Variability of the cold season climate in central asia. Part II: Hydroclimatic predictability

International audience Central Asia (CA) is subjected to a large variability of precipitation. This study presents a statistical model, relating precipitation anomalies in three subregions of CA in the cold season (November-March) with various predictors in the preceding October. Promising forecast...

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Published in:Journal of Climate
Main Authors: Gerlitz, Lars, Steirou, Eva, Schneider, Christoph, Moron, Vincent, Vorogushyn, Sergiy, Merz, Bruno
Other Authors: Hydrology Section, German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ), Humboldt-Universität zu Berlin = Humboldt University of Berlin = Université Humboldt de Berlin (HU Berlin), Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), University of Potsdam = Universität Potsdam
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2019
Subjects:
Online Access:https://hal.inrae.fr/hal-02618895
https://hal.inrae.fr/hal-02618895/document
https://hal.inrae.fr/hal-02618895/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Variability%20of%20the%20Cold%20Season%20Climate%20in%20Central%20Asia.%20Part%20II%20Hydroclimatic%20Predictability.pdf
https://doi.org/10.1175/JCLI-D-18-0892.1
id ftinraparis:oai:HAL:hal-02618895v1
record_format openpolar
institution Open Polar
collection Institut National de la Recherche Agronomique: ProdINRA
op_collection_id ftinraparis
language English
topic asia
seasonal forecasting
north atlantic oscillation
southern oscillation
climate prediction
[SDV]Life Sciences [q-bio]
[SDU]Sciences of the Universe [physics]
spellingShingle asia
seasonal forecasting
north atlantic oscillation
southern oscillation
climate prediction
[SDV]Life Sciences [q-bio]
[SDU]Sciences of the Universe [physics]
Gerlitz, Lars
Steirou, Eva
Schneider, Christoph
Moron, Vincent
Vorogushyn, Sergiy
Merz, Bruno
Variability of the cold season climate in central asia. Part II: Hydroclimatic predictability
topic_facet asia
seasonal forecasting
north atlantic oscillation
southern oscillation
climate prediction
[SDV]Life Sciences [q-bio]
[SDU]Sciences of the Universe [physics]
description International audience Central Asia (CA) is subjected to a large variability of precipitation. This study presents a statistical model, relating precipitation anomalies in three subregions of CA in the cold season (November-March) with various predictors in the preceding October. Promising forecast skill is achieved for two subregions covering 1) Uzbekistan, Turkmenistan, Kyrgyzstan, Tajikistan, and southern Kazakhstan and 2) Iran, Afghanistan, and Pakistan. ENSO in October is identified as the major predictor. Eurasian snow cover and the quasi-biennial oscillation further improve the forecast performance. To understand the physical mechanisms, an analysis of teleconnections between these predictors and the wintertime circulation over CA is conducted. The correlation analysis of predictors and large-scale circulation indices suggests a seasonal persistence of tropical circulation modes and a dynamical forcing of the westerly circulation by snow cover variations over Eurasia. An EOF analysis of pressure and humidity patterns allows separating the circulation variability over CA into westerly and tropical modes and confirms that the identified predictors affect the respective circulation characteristics. Based on the previously established weather type classification for CA, the predictors are investigated with regard to their effect on the regional circulation. The results suggest a modification of the Hadley cell due to ENSO variations, with enhanced moisture supply from the Arabian Gulf during El Nino. They further indicate an influence of Eurasian snow cover on the wintertime Arctic Oscillation (AO) and Northern Hemispheric Rossby wave tracks. Positive anomalies favor weather types associated with dry conditions, while negative anomalies promote the formation of a quasi-stationary trough over CA, which typically occurs during positive AO conditions.
