The 10-12-year atmospheric oscillation
This paper summarizes the results of work which is based on the discovery by Labitzke (1982, 1987) of a 10-12-year oscillation in the arctic stratospheric temperature. The oscillation modulates the extratropical effect of the Quasi-Biennial Oscillation in winter and is in phase with the 11-year suns...
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| Format: | Article |
| Language: | English |
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Borntraeger
1994-10-01
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| Series: | Meteorologische Zeitschrift |
| Subjects: | |
| Online Access: | http://dx.doi.org/10.1127/metz/3/1994/259 |
| _version_ | 1797320862182932480 |
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| author | H. van Loon K. Labitzke |
| author_facet | H. van Loon K. Labitzke |
| author_sort | H. van Loon |
| collection | DOAJ |
| description | This paper summarizes the results of work which is based on the discovery by Labitzke (1982, 1987) of a 10-12-year oscillation in the arctic stratospheric temperature. The oscillation modulates the extratropical effect of the Quasi-Biennial Oscillation in winter and is in phase with the 11-year sunspot cycle. Labitzke's original papers dealt only with the north polar stratospheric temperature in winter, but we have expanded the investigation to cover the whole year and most of the Northern Hemisphere. In months other than January, February and March, it is not necessary to group the data according to the phase of the QBO to find the solar signal. The signal appears as a basic, consistent pattern in the correlations between stratospheric geopotential heights and the solar cycle in which the highest correlations are south of about 45° N with a distinct maximum over the western, ocean-covered part of the hemisphere. The variation of the stratospheric heights on the 10-12-year scale are - in the area of high correlations with the solar cycle - associated with temperature changes on the same time scale in the middle and upper troposphere. Preliminary work suggests that the interannual variation of the tropical and subtropical vertical motions contains a component on the 10-12-year scale; but a mechanism which connects the solar and tropospheric-stratospheric oscillations on the 10-12-year scale has not yet been found. In January and February the correlations of a full time series of stratospheric quantities with the sun are smallest, although the basic pattern is the same as during the rest of the year. The small size of the correlations is due to the fact that they are of opposite sign in the east and west years of the Quasi-Biennial Oscillation. The correlation pattern in the east years is the same as in the ten other months of the year; in the west years the opposite sign is related to the fact that those major midwinter breakdowns of the stratospheric westerly (cyclonic) vortex which take place in the west years, have so far happened only in maxima of the 11-year sunspot cycle. |
| first_indexed | 2024-03-08T04:49:09Z |
| format | Article |
| id | doaj.art-eb9d1af96d1448148197c7e1cdf1fbc2 |
| institution | Directory Open Access Journal |
| issn | 0941-2948 |
| language | English |
| last_indexed | 2024-03-08T04:49:09Z |
| publishDate | 1994-10-01 |
| publisher | Borntraeger |
| record_format | Article |
| series | Meteorologische Zeitschrift |
| spelling | doaj.art-eb9d1af96d1448148197c7e1cdf1fbc22024-02-08T08:11:38ZengBorntraegerMeteorologische Zeitschrift0941-29481994-10-013525926610.1127/metz/3/1994/25989550The 10-12-year atmospheric oscillationH. van LoonK. LabitzkeThis paper summarizes the results of work which is based on the discovery by Labitzke (1982, 1987) of a 10-12-year oscillation in the arctic stratospheric temperature. The oscillation modulates the extratropical effect of the Quasi-Biennial Oscillation in winter and is in phase with the 11-year sunspot cycle. Labitzke's original papers dealt only with the north polar stratospheric temperature in winter, but we have expanded the investigation to cover the whole year and most of the Northern Hemisphere. In months other than January, February and March, it is not necessary to group the data according to the phase of the QBO to find the solar signal. The signal appears as a basic, consistent pattern in the correlations between stratospheric geopotential heights and the solar cycle in which the highest correlations are south of about 45° N with a distinct maximum over the western, ocean-covered part of the hemisphere. The variation of the stratospheric heights on the 10-12-year scale are - in the area of high correlations with the solar cycle - associated with temperature changes on the same time scale in the middle and upper troposphere. Preliminary work suggests that the interannual variation of the tropical and subtropical vertical motions contains a component on the 10-12-year scale; but a mechanism which connects the solar and tropospheric-stratospheric oscillations on the 10-12-year scale has not yet been found. In January and February the correlations of a full time series of stratospheric quantities with the sun are smallest, although the basic pattern is the same as during the rest of the year. The small size of the correlations is due to the fact that they are of opposite sign in the east and west years of the Quasi-Biennial Oscillation. The correlation pattern in the east years is the same as in the ten other months of the year; in the west years the opposite sign is related to the fact that those major midwinter breakdowns of the stratospheric westerly (cyclonic) vortex which take place in the west years, have so far happened only in maxima of the 11-year sunspot cycle.http://dx.doi.org/10.1127/metz/3/1994/259arctic stratospheresunspot cyclenorthern hemispheresubtropicalquasi-biennial oscillationqboarktische stratosphäresonnenfleckenzyklusnordhalbkugelsubtropisch |
| spellingShingle | H. van Loon K. Labitzke The 10-12-year atmospheric oscillation Meteorologische Zeitschrift arctic stratosphere sunspot cycle northern hemisphere subtropical quasi-biennial oscillation qbo arktische stratosphäre sonnenfleckenzyklus nordhalbkugel subtropisch |
| title | The 10-12-year atmospheric oscillation |
| title_full | The 10-12-year atmospheric oscillation |
| title_fullStr | The 10-12-year atmospheric oscillation |
| title_full_unstemmed | The 10-12-year atmospheric oscillation |
| title_short | The 10-12-year atmospheric oscillation |
| title_sort | 10 12 year atmospheric oscillation |
| topic | arctic stratosphere sunspot cycle northern hemisphere subtropical quasi-biennial oscillation qbo arktische stratosphäre sonnenfleckenzyklus nordhalbkugel subtropisch |
| url | http://dx.doi.org/10.1127/metz/3/1994/259 |
| work_keys_str_mv | AT hvanloon the1012yearatmosphericoscillation AT klabitzke the1012yearatmosphericoscillation AT hvanloon 1012yearatmosphericoscillation AT klabitzke 1012yearatmosphericoscillation |