South Atlantic sea surface temperature anomalies and air-sea interactions: stochastic models

Data on the South Atlantic monthly sea surface temperature anomalies (SSTA) are analysed using the maximum-entropy method. It is shown that the Markov first-order process can describe, to a first approximation, SSTA series. The region of maximum SSTA values coincides with the zone of maximum residua...

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Published in:Annales Geophysicae
Main Author: Dobrovolski, S. G.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.1007/s00585-994-0903-9
https://angeo.copernicus.org/articles/12/903/1994/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo33735 2023-05-15T13:31:38+02:00 South Atlantic sea surface temperature anomalies and air-sea interactions: stochastic models Dobrovolski, S. G. 2018-09-27 application/pdf https://doi.org/10.1007/s00585-994-0903-9 https://angeo.copernicus.org/articles/12/903/1994/ eng eng doi:10.1007/s00585-994-0903-9 https://angeo.copernicus.org/articles/12/903/1994/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.1007/s00585-994-0903-9 2020-07-20T16:28:16Z Data on the South Atlantic monthly sea surface temperature anomalies (SSTA) are analysed using the maximum-entropy method. It is shown that the Markov first-order process can describe, to a first approximation, SSTA series. The region of maximum SSTA values coincides with the zone of maximum residual white noise values (sub-Antarctic hydrological front). The theory of dynamic-stochastic climate models is applied to estimate the variability of South Atlantic SSTA and air-sea interactions. The Adem model is used as a deterministic block of the dynamic-stochastic model. Experiments show satisfactorily the SSTA intensification in the sub-Antarctic front zone, with appropriate standard deviations, and demonstrate the leading role of the abnormal drift currents in these processes. Text Antarc* Antarctic Copernicus Publications: E-Journals Antarctic Annales Geophysicae 12 9 903 909
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Data on the South Atlantic monthly sea surface temperature anomalies (SSTA) are analysed using the maximum-entropy method. It is shown that the Markov first-order process can describe, to a first approximation, SSTA series. The region of maximum SSTA values coincides with the zone of maximum residual white noise values (sub-Antarctic hydrological front). The theory of dynamic-stochastic climate models is applied to estimate the variability of South Atlantic SSTA and air-sea interactions. The Adem model is used as a deterministic block of the dynamic-stochastic model. Experiments show satisfactorily the SSTA intensification in the sub-Antarctic front zone, with appropriate standard deviations, and demonstrate the leading role of the abnormal drift currents in these processes.
format Text
author Dobrovolski, S. G.
spellingShingle Dobrovolski, S. G.
South Atlantic sea surface temperature anomalies and air-sea interactions: stochastic models
author_facet Dobrovolski, S. G.
author_sort Dobrovolski, S. G.
title South Atlantic sea surface temperature anomalies and air-sea interactions: stochastic models
title_short South Atlantic sea surface temperature anomalies and air-sea interactions: stochastic models
title_full South Atlantic sea surface temperature anomalies and air-sea interactions: stochastic models
title_fullStr South Atlantic sea surface temperature anomalies and air-sea interactions: stochastic models
title_full_unstemmed South Atlantic sea surface temperature anomalies and air-sea interactions: stochastic models
title_sort south atlantic sea surface temperature anomalies and air-sea interactions: stochastic models
publishDate 2018
url https://doi.org/10.1007/s00585-994-0903-9
https://angeo.copernicus.org/articles/12/903/1994/
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source eISSN: 1432-0576
op_relation doi:10.1007/s00585-994-0903-9
https://angeo.copernicus.org/articles/12/903/1994/
op_doi https://doi.org/10.1007/s00585-994-0903-9
container_title Annales Geophysicae
container_volume 12
container_issue 9
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