Climate and Global Change

Warm near the equator and cold at the poles, our planet is able to support a variety of living things because of its diverse regional climates. The average of all these regions makes up Earth's global climate. Climate has cooled and warmed throughout Earth history for various reasons. Rapid warming like we see today is unusual in the history of our planet. The scientific consensus is that climate is warming as a result of the addition of heat-trapping greenhouse gases which are increasing dramatically in the atmosphere as a result of human activities.

<a href="/earth/polar/cryosphere_permafrost1.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">Permafrost</a> is
ground that is below the freezing point of water (0C or 32F) for two
or more years. Permafrost is found at high latitudes like the
<a href="/earth/polar/polar_north.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">Arctic</a> and
<a href="/earth/polar/polar_south.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">Antarctic</a>.
It is also common at high altitudes - like mountainous areas wherever the
<a href="/earth/climate/cli_define.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">climate</a> is
cold. 
Permafrost has been thawing relatively quickly in recent years. Scientists
have found that the rate of permafrost thaw has increased because of <a href="/earth/climate/cli_effects.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">global
warming</a>.<p><small><em>Image courtesy of the    USGS</em></small></p>Although we humans have never experienced fast <a href="/earth/climate/climate.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">global
warming</a>, our
planet has. And our planet keeps records of what happened. The oldest
records that the
<a href="/earth/earth.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">Earth</a> keeps
are in its
<a href="/earth/geology/sed_intro.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">rocks</a>.
In this image, <a href="/headline_universe/olpa/methane_28may08.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">geologists Chris von der Borch and Dave
Mrofka</a> collect
sediment samples in South Australia. These rocks hold clues to help
explain why climate changed abruptly 635 million years ago.<p><small><em>                    Courtesy of Martin Kennedy, UCR</em></small></p>Many forms of air pollution are human-made. Industrial plants, power plants
and vehicles with internal combustion engines produce <a href="/earth/climate/nitrogen_airpollution.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">nitrogen
oxides</a>,
<a href="/earth/Atmosphere/vocs.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">VOCs</a>,
<a href="/physical_science/chemistry/carbon_monoxide.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">carbon monoxide</a>,
<a href="/physical_science/chemistry/carbon_dioxide.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">carbon dioxide</a>,
<a href="/physical_science/chemistry/sulfur_oxides.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">sulfur dioxide</a> and
<a href="/earth/Atmosphere/particulates.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">particulates</a>.
Some of these gases are <a href="/earth/climate/cli_greengas.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">greenhouse
gases</a>,
meaning that they retain heat in the Earth's atmosphere, due to the Earth's
<a href="/earth/climate/earth_greenhouse.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">greenhouse effect</a>.<p><small><em>Image copyright UCAR</em></small></p><b><i>Looking for online resources to use in support of climate change education?</i></b>  Our <a href="/teacher_resources/climate.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">Climate Change Educator Resources page</a> provides links to online content, classroom activities, interactives, and videos as well as resources provided by other leading organizations and agencies on this topic.  Our <a href="/teacher_resources/climate_change_course.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">Climate Change Course Content page</a> provides links to online content for a range of climate change associated topics.<p><small><em>Image courtesy of   Mila Zinkova, Creative Commons Attribution ShareAlike license</em></small></p>Greenland's <a href="http://www.windows2universe.org/earth/polar/cryosphere_glacier1.html">ice sheet</a> saw a record <a href="http://www.windows2universe.org/headline_universe/olpa/greenland_10dec07.html">melt</a> in July 2012.  Scientists studying this event have found that this melting event was triggered by an influx of unusually warm air and amplified by the presence of a blanket of thin low-level <a href="http://www.windows2universe.org/earth/Atmosphere/cloud.html">clouds</a> which pushed temperatures up above freezing.  For more information see the <a href="http://www.news.wisc.edu/21638">press release</a> from the University of Wisconsin Madison.<p><small><em>Image courtesy of University of Wisconsin-Madison</em></small></p>Scientists at the University of Michigan have found that <a href="/earth/polar/cryosphere_permafrost1.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">permafrost</a> in the <a href="/earth/polar/polar_north.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">Arctic</a> is extremely sensitive to sunlight.  Exposure to sunlight releases carbon gases trapped in the permafrost, including <a href="/earth/climate/earth_greenhouse.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">climate-warming</a> <a href="/physical_science/chemistry/carbon_dioxide.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">carbon dioxide</a>, to the <a href="/earth/Atmosphere/overview.html&edu=elem&dev=1/earth/Atmosphere/moons/megacities.html">atmosphere</a> much faster than previously thought.<p><small><em>George Kling, The University of Michigan</em></small></p>

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