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Short Introduction ZAMG, WLKC733 Thomas Krennert, ZAMG – Vienna, Synoptic Department email:...
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Transcript of Short Introduction ZAMG, WLKC733 Thomas Krennert, ZAMG – Vienna, Synoptic Department email:...
Short IntroductionShort IntroductionZAMG, WLKC733 ZAMG, WLKC733
Thomas Krennert, ZAMG – Vienna, Synoptic Department
email: [email protected]
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
ZAMG / SYN subjective
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
Start: ~1954 with Baur / Lauscher Usable records from ~1959 1957 - 1959 reconstructed Individual knowledge of forecaster
included: mixture of methods continued
Baur Lauscher Hess-Brezowski Schuepp Steinacker
More than 80 classes found Reduced to 43 / digitalized (-) Still identical classes (-) Only regards small domain (+) Largest catalogue of air mass
analysis and frontal passages
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
Classification: 43 Types
Air mass analysis: upper level (< 850 hPa), surface level (> 850 hPa)
Change of air mass: 2 levels during the day
Frontal passage: type and time of passage over Vienna / Austria.
Air mass analysis and frontal passages are missing for the years:
1957 - 1960
1968 - 1970
1976
1982
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
Subjective Weather Type Classification ZAMG / SYN-OP
Type Type Effect over
Eastern Alpine Region
Quantity
N / NE / E / SE / S / SW / W / NW
Flow regime cyclonic / anticyclonic
16
HM High pressure centre, Central Europe 1 HE High pressure centre, to the East C / A 2 HB High pressure centre, Great Britain C / A 2 HN High pressure centre, North Sea C / A 2 HF High pressure centre, Fennoscandia C / A 2 HBM High pressure ridge, Central Europe (Axis) 1 HNF High pressure field, North Sea and
Fennoscandia C / A 2
h Intermediate High 1 HR High pressure field, Boundary 1 f Weak pressure gradient C / A 2 TM Low pressure centre, Central Europe 1 TIW Low pressure centre, to the West 1 TWM Low pressure centre, Western
Mediterranean
TS Low pressure centre, to the South 1 TB Low pressure centre, Great Britain C / A 2 TRM Trough, Central Europe 1 TRW Trough, Western Europe C / A 2 HT Upper level low 1 UGL Changing Weather Type C / A 2 ===== 43
Air mass analysis ZAMG / SYN-OP Cold air masses Air mass (ZAMG) Naming Origin Properties
cPA (caK) Polar air from
Northern Siberia Northern Siberia (from NE, over Russia)
Extremely cold, dry
mPA (maK) Arctic Polar air Arctic (From N over Northern Sea) Very cold, moist cP (cGAK) Russian Polar air Eastern Europe (from NE / E over
Eastern Europe) Cold, dry
mP (mGAK) Polar air from Greenland
Arctic (from N, NW over Greenland Sea)
Moderately cold or cool, moist
cPT (cGAW) Old, returning Polar air
Arctic (from E, SE over South Eastern Europe)
Moderately cold, dry
mPT (mGAW) Warmed Polar air Arctic (from NW over Northern Europe)
Cool, moist
Warm air mass Air mass (ZAMG) Naming Origin Properties
cTP (cGTK) Continental Central Europe, South Eastern
Europe Dry, warm during summer, moderately cold during Winter
mTP (mGTK) Sea Air Northern Atlantic (from NW over British Isles)
Moist, mild or moderately warm
cT (cGTW) Continental tropic air Near East (from SE over Balkan peninsula)
Hot, dry
mT (mGTW) Atlantic tropic air During High over Azores (from SW over Iberian peninsula)
Moist, warm
cTS (cTW) African tropic air Sahara (from SE over Balkan peninsula)
Dry, hot
mTS (mTW) Mediterranean tropic air
North Africa (from S, SW over the Mediterranean)
Muggy, hot, hazy
Two layers: upper level (mostly < 850 hPa) / lower level (mostly > 850 hPa)
Fronts ZAMG / SYN-OP Decision tree: yes/no, type, passage over Vienna (UTC) Surface fronts: Cold / Warm / Occlusion Upper fronts: Cold / Warm, only in combination with significant surface weather Upper level trough Convergence line Thickness Ridge with rain or thunderstorms Baroclinic Boundary Masked Coldfront Comma
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
WLKC733
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
Flow pattern direction including indication of cyclonicity and precipitable water
Each parameter could be investigated seperately (alphanumeric output)
More equally distributed on smaller domains
Applicable only for small domains
Easily applicable operationally
Advantage within areas with orography
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
Method:
First two letters denote main wind sector number counting clockwise: sector 01=NE, 02=SE, 03=SW, 04=NW, 00=undefined (varying directions)
Wind direction at 700 hPa indicates flow Derived from u-, v- components of true wind 2/3 of all weighted wind directions have to be connected to a sector of 10° Sector is assigned to a quadrant (i.e. „SW“ = [190°, 280°])
Third letter denotes >A<nticyclonicity or >C<yclonicity at z925. 4th letter denotes >A<nticyclonicity or >C<yclonicity at z500.
For each grid point Weighted area mean value is calculated [gpdm2/km2 * 10.000]
5th letter denotes >D<ry or >W<et.
Weighted area mean value of precipitable water (whole atmosphere) Compared to area daily mean value (annual variation) Indicating values above or below of daily mean
)(2
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
1) parameters: z925,z500,u700,v700,pw
2) software: code available on cost733 - wiki
3) background: basic knowledge
4) time/CPU: few seconds
5) number of types: 40, could be reduced
7) key-patterns: subjective / thresholds
8) distance measure: thresholds
Profile WLKC733Profile WLKC733
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
6) literature:
Dittmann, E., 1995: Objektive Wetterlagenklassifikation, Offenbach am Main, Selbstverlag des Deutschen Wetterdienstes, Berichte des Deutschen Wetterdienstes, Band 197.
Bissolli, P., 1999: Kommen Westwetterlagen häufiger vor als früher? Klimastatusbericht 1999, 26-30, Deutscher Wetterdienst, Offenbach a.M.
Bissolli, P., Dittmann, E., 2001: The objective weather type classification of the German Weather Service and its possibilities of application to environmental and meteorological investigations, Meteorologische Zeitschrift, Volume 10, Number 4, 1 July 2001 , pp. 253-260(8)
Thomas Krennert, ZAMG – Vienna, Austria, Synoptic Department COST 733 WG2 Meeting Augsburg, March 2008
Adaptations:
Subjective weighting (after “experiments”) Small central domain with dominant weighting
15X
2X1X