Nonlinear (MARS) modeling of long-term variations of surface UV-B radiation as revealed from the analysis of Belsk, Poland data for the period 1976–2000

A new, powerful statistical technique, multivariate adaptive regression splines (MARS), is applied to reproduce monthly fractional deviations of UV-B doses over Belsk, Poland, during the snowless (May–October) part of the year in the period 1976–2000. Two kinds of regressors were used: local ones (t...

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Published in:Annales Geophysicae
Main Author: Krzyścin, J. W.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-21-1887-2003
https://angeo.copernicus.org/articles/21/1887/2003/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo35018 2023-05-15T17:34:22+02:00 Nonlinear (MARS) modeling of long-term variations of surface UV-B radiation as revealed from the analysis of Belsk, Poland data for the period 1976–2000 Krzyścin, J. W. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-21-1887-2003 https://angeo.copernicus.org/articles/21/1887/2003/ eng eng doi:10.5194/angeo-21-1887-2003 https://angeo.copernicus.org/articles/21/1887/2003/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-21-1887-2003 2020-07-20T16:27:41Z A new, powerful statistical technique, multivariate adaptive regression splines (MARS), is applied to reproduce monthly fractional deviations of UV-B doses over Belsk, Poland, during the snowless (May–October) part of the year in the period 1976–2000. Two kinds of regressors were used: local ones (total ozone, percentage of sky covered by low-, mid-, high-level clouds or total solar radiation over Belsk) and non-local ones, i.e. those describing the long-distance forcings on the surface UV-B due to changes in the global atmospheric circulation. Standard indices of the Quasi-Biennial, North Atlantic, El Niño-Southern Oscillations, and the 11-year solar activity were used as non-local regressors. The results there indicate that the MARS procedure is able to reproduce the observed year-to-year and decadal oscillations in the UV data. The MARS model yields better model-observation agreement than an ordinary least-squares fit based on the same set of regressors. It is found that MARS is capable of handling interactions between the local and non-local regressors, suggesting a possible nonlinear nature of connections between variables characterizing the atmospheric transparency over Belsk and the long-distance forcings. MARS enables a reconstruction of the surface UV-B variations over any site based on the cloud and ozone data presently stored on web pages. Key words. Atmospheric composition and structure (aerosols and particles; biosphere-atmosphere interactions) Text North Atlantic Copernicus Publications: E-Journals Annales Geophysicae 21 8 1887 1896
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description A new, powerful statistical technique, multivariate adaptive regression splines (MARS), is applied to reproduce monthly fractional deviations of UV-B doses over Belsk, Poland, during the snowless (May–October) part of the year in the period 1976–2000. Two kinds of regressors were used: local ones (total ozone, percentage of sky covered by low-, mid-, high-level clouds or total solar radiation over Belsk) and non-local ones, i.e. those describing the long-distance forcings on the surface UV-B due to changes in the global atmospheric circulation. Standard indices of the Quasi-Biennial, North Atlantic, El Niño-Southern Oscillations, and the 11-year solar activity were used as non-local regressors. The results there indicate that the MARS procedure is able to reproduce the observed year-to-year and decadal oscillations in the UV data. The MARS model yields better model-observation agreement than an ordinary least-squares fit based on the same set of regressors. It is found that MARS is capable of handling interactions between the local and non-local regressors, suggesting a possible nonlinear nature of connections between variables characterizing the atmospheric transparency over Belsk and the long-distance forcings. MARS enables a reconstruction of the surface UV-B variations over any site based on the cloud and ozone data presently stored on web pages. Key words. Atmospheric composition and structure (aerosols and particles; biosphere-atmosphere interactions)
format Text
author Krzyścin, J. W.
spellingShingle Krzyścin, J. W.
Nonlinear (MARS) modeling of long-term variations of surface UV-B radiation as revealed from the analysis of Belsk, Poland data for the period 1976–2000
author_facet Krzyścin, J. W.
author_sort Krzyścin, J. W.
title Nonlinear (MARS) modeling of long-term variations of surface UV-B radiation as revealed from the analysis of Belsk, Poland data for the period 1976–2000
title_short Nonlinear (MARS) modeling of long-term variations of surface UV-B radiation as revealed from the analysis of Belsk, Poland data for the period 1976–2000
title_full Nonlinear (MARS) modeling of long-term variations of surface UV-B radiation as revealed from the analysis of Belsk, Poland data for the period 1976–2000
title_fullStr Nonlinear (MARS) modeling of long-term variations of surface UV-B radiation as revealed from the analysis of Belsk, Poland data for the period 1976–2000
title_full_unstemmed Nonlinear (MARS) modeling of long-term variations of surface UV-B radiation as revealed from the analysis of Belsk, Poland data for the period 1976–2000
title_sort nonlinear (mars) modeling of long-term variations of surface uv-b radiation as revealed from the analysis of belsk, poland data for the period 1976–2000
publishDate 2018
url https://doi.org/10.5194/angeo-21-1887-2003
https://angeo.copernicus.org/articles/21/1887/2003/
genre North Atlantic
genre_facet North Atlantic
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-21-1887-2003
https://angeo.copernicus.org/articles/21/1887/2003/
op_doi https://doi.org/10.5194/angeo-21-1887-2003
container_title Annales Geophysicae
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container_issue 8
container_start_page 1887
op_container_end_page 1896
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