Northern tools and data for model comparisons
Transcription
Northern tools and data for model comparisons
Northern tools and data for model comparisons Home Page Title Page JJ II J I Page 1 of 19 Go Back Full Screen Close Quit Laura Rontu, FMI laura [email protected] Zhenya Atlaskin, RSHU [email protected] Timo Vihma, FMI [email protected] Kalle Eerola, FMI [email protected] Nastya Senkova, RSHU [email protected] Markku Kangas, FMI [email protected] December 10, 2005 Home Page Title Page JJ II J I Page 2 of 19 Go Back Full Screen Close Quit How to validate a new scheme? Standard station verification Details of bias Introduction to Sodankylä Sounding comparison Mast comparison Further possibilities How to validate a new scheme? Home Page Title Page JJ II J I Page 3 of 19 Go Back Full Screen Close Quit How to validate a new scheme? Northern winter problem In the model, too warm predicted near-surface temperatures in a stable Home Page arctic boundary layer. Differences between observation and forecast of the order of ten degrees are common. In reality, clear sky, no Title Page JJ II significant SW radiation, shallow surface layer with strong surface temperature inversion over snow covered surface. Relative humidity may be large but not close to saturation. Observed latent and sensible J I heat fluxes are small, in the model generally somewhat larger. Extra clouds/fog may form in HIRLAM. Page 3 of 19 Go Back Full Screen Close Quit SFS: a possible element of the solution Home Page Title Page JJ II J I Page 4 of 19 Go Back Full Screen Close Quit SFS: a possible element of the solution • Snow - Forest - Scheme by Stefan Gollvik et al. Home Page • Detailed handling of interactions in (snow covered) forest and open land Title Page JJ II • ISBA framework with diffusion equation in soil partly based on the old HIRLAM surface scheme developed for the Rossby Centre Climate Model J I Page 4 of 19 Go Back Full Screen Close Quit • references: Norrköping SRNWP workshop, Sodankylä summer school SFS: a possible element of the solution • Snow - Forest - Scheme by Stefan Gollvik et al. Home Page • Detailed handling of interactions in (snow covered) forest and open land Title Page JJ II • ISBA framework with diffusion equation in soil partly based on the old HIRLAM surface scheme developed for the Rossby Centre Climate Model J I • references: Norrköping SRNWP workshop, Sodankylä summer school The scheme is ready for one-dimensional and three-dimensional comparisons Page 4 of 19 How to know if it solves our problem? Go Back Full Screen Close Quit Standard station verification Verification statistics against Scn observations 40E (left) OMA (right) Period: 20050101 - 20050131 Surface pressure JJ II J 2 1 0 -1 0 6 Close Quit 3 2 1 0 -1 -2 -3 12 18 24 30 36 42 48 BIAS RMS 0 7 6 5 4 3 2 1 0 -1 -2 -3 -4 BIAS RMS 0 6 6 BIAS RMS 12 18 24 30 36 42 48 Forecast length (hours) Ten metre wind Mean speed and RMS vector error (m/s) Full Screen 5 4 Forecast length (hours) Page 5 of 19 Go Back BIAS RMS 3 -2 I BIAS RMS Two metre relative humidity BIAS RMS 12 18 24 30 36 42 48 Forecast length (hours) Mean and RMS error (%) Title Page Mean and RMS error (hPa) 5 4 Two metre temperature Mean and RMS error (K) Home Page 35 30 25 20 15 10 5 0 -5 -10 -15 BIAS RMS 0 6 BIAS RMS 12 18 24 30 36 42 48 Forecast length (hours) ZOBS or details of the bias (1) Home Page Title Page JJ II J I Page 6 of 19 Go Back Full Screen Close Quit ZOBS (2) Verification statistics Verification statistics observations WMO022221 Verification statistics experiment 40E observations WMO022221 Period + fc length: 200501+024 experiment 40E Period + fc length: 200501+024 Mean sea level pressure Mean Two metre sea level temperature pressure 0 4000 2 3000 1 2000 0 1000 -1 4000 3000 2000 1000 0 -2 0 960 970 980 990 1000 1010 1020 1030 -1 Observed pressure (hPa) Page 7-2of 19 960 970 980 990 1000 1010 1020 1030 8 8000 lassified and accumulated bias (m/s) 8 6 4 Close 2 0 4 4000 2 2000 0 0 8000 -2 -4 6000 -6 4000 class accum -8 -10 0 3 6 2000 9 12 15 18 21 024 27 Observed wind speed (m/s) -2 Quit -4 -6 -8 6000 class accum Classified and accumulated bias (%) 10 Ten6 metre wind Full Screen 10 88 77 66 5 54 43 32 1 2 0 1 -1 0-2 class -3 accum -1 -4 -2-24 -21 -18 -15 -12 -9 -6 -3 0 3 class Observed temperature (C) -3 accum -4 -24 -21 -18 -15 -12 -9 -6 -3 Two metre relative Ten metre humidity wind(C) Observed temperature Observed pressure (hPa) lassified and accumulated bias (m/s) lassified and accumulated bias (%) Go Back Classified and accumulated bias (m/s) Ten metre wind Observed pressure (hPa) Classified and accumulated bias (C) I 3 5000 Classified and accumulated bias (C) 1 4 5000 6000 88 8000 8 8000 class 77 class 7 7000 7000 accum accum 6000 6 6000 66 6000 6 6000 5 5 5000 54 4000 5 5000 4000 4 4000 43 4 3 20004000 3000 32 1 2000 2 3 3000 2000 2 0 0 1000 1 1 -1 2000 2 0 0 0-2 0 class 1000 1 -1 -3 accum -1 -4 -2 0 0 -15 -12 970 -9980-6 990 -3 1000 0 3 1010 6 1020 1030 -2 -24 -21 -18960 class -1 -3 Observed temperature (C) (hPa) Observed pressure accum -2 -4 960 -24 970-21980 -18 -15 990 -12 1000 -9 1010 -6 -3 10200 1030 3 6 8 7 10 40 35 25 4020 15 8 35 6 30 5 4 250 2 20-5 0 10 8 TwoTen metre relative wind humidity 9000 6 metre 30 10 -10 15 30 -2 10 -4 5 -6 0 -8 -5 6000 2 6000 8000 2000 0 3000 -2 6000 9000 -4 0 -6 class -8 accum 8000 4000 4 0 class accum -10 40 50 0 3 60 6 709 4000 2000 6000 80 12 1590 1810021 24 0 27 Observed relative Observed humidity wind speed (%) (m/s) 3000 0 class class accumaccum 8000 8000 6000 6000 4000 4000 2000 2000 0 0 6 0 3 6 Two Observed metre relative humidity (C) temperature Classified and accumulated bias (%) 2 6000 5 Two metre temperature Classified and accumulated bias (hPa) 3 6 7000 Classified and accumulated bias (m/s) II 7000 Classified and accumulated bias (C) 4 class accum Classified and accumulated bias (C) J 5 8 class 7 accum Two metre temperature Two metre Mean temperature sea level pressure Classified and accumulated bias (hPa) JJ 6 Classified and accumulated bias (hPa) Classified and accumulated bias (hPa) Mean sea level pressure 7 Period + fc length: 200501+024 lassified and accumulated bias (%) Home Page 8 Title Page observations WMO022221 Verification statistics experiment OMA observations WMO022221 Period + fc length: 200501+024 experiment OMA 40 35 Two metre relative humidity 9000 30 25 20 40 6000 15 35 10 3000 305 250 20-5 -10 15 30 10 9000 0 class accum 40 50 6000 60 70 80 90 Observed relative humidity (%) 100 3000 5 0 -5 0 class accum Details of the bias (3) Verification statistics Verification statistics observations WMO022122 Verification statistics experiment 40E observations WMO022122 Period + fc length: 200501+000 experiment 40E Period + fc length: 200501+000 Mean sea level pressure Mean Two metre sea level temperature pressure 0 4000 2 3000 1 2000 0 1000 -1 4000 3000 2000 1000 0 -2 0 960 970 980 990 1000 1010 1020 1030 -1 Observed pressure (hPa) Page 8-2of 19 960 970 980 990 1000 1010 1020 1030 8 8000 lassified and accumulated bias (m/s) 8 6 4 Close 2 0 4000 2 2000 0 0 8000 -2 -4 6000 -6 4000 class accum -8 -10 0 3 6 2000 9 12 15 18 21 024 27 Observed wind speed (m/s) -2 Quit -4 10 8 6 40 4020 10 30 4 2 0 -2 10 8 TwoTen metre relative wind humidity 12000 6 metre 30 0 20 -10 30 10 8000 2 6000 8000 2000 0 4000 -2 600012000 -4 0 -6 class -8 accum 