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The climate of Asia is dry across its southwestern region. Some of the largest daily temperature ranges on Earth occur in the western part of Asia . The monsoon circulation dominates across the southern and eastern regions, due to the Himalayas forcing the formation of a thermal low which draws in moisture during the summer.
Dry-winter subtropical highland climate (Cwb) is a type of climate mainly found in highlands inside the tropics of Central America, South America, Africa, and South and Southeast Asia or areas in the subtropics. Winters are noticeable and dry, and summers can be very rainy.
Asia (/ ˈ eɪ ʒ ə / ⓘ AY-zhə, UK also / ˈ eɪ ʃ ə / AY-shə) is the largest continent [note 1] [10] [11] in the world by both land area and population. [11] It covers an area of more than 44 million square kilometres, [note 2] about 30% of Earth's total land area and 8% of Earth's total surface area.
Climate change is also likely to pose a serious threat to the region's fisheries: [142] 3.35 million fishers in the Southeast Asia are reliant on coral reefs, [143]: 1479 and yet those reefs are highly vulnerable to even low-emission climate change and will likely be lost if global warming exceeds 1.5 °C (2.7 °F) [151] [152] By 2050–2070 ...
This is a list of countries and sovereign states by temperature. Average yearly temperature is calculated by averaging the minimum and maximum daily temperatures in the country, averaged for the years 1991 – 2020, from World Bank Group , derived from raw gridded climatologies from the Climatic Research Unit .
Climate of the United Arab Emirates (1 P) Pages in category "Climate of Asia by country" The following 2 pages are in this category, out of 2 total.
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In tropical Asia, the distribution and character of the rain forest changes with elevation in the mountains. In Thailand, for instance, the area of tropical forests could increase from 45% to 80% of the total forest cover, while in Sri Lanka, a substantial change in dry forest and decrease in wet forest might occur.