Systematic errors of the ECMWF operational forecasting model in mid‐latitudes

Abstract The systematic errors of the ECMWF spectral operational model (April 1983 to April 1985) in midlatitudes are described. The main errors are: * a zonalization of the time‐mean flow with considerably reduced diffluent flow at the jet exits; * a wavenumber‐2 pattern in the mean height error fi...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Arpe, K., Klinker, E.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1986
Subjects:
Online Access:http://dx.doi.org/10.1002/qj.49711247111
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spelling crwiley:10.1002/qj.49711247111 2024-06-02T08:04:24+00:00 Systematic errors of the ECMWF operational forecasting model in mid‐latitudes Arpe, K. Klinker, E. 1986 http://dx.doi.org/10.1002/qj.49711247111 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49711247111 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49711247111 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 112, issue 471, page 181-202 ISSN 0035-9009 1477-870X journal-article 1986 crwiley https://doi.org/10.1002/qj.49711247111 2024-05-03T11:22:01Z Abstract The systematic errors of the ECMWF spectral operational model (April 1983 to April 1985) in midlatitudes are described. The main errors are: * a zonalization of the time‐mean flow with considerably reduced diffluent flow at the jet exits; * a wavenumber‐2 pattern in the mean height error field with forecast heights too low over Europe and the Bering Strait, and too high over Canada and Siberia; * an upward shift of the subtropical jet and the tropopause; * a cooling of the stratosphere; * a cooling of the middle troposphere which decreases the static stability in the lower troposphere; * an increase of the horizontal and vertical tilts of baroclinic waves; * changes in the geographical distributions of baroclinic waves and cyclones, with enhanced activity near jet exits and reduced activity near areas of cyclogenesis; * a drop of eddy kinetic energy during the 10‐day forecasts, first in the baroclinic waves and later in the long waves. The errors in both hemispheres have similar characteristics. The relations between the different errors and possible causes are discussed and comparisons with the errors of the former ECMWF operational grid point model are made. The introduction of the spectral model has led to significant improvements in the speed of baroclinic waves, which are now predicted more accurately up to day 3. Article in Journal/Newspaper Bering Strait Siberia Wiley Online Library Bering Strait Canada Quarterly Journal of the Royal Meteorological Society 112 471 181 202
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The systematic errors of the ECMWF spectral operational model (April 1983 to April 1985) in midlatitudes are described. The main errors are: * a zonalization of the time‐mean flow with considerably reduced diffluent flow at the jet exits; * a wavenumber‐2 pattern in the mean height error field with forecast heights too low over Europe and the Bering Strait, and too high over Canada and Siberia; * an upward shift of the subtropical jet and the tropopause; * a cooling of the stratosphere; * a cooling of the middle troposphere which decreases the static stability in the lower troposphere; * an increase of the horizontal and vertical tilts of baroclinic waves; * changes in the geographical distributions of baroclinic waves and cyclones, with enhanced activity near jet exits and reduced activity near areas of cyclogenesis; * a drop of eddy kinetic energy during the 10‐day forecasts, first in the baroclinic waves and later in the long waves. The errors in both hemispheres have similar characteristics. The relations between the different errors and possible causes are discussed and comparisons with the errors of the former ECMWF operational grid point model are made. The introduction of the spectral model has led to significant improvements in the speed of baroclinic waves, which are now predicted more accurately up to day 3.
format Article in Journal/Newspaper
author Arpe, K.
Klinker, E.
spellingShingle Arpe, K.
Klinker, E.
Systematic errors of the ECMWF operational forecasting model in mid‐latitudes
author_facet Arpe, K.
Klinker, E.
author_sort Arpe, K.
title Systematic errors of the ECMWF operational forecasting model in mid‐latitudes
title_short Systematic errors of the ECMWF operational forecasting model in mid‐latitudes
title_full Systematic errors of the ECMWF operational forecasting model in mid‐latitudes
title_fullStr Systematic errors of the ECMWF operational forecasting model in mid‐latitudes
title_full_unstemmed Systematic errors of the ECMWF operational forecasting model in mid‐latitudes
title_sort systematic errors of the ecmwf operational forecasting model in mid‐latitudes
publisher Wiley
publishDate 1986
url http://dx.doi.org/10.1002/qj.49711247111
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49711247111
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49711247111
geographic Bering Strait
Canada
geographic_facet Bering Strait
Canada
genre Bering Strait
Siberia
genre_facet Bering Strait
Siberia
op_source Quarterly Journal of the Royal Meteorological Society
volume 112, issue 471, page 181-202
ISSN 0035-9009 1477-870X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/qj.49711247111
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 112
container_issue 471
container_start_page 181
op_container_end_page 202
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