Influence of the East Atlantic/West Russia pattern on precipitation over Serbia
Abstract It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North Americ...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Tošić, Ivana [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Systematik: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2021 |
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| Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Springer Vienna, 1986, 146(2021), 3-4 vom: 20. Sept., Seite 997-1006 |
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| Übergeordnetes Werk: |
volume:146 ; year:2021 ; number:3-4 ; day:20 ; month:09 ; pages:997-1006 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00704-021-03777-9 |
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| Katalog-ID: |
OLC2077351578 |
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| 520 | |a Abstract It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North American pattern (PNA), which characterize the climate variability in the Northern Hemisphere. In this study, the influence of the EA/WR pattern on precipitation over Europe is examined, with a focus on Serbia. In addition, we explore the combined effects of positive and negative phases of the NAO and EA pattern with the EA/WR pattern, on precipitation over Europe and Serbia. Precipitation data are obtained from the Global Precipitation Climatology Centre (GPCC) and 15 stations from the national observational network in Serbia. Precipitation anomalies have been explored in relation to positive and negative phases of the EA/WR pattern using the monthly GPCC dataset. For the negative (positive) EA/WR phase, positive (negative) precipitation anomalies prevail over the Balkan Peninsula and central Mediterranean in January, February, May, and November, while a negative (positive) one dominates in March, April, September, and during the summer months. There is a strong positive (negative) signal over Portugal in October and over Greece and the Ionian Sea in December, for the positive (negative) EA/WR phase. The precipitation anomalies associated with the negative phase of the EA/WR pattern reflect above (up to 6 mm) average precipitation over Serbia. The positive phase of the EA/WR pattern caused precipitation anomalies below (up to − 8 mm) average precipitation over Serbia. We find that the NAO and EA patterns enhance the influence of the EA/WR pattern on precipitation changes over Serbia. High positive values of precipitation anomalies existed over Serbia for the negative phases of the EA/WR pattern and NAO (up to 12 mm), and EA pattern (up to 10 mm). Negative precipitation anomalies (up to − 12 mm) over Serbia are caused by the positive phase of the EA/WR pattern in combination with the positive phases of the NAO and EA pattern. | ||
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10.1007/s00704-021-03777-9 doi (DE-627)OLC2077351578 (DE-He213)s00704-021-03777-9-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Tošić, Ivana verfasserin (orcid)0000-0002-7259-8828 aut Influence of the East Atlantic/West Russia pattern on precipitation over Serbia 2021 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2021 Abstract It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North American pattern (PNA), which characterize the climate variability in the Northern Hemisphere. In this study, the influence of the EA/WR pattern on precipitation over Europe is examined, with a focus on Serbia. In addition, we explore the combined effects of positive and negative phases of the NAO and EA pattern with the EA/WR pattern, on precipitation over Europe and Serbia. Precipitation data are obtained from the Global Precipitation Climatology Centre (GPCC) and 15 stations from the national observational network in Serbia. Precipitation anomalies have been explored in relation to positive and negative phases of the EA/WR pattern using the monthly GPCC dataset. For the negative (positive) EA/WR phase, positive (negative) precipitation anomalies prevail over the Balkan Peninsula and central Mediterranean in January, February, May, and November, while a negative (positive) one dominates in March, April, September, and during the summer months. There is a strong positive (negative) signal over Portugal in October and over Greece and the Ionian Sea in December, for the positive (negative) EA/WR phase. The precipitation anomalies associated with the negative phase of the EA/WR pattern reflect above (up to 6 mm) average precipitation over Serbia. The positive phase of the EA/WR pattern caused precipitation anomalies below (up to − 8 mm) average precipitation over Serbia. We find that the NAO and EA patterns enhance the influence of the EA/WR pattern on precipitation changes over Serbia. High positive values of precipitation anomalies existed over Serbia for the negative phases of the EA/WR pattern and NAO (up to 12 mm), and EA pattern (up to 10 mm). Negative precipitation anomalies (up to − 12 mm) over Serbia are caused by the positive phase of the EA/WR pattern in combination with the positive phases of the NAO and EA pattern. Putniković, Suzana aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 146(2021), 3-4 vom: 20. Sept., Seite 997-1006 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:146 year:2021 number:3-4 day:20 month:09 pages:997-1006 https://doi.org/10.1007/s00704-021-03777-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 146 2021 3-4 20 09 997-1006 |
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10.1007/s00704-021-03777-9 doi (DE-627)OLC2077351578 (DE-He213)s00704-021-03777-9-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Tošić, Ivana verfasserin (orcid)0000-0002-7259-8828 aut Influence of the East Atlantic/West Russia pattern on precipitation over Serbia 2021 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2021 Abstract It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North American pattern (PNA), which characterize the climate variability in the Northern Hemisphere. In this study, the influence of the EA/WR pattern on precipitation over Europe is examined, with a focus on Serbia. In addition, we explore the combined effects of positive and negative phases of the NAO and EA pattern with the EA/WR pattern, on precipitation over Europe and Serbia. Precipitation data are obtained from the Global Precipitation Climatology Centre (GPCC) and 15 stations from the national observational network in Serbia. Precipitation anomalies have been explored in relation to positive and negative phases of the EA/WR pattern using the monthly GPCC dataset. For the negative (positive) EA/WR phase, positive (negative) precipitation anomalies prevail over the Balkan Peninsula and central Mediterranean in January, February, May, and November, while a negative (positive) one dominates in March, April, September, and during the summer months. There is a strong positive (negative) signal over Portugal in October and over Greece and the Ionian Sea in December, for the positive (negative) EA/WR phase. The precipitation anomalies associated with the negative phase of the EA/WR pattern reflect above (up to 6 mm) average precipitation over Serbia. The positive phase of the EA/WR pattern caused precipitation anomalies below (up to − 8 mm) average precipitation over Serbia. We find that the NAO and EA patterns enhance the influence of the EA/WR pattern on precipitation changes over Serbia. High positive values of precipitation anomalies existed over Serbia for the negative phases of the EA/WR pattern and NAO (up to 12 mm), and EA pattern (up to 10 mm). Negative precipitation anomalies (up to − 12 mm) over Serbia are caused by the positive phase of the EA/WR pattern in combination with the positive phases of the NAO and EA pattern. Putniković, Suzana aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 146(2021), 3-4 vom: 20. Sept., Seite 997-1006 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:146 year:2021 number:3-4 day:20 month:09 pages:997-1006 https://doi.org/10.1007/s00704-021-03777-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 146 2021 3-4 20 09 997-1006 |
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10.1007/s00704-021-03777-9 doi (DE-627)OLC2077351578 (DE-He213)s00704-021-03777-9-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Tošić, Ivana verfasserin (orcid)0000-0002-7259-8828 aut Influence of the East Atlantic/West Russia pattern on precipitation over Serbia 2021 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2021 Abstract It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North American pattern (PNA), which characterize the climate variability in the Northern Hemisphere. In this study, the influence of the EA/WR pattern on precipitation over Europe is examined, with a focus on Serbia. In addition, we explore the combined effects of positive and negative phases of the NAO and EA pattern with the EA/WR pattern, on precipitation over Europe and Serbia. Precipitation data are obtained from the Global Precipitation Climatology Centre (GPCC) and 15 stations from the national observational network in Serbia. Precipitation anomalies have been explored in relation to positive and negative phases of the EA/WR pattern using the monthly GPCC dataset. For the negative (positive) EA/WR phase, positive (negative) precipitation anomalies prevail over the Balkan Peninsula and central Mediterranean in January, February, May, and November, while a negative (positive) one dominates in March, April, September, and during the summer months. There is a strong positive (negative) signal over Portugal in October and over Greece and the Ionian Sea in December, for the positive (negative) EA/WR phase. The precipitation anomalies associated with the negative phase of the EA/WR pattern reflect above (up to 6 mm) average precipitation over Serbia. The positive phase of the EA/WR pattern caused precipitation anomalies below (up to − 8 mm) average precipitation over Serbia. We find that the NAO and EA patterns enhance the influence of the EA/WR pattern on precipitation changes over Serbia. High positive values of precipitation anomalies existed over Serbia for the negative phases of the EA/WR pattern and NAO (up to 12 mm), and EA pattern (up to 10 mm). Negative precipitation anomalies (up to − 12 mm) over Serbia are caused by the positive phase of the EA/WR pattern in combination with the positive phases of the NAO and EA pattern. Putniković, Suzana aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 146(2021), 3-4 vom: 20. Sept., Seite 997-1006 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:146 year:2021 number:3-4 day:20 month:09 pages:997-1006 https://doi.org/10.1007/s00704-021-03777-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 146 2021 3-4 20 09 997-1006 |
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10.1007/s00704-021-03777-9 doi (DE-627)OLC2077351578 (DE-He213)s00704-021-03777-9-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Tošić, Ivana verfasserin (orcid)0000-0002-7259-8828 aut Influence of the East Atlantic/West Russia pattern on precipitation over Serbia 2021 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2021 Abstract It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North American pattern (PNA), which characterize the climate variability in the Northern Hemisphere. In this study, the influence of the EA/WR pattern on precipitation over Europe is examined, with a focus on Serbia. In addition, we explore the combined effects of positive and negative phases of the NAO and EA pattern with the EA/WR pattern, on precipitation over Europe and Serbia. Precipitation data are obtained from the Global Precipitation Climatology Centre (GPCC) and 15 stations from the national observational network in Serbia. Precipitation anomalies have been explored in relation to positive and negative phases of the EA/WR pattern using the monthly GPCC dataset. For the negative (positive) EA/WR phase, positive (negative) precipitation anomalies prevail over the Balkan Peninsula and central Mediterranean in January, February, May, and November, while a negative (positive) one dominates in March, April, September, and during the summer months. There is a strong positive (negative) signal over Portugal in October and over Greece and the Ionian Sea in December, for the positive (negative) EA/WR phase. The precipitation anomalies associated with the negative phase of the EA/WR pattern reflect above (up to 6 mm) average precipitation over Serbia. The positive phase of the EA/WR pattern caused precipitation anomalies below (up to − 8 mm) average precipitation over Serbia. We find that the NAO and EA patterns enhance the influence of the EA/WR pattern on precipitation changes over Serbia. High positive values of precipitation anomalies existed over Serbia for the negative phases of the EA/WR pattern and NAO (up to 12 mm), and EA pattern (up to 10 mm). Negative precipitation anomalies (up to − 12 mm) over Serbia are caused by the positive phase of the EA/WR pattern in combination with the positive phases of the NAO and EA pattern. Putniković, Suzana aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 146(2021), 3-4 vom: 20. Sept., Seite 997-1006 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:146 year:2021 number:3-4 day:20 month:09 pages:997-1006 https://doi.org/10.1007/s00704-021-03777-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 146 2021 3-4 20 09 997-1006 |
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influence of the east atlantic/west russia pattern on precipitation over serbia |
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Influence of the East Atlantic/West Russia pattern on precipitation over Serbia |
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Abstract It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North American pattern (PNA), which characterize the climate variability in the Northern Hemisphere. In this study, the influence of the EA/WR pattern on precipitation over Europe is examined, with a focus on Serbia. In addition, we explore the combined effects of positive and negative phases of the NAO and EA pattern with the EA/WR pattern, on precipitation over Europe and Serbia. Precipitation data are obtained from the Global Precipitation Climatology Centre (GPCC) and 15 stations from the national observational network in Serbia. Precipitation anomalies have been explored in relation to positive and negative phases of the EA/WR pattern using the monthly GPCC dataset. For the negative (positive) EA/WR phase, positive (negative) precipitation anomalies prevail over the Balkan Peninsula and central Mediterranean in January, February, May, and November, while a negative (positive) one dominates in March, April, September, and during the summer months. There is a strong positive (negative) signal over Portugal in October and over Greece and the Ionian Sea in