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Conceptual Models (CMs): Cold Air Cloudiness (CAC), Enhanced Cumulus (EC ) and Comma. How to use MSG satellite images similarities to and improvements over MTP. Contact person: Veronika Zwatz-Meise zwatz-meise@zamg.ac.at Version 1.0. 13 July 2004.
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Conceptual Models (CMs):Cold Air Cloudiness (CAC), Enhanced Cumulus (EC)and Comma How to use MSG satellite images similarities to and improvements over MTP Contact person: Veronika Zwatz-Meise zwatz-meise@zamg.ac.at Version 1.0. 13 July 2004
CMs:CAC, EC and Comma(Cold Air Cloudiness and Enhanced Cumulus) • MTP channels in comparison with the corresponding MSG channels • CMs: CAC+EC: IR image + relevant NWP parameters • MSG additional channels + Channel combinations
MTP: ir CAC EC Co As the image time between MTP and MSG differs, a shift between the cloud systems can be noticed in the two images
MSG: Ch09 CAC EC Co Sharper contours through improved space resolution
MSG: Ch10 CAC EC Co Visual inspection shows only very slight changes between Ch09 and Ch10; quantitative evaluation necessary
MTP: vis CAC EC Co
Looks relatively similar; but: somewhat coarser space resolution MSG: Ch01 CAC EC Co Grey clouds represent transperent clouds
Compared to Ch01: no strong differences in the cloud features over the ocean; but: much better land recognition MSG: Ch02 CAC EC Co Visibility of transperent clouds worse thanin Ch01
MTP:VIS(2x)+IR CAC EC Co Blue: high cloud is very dominant
Sharper contours and more detailed grey-shades through improved space resolution in IR and additional information from 2 different VIS channels MSG:129 CAC EC Co Dark blue: High cloud light blue: thick cells yellow: less thick cloud cells
CMs:CAC, EC and Comma(Cold Air Cloudiness and Enhanced Cumulus) • MTP channels in comparison with the corresponding MSG channels • CM CAC+EC: IR image + relevant NWP parameters • MSG additional channels + Channel combinations
H500 CAC, EC and Comma within huge upper level trough
Thickness CAC, EC and Comma within huge thickness trough
Thickness (green) + TA (red) CAC, EC and Comma within huge thickness trough and mainly under CA
Showalter index EC: unstable (Show < 3) Comma: Show > 5; much less unstable
PVA at 500 hPa EC and Comma: both are accompanied by distinct PVA max
Height and PVA at 500 EC and Comma: both PVA max are connected to upper level troughs
Isotachs 300 EC and Comma: both are on cyclonic side of jet streaks but: Comma is in left exit region
Isotachs and PVA 300 EC: no PVA max at 300 Comma: distinct PVA max in left exit region of the jet streak
CMs:CAC, EC and Comma(Cold Air Cloudiness and Enhanced Cumulus) • MTP channels in comparison with the corresponding MSG channels • CM CAC+EC: IR image + relevant NWP parameters • MSG additional channels + Channel combinations
MSG:129 CAC EC Co CAC: yellow: low cloud tops EC: yellow + blue: vertically extended cells Co: blue: mainly cold cloud tops
MSG: Ch03 CAC CAC: white: water cloud EC: white + dark grey: water cloud + ice cloud superimposed Co: dark grey: mainly cold cloud tops EC Co
MSG:321 CAC EC Co Grey shades: from Vis channels Cyan: represents the ice clouds from Ch03
MSG: Ch04 CAC EC Co CAC: grey: warm cloud tops EC and Co: cold cloud tops
MSG:139 CAC EC CAC: yellow: low/warm cloud tops EC: magenta + blue: vertically extended cells Co: blue: mainly cold cloud tops some magenta spots visible Co
MSG:134 CAC EC CAC: yellow: low/warm cloud tops EC: yellow + brown: vertically extended cells Co: brown: mainly cold cloud tops some yellow spots visible Co