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Productivity in Highland Ethiopia, 1900–1987," Journal of Interdisciplinary History, 20:3, pp. 389–416. (Retrieved November 18, 2006 from JSTOR database)
Climate change in Ethiopia is affecting the people in Ethiopia due to increased floods, heat waves and infectious diseases. [4] In the Awash basin in central Ethiopia floods and droughts are common. Agriculture in the basin is mainly rainfed (without irrigation systems). This applies to around 98% of total cropland as of 2012.
[6] Ethiopia's climate is predicted to warm between 0.7°C and 2.3°C by the end of the 2020s and between 1.4°C and 2.9°C by the 2050s. The county's vulnerability to climate change could increase poverty and dependency on rain-fed agriculture.
Other climatic factors such as average temperature and temperature range may also affect erosion, via their effects on vegetation and soil properties. In general, given similar vegetation and ecosystems, areas with more precipitation (especially high-intensity rainfall), more wind, or more storms are expected to have more erosion.
[1] [2] Climate is a key extrinsic variable, controlling the water to rock ratio, pH, and alkalinity, all of which impact the rate of weathering. [1] The Goldich dissolution series concerns intrinsic mineral qualities, which were proven both by Goldich as well as preceding scientists to also be important for constraining weathering rates.
The Climate Book: Causes, effects and possible solutions to the climate crisis: Greta Thunberg and many others: 2022 ISBN 978-0-241-54747-2: Climate Capitalism: Capitalism in the Age of Climate Change: Climate change: efficient energy use and renewable energy: Hunter Lovins and Boyd Cohen: 2011: ISBN 978-0-8090-3473-4
The hottest air temperature ever recorded was 57.7 °C (135.9 °F) at 'Aziziya, Libya, on 13 September 1922, [54] but that reading is queried. The highest recorded average annual temperature was 34.4 °C (93.9 °F) at Dallol, Ethiopia. [55] The coldest recorded average annual temperature was −55.1 °C (−67.2 °F) at Vostok Station, Antarctica.
Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect.