North Atlantic Oscillation – Concepts And Studies
Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of vari...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wanner, Heinz [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2001 |
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| Anmerkung: |
© Kluwer Academic Publishers 2001 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Surveys in geophysics - Kluwer Academic Publishers, 1986, 22(2001), 4 vom: Juli, Seite 321-381 |
|---|---|
| Übergeordnetes Werk: |
volume:22 ; year:2001 ; number:4 ; month:07 ; pages:321-381 |
| Links: |
|---|
| DOI / URN: |
10.1023/A:1014217317898 |
|---|
| Katalog-ID: |
OLC2034986822 |
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| 520 | |a Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of variability in the Northern Hemisphere winter climate. The NAO teleconnection is characterised by a meridional displacement of atmospheric mass over the North Atlantic area. Its state is usually expressed by the standardised air pressure difference between the Azores High and the Iceland Low. ThisNAO index is a measure of the strength of the westerly flow (positive with strong westerlies, and vice versa). Together with the El Niño/Southern Oscillation (ENSO) phenomenon, the NAO is a major source of seasonal to interdecadal variability in the global atmosphere. On interannual and shorter time scales, the NAO dynamics can be explained as a purely internal mode of variability of the atmospheric circulation. Interdecadal variability maybe influenced, however, by ocean and sea-ice processes. | ||
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| 700 | 1 | |a Xoplaki, Eleni |4 aut | |
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10.1023/A:1014217317898 doi (DE-627)OLC2034986822 (DE-He213)A:1014217317898-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wanner, Heinz verfasserin aut North Atlantic Oscillation – Concepts And Studies 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2001 Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of variability in the Northern Hemisphere winter climate. The NAO teleconnection is characterised by a meridional displacement of atmospheric mass over the North Atlantic area. Its state is usually expressed by the standardised air pressure difference between the Azores High and the Iceland Low. ThisNAO index is a measure of the strength of the westerly flow (positive with strong westerlies, and vice versa). Together with the El Niño/Southern Oscillation (ENSO) phenomenon, the NAO is a major source of seasonal to interdecadal variability in the global atmosphere. On interannual and shorter time scales, the NAO dynamics can be explained as a purely internal mode of variability of the atmospheric circulation. Interdecadal variability maybe influenced, however, by ocean and sea-ice processes. Brönnimann, Stefan aut Casty, Carlo aut Gyalistras, Dimitrios aut Luterbacher, Jürg aut Schmutz, Christoph aut Stephenson, David B. aut Xoplaki, Eleni aut Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 22(2001), 4 vom: Juli, Seite 321-381 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:22 year:2001 number:4 month:07 pages:321-381 https://doi.org/10.1023/A:1014217317898 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_4012 AR 22 2001 4 07 321-381 |
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10.1023/A:1014217317898 doi (DE-627)OLC2034986822 (DE-He213)A:1014217317898-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wanner, Heinz verfasserin aut North Atlantic Oscillation – Concepts And Studies 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2001 Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of variability in the Northern Hemisphere winter climate. The NAO teleconnection is characterised by a meridional displacement of atmospheric mass over the North Atlantic area. Its state is usually expressed by the standardised air pressure difference between the Azores High and the Iceland Low. ThisNAO index is a measure of the strength of the westerly flow (positive with strong westerlies, and vice versa). Together with the El Niño/Southern Oscillation (ENSO) phenomenon, the NAO is a major source of seasonal to interdecadal variability in the global atmosphere. On interannual and shorter time scales, the NAO dynamics can be explained as a purely internal mode of variability of the atmospheric circulation. Interdecadal variability maybe influenced, however, by ocean and sea-ice processes. Brönnimann, Stefan aut Casty, Carlo aut Gyalistras, Dimitrios aut Luterbacher, Jürg aut Schmutz, Christoph aut Stephenson, David B. aut Xoplaki, Eleni aut Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 22(2001), 4 vom: Juli, Seite 321-381 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:22 year:2001 number:4 month:07 pages:321-381 https://doi.org/10.1023/A:1014217317898 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_4012 AR 22 2001 4 07 321-381 |
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10.1023/A:1014217317898 doi (DE-627)OLC2034986822 (DE-He213)A:1014217317898-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wanner, Heinz verfasserin aut North Atlantic Oscillation – Concepts And Studies 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2001 Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of variability in the Northern Hemisphere winter climate. The NAO teleconnection is characterised by a meridional displacement of atmospheric mass over the North Atlantic area. Its state is usually expressed by the standardised air pressure difference between the Azores High and the Iceland Low. ThisNAO index is a measure of the strength of the westerly flow (positive with strong westerlies, and vice versa). Together with the El Niño/Southern Oscillation (ENSO) phenomenon, the NAO is a major source of seasonal to interdecadal variability in the global atmosphere. On interannual and shorter time scales, the NAO dynamics can be explained as a purely internal mode of variability of the atmospheric circulation. Interdecadal variability maybe influenced, however, by ocean and sea-ice processes. Brönnimann, Stefan aut Casty, Carlo aut Gyalistras, Dimitrios aut Luterbacher, Jürg aut Schmutz, Christoph aut Stephenson, David B. aut Xoplaki, Eleni aut Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 22(2001), 4 vom: Juli, Seite 321-381 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:22 year:2001 number:4 month:07 pages:321-381 https://doi.org/10.1023/A:1014217317898 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_4012 AR 22 2001 4 07 321-381 |
