Atmospheric teleconnections between the Arctic and the eastern Baltic Sea regions

The teleconnections between meteorological parameters of the Arctic and the eastern Baltic Sea regions were analysed based on the NCEP-CFSR and ERA-Interim reanalysis data for 1979–2015. The eastern Baltic Sea region was characterised by meteorological values at a testing point (TP) in southern Esto...

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Published in:Earth System Dynamics
Main Authors: Jakobson, Liisi, Jakobson, Erko, Post, Piia, Jaagus, Jaak
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/esd-8-1019-2017
https://esd.copernicus.org/articles/8/1019/2017/
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spelling ftcopernicus:oai:publications.copernicus.org:esd58263 2023-05-15T14:47:07+02:00 Atmospheric teleconnections between the Arctic and the eastern Baltic Sea regions Jakobson, Liisi Jakobson, Erko Post, Piia Jaagus, Jaak 2018-09-27 application/pdf https://doi.org/10.5194/esd-8-1019-2017 https://esd.copernicus.org/articles/8/1019/2017/ eng eng doi:10.5194/esd-8-1019-2017 https://esd.copernicus.org/articles/8/1019/2017/ eISSN: 2190-4987 Text 2018 ftcopernicus https://doi.org/10.5194/esd-8-1019-2017 2020-07-20T16:23:33Z The teleconnections between meteorological parameters of the Arctic and the eastern Baltic Sea regions were analysed based on the NCEP-CFSR and ERA-Interim reanalysis data for 1979–2015. The eastern Baltic Sea region was characterised by meteorological values at a testing point (TP) in southern Estonia (58° N, 26° E). Temperature at the 1000 hPa level at the TP have a strong negative correlation with the Greenland sector (the region between 55–80° N and 20–80° W) during all seasons except summer. Significant teleconnections are present in temperature profiles from 1000 to 500 hPa. The strongest teleconnections between the same parameter at the eastern Baltic Sea region and the Arctic are found in winter, but they are clearly affected by the Arctic Oscillation (AO) index. After removal of the AO index variability, correlations in winter were below ±0.5, while in other seasons there remained regions with strong (| R | > 0.5, p < 0.002) correlations. Strong correlations (| R | > 0.5) are also present between different climate variables (sea-level pressure, specific humidity, wind speed) at the TP and different regions of the Arctic. These teleconnections cannot be explained solely with the variability of circulation indices. The positive temperature anomaly of mild winter at the Greenland sector shifts towards east during the next seasons, reaching the Baltic Sea region in summer. This evolution is present at 60 and 65° N but is missing at higher latitudes. The most permanent lagged correlations in 1000 hPa temperature reveal that the temperature in summer at the TP is strongly predestined by temperature in the Greenland sector in the previous spring and winter. Text Arctic Greenland Copernicus Publications: E-Journals Arctic Greenland Earth System Dynamics 8 4 1019 1030
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The teleconnections between meteorological parameters of the Arctic and the eastern Baltic Sea regions were analysed based on the NCEP-CFSR and ERA-Interim reanalysis data for 1979–2015. The eastern Baltic Sea region was characterised by meteorological values at a testing point (TP) in southern Estonia (58° N, 26° E). Temperature at the 1000 hPa level at the TP have a strong negative correlation with the Greenland sector (the region between 55–80° N and 20–80° W) during all seasons except summer. Significant teleconnections are present in temperature profiles from 1000 to 500 hPa. The strongest teleconnections between the same parameter at the eastern Baltic Sea region and the Arctic are found in winter, but they are clearly affected by the Arctic Oscillation (AO) index. After removal of the AO index variability, correlations in winter were below ±0.5, while in other seasons there remained regions with strong (| R | > 0.5, p < 0.002) correlations. Strong correlations (| R | > 0.5) are also present between different climate variables (sea-level pressure, specific humidity, wind speed) at the TP and different regions of the Arctic. These teleconnections cannot be explained solely with the variability of circulation indices. The positive temperature anomaly of mild winter at the Greenland sector shifts towards east during the next seasons, reaching the Baltic Sea region in summer. This evolution is present at 60 and 65° N but is missing at higher latitudes. The most permanent lagged correlations in 1000 hPa temperature reveal that the temperature in summer at the TP is strongly predestined by temperature in the Greenland sector in the previous spring and winter.
format Text
author Jakobson, Liisi
Jakobson, Erko
Post, Piia
Jaagus, Jaak
spellingShingle Jakobson, Liisi
Jakobson, Erko
Post, Piia
Jaagus, Jaak
Atmospheric teleconnections between the Arctic and the eastern Baltic Sea regions
author_facet Jakobson, Liisi
Jakobson, Erko
Post, Piia
Jaagus, Jaak
author_sort Jakobson, Liisi
title Atmospheric teleconnections between the Arctic and the eastern Baltic Sea regions
title_short Atmospheric teleconnections between the Arctic and the eastern Baltic Sea regions
title_full Atmospheric teleconnections between the Arctic and the eastern Baltic Sea regions
title_fullStr Atmospheric teleconnections between the Arctic and the eastern Baltic Sea regions
title_full_unstemmed Atmospheric teleconnections between the Arctic and the eastern Baltic Sea regions
title_sort atmospheric teleconnections between the arctic and the eastern baltic sea regions
publishDate 2018
url https://doi.org/10.5194/esd-8-1019-2017
https://esd.copernicus.org/articles/8/1019/2017/
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Greenland
genre_facet Arctic
Greenland
op_source eISSN: 2190-4987
op_relation doi:10.5194/esd-8-1019-2017
https://esd.copernicus.org/articles/8/1019/2017/
op_doi https://doi.org/10.5194/esd-8-1019-2017
container_title Earth System Dynamics
container_volume 8
container_issue 4
container_start_page 1019
op_container_end_page 1030
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