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Abstract. Atmospheric circulation indices can be used to explain the variability of runoff on a continental scale. Beside well-known regional anomalies of precipitation and runoff that correlate with phases of the North Atlantic Oscillation (NAO) there are also drifting fields of annual discharge an...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.384.6008 2023-05-15T17:30:56+02:00 time series R. Rödel The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.384.6008 http://hal.archives-ouvertes.fr/docs/00/29/69/61/PDF/adgeo-9-93-2006.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.384.6008 http://hal.archives-ouvertes.fr/docs/00/29/69/61/PDF/adgeo-9-93-2006.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://hal.archives-ouvertes.fr/docs/00/29/69/61/PDF/adgeo-9-93-2006.pdf text ftciteseerx 2016-09-18T00:30:19Z Abstract. Atmospheric circulation indices can be used to explain the variability of runoff on a continental scale. Beside well-known regional anomalies of precipitation and runoff that correlate with phases of the North Atlantic Oscillation (NAO) there are also drifting fields of annual discharge anomalies. Following the trend of the NAO, these fields move along a longitudinal axis from western Europe to the Lena catchment in Siberia and back again. The same pattern is observable in the changing flow regimes. This paper describes the origin and causes of these anomaly fields and explains them as the results of important climate variations in the northern hemisphere. 1 Text North Atlantic North Atlantic oscillation Siberia Unknown |
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ftciteseerx |
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English |
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Abstract. Atmospheric circulation indices can be used to explain the variability of runoff on a continental scale. Beside well-known regional anomalies of precipitation and runoff that correlate with phases of the North Atlantic Oscillation (NAO) there are also drifting fields of annual discharge anomalies. Following the trend of the NAO, these fields move along a longitudinal axis from western Europe to the Lena catchment in Siberia and back again. The same pattern is observable in the changing flow regimes. This paper describes the origin and causes of these anomaly fields and explains them as the results of important climate variations in the northern hemisphere. 1 |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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R. Rödel |
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R. Rödel time series |
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R. Rödel |
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R. Rödel |
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time series |
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time series |
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time series |
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time series |
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time series |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.384.6008 http://hal.archives-ouvertes.fr/docs/00/29/69/61/PDF/adgeo-9-93-2006.pdf |
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North Atlantic North Atlantic oscillation Siberia |
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North Atlantic North Atlantic oscillation Siberia |
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http://hal.archives-ouvertes.fr/docs/00/29/69/61/PDF/adgeo-9-93-2006.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.384.6008 http://hal.archives-ouvertes.fr/docs/00/29/69/61/PDF/adgeo-9-93-2006.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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