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10.1023/A:1014217317898 doi (DE-627)OLC2034986822 (DE-He213)A:1014217317898-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wanner, Heinz verfasserin aut North Atlantic Oscillation – Concepts And Studies 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2001 Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of variability in the Northern Hemisphere winter climate. The NAO teleconnection is characterised by a meridional displacement of atmospheric mass over the North Atlantic area. Its state is usually expressed by the standardised air pressure difference between the Azores High and the Iceland Low. ThisNAO index is a measure of the strength of the westerly flow (positive with strong westerlies, and vice versa). Together with the El Niño/Southern Oscillation (ENSO) phenomenon, the NAO is a major source of seasonal to interdecadal variability in the global atmosphere. On interannual and shorter time scales, the NAO dynamics can be explained as a purely internal mode of variability of the atmospheric circulation. Interdecadal variability maybe influenced, however, by ocean and sea-ice processes. Brönnimann, Stefan aut Casty, Carlo aut Gyalistras, Dimitrios aut Luterbacher, Jürg aut Schmutz, Christoph aut Stephenson, David B. aut Xoplaki, Eleni aut Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 22(2001), 4 vom: Juli, Seite 321-381 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:22 year:2001 number:4 month:07 pages:321-381 https://doi.org/10.1023/A:1014217317898 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_4012 AR 22 2001 4 07 321-381 |
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10.1023/A:1014217317898 doi (DE-627)OLC2034986822 (DE-He213)A:1014217317898-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Wanner, Heinz verfasserin aut North Atlantic Oscillation – Concepts And Studies 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2001 Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of variability in the Northern Hemisphere winter climate. The NAO teleconnection is characterised by a meridional displacement of atmospheric mass over the North Atlantic area. Its state is usually expressed by the standardised air pressure difference between the Azores High and the Iceland Low. ThisNAO index is a measure of the strength of the westerly flow (positive with strong westerlies, and vice versa). Together with the El Niño/Southern Oscillation (ENSO) phenomenon, the NAO is a major source of seasonal to interdecadal variability in the global atmosphere. On interannual and shorter time scales, the NAO dynamics can be explained as a purely internal mode of variability of the atmospheric circulation. Interdecadal variability maybe influenced, however, by ocean and sea-ice processes. Brönnimann, Stefan aut Casty, Carlo aut Gyalistras, Dimitrios aut Luterbacher, Jürg aut Schmutz, Christoph aut Stephenson, David B. aut Xoplaki, Eleni aut Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 22(2001), 4 vom: Juli, Seite 321-381 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:22 year:2001 number:4 month:07 pages:321-381 https://doi.org/10.1023/A:1014217317898 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_4012 AR 22 2001 4 07 321-381 |
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North Atlantic Oscillation – Concepts And Studies |
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Wanner, Heinz |
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Surveys in geophysics |
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Wanner, Heinz Brönnimann, Stefan Casty, Carlo Gyalistras, Dimitrios Luterbacher, Jürg Schmutz, Christoph Stephenson, David B. Xoplaki, Eleni |
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Wanner, Heinz |
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10.1023/A:1014217317898 |
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550 |
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north atlantic oscillation – concepts and studies |
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North Atlantic Oscillation – Concepts And Studies |
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Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of variability in the Northern Hemisphere winter climate. The NAO teleconnection is characterised by a meridional displacement of atmospheric mass over the North Atlantic area. Its state is usually expressed by the standardised air pressure difference between the Azores High and the Iceland Low. ThisNAO index is a measure of the strength of the westerly flow (positive with strong westerlies, and vice versa). Together with the El Niño/Southern Oscillation (ENSO) phenomenon, the NAO is a major source of seasonal to interdecadal variability in the global atmosphere. On interannual and shorter time scales, the NAO dynamics can be explained as a purely internal mode of variability of the atmospheric circulation. Interdecadal variability maybe influenced, however, by ocean and sea-ice processes. © Kluwer Academic Publishers 2001 |
| abstractGer |
Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of variability in the Northern Hemisphere winter climate. The NAO teleconnection is characterised by a meridional displacement of atmospheric mass over the North Atlantic area. Its state is usually expressed by the standardised air pressure difference between the Azores High and the Iceland Low. ThisNAO index is a measure of the strength of the westerly flow (positive with strong westerlies, and vice versa). Together with the El Niño/Southern Oscillation (ENSO) phenomenon, the NAO is a major source of seasonal to interdecadal variability in the global atmosphere. On interannual and shorter time scales, the NAO dynamics can be explained as a purely internal mode of variability of the atmospheric circulation. Interdecadal variability maybe influenced, however, by ocean and sea-ice processes. © Kluwer Academic Publishers 2001 |
| abstract_unstemmed |
Abstract This paper aims to provide a comprehensive review of previous studies and concepts concerning the North Atlantic Oscillation. The North Atlantic Oscillation (NAO) and its recent homologue, the Arctic Oscillation/Northern Hemisphere annular mode (AO/NAM), are the most prominent modes of variability in the Northern Hemisphere winter climate. The NAO teleconnection is characterised by a meridional displacement of atmospheric mass over the North Atlantic area. Its state is usually expressed by the standardised air pressure difference between the Azores High and the Iceland Low. ThisNAO index is a measure of the strength of the westerly flow (positive with strong westerlies, and vice versa). Together with the El Niño/Southern Oscillation (ENSO) phenomenon, the NAO is a major source of seasonal to interdecadal variability in the global atmosphere. On interannual and shorter time scales, the NAO dynamics can be explained as a purely internal mode of variability of the atmospheric circulation. Interdecadal variability maybe influenced, however, by ocean and sea-ice processes. © Kluwer Academic Publishers 2001 |
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Brönnimann, Stefan Casty, Carlo Gyalistras, Dimitrios Luterbacher, Jürg Schmutz, Christoph Stephenson, David B. Xoplaki, Eleni |
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