Future climate change
The climatic effects of rising CO 2 levels will become increasingly significantin the future. Consumption of estimated reserves of fossil fuels in the next two or three centuries will add far more CO 2 to the atmosphere than has been emitted to date unless ambitious conservation efforts or technolog...
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ftzenodo:oai:zenodo.org:7678446 2024-09-15T18:11:59+00:00 Future climate change Raviraja. S 2023-01-30 https://doi.org/10.5281/zenodo.7678446 https://doi.org/10.30574/gscarr.2023.14.1.0373 eng eng Zenodo https://zenodo.org/communities/gscarr https://doi.org/10.5281/zenodo.7678445 https://doi.org/10.5281/zenodo.7678446 oai:zenodo.org:7678446 https://doi.org/10.30574/gscarr.2023.14.1.0373 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode GSC Advanced Research and Reviews, 14(1), 050-054, (2023-01-30) Atmosphere Climate CO2 Ocean info:eu-repo/semantics/article 2023 ftzenodo https://doi.org/10.5281/zenodo.767844610.30574/gscarr.2023.14.1.037310.5281/zenodo.7678445 2024-07-27T02:24:49Z The climatic effects of rising CO 2 levels will become increasingly significantin the future. Consumption of estimated reserves of fossil fuels in the next two or three centuries will add far more CO 2 to the atmosphere than has been emitted to date unless ambitious conservation efforts or technological innovations reduce the influx. Atmospheric CO 2 concentrations will increase to levels at least twice and possibly four times the highest amounts measured in the last 800,000 years spanned by ice-core records. This warming will overwhelm natural variations in climate and cause climatic and environmental changes unprecedented in human experience. Atmospheric CO 2 levels will eventually decrease as the ocean slowly absorbs much of the excess carbon, but this process will acidify the oceans. After the main pulse of fossil-fuel emissions has passed, atmosphericCO 2 values will decrease back toward preindustrial levels, but enough CO 2 willremain in the atmosphere to prevent future glaciations for tens of thousands of years. Article in Journal/Newspaper ice core Zenodo |
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Atmosphere Climate CO2 Ocean |
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Atmosphere Climate CO2 Ocean Raviraja. S Future climate change |
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Atmosphere Climate CO2 Ocean |
description |
The climatic effects of rising CO 2 levels will become increasingly significantin the future. Consumption of estimated reserves of fossil fuels in the next two or three centuries will add far more CO 2 to the atmosphere than has been emitted to date unless ambitious conservation efforts or technological innovations reduce the influx. Atmospheric CO 2 concentrations will increase to levels at least twice and possibly four times the highest amounts measured in the last 800,000 years spanned by ice-core records. This warming will overwhelm natural variations in climate and cause climatic and environmental changes unprecedented in human experience. Atmospheric CO 2 levels will eventually decrease as the ocean slowly absorbs much of the excess carbon, but this process will acidify the oceans. After the main pulse of fossil-fuel emissions has passed, atmosphericCO 2 values will decrease back toward preindustrial levels, but enough CO 2 willremain in the atmosphere to prevent future glaciations for tens of thousands of years. |
format |
Article in Journal/Newspaper |
author |
Raviraja. S |
author_facet |
Raviraja. S |
author_sort |
Raviraja. S |
title |
Future climate change |
title_short |
Future climate change |
title_full |
Future climate change |
title_fullStr |
Future climate change |
title_full_unstemmed |
Future climate change |
title_sort |
future climate change |
publisher |
Zenodo |
publishDate |
2023 |
url |
https://doi.org/10.5281/zenodo.7678446 https://doi.org/10.30574/gscarr.2023.14.1.0373 |
genre |
ice core |
genre_facet |
ice core |
op_source |
GSC Advanced Research and Reviews, 14(1), 050-054, (2023-01-30) |
op_relation |
https://zenodo.org/communities/gscarr https://doi.org/10.5281/zenodo.7678445 https://doi.org/10.5281/zenodo.7678446 oai:zenodo.org:7678446 https://doi.org/10.30574/gscarr.2023.14.1.0373 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.767844610.30574/gscarr.2023.14.1.037310.5281/zenodo.7678445 |
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1810449580263735296 |