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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Main Authors: Fedorov, Valery, Fedorova, Ekaterina, Zalihanov, Alim
Format: Article in Journal/Newspaper
Language:Russian
Published: Zenodo 2022
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.6371865
https://zenodo.org/record/6371865
id ftdatacite:10.5281/zenodo.6371865
record_format openpolar
spelling ftdatacite:10.5281/zenodo.6371865 2023-05-15T15:09:06+02:00 Estimative Forecast of Changes in the Individual Components of Environment based on a regression model Fedorov, Valery Fedorova, Ekaterina Zalihanov, Alim 2022 https://dx.doi.org/10.5281/zenodo.6371865 https://zenodo.org/record/6371865 ru rus Zenodo https://zenodo.org/communities/jeees https://dx.doi.org/10.5281/zenodo.6371864 https://zenodo.org/communities/jeees Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY estimative forecast insolation contrast range World Ocean level area of the sea ice glacier mass balance regression model article-journal ScholarlyArticle JournalArticle 2022 ftdatacite https://doi.org/10.5281/zenodo.6371865 https://doi.org/10.5281/zenodo.6371864 2022-04-01T17:27:16Z 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 km 2 or by 29.4%, the minimal one – by 5.65 million km 2 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 DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
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
Fedorov, Valery
Fedorova, Ekaterina
Zalihanov, Alim
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 km 2 or by 29.4%, the minimal one – by 5.65 million km 2 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 Fedorov, Valery
Fedorova, Ekaterina
Zalihanov, Alim
author_facet Fedorov, Valery
Fedorova, Ekaterina
Zalihanov, Alim
author_sort Fedorov, Valery
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
publisher Zenodo
publishDate 2022
url https://dx.doi.org/10.5281/zenodo.6371865
https://zenodo.org/record/6371865
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_relation https://zenodo.org/communities/jeees
https://dx.doi.org/10.5281/zenodo.6371864
https://zenodo.org/communities/jeees
op_rights Open Access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5281/zenodo.6371865
https://doi.org/10.5281/zenodo.6371864
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