Atmospheric Chemistry and Climate in the Anthropocene / Chemia Atmosferyczna I Klimat W Antropocenie

Abstract Humankind actions are exerting increasing effect on the environment on all scales, in a lot of ways overcoming natural processes. During the last 100 years human population went up from little more than one to six billion and economic activity increased nearly ten times between 1950 and the...

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Published in:Chemistry-Didactics-Ecology-Metrology
Main Authors: Crutzen, Paul J., Wacławek, Stanisław
Format: Article in Journal/Newspaper
Language:English
Published: Walter de Gruyter GmbH 2014
Subjects:
Online Access:http://dx.doi.org/10.1515/cdem-2014-0001
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spelling crdegruyter:10.1515/cdem-2014-0001 2024-09-30T14:27:08+00:00 Atmospheric Chemistry and Climate in the Anthropocene / Chemia Atmosferyczna I Klimat W Antropocenie Crutzen, Paul J. Wacławek, Stanisław 2014 http://dx.doi.org/10.1515/cdem-2014-0001 http://content.sciendo.com/view/journals/cdem/19/1-2/article-p9.xml https://www.sciendo.com/article/10.1515/cdem-2014-0001 en eng Walter de Gruyter GmbH http://creativecommons.org/licenses/by-nc-nd/3.0/ Chemistry-Didactics-Ecology-Metrology volume 19, issue 1-2, page 9-28 ISSN 2084-4506 journal-article 2014 crdegruyter https://doi.org/10.1515/cdem-2014-0001 2024-09-17T04:10:32Z Abstract Humankind actions are exerting increasing effect on the environment on all scales, in a lot of ways overcoming natural processes. During the last 100 years human population went up from little more than one to six billion and economic activity increased nearly ten times between 1950 and the present time. In the last few decades of the twentieth century, anthropogenic chlorofluorocarbon release have led to a dramatic decrease in levels of stratospheric ozone, creating ozone hole over the Antarctic, as a result UV-B radiation from the sun increased, leading for example to enhanced risk of skin cancer. Releasing more of a greenhouse gases by mankind, such as CO 2 , CH 4 , NO x to the atmosphere increases the greenhouse effect. Even if emission increase has held back, atmospheric greenhouse gas concentrations would continue to raise and remain high for hundreds of years, thus warming Earth’s climate. Warming temperatures contribute to sea level growth by melting mountain glaciers and ice caps, because of these portions of the Greenland and Antarctic ice sheets melt or flow into the ocean. Ice loss from the Greenland and Antarctic ice sheets could contribute an additional 19-58 centimeters of sea level rise, hinge on how the ice sheets react. Taking into account these and many other major and still growing footprints of human activities on earth and atmosphere without any doubt we can conclude that we are living in new geological epoch named by P. Crutzen and E. Stoermer in 2000 - “Anthropocene”. For the benefit of our children and their future, we must do more to struggle climate changes that have had occurred gradually over the last century. Article in Journal/Newspaper Antarc* Antarctic Greenland De Gruyter Antarctic The Antarctic Greenland Chemistry-Didactics-Ecology-Metrology 19 1-2 9 28
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description Abstract Humankind actions are exerting increasing effect on the environment on all scales, in a lot of ways overcoming natural processes. During the last 100 years human population went up from little more than one to six billion and economic activity increased nearly ten times between 1950 and the present time. In the last few decades of the twentieth century, anthropogenic chlorofluorocarbon release have led to a dramatic decrease in levels of stratospheric ozone, creating ozone hole over the Antarctic, as a result UV-B radiation from the sun increased, leading for example to enhanced risk of skin cancer. Releasing more of a greenhouse gases by mankind, such as CO 2 , CH 4 , NO x to the atmosphere increases the greenhouse effect. Even if emission increase has held back, atmospheric greenhouse gas concentrations would continue to raise and remain high for hundreds of years, thus warming Earth’s climate. Warming temperatures contribute to sea level growth by melting mountain glaciers and ice caps, because of these portions of the Greenland and Antarctic ice sheets melt or flow into the ocean. Ice loss from the Greenland and Antarctic ice sheets could contribute an additional 19-58 centimeters of sea level rise, hinge on how the ice sheets react. Taking into account these and many other major and still growing footprints of human activities on earth and atmosphere without any doubt we can conclude that we are living in new geological epoch named by P. Crutzen and E. Stoermer in 2000 - “Anthropocene”. For the benefit of our children and their future, we must do more to struggle climate changes that have had occurred gradually over the last century.
format Article in Journal/Newspaper
author Crutzen, Paul J.
Wacławek, Stanisław
spellingShingle Crutzen, Paul J.
Wacławek, Stanisław
Atmospheric Chemistry and Climate in the Anthropocene / Chemia Atmosferyczna I Klimat W Antropocenie
author_facet Crutzen, Paul J.
Wacławek, Stanisław
author_sort Crutzen, Paul J.
title Atmospheric Chemistry and Climate in the Anthropocene / Chemia Atmosferyczna I Klimat W Antropocenie
title_short Atmospheric Chemistry and Climate in the Anthropocene / Chemia Atmosferyczna I Klimat W Antropocenie
title_full Atmospheric Chemistry and Climate in the Anthropocene / Chemia Atmosferyczna I Klimat W Antropocenie
title_fullStr Atmospheric Chemistry and Climate in the Anthropocene / Chemia Atmosferyczna I Klimat W Antropocenie
title_full_unstemmed Atmospheric Chemistry and Climate in the Anthropocene / Chemia Atmosferyczna I Klimat W Antropocenie
title_sort atmospheric chemistry and climate in the anthropocene / chemia atmosferyczna i klimat w antropocenie
publisher Walter de Gruyter GmbH
publishDate 2014
url http://dx.doi.org/10.1515/cdem-2014-0001
http://content.sciendo.com/view/journals/cdem/19/1-2/article-p9.xml
https://www.sciendo.com/article/10.1515/cdem-2014-0001
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The Antarctic
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op_source Chemistry-Didactics-Ecology-Metrology
volume 19, issue 1-2, page 9-28
ISSN 2084-4506
op_rights http://creativecommons.org/licenses/by-nc-nd/3.0/
op_doi https://doi.org/10.1515/cdem-2014-0001
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