Adding value to extended-range forecasts in northern Europe by statistical post-processing using stratospheric observations

The strength of the stratospheric polar vortex influences the surface weather in the Northern Hemisphere in winter; a weaker (stronger) than average stratospheric polar vortex is connected to negative (positive) Arctic Oscillation (AO) and colder (warmer) than average surface temperatures in norther...

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Published in:Atmospheric Chemistry and Physics
Main Authors: N. Korhonen, O. Hyvärinen, M. Kämäräinen, D. S. Richardson, H. Järvinen, H. Gregow
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/acp-20-8441-2020
https://doaj.org/article/f8a583301ab44f718a823843b58d067a
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spelling ftdoajarticles:oai:doaj.org/article:f8a583301ab44f718a823843b58d067a 2023-05-15T15:13:07+02:00 Adding value to extended-range forecasts in northern Europe by statistical post-processing using stratospheric observations N. Korhonen O. Hyvärinen M. Kämäräinen D. S. Richardson H. Järvinen H. Gregow 2020-07-01T00:00:00Z https://doi.org/10.5194/acp-20-8441-2020 https://doaj.org/article/f8a583301ab44f718a823843b58d067a EN eng Copernicus Publications https://www.atmos-chem-phys.net/20/8441/2020/acp-20-8441-2020.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-20-8441-2020 1680-7316 1680-7324 https://doaj.org/article/f8a583301ab44f718a823843b58d067a Atmospheric Chemistry and Physics, Vol 20, Pp 8441-8451 (2020) Physics QC1-999 Chemistry QD1-999 article 2020 ftdoajarticles https://doi.org/10.5194/acp-20-8441-2020 2022-12-31T14:59:14Z The strength of the stratospheric polar vortex influences the surface weather in the Northern Hemisphere in winter; a weaker (stronger) than average stratospheric polar vortex is connected to negative (positive) Arctic Oscillation (AO) and colder (warmer) than average surface temperatures in northern Europe within weeks or months. This holds the potential for forecasting in that timescale. We investigate here if the strength of the stratospheric polar vortex at the start of the forecast could be used to improve the extended-range temperature forecasts of the European Centre for Medium-Range Weather Forecasts (ECMWF) and to find periods with higher prediction skill scores. For this, we developed a stratospheric wind indicator (SWI) based on the strength of the stratospheric polar vortex and the phase of the AO during the following weeks. We demonstrate that there was a statistically significant difference in the observed surface temperature in northern Europe within the 3–6 weeks, depending on the SWI at the start of the forecast. When our new SWI was applied in post-processing the ECMWF's 2-week mean temperature reforecasts for weeks 3–4 and 5–6 in northern Europe during boreal winter, the skill scores of those weeks were slightly improved. This indicates there is some room for improving the extended-range forecasts, if the stratosphere–troposphere links were better captured in the modelling. In addition to this, we found that during the boreal winter, in cases where the polar vortex was weak at the start of the forecast, the mean skill scores of the 3–6 weeks' surface temperature forecasts were higher than average. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Atmospheric Chemistry and Physics 20 14 8441 8451
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Physics
QC1-999
Chemistry
QD1-999
spellingShingle Physics
QC1-999
Chemistry
QD1-999
N. Korhonen
O. Hyvärinen
M. Kämäräinen
D. S. Richardson
H. Järvinen
H. Gregow
Adding value to extended-range forecasts in northern Europe by statistical post-processing using stratospheric observations
topic_facet Physics
QC1-999
Chemistry
QD1-999
description The strength of the stratospheric polar vortex influences the surface weather in the Northern Hemisphere in winter; a weaker (stronger) than average stratospheric polar vortex is connected to negative (positive) Arctic Oscillation (AO) and colder (warmer) than average surface temperatures in northern Europe within weeks or months. This holds the potential for forecasting in that timescale. We investigate here if the strength of the stratospheric polar vortex at the start of the forecast could be used to improve the extended-range temperature forecasts of the European Centre for Medium-Range Weather Forecasts (ECMWF) and to find periods with higher prediction skill scores. For this, we developed a stratospheric wind indicator (SWI) based on the strength of the stratospheric polar vortex and the phase of the AO during the following weeks. We demonstrate that there was a statistically significant difference in the observed surface temperature in northern Europe within the 3–6 weeks, depending on the SWI at the start of the forecast. When our new SWI was applied in post-processing the ECMWF's 2-week mean temperature reforecasts for weeks 3–4 and 5–6 in northern Europe during boreal winter, the skill scores of those weeks were slightly improved. This indicates there is some room for improving the extended-range forecasts, if the stratosphere–troposphere links were better captured in the modelling. In addition to this, we found that during the boreal winter, in cases where the polar vortex was weak at the start of the forecast, the mean skill scores of the 3–6 weeks' surface temperature forecasts were higher than average.
format Article in Journal/Newspaper
author N. Korhonen
O. Hyvärinen
M. Kämäräinen
D. S. Richardson
H. Järvinen
H. Gregow
author_facet N. Korhonen
O. Hyvärinen
M. Kämäräinen
D. S. Richardson
H. Järvinen
H. Gregow
author_sort N. Korhonen
title Adding value to extended-range forecasts in northern Europe by statistical post-processing using stratospheric observations
title_short Adding value to extended-range forecasts in northern Europe by statistical post-processing using stratospheric observations
title_full Adding value to extended-range forecasts in northern Europe by statistical post-processing using stratospheric observations
title_fullStr Adding value to extended-range forecasts in northern Europe by statistical post-processing using stratospheric observations
title_full_unstemmed Adding value to extended-range forecasts in northern Europe by statistical post-processing using stratospheric observations
title_sort adding value to extended-range forecasts in northern europe by statistical post-processing using stratospheric observations
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/acp-20-8441-2020
https://doaj.org/article/f8a583301ab44f718a823843b58d067a
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Atmospheric Chemistry and Physics, Vol 20, Pp 8441-8451 (2020)
op_relation https://www.atmos-chem-phys.net/20/8441/2020/acp-20-8441-2020.pdf
https://doaj.org/toc/1680-7316
https://doaj.org/toc/1680-7324
doi:10.5194/acp-20-8441-2020
1680-7316
1680-7324
https://doaj.org/article/f8a583301ab44f718a823843b58d067a
op_doi https://doi.org/10.5194/acp-20-8441-2020
container_title Atmospheric Chemistry and Physics
container_volume 20
container_issue 14
container_start_page 8441
op_container_end_page 8451
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