. The air then heats as it spreads over tropical regions and rises again. Hot arid climates can also be found in rain shadows mountainous regions with arid areas behind them. The mountains cause relief rainfall and then the dry air blows across the landscape drying it out. =Describe the relief and climatic characteristics that make these environments extreme. Explain how these characteristics present challenges for resource development and human habitation. = = Population = = Physical Characteristics = = Glacial Environments = = Peri glacial Environments = A periglacial environment is a place where the temperature is seasonally below the freezing point. but never covered by ice. They have a layer of permafrost on or below the surface. Periglacial ...
format Book
title Wikibooks: IB Geography/Extreme environments
spellingShingle Wikibooks: IB Geography/Extreme environments
title_short Wikibooks: IB Geography/Extreme environments
title_full Wikibooks: IB Geography/Extreme environments
title_fullStr Wikibooks: IB Geography/Extreme environments
title_full_unstemmed Wikibooks: IB Geography/Extreme environments
title_sort wikibooks: ib geography/extreme environments
url https://en.wikibooks.org/wiki/IB_Geography/Extreme_environments
genre Ice
permafrost
genre_facet Ice
permafrost
_version_ 1769006556745039872