![Page 1: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/1.jpg)
Representation of low Representation of low cloudiness/stratus in Aladin/AUT: cloudiness/stratus in Aladin/AUT:
Improvements and existing problemsImprovements and existing problems
• Areal extension of stratus layer
• The problem of horizontal diffusion
• Increasing the horizontal resolution
• Summer case 8.7.2004
![Page 2: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/2.jpg)
Areal Extension
Satellite VIS Image: 9.11.2003 12UTC
![Page 3: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/3.jpg)
Operational Aladin-Austria model run: 9.11.2003 00UTC + 12 hours forecast
![Page 4: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/4.jpg)
Satellite VIS Image: 10.11.2003 12UTC
![Page 5: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/5.jpg)
Operational Aladin-Austria model run: 9.11.2003 00UTC + 36 hours forecast
![Page 6: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/6.jpg)
Problem of Horizontal Diffusion
Aladin-Austria: 9.11.2003 00UTC +08 hours with operational horizontal diffusion settings. The stratus layer hardly penetrates into the Danube valley.
Aladin-Austria: 9.11.2003 00UTC +08 hours exp. run with horizontal diffusion of temperature set to 0. The stratus layer slightly propagates into the Danube valley.
![Page 7: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/7.jpg)
Aladin-Austria: 9.11.2003 00UTC +32 hours with operational horizontal diffusion settings. The stratus layer hardly penetrates into the Danube valley. No signal of low clouds in the basin of Klagenfurt.
Aladin-Austria: 9.11.2003 00UTC +32 hours exp. run with horizontal diffusion of temperature set to 0. Stratus forms in the Danube valley and in the basin of Klagenfurt.
![Page 8: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/8.jpg)
Pseudo-Temp for Klagenfurt, 9.11.2003 00UTC + 32h, operational model. Surface inversion developed, 2m-temperature too cold (cloud free).
Pseudo-Temp for Klagenfurt, 9.11.2003 00UTC + 32h, exp. run with HD of T =0. Elevated inversion with saturated layer below, 2m-temperature more realistic.
![Page 9: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/9.jpg)
Increasing the horizontal resolution
9.11.2003 00UTC +08h: Exp. Model run with 2.3km horizontal resolution. Forecast of low clouds slightly improved in the Danube valley, but no signal in basin of Klagenfurt.
9.11.2003 00UTC +32h: Exp. Model run with 2.3km horizontal resolution. Forecast of low clouds significantly improved in the Danube valley, but again no signal in basin of Klagenfurt.
![Page 10: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/10.jpg)
Summer Case: 8.7.2004
Satellite VIS Image: 8.7.2004 06 UTC. Low stratus developed during the night in the northern and eastern parts of Austria.
ATP500 + MSLPRESSURE, Aladin-Austria operational model forecast. Run: 7.8.2004 00 UTC + 06 hours
![Page 11: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/11.jpg)
Aladin-Austria operational model run: 8.7.2004 00UTC + 06 hours forecast. Low stratus layer covers northeastern parts of Austria, but not the Danube valley.
Aladin-Austria exp. Run with HD of T = 0 8.7.2004 00UTC + 06 hours forecast. Low stratus layer covers northeastern parts of Austria and even extends through the Danube valley.
![Page 12: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/12.jpg)
Additional experiments
• High horiz. Resolution (2.3km) with different vertical resolution (37 vs. 45 levels): no significant improvement
• Modification of the sub-inversion cloudiness scheme with flexible thickness of quasi-saturated layer: improvement of spatial extension (but danger of entering the greyzone of overestimation?)
![Page 13: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/13.jpg)
Additional experiments
• Exp. with half/a tenth part of operational HD settings: improvements of low cloudiness forecast rather linear to decrease of HD of T.
• Exp. without SK-scheme but with HD=0 : vertical temperature profile only slightly improved, but existence of clouds necessary for the development of sharp and pronounced inversions (due to cloud top cooling and heating of sub-cloud layer).
![Page 14: Representation of low cloudiness/stratus in Aladin/AUT: Improvements and existing problems Areal extension of stratus layer The problem of horizontal diffusion](https://reader035.vdocuments.us/reader035/viewer/2022062718/56649eb55503460f94bbda37/html5/thumbnails/14.jpg)
Summary
• Spatial extension of stratus layer quite realistic, only few cases with overestimation
• Deficiencies in alpine valleys and basins: partly due to destruction of inversion by HD, partly due to wrong initial conditions.
• Simply increasing the horizontal resolution does not solve the problem in alpine valleys, need of other physical parameterizations.