December, for the positive (negative) EA/WR phase. The precipitation anomalies associated with the negative phase of the EA/WR pattern reflect above (up to 6 mm) average precipitation over Serbia. The positive phase of the EA/WR pattern caused precipitation anomalies below (up to − 8 mm) average precipitation over Serbia. We find that the NAO and EA patterns enhance the influence of the EA/WR pattern on precipitation changes over Serbia. High positive values of precipitation anomalies existed over Serbia for the negative phases of the EA/WR pattern and NAO (up to 12 mm), and EA pattern (up to 10 mm). Negative precipitation anomalies (up to − 12 mm) over Serbia are caused by the positive phase of the EA/WR pattern in combination with the positive phases of the NAO and EA pattern. © The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2021 |
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Abstract It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North American pattern (PNA), which characterize the climate variability in the Northern Hemisphere. In this study, the influence of the EA/WR pattern on precipitation over Europe is examined, with a focus on Serbia. In addition, we explore the combined effects of positive and negative phases of the NAO and EA pattern with the EA/WR pattern, on precipitation over Europe and Serbia. Precipitation data are obtained from the Global Precipitation Climatology Centre (GPCC) and 15 stations from the national observational network in Serbia. Precipitation anomalies have been explored in relation to positive and negative phases of the EA/WR pattern using the monthly GPCC dataset. For the negative (positive) EA/WR phase, positive (negative) precipitation anomalies prevail over the Balkan Peninsula and central Mediterranean in January, February, May, and November, while a negative (positive) one dominates in March, April, September, and during the summer months. There is a strong positive (negative) signal over Portugal in October and over Greece and the Ionian Sea in December, for the positive (negative) EA/WR phase. The precipitation anomalies associated with the negative phase of the EA/WR pattern reflect above (up to 6 mm) average precipitation over Serbia. The positive phase of the EA/WR pattern caused precipitation anomalies below (up to − 8 mm) average precipitation over Serbia. We find that the NAO and EA patterns enhance the influence of the EA/WR pattern on precipitation changes over Serbia. High positive values of precipitation anomalies existed over Serbia for the negative phases of the EA/WR pattern and NAO (up to 12 mm), and EA pattern (up to 10 mm). Negative precipitation anomalies (up to − 12 mm) over Serbia are caused by the positive phase of the EA/WR pattern in combination with the positive phases of the NAO and EA pattern. © The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2021 |
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Abstract It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North American pattern (PNA), which characterize the climate variability in the Northern Hemisphere. In this study, the influence of the EA/WR pattern on precipitation over Europe is examined, with a focus on Serbia. In addition, we explore the combined effects of positive and negative phases of the NAO and EA pattern with the EA/WR pattern, on precipitation over Europe and Serbia. Precipitation data are obtained from the Global Precipitation Climatology Centre (GPCC) and 15 stations from the national observational network in Serbia. Precipitation anomalies have been explored in relation to positive and negative phases of the EA/WR pattern using the monthly GPCC dataset. For the negative (positive) EA/WR phase, positive (negative) precipitation anomalies prevail over the Balkan Peninsula and central Mediterranean in January, February, May, and November, while a negative (positive) one dominates in March, April, September, and during the summer months. There is a strong positive (negative) signal over Portugal in October and over Greece and the Ionian Sea in December, for the positive (negative) EA/WR phase. The precipitation anomalies associated with the negative phase of the EA/WR pattern reflect above (up to 6 mm) average precipitation over Serbia. The positive phase of the EA/WR pattern caused precipitation anomalies below (up to − 8 mm) average precipitation over Serbia. We find that the NAO and EA patterns enhance the influence of the EA/WR pattern on precipitation changes over Serbia. High positive values of precipitation anomalies existed over Serbia for the negative phases of the EA/WR pattern and NAO (up to 12 mm), and EA pattern (up to 10 mm). Negative precipitation anomalies (up to − 12 mm) over Serbia are caused by the positive phase of the EA/WR pattern in combination with the positive phases of the NAO and EA pattern. © The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2021 |
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