Estimative Forecast of Changes in the Individual Components of Environment based on a regression model
The study presents the results of an estimative forecast for the individual components of environment in XXI century. The forecast is based on a regression model and insolation contrast range as a predictor. It was determined that the level of the World Ocean by the end of the current century will r...
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ftzenodo:oai:zenodo.org:6371865 2023-06-06T11:51:12+02:00 Estimative Forecast of Changes in the Individual Components of Environment based on a regression model Valery Fedorov Ekaterina Fedorova Alim Zalihanov 2022-03-21 https://zenodo.org/record/6371865 https://doi.org/10.5281/zenodo.6371865 rus rus doi:10.5281/zenodo.6371864 https://zenodo.org/communities/jeees https://zenodo.org/record/6371865 https://doi.org/10.5281/zenodo.6371865 oai:zenodo.org:6371865 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Journal of Environmental Earth and Еnergy Study (JEEES) 62-80 estimative forecast insolation contrast range World Ocean level area of the sea ice glacier mass balance regression model info:eu-repo/semantics/article publication-article 2022 ftzenodo https://doi.org/10.5281/zenodo.637186510.5281/zenodo.6371864 2023-04-13T23:38:53Z The study presents the results of an estimative forecast for the individual components of environment in XXI century. The forecast is based on a regression model and insolation contrast range as a predictor. It was determined that the level of the World Ocean by the end of the current century will reach the value of 476 mm (relative to the beginning of the XXI century). The raise comparatively to 2020 will be 168 mm. Average annual area of the sea ice in the Northern Hemisphere since 2020 to 2100 will decrease by 3.39 million km2 or by 29.4%, the minimal one – by 5.65 million km2 or 77.1%. By 2050 comparatively to 2018 decrease of the sea ice area in Arctic Ocean will be 18.3% for the average annual area, 10.1% - for the maximal, and 60.3% - for the minimal area. On average, for the nine glacial regions of the Northern Hemisphere, the reduction in the ice mass balance from 1900 to 2050 is estimated at 42.9 m of water equivalent (w.e.). From 2020 to 2050 on average, for the glaciers covered by balance observations in the Northern Hemisphere, the reduction in ice mass is expected to be 8.8 m w.e. Article in Journal/Newspaper Arctic Arctic Ocean Sea ice Zenodo Arctic Arctic Ocean |
institution |
Open Polar |
collection |
Zenodo |
op_collection_id |
ftzenodo |
language |
Russian |
topic |
estimative forecast insolation contrast range World Ocean level area of the sea ice glacier mass balance regression model |
spellingShingle |
estimative forecast insolation contrast range World Ocean level area of the sea ice glacier mass balance regression model Valery Fedorov Ekaterina Fedorova Alim Zalihanov Estimative Forecast of Changes in the Individual Components of Environment based on a regression model |
topic_facet |
estimative forecast insolation contrast range World Ocean level area of the sea ice glacier mass balance regression model |
description |
The study presents the results of an estimative forecast for the individual components of environment in XXI century. The forecast is based on a regression model and insolation contrast range as a predictor. It was determined that the level of the World Ocean by the end of the current century will reach the value of 476 mm (relative to the beginning of the XXI century). The raise comparatively to 2020 will be 168 mm. Average annual area of the sea ice in the Northern Hemisphere since 2020 to 2100 will decrease by 3.39 million km2 or by 29.4%, the minimal one – by 5.65 million km2 or 77.1%. By 2050 comparatively to 2018 decrease of the sea ice area in Arctic Ocean will be 18.3% for the average annual area, 10.1% - for the maximal, and 60.3% - for the minimal area. On average, for the nine glacial regions of the Northern Hemisphere, the reduction in the ice mass balance from 1900 to 2050 is estimated at 42.9 m of water equivalent (w.e.). From 2020 to 2050 on average, for the glaciers covered by balance observations in the Northern Hemisphere, the reduction in ice mass is expected to be 8.8 m w.e. |
format |
Article in Journal/Newspaper |
author |
Valery Fedorov Ekaterina Fedorova Alim Zalihanov |
author_facet |
Valery Fedorov Ekaterina Fedorova Alim Zalihanov |
author_sort |
Valery Fedorov |
title |
Estimative Forecast of Changes in the Individual Components of Environment based on a regression model |
title_short |
Estimative Forecast of Changes in the Individual Components of Environment based on a regression model |
title_full |
Estimative Forecast of Changes in the Individual Components of Environment based on a regression model |
title_fullStr |
Estimative Forecast of Changes in the Individual Components of Environment based on a regression model |
title_full_unstemmed |
Estimative Forecast of Changes in the Individual Components of Environment based on a regression model |
title_sort |
estimative forecast of changes in the individual components of environment based on a regression model |
publishDate |
2022 |
url |
https://zenodo.org/record/6371865 https://doi.org/10.5281/zenodo.6371865 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Sea ice |
genre_facet |
Arctic Arctic Ocean Sea ice |
op_source |
Journal of Environmental Earth and Еnergy Study (JEEES) 62-80 |
op_relation |
doi:10.5281/zenodo.6371864 https://zenodo.org/communities/jeees https://zenodo.org/record/6371865 https://doi.org/10.5281/zenodo.6371865 oai:zenodo.org:6371865 |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.637186510.5281/zenodo.6371864 |
_version_ |
1767956917400895488 |