author2 Hydrology Section
German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ)
Humboldt-Universität zu Berlin = Humboldt University of Berlin = Université Humboldt de Berlin (HU Berlin)
Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE)
Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
University of Potsdam = Universität Potsdam
format Article in Journal/Newspaper
author Gerlitz, Lars
Steirou, Eva
Schneider, Christoph
Moron, Vincent
Vorogushyn, Sergiy
Merz, Bruno
author_facet Gerlitz, Lars
Steirou, Eva
Schneider, Christoph
Moron, Vincent
Vorogushyn, Sergiy
Merz, Bruno
author_sort Gerlitz, Lars
title Variability of the cold season climate in central asia. Part II: Hydroclimatic predictability
title_short Variability of the cold season climate in central asia. Part II: Hydroclimatic predictability
title_full Variability of the cold season climate in central asia. Part II: Hydroclimatic predictability
title_fullStr Variability of the cold season climate in central asia. Part II: Hydroclimatic predictability
title_full_unstemmed Variability of the cold season climate in central asia. Part II: Hydroclimatic predictability
title_sort variability of the cold season climate in central asia. part ii: hydroclimatic predictability
publisher HAL CCSD
publishDate 2019
url https://hal.inrae.fr/hal-02618895
https://hal.inrae.fr/hal-02618895/document
https://hal.inrae.fr/hal-02618895/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Variability%20of%20the%20Cold%20Season%20Climate%20in%20Central%20Asia.%20Part%20II%20Hydroclimatic%20Predictability.pdf
https://doi.org/10.1175/JCLI-D-18-0892.1
geographic Arctic
geographic_facet Arctic
genre Arctic
North Atlantic
North Atlantic oscillation
genre_facet Arctic
North Atlantic
North Atlantic oscillation
op_source ISSN: 0894-8755
EISSN: 1520-0442
Journal of Climate
https://hal.inrae.fr/hal-02618895
Journal of Climate, 2019, 32 (18), pp.6015-6033. ⟨10.1175/JCLI-D-18-0892.1⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-18-0892.1
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doi:10.1175/JCLI-D-18-0892.1
PRODINRA: 487212
WOS: 000481822600003
op_rights http://creativecommons.org/licenses/by/
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op_doi https://doi.org/10.1175/JCLI-D-18-0892.1
container_title Journal of Climate
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spelling ftinraparis:oai:HAL:hal-02618895v1 2024-06-23T07:50:45+00:00 Variability of the cold season climate in central asia. Part II: Hydroclimatic predictability Gerlitz, Lars Steirou, Eva Schneider, Christoph Moron, Vincent Vorogushyn, Sergiy Merz, Bruno Hydrology Section German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ) Humboldt-Universität zu Berlin = Humboldt University of Berlin = Université Humboldt de Berlin (HU Berlin) Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) University of Potsdam = Universität Potsdam 2019 https://hal.inrae.fr/hal-02618895 https://hal.inrae.fr/hal-02618895/document https://hal.inrae.fr/hal-02618895/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Variability%20of%20the%20Cold%20Season%20Climate%20in%20Central%20Asia.%20Part%20II%20Hydroclimatic%20Predictability.pdf https://doi.org/10.1175/JCLI-D-18-0892.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-18-0892.1 hal-02618895 https://hal.inrae.fr/hal-02618895 https://hal.inrae.fr/hal-02618895/document https://hal.inrae.fr/hal-02618895/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Variability%20of%20the%20Cold%20Season%20Climate%20in%20Central%20Asia.%20Part%20II%20Hydroclimatic%20Predictability.pdf doi:10.1175/JCLI-D-18-0892.1 PRODINRA: 487212 WOS: 000481822600003 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://hal.inrae.fr/hal-02618895 Journal of Climate, 2019, 32 (18), pp.6015-6033. ⟨10.1175/JCLI-D-18-0892.1⟩ asia seasonal forecasting north atlantic oscillation southern oscillation climate prediction [SDV]Life Sciences [q-bio] [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2019 ftinraparis https://doi.org/10.1175/JCLI-D-18-0892.1 2024-06-11T14:56:15Z International audience Central Asia (CA) is subjected to a large variability of precipitation. This study presents a statistical model, relating precipitation anomalies in three subregions of CA in the cold season (November-March) with various predictors in the preceding October. Promising forecast skill is achieved for two subregions covering 1) Uzbekistan, Turkmenistan, Kyrgyzstan, Tajikistan, and southern Kazakhstan and 2) Iran, Afghanistan, and Pakistan. ENSO in October is identified as the major predictor. Eurasian snow cover and the quasi-biennial oscillation further improve the forecast performance. To understand the physical mechanisms, an analysis of teleconnections between these predictors and the wintertime circulation over CA is conducted. The correlation analysis of predictors and large-scale circulation indices suggests a seasonal persistence of tropical circulation modes and a dynamical forcing of the westerly circulation by snow cover variations over Eurasia. An EOF analysis of pressure and humidity patterns allows separating the circulation variability over CA into westerly and tropical modes and confirms that the identified predictors affect the respective circulation characteristics. Based on the previously established weather type classification for CA, the predictors are investigated with regard to their effect on the regional circulation. The results suggest a modification of the Hadley cell due to ENSO variations, with enhanced moisture supply from the Arabian Gulf during El Nino. They further indicate an influence of Eurasian snow cover on the wintertime Arctic Oscillation (AO) and Northern Hemispheric Rossby wave tracks. Positive anomalies favor weather types associated with dry conditions, while negative anomalies promote the formation of a quasi-stationary trough over CA, which typically occurs during positive AO conditions. Article in Journal/Newspaper Arctic North Atlantic North Atlantic oscillation Institut National de la Recherche Agronomique: ProdINRA Arctic Journal of Climate 32 18 6015 6033