Robust stochastic seasonal precipitation scenarios

Abstract In this paper, a stochastic statistical forecasting methodology is employed for long‐term predictions of winter precipitation over Greece. Lagged climatic indices and North Atlantic (NA) sea‐level pressure (SLP) field are explored as potential predictors of the teleconnection. Rather than e...

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Published in:International Journal of Climatology
Main Authors: Kioutsioukis, Ioannis, Rapsomanikis, Spyridon, Loupa, Rea
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2006
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.1351
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spelling crwiley:10.1002/joc.1351 2024-06-02T08:11:12+00:00 Robust stochastic seasonal precipitation scenarios Kioutsioukis, Ioannis Rapsomanikis, Spyridon Loupa, Rea 2006 http://dx.doi.org/10.1002/joc.1351 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1351 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1351 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 26, issue 14, page 2077-2095 ISSN 0899-8418 1097-0088 journal-article 2006 crwiley https://doi.org/10.1002/joc.1351 2024-05-03T10:48:22Z Abstract In this paper, a stochastic statistical forecasting methodology is employed for long‐term predictions of winter precipitation over Greece. Lagged climatic indices and North Atlantic (NA) sea‐level pressure (SLP) field are explored as potential predictors of the teleconnection. Rather than employing traditional stationary models, two dynamic regression‐modelling schemes are analysed and validated and their parameter variation is interpreted. Dynamic regression models, in contrast to static (constant parameter) regression models, have time variable parameters (TVPs) evaluated through recursive optimisation and are suitable for analysis of non‐stationary phenomena like most atmospheric processes. The analysis of the spectrum with non‐stationary models points out that the most influential seasonal components of the winter precipitation anomalies have periods of 14 and 3.5 years, explain 40% of its variance, possess significant amplitude change and correlate significantly with the North Atlantic Oscillation Index Anomaly (NAOIA) and Southern Oscillation Index Anomaly, indicating their climatic origin. Furthermore, the forecasting skill of the dynamic models ( R 2 = 0.71), in addition to reproducing the peaks, was found superior even to the hindcasting skill of the stationary model ( R 2 = 0.55). Copyright © 2006 Royal Meteorological Society Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library International Journal of Climatology 26 14 2077 2095
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract In this paper, a stochastic statistical forecasting methodology is employed for long‐term predictions of winter precipitation over Greece. Lagged climatic indices and North Atlantic (NA) sea‐level pressure (SLP) field are explored as potential predictors of the teleconnection. Rather than employing traditional stationary models, two dynamic regression‐modelling schemes are analysed and validated and their parameter variation is interpreted. Dynamic regression models, in contrast to static (constant parameter) regression models, have time variable parameters (TVPs) evaluated through recursive optimisation and are suitable for analysis of non‐stationary phenomena like most atmospheric processes. The analysis of the spectrum with non‐stationary models points out that the most influential seasonal components of the winter precipitation anomalies have periods of 14 and 3.5 years, explain 40% of its variance, possess significant amplitude change and correlate significantly with the North Atlantic Oscillation Index Anomaly (NAOIA) and Southern Oscillation Index Anomaly, indicating their climatic origin. Furthermore, the forecasting skill of the dynamic models ( R 2 = 0.71), in addition to reproducing the peaks, was found superior even to the hindcasting skill of the stationary model ( R 2 = 0.55). Copyright © 2006 Royal Meteorological Society
format Article in Journal/Newspaper
author Kioutsioukis, Ioannis
Rapsomanikis, Spyridon
Loupa, Rea
spellingShingle Kioutsioukis, Ioannis
Rapsomanikis, Spyridon
Loupa, Rea
Robust stochastic seasonal precipitation scenarios
author_facet Kioutsioukis, Ioannis
Rapsomanikis, Spyridon
Loupa, Rea
author_sort Kioutsioukis, Ioannis
title Robust stochastic seasonal precipitation scenarios
title_short Robust stochastic seasonal precipitation scenarios
title_full Robust stochastic seasonal precipitation scenarios
title_fullStr Robust stochastic seasonal precipitation scenarios
title_full_unstemmed Robust stochastic seasonal precipitation scenarios
title_sort robust stochastic seasonal precipitation scenarios
publisher Wiley
publishDate 2006
url http://dx.doi.org/10.1002/joc.1351
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1351
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1351
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source International Journal of Climatology
volume 26, issue 14, page 2077-2095
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.1351
container_title International Journal of Climatology
container_volume 26
container_issue 14
container_start_page 2077
op_container_end_page 2095
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