8000 4000 4 0 class accum -10 40 50 0 3 60 6 709 -6 class accum -8 4000 2000 8000 80 12 1590 1810021 24 0 27 Observed relative Observed humidity wind speed (%) (m/s) 0 4000 0 class class accumaccum 8000 8000 6000 6000 4000 4000 2000 2000 0 0 6 0 3 6 Two Observed metre relative humidity (C) temperature -4 -6 -8 6000 4 Classified and accumulated bias (%) 10 Ten6 metre wind Full Screen 10 88 77 66 5 54 43 32 1 2 0 1 -1 0-2 class -3 accum -1 -4 -2-24 -21 -18 -15 -12 -9 -6 -3 0 3 class Observed temperature (C) -3 accum -4 -24 -21 -18 -15 -12 -9 -6 -3 Two metre relative Ten metre humidity wind(C) Observed temperature Observed pressure (hPa) lassified and accumulated bias (m/s) lassified and accumulated bias (%) Go Back Classified and accumulated bias (m/s) Ten metre wind Observed pressure (hPa) Classified and accumulated bias (C) I 3 5000 Classified and accumulated bias (C) 1 4 5000 6000 88 8000 8 8000 class 77 class 7 7000 7000 accum accum 6000 6 6000 66 6000 6 6000 5 5 5000 54 4000 5 5000 4000 4 4000 43 4 3 20004000 3000 32 1 2000 2 3 3000 2000 2 0 0 1000 1 1 -1 2000 2 0 0 0-2 0 class 1000 1 -1 -3 accum -1 -4 -2 0 0 -15 -12 970 -9980-6 990 -3 1000 0 3 1010 6 1020 1030 -2 -24 -21 -18960 class -1 -3 Observed temperature (C) (hPa) Observed pressure accum -2 -4 960 -24 970-21980 -18 -15 990 -12 1000 -9 1010 -6 -3 10200 1030 3 6 8 7 Classified and accumulated bias (%) 2 6000 5 Two metre temperature Classified and accumulated bias (hPa) 3 6 7000 Classified and accumulated bias (m/s) II 7000 Classified and accumulated bias (C) 4 class accum Classified and accumulated bias (C) J 5 8 class 7 accum Two metre temperature Two metre Mean temperature sea level pressure Classified and accumulated bias (hPa) JJ 6 Classified and accumulated bias (hPa) Classified and accumulated bias (hPa) Mean sea level pressure 7 Period + fc length: 200501+000 lassified and accumulated bias (%) Home Page 8 Title Page observations WMO022122 Verification statistics experiment OMA observations WMO022122 Period + fc length: 200501+000 experiment OMA 40 Two metre relative humidity 12000 30 20 40 8000 10 4000 30 0 20 -10 30 10 12000 0 class accum 40 50 8000 60 70 80 90 Observed relative humidity (%) 0 100 4000 0 class accum Introduction to Sodankylä - FMI ARC What makes Sodankylä observations interesting? Home Page Title Page JJ II J I Page 9 of 19 Go Back Full Screen Close Quit Introduction to Sodankylä - FMI ARC What makes Sodankylä observations interesting? Boreal - subarctic enviroment Home Page • (long-living) Stable boundary layer, cold Ts • Boreal forest, snow, low solar elevations Title Page JJ II J I Page 9 of 19 Go Back Full Screen Close Quit Introduction to Sodankylä - FMI ARC What makes Sodankylä observations interesting? Boreal - subarctic enviroment Home Page • (long-living) Stable boundary layer, cold Ts • Boreal forest, snow, low solar elevations Title Page JJ II Unique combination of measurements • Sounding data • Mast measurements: profiles and fluxes J I • AWS - SYNOP data + ceilometer • Soil and snow temperature measurements Page 9 of 19 • Radar measurements within 40 km Go Back Full Screen Close Quit Introduction to Sodankylä - FMI ARC What makes Sodankylä observations interesting? Boreal - subarctic enviroment Home Page • (long-living) Stable boundary layer, cold Ts • Boreal forest, snow, low solar elevations Title Page JJ II Unique combination of measurements • Sounding data • Mast measurements: profiles and fluxes J I • AWS - SYNOP data + ceilometer • Soil and snow temperature measurements Page 9 of 19 • Radar measurements within 40 km Go Back Operational and continuous observations • Used for operational monitoring Full Screen • Quality control: + and Close • Data/Tools availability: + and • Possibility for special observation periods Quit Sounding comparisons Home Page Title Page JJ II J I Page 10 of 19 Go Back Full Screen Close Quit Home Page Title Page JJ II J I Page 11 of 19 Go Back Full Screen Close Quit Home Page Title Page JJ II J I Page 12 of 19 Go Back Full Screen Close Quit Sounding v.s. model as a function of temperature Home Page Title Page JJ II J I Page 13 of 19 Go Back Full Screen Close Quit Data for SCM Home Page Title Page JJ II J I Page 14 of 19 Go Back Full Screen Close Quit Data for SCM • Sounding data as initial profile • HIRLAM experiment data as initial profile Home Page Title Page JJ II J I Page 14 of 19 Go Back Full Screen Close Quit • Observed fluxes etc as lower boundary condition Data for SCM • Sounding data as initial profile • HIRLAM experiment data as initial profile Home Page • Observed fluxes etc as lower boundary condition Tools to pick HIRLAM profile in ASCII Title Page JJ II J I Page 14 of 19 Go Back Full Screen Close Quit Tools to write ASCII input based on HIRLAM profile Tools to handle sounding data Mast comparisons Home Page Title Page JJ II J I Page 15 of 19 Go Back Full Screen Close Quit Home Page Title Page JJ II J I Page 16 of 19 Go Back Full Screen Close Quit How to make the sounding and mast comparison pictures? Raw material Home Page Title Page JJ II J I Page 17 of 19 Go Back Full Screen Close Quit How to make the sounding and mast comparison pictures? Raw material • Sodankylä soundings - ASCII tables Home Page • Mast profiles: T, RH, wind - raw observation ASCII files Title Page JJ II • Mast fluxes: senf, latf, momf, SWdn, SWup, LWup - raw observation ASCII files • (LWdown separate measurements J I - raw observation ASCII files) • HIRLAM analyses and forecast Page 17 of 19 - GRIB files, possibly subareas/ASCII profiles Go Back Full Screen Close Quit Home Page Title Page JJ II J I Page 18 of 19 Go Back Full Screen Close Quit Tools • Main shell scripts RunSounding, RunMast Home Page • Fortran programmes interpol.f90 and sodaconv.f90 • ( Tools to pick subareas and profiles from HIRLAM ) Title Page JJ II J I Page 18 of 19 Go Back Full Screen Close Quit • Grads scripts for drawing Tools • Main shell scripts RunSounding, RunMast Home Page • Fortran programmes interpol.f90 and sodaconv.f90 • ( Tools to pick subareas and profiles from HIRLAM ) Title Page JJ II • Grads scripts for drawing Output • Readable converted and interpolated ASCII data J I - for drawing, reading, calculations • Grads pictures Page 18 of 19 Go Back Full Screen Close Quit Further possibilities Home Page Title Page JJ II J I Page 19 of 19 Go Back Full Screen Close Quit Further possibilities • Surface energy balance studies • Radiation balance and clouds Home Page • Comparison of snow and soil temperatures • High temporal resolution AWS data Title Page JJ II • Mast data for surface layer studies, e.g.: stability dependency of roughness definition of PBL height based on fluxes J I • High resolution sounding data for PBL studies • Combination of FMI ARC data with Luosto radar Page 19 of 19 Go Back Full Screen Close Quit Further possibilities • Surface energy balance studies • Radiation balance and clouds Home Page • Comparison of snow and soil temperatures • High temporal resolution AWS data Title Page JJ II • Mast data for surface layer studies, e.g.: stability dependency of roughness definition of PBL height based on fluxes J I • High resolution sounding data for PBL studies • Combination of FMI ARC data with Luosto radar Page 19 of 19 Need for a Sodankylä Data and Tool Base ! 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