Empirical estimation of anthropogenic and natural contributions to surface air temperature trends at different latitudes

How strong are quantitative contributions of the key natural modes of climate variability and the anthropogenic factor characterized by the changes of the radiative forcing of greenhouse gases in the atmosphere to the trends of the surface air temperature at different latitudes of the Northern and S...

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Main Authors: Mokhov, I. I., Smirnov, D. A.
Format: Article in Journal/Newspaper
Language:unknown
Published: arXiv 2021
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.2112.01272
https://arxiv.org/abs/2112.01272
id ftdatacite:10.48550/arxiv.2112.01272
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spelling ftdatacite:10.48550/arxiv.2112.01272 2023-05-15T13:33:11+02:00 Empirical estimation of anthropogenic and natural contributions to surface air temperature trends at different latitudes Mokhov, I. I. Smirnov, D. A. 2021 https://dx.doi.org/10.48550/arxiv.2112.01272 https://arxiv.org/abs/2112.01272 unknown arXiv Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences Article CreativeWork article Preprint 2021 ftdatacite https://doi.org/10.48550/arxiv.2112.01272 2022-03-10T13:14:54Z How strong are quantitative contributions of the key natural modes of climate variability and the anthropogenic factor characterized by the changes of the radiative forcing of greenhouse gases in the atmosphere to the trends of the surface air temperature at different latitudes of the Northern and Southern Hemispheres on various time intervals? Such contributions to trends are estimated here from observation data with the simplest empirical models. Trivariate autoregressive models are fitted to the data since the 19th century and used to assess the impact of the anthropogenic forcing together with different natural climate modes including Atlantic Multidecadal Oscillation, El-Nino / Southern Oscillation, Interdecadal Pacific Oscillation, Pacific Decadal Oscillation, and Antarctic Oscillation. For relatively short intervals of the length of two or three decades, we note considerable contributions of the climate variability modes which are comparable to the contributions of the greenhouse gases and even exceed the latter. For longer intervals of about half a century and greater, the contributions of greenhouse gases dominate at all latitudes as follows from the present analysis of data for polar, middle and tropical regions. : 15 pages, 2 figures Article in Journal/Newspaper Antarc* Antarctic DataCite Metadata Store (German National Library of Science and Technology) Antarctic Pacific
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
spellingShingle Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
Mokhov, I. I.
Smirnov, D. A.
Empirical estimation of anthropogenic and natural contributions to surface air temperature trends at different latitudes
topic_facet Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
description How strong are quantitative contributions of the key natural modes of climate variability and the anthropogenic factor characterized by the changes of the radiative forcing of greenhouse gases in the atmosphere to the trends of the surface air temperature at different latitudes of the Northern and Southern Hemispheres on various time intervals? Such contributions to trends are estimated here from observation data with the simplest empirical models. Trivariate autoregressive models are fitted to the data since the 19th century and used to assess the impact of the anthropogenic forcing together with different natural climate modes including Atlantic Multidecadal Oscillation, El-Nino / Southern Oscillation, Interdecadal Pacific Oscillation, Pacific Decadal Oscillation, and Antarctic Oscillation. For relatively short intervals of the length of two or three decades, we note considerable contributions of the climate variability modes which are comparable to the contributions of the greenhouse gases and even exceed the latter. For longer intervals of about half a century and greater, the contributions of greenhouse gases dominate at all latitudes as follows from the present analysis of data for polar, middle and tropical regions. : 15 pages, 2 figures
format Article in Journal/Newspaper
author Mokhov, I. I.
Smirnov, D. A.
author_facet Mokhov, I. I.
Smirnov, D. A.
author_sort Mokhov, I. I.
title Empirical estimation of anthropogenic and natural contributions to surface air temperature trends at different latitudes
title_short Empirical estimation of anthropogenic and natural contributions to surface air temperature trends at different latitudes
title_full Empirical estimation of anthropogenic and natural contributions to surface air temperature trends at different latitudes
title_fullStr Empirical estimation of anthropogenic and natural contributions to surface air temperature trends at different latitudes
title_full_unstemmed Empirical estimation of anthropogenic and natural contributions to surface air temperature trends at different latitudes
title_sort empirical estimation of anthropogenic and natural contributions to surface air temperature trends at different latitudes
publisher arXiv
publishDate 2021
url https://dx.doi.org/10.48550/arxiv.2112.01272
https://arxiv.org/abs/2112.01272
geographic Antarctic
Pacific
geographic_facet Antarctic
Pacific
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.48550/arxiv.2112.01272
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