Researchers have begun to notice visible signs of drastic climate
change in the Arctic and are actively contributing to finding solutions to help
prevent dangerous human produced interferences with the climate system. The
rate of climate warming in the Arctic is something that researchers find to be
detrimental to the longevity of the ecosystems. Advocators are pushing for ways
to elicit the issue and warn people of the closeness of abrupt changes and
policy making. Experts are concerned with finding ways to soften the causes of
climate warming, warn about the drastic changes and for reinforced adaptation
and recovery capacity of the ecosystems and populations. The Arctic is prone to
show changes that can drastically affect the Global Earth system. The Arctic is
showing signs of tipping elements. Which are components of the earth system
that shows signs of tipping. Human activities like transportation, shipping,
and resource exploitation greatly contributes to the climate changes in the
Arctic.
In the long run the issue can affect all aspects of our
global earth system and the ecosystems that make our world unique and complex.
This in turn can greatly affect the way we live our daily lives through work,
school, and family life. Gas emissions continue to negatively affect the
climate change throughout our environment. With climate changes we will have to
eventually make changes in our everyday lives such as; transportation to work, agricultural
growth, and availability of resources in our society. What we should analyze is
the ways in which we contribute to destructing the ozone layers resulting in
global climate changes. If we as a society begin to implement methods that
preserve our society as much as possible, we can contribute greatly to the halt
of climate change in the Arctic as well as other tipping points in our world.
CSIC, Consejo
Superior de Investigaciones Científicas (2012, January 30). Arctic is already
suffering the effects of a dangerous climate change. ScienceDaily. Retrieved February 3,
2012, from http://www.sciencedaily.com /releases/2012/01/120130171913.htm
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