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Seasonal variability of gravity waves and tidal/gravity-wave interactions in the Arctic and Antarctic MLT Charlie Beldon & Nick Mitchell Centre for Space, Atmospheric and Oceanic Science Department of Electronic and Electrical Engineering University of Bath [email_address] COSPAR 2008
Outline ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Rothera, Antarctica (68ºS, 68ºW) Esrange, Sweden (68ºN, 21ºE) Location of Radars
Introduction – meteor radar winds ,[object Object],[object Object],[object Object],[object Object],Calculate zonal and meridional winds by a least-squares fit of horizontal velocities
Introduction – meteor radar winds Final Data product: Winds at heights of  ~ 80-100 km Time resolution  ~ 1-2 hours Height resolution  ~ 2-3 km ,[object Object],[object Object],[object Object],[object Object],Calculate zonal and meridional winds by a least-squares fit of horizontal velocities
Gravity waves - method ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Gravity waves - method ,[object Object],[object Object],[object Object],[object Object]
Gravity waves - method Final Data Product: Variance from waves with period ~ 20 mins – 2 hours, λ h ~< 400 km ,[object Object],[object Object],[object Object],[object Object]
Example of the data
Seasonal behaviour
 
Summer Profiles:
 
Summer Profiles:
What controls the summer wave activity? Rothera Esrange
[object Object],What controls the summer wave activity? 100 80 60 -50  0  50 Zonal Wind
[object Object],[object Object],What controls the summer wave activity? 100 80 60 -50  0  50 Zonal Wind 100 90 80 -20  -10  0 Meridional Wind
[object Object],[object Object],[object Object],What controls the summer wave activity? 100 80 60 -50  0  50 Zonal Wind 100 90 80 -20  -10  0 Meridional Wind 120  140  160  180  200 100 90 80 Temperature
Exclusion circles 20 km Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed URAP zonal winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 30 km URAP zonal winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 40 km URAP zonal winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 50 km URAP zonal winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 60 km Meridional Phase Speed URAP zonal winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 70 km URAP zonal winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 80 km URAP zonal winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 81.1 km Radar zonal and meridional winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 84.6 km Radar zonal and meridional winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 87.5 km Radar zonal and meridional winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 90.4 km Radar zonal and meridional winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 93.3 km Radar zonal and meridional winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed 96.8 km Radar zonal and meridional winds
Exclusion circles Zonal Phase Speed -50  0  50  50 0 -50 Meridional Phase Speed ,[object Object],[object Object],[object Object]
What controls the wave activity? (Temperature data from L ü bken  et al,  2004, falling sphere climatology)
(Temperature data from L ü bken falling sphere climatology) What controls the wave activity? ,[object Object]
Equinoctial minima – filtering of low phase-speed waves Seasonal cycle
COMPOSITE YEAR VARIANCE, ESRANGE Note : Esrange data shifted by 6 months Arctic/Antarctic comparisons COMPOSITE YEAR VARIANCE, ROTHERA
[object Object],[object Object],Arctic/Antarctic comparisons RATIO OF COMPOSITE YEAR VARIANCES, ROTHERA/ESRANGE
[object Object],Arctic/Antarctic comparisons
[object Object],Arctic/Antarctic comparisons
Tidal/gravity-wave interactions
Modulations of gravity-wave activity AMPLITUDE (m 2 s -2 ) PERIOD (DAYS)
Modulation of gravity-wave activity - tides ,[object Object],[object Object],[object Object],[object Object],[object Object],VARIANCE ZONAL WIND
Modulation of gravity-wave activity - tides VARIANCE ZONAL WIND VARIANCE ZONAL WIND ,[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Conclusions
 
 
 
 
 
 
i.e.,  more gravity-wave activity in spring over Rothera than Esrange less gravity-wave activity in summer over Rothera at greater heights Inter-hemispheric Comparisons
 
Meridional Winds
Modulation of Gravity-wave Activity
Gravity wave scales sizes Meteor radars cannot easily resolve individual waves of short horizontal wavelength (< ~ 1,000 km) or high frequency (periods < ~ 2 hours)
Equinoctial minima – filtering of low phase-speed waves Seasonal Cycle - Filtering
NB, six routine height gates of 5, 3, 3, 3, 3, 5 km  Meteor radar winds January 6, 2007 over Rothera (68 ˚S) Can not easily resolve individual waves of short horizontal wavelength (< ~ 1,000 km) or high frequency (periods < ~ 2 hours)
January 6, 2007 over Rothera (68 ˚S) Meteor radar winds NB, six routine height gates of 5, 3, 3, 3, 3, 5 km
Seasonal cycle ,[object Object],[object Object]
[object Object],[object Object],How much variance from measurement uncertainty?
[object Object],Inter-hemispheric comparisons
Seasonal cycle and short-term variability Rothera (68˚S) Variance (m 2 s -2 ) Variance (m 2 s -2 )
12-hours 24-hours Modulation of gravity-wave activity
Modulation of gravity-wave activity

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Seasonal variability of gravity waves and tidal/gravity-wave interactions in the Arctic and Antarctic MLT