airmass tracked by ballons and forecasts – same airmass revisited with research aircraft
DESCRIPTION
ASTEX case Gunilla Svensson Department of Meteorology and the Bert Bolin Centre for Climate Research Stockholm University, Sweden. Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft. ASTEX 1 st Lagrangian experiment. - PowerPoint PPT PresentationTRANSCRIPT
![Page 1: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/1.jpg)
ASTEX case Gunilla Svensson
Department of Meteorology and the Bert Bolin Centre for Climate Research
Stockholm University, Sweden
![Page 2: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/2.jpg)
Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft
![Page 3: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/3.jpg)
ASTEX 1st Lagrangian experiment
EUCLIPSE/GCSS Meeting, 29-30 September 2010 Svensson et al., 2000
![Page 4: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/4.jpg)
ASTEX 1st Lagrangian experiment
EUCLIPSE/GCSS Meeting, 29-30 September 2010 Svensson et al., 2000
![Page 5: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/5.jpg)
ASTEX 1st Lagrangian experiment
1-D version of the MIUU mesoscale model
• Hydrostatic pressure• Prescribed background flow (geostrophic wind)• Surface fluxes (Fairall et al, surface layer similarity and roughness
sub-layer treatment)• Second-order turbulence closure (Mellor-Yamada type with
prognostic TKE)• Subgrid-scale condesation• Short and long-wave radiation (Fu&Liou, delta four-stream and
correlated k-distribution)• A simplified algorithm for prognostic drizzle water
• conversion of cloud water to drizzle • collection of cloud drops by raindrops• fall-out of rain drops• evaporation of rain drops in sub-saturated air
EUCLIPSE/GCSS Meeting, 29-30 September 2010 Svensson et al., 2000
![Page 6: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/6.jpg)
A sub-grid scale cloud scheme in this framework:
*(T, q)
T´
q´
Temperature
Spec
ific
hum
idit
y
qs
![Page 7: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/7.jpg)
Model results
![Page 8: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/8.jpg)
![Page 9: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/9.jpg)
![Page 10: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/10.jpg)
![Page 11: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/11.jpg)
![Page 12: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/12.jpg)
Latent heat flux and drizzle rate
![Page 13: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/13.jpg)
• SST or subsidence driving the change from Sc to Cu?
• Drizzle only a few mm per day does it matter?
• Subsidence very small vertical motions, is it important?
In a model it is possible to pick these pieces apart –
never possible in real life
Sensitivity experiments
![Page 14: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/14.jpg)
![Page 15: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/15.jpg)
![Page 16: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/16.jpg)
Z clo
ud-to
pLW
PAl
bed
oDr
izzl
eZ c
loud
-bas
e
Sensitivity experimentsTK
E
![Page 17: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/17.jpg)
Vertical velocity at PBL topHIRLAM simulation
EUCLIPSE/GCSS Meeting, 29-30 September 2010 Sigg and Svensson, 2004
Oscillations are due to inertia-gravity waves that propagate from the non-elliptic areas where gradient-wind balance cannot be maintained.
![Page 18: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/18.jpg)
Synoptic-scale divergence
Filtered vertical velocities removing scales smaller than 15h
South
North
EUCLIPSE/GCSS Meeting, 29-30 September 2010 Sigg and Svensson, 2004
![Page 19: Airmass tracked by ballons and forecasts – same airmass revisited with research aircraft](https://reader035.vdocuments.site/reader035/viewer/2022062520/56815d96550346895dcbb45c/html5/thumbnails/19.jpg)
END