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Published byDennis Stokes Modified over 9 years ago
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CARIBIC meteorological support Update Peter van Velthoven, KNMI Status: complete up to June 2007
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WAS-trajectories 8 day backward trajectories every 6 seconds (0.1 min) WAS-samples are taken within a minute so the trajectories stick very close together, therefore: 15 additional trajectories are calculated in a cube centred around the sample to indicate uncertainty. p was 1.03 p was 0.97 p was 0.8 longitude 0.8 latitude WAS pressure
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WAS sample 22 from flight 153 31 May 2006 WAS trajectories (each 6 secs) WAS “volume” trajectories Ordinary trajectories for 1 flight hour (5-day back)
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New ECMWF scheme for water vapour (super)saturation over ice From 13 september 2006 onward Tompkins, Gierens & Rädel: QJRMS, 133, 622, p.53, 2006 ECMWF newsletter 109, p. 26, 2006
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New ECMWF scheme for water vapour (super)saturation over ice
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The CARIBIC flights Frankfurt-Canton: PV folds around the Tibetan plateau
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Flight 130/133 November 2005 Most southern flight (into tropical air)
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Flight 146/149 April 2006 Streamer / deep fold
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Flight 150/153 May 2006: fold + deep clouds
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Flight 154/157 5-7 July 2006 Above/in fold (subtropical TP break)
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Flight 155/156 6 July 2006 Canton-Manila Mid tropospheric fold
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Flight 158/161 31 July/2 August 2006 PV remnants
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Flight 162/165 September 2006 Deep convective cloud?
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Flight 166/169 October 2006 : 2(!) folds
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Flight 170/173 November 2006 Cold air outbreak Deep into stratosphere 8-9 PVU
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Flight 174/177 December 2006 Blocking anticyclone/high + fold fold
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Flight 178/181 February 2007 Above/below relatively flat tropopause in high
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Flight 182/185 March 2007 deep folds steep tropopause
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Flight 186/189 April 2007 PV remnant
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Flight 190/193 May 2007 Close to tropopause (TP) in “high” Subtropical TP break sampled at 2 levels
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Flight 178/181 June 2007 Subtropical TP break sampled at 2 levels Real PV minimum or model artefact? Tracer signatures?
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Summary Frankfurt-Canton-Manila Frequent sampling of subtropical tropopause break Examples of flying in/above fold Frankfurt to/from Canton Sometimes strong subtropial (blocking) highs over Asia Tibetan mountains seem to be preferred location for folds
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FIN Questions?
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