Use of potential vorticity fields, Meteosat water vapour imagery and pseudo water vapour images for evaluating numerical model behaviour

Abstract During November and December 1998, ten cyclonic disturbances over the North Atlantic and Mediterranean area were studied. Features in potential vorticity (PV) fields were tracked in the analyses and short‐range forecasts of the Spanish version of the HIRLAM model (HIRLAM‐INM) and the ECMWF...

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Published in:Meteorological Applications
Main Authors: Georgiev, Christo G, Martín, Francisco
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2001
Subjects:
Online Access:http://dx.doi.org/10.1017/s1350482701001050
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1017%2FS1350482701001050
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1017/S1350482701001050
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spelling crwiley:10.1017/s1350482701001050 2024-06-02T08:11:30+00:00 Use of potential vorticity fields, Meteosat water vapour imagery and pseudo water vapour images for evaluating numerical model behaviour Georgiev, Christo G Martín, Francisco 2001 http://dx.doi.org/10.1017/s1350482701001050 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1017%2FS1350482701001050 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1017/S1350482701001050 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Meteorological Applications volume 8, issue 1, page 57-69 ISSN 1350-4827 1469-8080 journal-article 2001 crwiley https://doi.org/10.1017/s1350482701001050 2024-05-03T10:58:05Z Abstract During November and December 1998, ten cyclonic disturbances over the North Atlantic and Mediterranean area were studied. Features in potential vorticity (PV) fields were tracked in the analyses and short‐range forecasts of the Spanish version of the HIRLAM model (HIRLAM‐INM) and the ECMWF model. They were superimposed on the corresponding Meteosat water vapour (WV) images with the aim of ascertaining the qualitative relationship between Meteosat WV imagery and PV fields that might be used to assess NWP model behaviour. Two cases predicted incorrectly by HIRLAM‐INM were studied in detail: a rapidly deepening depression over the Atlantic (26–27 November 1998) and a cut‐off low process over the western Mediterranean (3–4 December 1998). For evaluating HIRLAM‐INM model behaviour, absolute vorticity at 2 PVU surface, positive PV anomalies at 500 hPa as well as pseudo WV images were compared with Meteosat WV pictures. Being synthetic products of the numerical model, the pseudo WV images were used to indicate the strength of the relationship between the Meteosat WV imagery and the PV fields, and to indicate whether any mismatches correspond to real NWP model errors. It is demonstrated that the HIRLAM‐INM phase error at 3–4 December 1998 was clearly seen in the comparison between Meteosat and pseudo WV images. Copyright © 2001 Royal Meteorological Society Article in Journal/Newspaper North Atlantic Wiley Online Library Meteorological Applications 8 1 57 69
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract During November and December 1998, ten cyclonic disturbances over the North Atlantic and Mediterranean area were studied. Features in potential vorticity (PV) fields were tracked in the analyses and short‐range forecasts of the Spanish version of the HIRLAM model (HIRLAM‐INM) and the ECMWF model. They were superimposed on the corresponding Meteosat water vapour (WV) images with the aim of ascertaining the qualitative relationship between Meteosat WV imagery and PV fields that might be used to assess NWP model behaviour. Two cases predicted incorrectly by HIRLAM‐INM were studied in detail: a rapidly deepening depression over the Atlantic (26–27 November 1998) and a cut‐off low process over the western Mediterranean (3–4 December 1998). For evaluating HIRLAM‐INM model behaviour, absolute vorticity at 2 PVU surface, positive PV anomalies at 500 hPa as well as pseudo WV images were compared with Meteosat WV pictures. Being synthetic products of the numerical model, the pseudo WV images were used to indicate the strength of the relationship between the Meteosat WV imagery and the PV fields, and to indicate whether any mismatches correspond to real NWP model errors. It is demonstrated that the HIRLAM‐INM phase error at 3–4 December 1998 was clearly seen in the comparison between Meteosat and pseudo WV images. Copyright © 2001 Royal Meteorological Society
format Article in Journal/Newspaper
author Georgiev, Christo G
Martín, Francisco
spellingShingle Georgiev, Christo G
Martín, Francisco
Use of potential vorticity fields, Meteosat water vapour imagery and pseudo water vapour images for evaluating numerical model behaviour
author_facet Georgiev, Christo G
Martín, Francisco
author_sort Georgiev, Christo G
title Use of potential vorticity fields, Meteosat water vapour imagery and pseudo water vapour images for evaluating numerical model behaviour
title_short Use of potential vorticity fields, Meteosat water vapour imagery and pseudo water vapour images for evaluating numerical model behaviour
title_full Use of potential vorticity fields, Meteosat water vapour imagery and pseudo water vapour images for evaluating numerical model behaviour
title_fullStr Use of potential vorticity fields, Meteosat water vapour imagery and pseudo water vapour images for evaluating numerical model behaviour
title_full_unstemmed Use of potential vorticity fields, Meteosat water vapour imagery and pseudo water vapour images for evaluating numerical model behaviour
title_sort use of potential vorticity fields, meteosat water vapour imagery and pseudo water vapour images for evaluating numerical model behaviour
publisher Wiley
publishDate 2001
url http://dx.doi.org/10.1017/s1350482701001050
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1017%2FS1350482701001050
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1017/S1350482701001050
genre North Atlantic
genre_facet North Atlantic
op_source Meteorological Applications
volume 8, issue 1, page 57-69
ISSN 1350-4827 1469-8080
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1017/s1350482701001050
container_title Meteorological Applications
container_volume 8
container_issue 1
container_start_page 57
op_container_end_page 69
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