The Climate-system Historical Forecast Project: do stratosphere-resolving models make better seasonal climate predictions in boreal winter?
Using an international, multi-model suite of historical forecasts from the World Climate Research Programme (WCRP) Climate-system Historical Forecast Project (CHFP), we compare the seasonal prediction skill in boreal wintertime between models that resolve the stratosphere and its dynamics (high-top&...
Published in: | Quarterly Journal of the Royal Meteorological Society |
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Online Access: | https://eprints.ucm.es/id/eprint/38405/ https://eprints.ucm.es/id/eprint/38405/1/calvofernandez34postprint.pdf https://doi.org/10.1002/qj.2743 |
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ftunivcmadrid:oai:www.ucm.es:38405 2023-05-15T17:28:43+02:00 The Climate-system Historical Forecast Project: do stratosphere-resolving models make better seasonal climate predictions in boreal winter? Calvo Fernández, Natalia Iza San Juan, Maddalen otros, . 2016-04 application/pdf https://eprints.ucm.es/id/eprint/38405/ https://eprints.ucm.es/id/eprint/38405/1/calvofernandez34postprint.pdf https://doi.org/10.1002/qj.2743 en eng Wiley-Blackwell https://eprints.ucm.es/id/eprint/38405/1/calvofernandez34postprint.pdf info:eu-repo/semantics/openAccess Astrofísica Astronomía info:eu-repo/semantics/article PeerReviewed 2016 ftunivcmadrid https://doi.org/10.1002/qj.2743 2022-05-12T20:02:17Z Using an international, multi-model suite of historical forecasts from the World Climate Research Programme (WCRP) Climate-system Historical Forecast Project (CHFP), we compare the seasonal prediction skill in boreal wintertime between models that resolve the stratosphere and its dynamics (high-top') and models that do not (low-top'). We evaluate hindcasts that are initialized in November, and examine the model biases in the stratosphere and how they relate to boreal wintertime (December-March) seasonal forecast skill. We are unable to detect more skill in the high-top ensemble-mean than the low-top ensemble-mean in forecasting the wintertime North Atlantic Oscillation, but model performance varies widely. Increasing the ensemble size clearly increases the skill for a given model. We then examine two major processes involving stratosphere-troposphere interactions (the El Niño/Southern Oscillation (ENSO) and the Quasi-Biennial Oscillation (QBO)) and how they relate to predictive skill on intraseasonal to seasonal time-scales, particularly over the North Atlantic and Eurasia regions. High-top models tend to have a more realistic stratospheric response to El Niño and the QBO compared to low-top models. Enhanced conditional wintertime skill over high latitudes and the North Atlantic region during winters with El Niño conditions suggests a possible role for a stratospheric pathway. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Universidad Complutense de Madrid (UCM): E-Prints Complutense Quarterly Journal of the Royal Meteorological Society 142 696 1413 1427 |
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Open Polar |
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Universidad Complutense de Madrid (UCM): E-Prints Complutense |
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ftunivcmadrid |
language |
English |
topic |
Astrofísica Astronomía |
spellingShingle |
Astrofísica Astronomía Calvo Fernández, Natalia Iza San Juan, Maddalen otros, . The Climate-system Historical Forecast Project: do stratosphere-resolving models make better seasonal climate predictions in boreal winter? |
topic_facet |
Astrofísica Astronomía |
description |
Using an international, multi-model suite of historical forecasts from the World Climate Research Programme (WCRP) Climate-system Historical Forecast Project (CHFP), we compare the seasonal prediction skill in boreal wintertime between models that resolve the stratosphere and its dynamics (high-top') and models that do not (low-top'). We evaluate hindcasts that are initialized in November, and examine the model biases in the stratosphere and how they relate to boreal wintertime (December-March) seasonal forecast skill. We are unable to detect more skill in the high-top ensemble-mean than the low-top ensemble-mean in forecasting the wintertime North Atlantic Oscillation, but model performance varies widely. Increasing the ensemble size clearly increases the skill for a given model. We then examine two major processes involving stratosphere-troposphere interactions (the El Niño/Southern Oscillation (ENSO) and the Quasi-Biennial Oscillation (QBO)) and how they relate to predictive skill on intraseasonal to seasonal time-scales, particularly over the North Atlantic and Eurasia regions. High-top models tend to have a more realistic stratospheric response to El Niño and the QBO compared to low-top models. Enhanced conditional wintertime skill over high latitudes and the North Atlantic region during winters with El Niño conditions suggests a possible role for a stratospheric pathway. |
format |
Article in Journal/Newspaper |
author |
Calvo Fernández, Natalia Iza San Juan, Maddalen otros, . |
author_facet |
Calvo Fernández, Natalia Iza San Juan, Maddalen otros, . |
author_sort |
Calvo Fernández, Natalia |
title |
The Climate-system Historical Forecast Project: do stratosphere-resolving models make better seasonal climate predictions in boreal winter? |
title_short |
The Climate-system Historical Forecast Project: do stratosphere-resolving models make better seasonal climate predictions in boreal winter? |
title_full |
The Climate-system Historical Forecast Project: do stratosphere-resolving models make better seasonal climate predictions in boreal winter? |
title_fullStr |
The Climate-system Historical Forecast Project: do stratosphere-resolving models make better seasonal climate predictions in boreal winter? |
title_full_unstemmed |
The Climate-system Historical Forecast Project: do stratosphere-resolving models make better seasonal climate predictions in boreal winter? |
title_sort |
climate-system historical forecast project: do stratosphere-resolving models make better seasonal climate predictions in boreal winter? |
publisher |
Wiley-Blackwell |
publishDate |
2016 |
url |
https://eprints.ucm.es/id/eprint/38405/ https://eprints.ucm.es/id/eprint/38405/1/calvofernandez34postprint.pdf https://doi.org/10.1002/qj.2743 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
https://eprints.ucm.es/id/eprint/38405/1/calvofernandez34postprint.pdf |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1002/qj.2743 |
container_title |
Quarterly Journal of the Royal Meteorological Society |
container_volume |
142 |
container_issue |
696 |
container_start_page |
1413 |
op_container_end_page |
1427 |
_version_ |
1766121582464335872 |