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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Bibliographic Details
Main Author: Raviraja. S
Format: Article in Journal/Newspaper
Language:English
Published: Zenodo 2023
Subjects:
CO2
Online Access:https://doi.org/10.5281/zenodo.7678446
https://doi.org/10.30574/gscarr.2023.14.1.0373
id ftzenodo:oai:zenodo.org:7678446
record_format openpolar
spelling 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
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Atmosphere
Climate
CO2
Ocean
spellingShingle Atmosphere
Climate
CO2
Ocean
Raviraja. S
Future climate change
topic_facet 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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