Subject
photo credits: Wikimedia Commons
In common usage, climate change describes global warming—the ongoing increase in global average temperature—and its effects on Earth's climate system. Climate change in a broader sense also includes previous long-term changes to Earth's climate. The current rise in global average temperature is primarily caused by humans burning fossil fuels since the Industrial Revolution. Fossil fuel use, deforestation, and some agricultural and industrial practices add to greenhouse gases. These gases absorb some of the heat that the Earth radiates after it warms from sunlight, warming the lower atmosphere. Carbon dioxide, the primary greenhouse gas driving global warming, has grown by about 50% and is at levels unseen for millions of years. Climate change has an increasingly large impact on the environment. Deserts are expanding, while heat waves and wildfires are becoming more common. Amplified warming in the Arctic has contributed to thawing permafrost, retreat of glaciers and sea ice decline. Higher temperatures are also causing more intense storms, droughts, and other weather extremes. Rapid environmental change in mountains, coral reefs, and the Arctic is forcing many species to relocate or become extinct. Even if efforts to minimize future warming are successful, some effects will continue for centuries. These include ocean heating, ocean acidification and sea level rise. Climate change threatens people with increased flooding, extreme heat, increased food and water scarcity, more disease, and economic loss. Human migration and conflict can also be a result. The World Health Organization calls climate change one of the biggest threats to global health in the 21st century. Societies and ecosystems will experience more severe risks without action to limit warming. Adapting to climate change through efforts like flood control measures or drought-resistant crops partially reduces climate change risks, although some limits to adaptation have already been reached. Poorer communities are responsible for a small share of global emissions, yet have the least ability to adapt and are most vulnerable to climate change. Many climate change impacts have been felt in recent years, with 2023 the warmest on record at +1.48 °C (2.66 °F) since regular tracking began in 1850. Additional warming will increase these impacts and can trigger tipping points, such as melting all of the Greenland ice sheet. Under the 2015 Paris Agreement, nations collectively agreed to keep warming "well under 2 °C". However, with pledges made under the Agreement, global warming would still reach about 2.7 °C (4.9 °F) by the end of the century. Limiting warming to 1.5 °C would require halving emissions by 2030 and achieving net-zero emissions by 2050. Fossil fuel use can be phased out by conserving energy and switching to energy sources that do not produce significant carbon pollution. These energy sources include wind, solar, hydro, and nuclear power. Cleanly generated electricity can replace fossil fuels for powering transportation, heating buildings, and running industrial processes. Carbon can also be removed from the atmosphere, for instance by increasing forest cover and farming with methods that capture carbon in soil. Source: Wikipedia (en)
Works about climate change 39
-
Is our climate changing?
-
Climatic Change with Special Reference to Wales and its Agriculture
-
Anatolia, Levant, Middle East. Arlene Miller Rosen. Civilizing Climate: Social responses to Climate Change in the Ancient Near East, 2007. xiv+202 pages, 31 illustrations, 8 tables. Lanham, New York, Toronto & Plymouth: AltaMira; 978-0-7591-0493-8 ha
Why the Cheetah Cheats
-
Encyclopedia of Global Warming & Climate Change
-
Lessons from the past: coping with natural hazards and climate changeGwen Robbins Schug. Bioarchaeology and climate change: a view from South Asian prehistory. xviii+180 pages, 17 illustrations, 21 tables. 2011. Gainesville (FL): University Press of
-
Climate Change and the Course of Global History
-
Robert Van de Noort. Climate change archaeology: building resilience from research in the world's coastal wetlands. x+272 pages, 54 b&w illustrations, 1 table. 2013. Oxford: Oxford University Press; 978-0-19-969955-1 hardback £60
-
Climate Change Archaeology: Building Resilience from Research in the World’s Coastal Wetlands. Robert Van De Noort. 2013. Oxford University Press, New York, xii + 272 pp. $125 (cloth), ISBN: 978-0-19-969955-1
-
Limit to climate change adaptation
Handeln statt Hoffen
Internationalism or Extinction
-
T&T Clark Companion on Christian Theology and Climate Change
Greta, la ragazza che sta cambiando il mondo
Klimakiller – Krieg: Militärkritik und öko-pazifistische Perspektiven zum Klimawandel
-
Executive Order 13990
-
Executive Order 14013
-
Animal Agriculture is the Leading Cause of Climate Change - A Position Paper
-
Climate Change and Energy Transition Act
-
De què parlem mentre no parlem de tota aquesta merda?
-
Effetti farfalla
-
Uncanny and Improbable Events
Climate Change as Class War
-
The Living Mountain: A Fable for Our Times
-
Climate change in Germany
-
Plano de Desarmamento e Plano de Paz
The Great Derangement
Gun Island
-
Cut for Time: Climate Change (Kumail Nanjiani)
The Nutmeg's Curse: Parables for a Planet in Crisis
-
Poles Apart
Les Révoltes du ciel
Subject -