Dinosaurs lived a long time, geologically speaking, in part because the weather was favorable to them. Giant mammals lived during the ice ages because conditions were favorable. Earth's climate has been warmer and colder in Earth history, but mostly it's been warmer.
Climate has changed throughout Earth history. Much of the time Earth's climate was hotter and more humid than it is today, but climate has also been colder, as when glaciers covered much more of the planet. The most recent ice ages were in the Pleistocene Epoch, between 1.8 million and 10,000 years ago (Figure below). Glaciers advanced and retreated in cycles, known as glacial and interglacial periods. With so much of the world’s water bound into the ice, sea level was about 125 meters (395 feet) lower than it is today. Many scientists think that we are now in a warm, interglacial period that has lasted about 10,000 years.
The maximum extent of Northern Hemisphere glaciers during the Pleistocene epoch.
For the past 1500 years, climate has been relatively mild and stable when compared with much of Earth’s history. Why has climate stability been beneficial for human civilization? Stability has allowed the expansion of agriculture and the development of towns and cities.
Fairly small temperature changes can have major effects on global climate. The average global temperature during glacial periods was only about 5.5oC (10oF) less than Earth’s current average temperature. Temperatures during the interglacial periods were about 1.1oC (2.0oF) higher than today (Figure below).
Since the end of the Pleistocene, the global average temperature has risen about 4oC (7oF). Glaciers are retreating and sea level is rising. While climate is getting steadily warmer, there have been a few more extreme warm and cool times in the last 10,000 years. Changes in climate have had effects on human civilization.
The graph is a compilation of 5 reconstructions (the green line is the mean of the five records) of mean temperature changes. This illustrates the high temperatures of the Medieval Warm Period, the lows of the Little Ice Age, and the very high (and climbing) temperature of this decade.
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| Cover Image | Attributions |
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| Credit: DariuszSankowski Source: https://pixabay.com/photos/dinosaur-gad-mammal-dino-extinct-958011/ License: Pixabay License |
| Image | Reference | Attributions |
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| Credit: DariuszSankowski Source: https://pixabay.com/photos/dinosaur-gad-mammal-dino-extinct-958011/ License: Pixabay License | ||
| Credit: Courtesy of US Geological Survey Source: http://commons.wikimedia.org/wiki/File:Pleistocene_north_ice_map.jpg License: Public Domain | ||
| Credit: U Büntgen, C Raible, et al. Source: http://www.plosone.org/article/info%253Adoi%252F10.1371%252Fjournal.pone.0025133 License: CC BY 2.5 |
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