New criteria and requirements for reducing and stopping the global warming

Abstract It has long been known that the absorption of terrestrial energy by water molecules is the largest one (60-75 %), comparing with the lower value (20-24 %) of carbon dioxide molecules. The other gases with greenhouse effect absorb this energy in much smaller extent (8-12 %). In the last 360...

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Main Author: Muzsnay, Csaba
Format: Text
Language:English
Published: European Chemical Bulletin 2013
Subjects:
Online Access:https://dx.doi.org/10.17628/ecb.2013.2.485-489
http://www.eurchembull.com/index.php/ECB/article/view/280
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spelling ftdatacite:10.17628/ecb.2013.2.485-489 2023-05-15T17:40:00+02:00 New criteria and requirements for reducing and stopping the global warming Muzsnay, Csaba 2013 https://dx.doi.org/10.17628/ecb.2013.2.485-489 http://www.eurchembull.com/index.php/ECB/article/view/280 en eng European Chemical Bulletin Text Article article-journal ScholarlyArticle 2013 ftdatacite https://doi.org/10.17628/ecb.2013.2.485-489 2021-11-05T12:55:41Z Abstract It has long been known that the absorption of terrestrial energy by water molecules is the largest one (60-75 %), comparing with the lower value (20-24 %) of carbon dioxide molecules. The other gases with greenhouse effect absorb this energy in much smaller extent (8-12 %). In the last 360 years, considering from the industrial revolution, the amount of water vapor resulting on the basis of eight types of major processes, by direct and indirect human activities, and getting into the atmosphere was continuously growing. These are determined, by the appearance of very numerous human activities originated water-vapor/steam generators, the continuous increase of the greenhouse effect and the climate change. The following levels of special and extraordinary behavior of the atmospheric water vapor can be distinguished: 1) molecular, 2) associative (cluster) level, 3) condensation level which can be joined to phase transformations - mainly in the clouds, 4) the level of precipitate formation followed by intense moisture transport, 5) the level of firm difference existing between the atmospheric relations of the Northern and the Southern Hemisphere, mainly due to human activities. The atmosphere near the Earth's surface (in the troposphere) has such a well delimited temperature and pressure domain, in which water with its unique property occurs in all three phases. Water vapors condense easily. The triple point of the other atmospheric components is not achieved. This unique and extraordinary feature of the water plays a determining role in the meteorological processes of the Earth and the development of the climatic relations. All this warming, among other things, is manifested in the melting of the ice of the North Pole and the elevation of the snow altitude line. The primary task is the stopping of the warming of theNorth Pole Region and the promotion of its cooling. Global solutions appear as mandatory needs, which are very costly to start because extensive investments are required. : European Chemical Bulletin, Vol 2, No 7 (2013): European Chemical Bulletin Text North Pole DataCite Metadata Store (German National Library of Science and Technology) North Pole
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description Abstract It has long been known that the absorption of terrestrial energy by water molecules is the largest one (60-75 %), comparing with the lower value (20-24 %) of carbon dioxide molecules. The other gases with greenhouse effect absorb this energy in much smaller extent (8-12 %). In the last 360 years, considering from the industrial revolution, the amount of water vapor resulting on the basis of eight types of major processes, by direct and indirect human activities, and getting into the atmosphere was continuously growing. These are determined, by the appearance of very numerous human activities originated water-vapor/steam generators, the continuous increase of the greenhouse effect and the climate change. The following levels of special and extraordinary behavior of the atmospheric water vapor can be distinguished: 1) molecular, 2) associative (cluster) level, 3) condensation level which can be joined to phase transformations - mainly in the clouds, 4) the level of precipitate formation followed by intense moisture transport, 5) the level of firm difference existing between the atmospheric relations of the Northern and the Southern Hemisphere, mainly due to human activities. The atmosphere near the Earth's surface (in the troposphere) has such a well delimited temperature and pressure domain, in which water with its unique property occurs in all three phases. Water vapors condense easily. The triple point of the other atmospheric components is not achieved. This unique and extraordinary feature of the water plays a determining role in the meteorological processes of the Earth and the development of the climatic relations. All this warming, among other things, is manifested in the melting of the ice of the North Pole and the elevation of the snow altitude line. The primary task is the stopping of the warming of theNorth Pole Region and the promotion of its cooling. Global solutions appear as mandatory needs, which are very costly to start because extensive investments are required. : European Chemical Bulletin, Vol 2, No 7 (2013): European Chemical Bulletin
format Text
author Muzsnay, Csaba
spellingShingle Muzsnay, Csaba
New criteria and requirements for reducing and stopping the global warming
author_facet Muzsnay, Csaba
author_sort Muzsnay, Csaba
title New criteria and requirements for reducing and stopping the global warming
title_short New criteria and requirements for reducing and stopping the global warming
title_full New criteria and requirements for reducing and stopping the global warming
title_fullStr New criteria and requirements for reducing and stopping the global warming
title_full_unstemmed New criteria and requirements for reducing and stopping the global warming
title_sort new criteria and requirements for reducing and stopping the global warming
publisher European Chemical Bulletin
publishDate 2013
url https://dx.doi.org/10.17628/ecb.2013.2.485-489
http://www.eurchembull.com/index.php/ECB/article/view/280
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op_doi https://doi.org/10.17628/ecb.2013.2.485-489
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