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Earth constantly absorbs energy from sunlight and emits thermal radiation as infrared light. In the long run, Earth radiates the same amount of energy per second as it absorbs, because the amount of thermal radiation emitted depends upon temperature: If Earth absorbs more energy per second than it radiates, Earth heats up and the thermal radiation will increase, until balance is restored; if ...
Climate change can also be used more broadly to include changes to the climate that have happened throughout Earth's history. [32] Global warming—used as early as 1975 [33] —became the more popular term after NASA climate scientist James Hansen used it in his 1988 testimony in the U.S. Senate. [34] Since the 2000s, climate change has ...
The climate march in New York City saw thousands band together in an effort to bring awareness to the growing climate concerns and promote sustainability. It is often difficult to mediate out ...
In particular, climate change art has been used both to make scientific data more accessible to non-scientists and to express people's fears. [13] Some research indicates that climate change art is not particularly effective in changing peoples views, though art with a "hopeful" message gives people ideas for change. [13]
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Project Drawdown is a climate change mitigation project initiated by Paul Hawken and climate activist Amanda Joy Ravenhill. The Project Drawdown website includes video lessons [3] that explain the analysis and insights behind the efforts and research that make up the science behind the project. The list, which encompasses only technologically ...
Some climate change effects: wildfire caused by heat and dryness, bleached coral caused by ocean acidification and heating, environmental migration caused by desertification, and coastal flooding caused by storms and sea level rise. Effects of climate change are well documented and growing for Earth's natural environment and human societies. Changes to the climate system include an overall ...
Older Dryas cold, interrupts warm period for some centuries (B-S) 12,000–11,000: Allerød oscillation warm & moist (B-S) 11,400–9,500: Huelmo–Mascardi Cold Reversal cold in Southern Hemisphere: 10,800–9,500: Younger Dryas sudden cold and dry period in Northern Hemisphere (B-S) 9,500–5,500
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