0Lower-stratospheric Rossby wave trains in the Southern Hemisphere:
Behaviour of quasi-stationary circulation anomalies observed in the lower stratosphere of the extratropical Southern Hemisphere during austral late winter of 1997 is studied. The anomalies are de ned as daily low-pass-ltered departures from the circulation varying slowly with the seasonal cycle. A w...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.600.8470 2023-05-15T18:02:13+02:00 0Lower-stratospheric Rossby wave trains in the Southern Hemisphere: Kazuaki Nishii Hisashi Nakamura The Pennsylvania State University CiteSeerX Archives 2003 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.600.8470 http://www-aos.eps.s.u-tokyo.ac.jp/~nishii/paper/QJRMS-NishiiNakamura04.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.600.8470 http://www-aos.eps.s.u-tokyo.ac.jp/~nishii/paper/QJRMS-NishiiNakamura04.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www-aos.eps.s.u-tokyo.ac.jp/~nishii/paper/QJRMS-NishiiNakamura04.pdf Blocking Low-frequency variability Polar-night jet Refractive index Troposphere text 2003 ftciteseerx 2016-01-08T14:02:06Z Behaviour of quasi-stationary circulation anomalies observed in the lower stratosphere of the extratropical Southern Hemisphere during austral late winter of 1997 is studied. The anomalies are de ned as daily low-pass-ltered departures from the circulation varying slowly with the seasonal cycle. A wave-activity ux and refractive index for stationary Rossby waves are utilized in our analysis, each of which was dened locally for the zonally varying westerlies. Subseasonal uctuations in the lower stratosphere were often associated with zonally conned wave trains emanating upward from localized, quasi-stationary anomalies in the troposphere including blocking ridges. The three-dimensional propagation of the waves was found sensitive to the structure of a local waveguide. Upward injection of Rossby wave activity into the stratosphere tended to occur slightly upstream or just beneath of a lower-stratospheric waveguide associated with the developed polar-night jet (PNJ), which led to the subsequent formation of a well-dened wave train downstream along that jet. The distribution of the lower-stratospheric subseasonal variability thus exhibits signicant zonal asymmetries, re ecting those in the PNJ structure and the distribution of tropospheric disturbances. Seasonal evolution of the PNJ and that of the tropospheric intraseasonal variability substantially modulated the lower-stratospheric activity of subseasonal uctuations. Text polar night Unknown Austral |
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Blocking Low-frequency variability Polar-night jet Refractive index Troposphere |
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Blocking Low-frequency variability Polar-night jet Refractive index Troposphere Kazuaki Nishii Hisashi Nakamura 0Lower-stratospheric Rossby wave trains in the Southern Hemisphere: |
topic_facet |
Blocking Low-frequency variability Polar-night jet Refractive index Troposphere |
description |
Behaviour of quasi-stationary circulation anomalies observed in the lower stratosphere of the extratropical Southern Hemisphere during austral late winter of 1997 is studied. The anomalies are de ned as daily low-pass-ltered departures from the circulation varying slowly with the seasonal cycle. A wave-activity ux and refractive index for stationary Rossby waves are utilized in our analysis, each of which was dened locally for the zonally varying westerlies. Subseasonal uctuations in the lower stratosphere were often associated with zonally conned wave trains emanating upward from localized, quasi-stationary anomalies in the troposphere including blocking ridges. The three-dimensional propagation of the waves was found sensitive to the structure of a local waveguide. Upward injection of Rossby wave activity into the stratosphere tended to occur slightly upstream or just beneath of a lower-stratospheric waveguide associated with the developed polar-night jet (PNJ), which led to the subsequent formation of a well-dened wave train downstream along that jet. The distribution of the lower-stratospheric subseasonal variability thus exhibits signicant zonal asymmetries, re ecting those in the PNJ structure and the distribution of tropospheric disturbances. Seasonal evolution of the PNJ and that of the tropospheric intraseasonal variability substantially modulated the lower-stratospheric activity of subseasonal uctuations. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Kazuaki Nishii Hisashi Nakamura |
author_facet |
Kazuaki Nishii Hisashi Nakamura |
author_sort |
Kazuaki Nishii |
title |
0Lower-stratospheric Rossby wave trains in the Southern Hemisphere: |
title_short |
0Lower-stratospheric Rossby wave trains in the Southern Hemisphere: |
title_full |
0Lower-stratospheric Rossby wave trains in the Southern Hemisphere: |
title_fullStr |
0Lower-stratospheric Rossby wave trains in the Southern Hemisphere: |
title_full_unstemmed |
0Lower-stratospheric Rossby wave trains in the Southern Hemisphere: |
title_sort |
0lower-stratospheric rossby wave trains in the southern hemisphere: |
publishDate |
2003 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.600.8470 http://www-aos.eps.s.u-tokyo.ac.jp/~nishii/paper/QJRMS-NishiiNakamura04.pdf |
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Austral |
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Austral |
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polar night |
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polar night |
op_source |
http://www-aos.eps.s.u-tokyo.ac.jp/~nishii/paper/QJRMS-NishiiNakamura04.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.600.8470 http://www-aos.eps.s.u-tokyo.ac.jp/~nishii/paper/QJRMS-NishiiNakamura04.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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1766172008510390272 |