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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.
The 2007 IPCC Fourth Assessment Report concluded that over the last three decades human-induced warming had likely had an influence on many biological systems. [25] [26] [27] The Sixth Assessment Report found that half of all species with long-term data had shifted their ranges poleward (or upward for mountain species).
The climate in Texas is changing partially due to global warming and rising trends in greenhouse gas emissions. [1] As of 2016, most area of Texas had already warmed by 1.5 °F (0.83 °C) since the previous century because of greenhouse gas emissions by the United States and other countries. [ 1 ]
A rain shadow is a dry area on the leeward side of a mountainous area (away from the wind). The mountains block the passage of rain-producing weather systems and cast a "shadow" of dryness behind them. Wind and moist air are drawn by the prevailing winds towards the top of the mountains, condensing and precipitating before it crosses the top.
A house burns in the Steiner Ranch neighborhood in Austin on Sept. 4, 2011. Wildfires broke out all over Central Texas on that day, including a massive fire in Bastrop County that eventually ...
How Earth systems interact across a mountain belt is dependent upon the mountain belts location and orientation. [1] Different mountain belts exist at different latitudes which means that different mountain belts experience different climatic conditions including temperature and degree of glaciation (which can shape relief [50] [51]). This ...
With the formation this week of yet another summer heat dome over Texas and much of the American Southwest, many residents are struggling to cope with a sweltering new normal made worse by climate ...
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