SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 1/8 Long duration validation.

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Presentation transcript:

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 1/8 Long duration validation of PGE11

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 2/8 Long duration validation of PGE11 Plan  Research activity (visiting scientist: Oleksiy Kryvobok)  Use of other PGEs and HRVis for RDT improvement  Tuning PGE11 satellite-based discrimination using SEVIRI data  Long duration validation of RDT v1.2 release  Perspectives

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 3/8 Long duration validation of PGE11 Research activity (Visiting Scientist)  Use PGE output : PGE06 (TPW), PGE07 (LPW), PGE08 (SAI), PGE12 (AMA)  To improve discrimination skill of RDT with stability and water vapor information As a mask in order to focus on the interest areas Or as additional discrimination parameters  Monitoring characteristics of young convective clouds using HRVIS data  To improve the precocity of detection (Sub-pixel detection)  To correct for partial pixel filling in cloud cooling rate estimation  Results: Much work needed before implementation  PGEs 06, 07, 09 and 12 An overview of PGEs qualities, version V.0.1, stop the study  Sub-pixel approach Major improvements are necessary on reflectance processing  Clear sky reflectance map at HRVIS resolution and/or  More accurate 3-D radiative transfer for estimation of cloudy reflectance (small and edge cloud)

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 4/8 Long duration validation of PGE11 Tuning PGE11 Satellite-Based Discrimination using SEVIRI data  Reminder : Principle of the satellite-based discrimination  Multi-level segmentation (3 levels)  Best discrimination parameter chosen independently for each final class  Initial results  Similar to Rapid Scan for low cost ratio (cost ratio = False Detection unit cost / Non Detection unit cost)  Poorer than results for GOES data (despite closeness in spatial resolution) Interpretation: Cells first detected at cold temperature are too numerous with MSG  Adaptation of detection method to MSG data  Minimum cloud tower height  T tower = 6°C Improves matching with lightning flashes Reduce number of cells first detected at cold temperature  Electrical filter: focus on cell with strong electrical activity Discard non convective cloud labelled as convective due to lack of accuracy of lightning flashes matching

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 5/8 Long duration validation of PGE11 Long Duration Validation  Overall quality of discrimination  Overdiscrimination on the learning data set  Variability of the discrimination skill with the period of year (poor for cold period)  Link between electrical activity and discrimination skill  Precocity of the discrimination  Half of convective systems are diagnosed as convective before their strong electrical activity occurrence.  Around 80% of clouds cells are diagnosed as convective no later than 30 minutes after the first flash occurrence  Conclusion  The quality of discrimination during summer period is better with V1.2 and MSG data than with GOES  Cold periods show low probability of detection (POD).  It is recommended to use RDT with lightning flashes and filters of convective systems Improve score of POD (necessary for cold period) Remove long duration trajectories without interest

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 6/8 Long duration validation of PGE11 Perspectives (short and medium term)  Improve population definition  Better separate developing thunderstorm from mature system To build an homogenous population of convective cloud To focus on RDT main purpose (developping TS)  Examine various ground truth For improving quality of the learning sample Data independent from satellite: lack of accuracy in matching method generates noise in learning data set Satellite data (e.g. cooling rate): lack of direct link with sensible weather provide an efficient tuning on area without ground observation network  Change the discrimination method  Reduce final classes number for removing overdiscrimination Classify mainly using minimal temperature reached  Discard multilevel segmentation and build discrimination on principal component and factorial analysis Introduce additional promising discrimination parameters Better combine discrimination parameters

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 7/8 Long duration validation of PGE11 Long term perspectives (not all will be covered)  Better use Cloud Mask for early detection  Reconsider using other PGEs as input for better discrimination,  Or rather consider convection-related diagnostic from mesoscale assimilation at high refresh rate (< 3h) : boundary layer moisture supply, middle-level dryness, CAPE from most unstable level, DCAPE, low-level convergence, upper-level forcing  Improve precocity if Cloud Mask improved to HiRes  Test RDT algorithm for Upper-Level-Dynamic monitoring : tracking dry cores in WV, high value cores in O3 product

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 8/8 Long duration validation of PGE11 Thanks for your attention Time for comments, requests, discussion …

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 9/8 Long duration validation of PGE11 Track Duration (22 classes): 15minutes to >450 minutes Minimum Temperature reached (7 classes): 0°C to  50°C Area at threshold brightness: 0 to  1000 Mean Peripheral gradient 95 percentile Peripheral gradient Minimum Temperature- based cooling rates Mean Temperature- based cooling rates Initial Temperature- based cooling rates The best discrimination parameter

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 10/8 Long duration validation of PGE11 Adaptation of detection method with MSG data:  T tower = 6°C Characteristics of convective trajectories start. MSG(left) and GOES (right) cases :  T tower = 3°C Lightning flashes pairing with MSG  T tower = 3°C (left) and  T tower = 6°C (right)

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 11/8 Long duration validation of PGE11

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 12/8 Long duration validation of PGE11

SAF - Nowcasting Product Assessment Review Worshop (Madrid 17 – 18 – 19 0ctober 2005 Yann Guillou Météo-France (DPR) Page 13/8 Long duration validation of PGE11 Highest vertical development for defining tracked cells and attempting discrimination, either : fixed temperature (parameter T cold ) ~ –30°C, tropopause related temperature Cloud Type « high & thick cloud » diagnostic brightness difference with water vapor channel Bubblings are depicted, but not individually tracked