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    Impact of the Antarctic Ozone Hole on the Vertical Coupling of the Stratosphere–Mesosphere–Lower Thermosphere System 

    Source: Journal of the Atmospheric Sciences:;2016:;Volume( 073 ):;issue: 006:;page 2509
    Author(s): Lubis, Sandro W.; Omrani, Nour-Eddine; Matthes, Katja; Wahl, Sebastian
    Publisher: American Meteorological Society
    Abstract: here is evidence that the strengthened stratospheric westerlies arising from the Antarctic ozone hole?induced cooling cause a polar mesospheric warming and a subsequent cooling in the lower thermosphere. While previous ...
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    Influence of the Quasi-Biennial Oscillation and Sea Surface Temperature Variability on Downward Wave Coupling in the Northern Hemisphere 

    Source: Journal of the Atmospheric Sciences:;2016:;Volume( 073 ):;issue: 005:;page 1943
    Author(s): Lubis, Sandro W.; Matthes, Katja; Omrani, Nour-Eddine; Harnik, Nili; Wahl, Sebastian
    Publisher: American Meteorological Society
    Abstract: ownward wave coupling occurs when an upward-propagating planetary wave from the troposphere decelerates the flow in the upper stratosphere and forms a downward reflecting surface that redirects waves back to the troposphere. ...
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    Downward Wave Coupling between the Stratosphere and Troposphere under Future Anthropogenic Climate Change 

    Source: Journal of Climate:;2018:;volume 031:;issue 010:;page 4135
    Author(s): Lubis, Sandro W.; Matthes, Katja; Harnik, Nili; Omrani, Nour-Eddine; Wahl, Sebastian
    Publisher: American Meteorological Society
    Abstract: AbstractDownward wave coupling (DWC) is an important process that characterizes the dynamical coupling between the stratosphere and troposphere via planetary wave reflection. A recent modeling study has indicated that ...
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