Presentation is loading. Please wait.

Presentation is loading. Please wait.

Verification of COSMO-LEPS and coupling with a hydrologic model

Similar presentations


Presentation on theme: "Verification of COSMO-LEPS and coupling with a hydrologic model"— Presentation transcript:

1 Verification of COSMO-LEPS and coupling with a hydrologic model
André Walser1) and Simon Jaun2) 1)MeteoSwiss 2)Institute for Atmospheric and Climate Science, ETH

2 Overview Part 1: Status report of Task 4.2 of PP Interpretation: Use of COSMO-LEPS in hydrologic models Part 2: COSMO-LEPS verification against SYNOP messages

3 Model chain ECMWF EPS  COSMO-LEPS  PREVAH Global ensembles ECMWF EPS
Downscaling with COSMO-LEPS PREVAH as hydrologic model Fig. M. Verbunt ECMWF EPS  COSMO-LEPS  PREVAH Uncertainties in the hydrologic model/processes not considered

4 Data flow for MAP D-PHASE
Main partner WSL: Swiss Federal Institute for Forest, Snow and Landscape Research

5 “MAP D-PHASE Catchments”

6 Product delivered for D-PHASE VP

7 Comparison different models
August 2007 event Linth at Mollis, initial time

8 Comparison different models
August 2007 event Linth at Mollis, initial time

9 Comparison different models
August 2007 event Linth at Mollis, initial time

10 Verification August 2005 Event
Probability to exceed 10y event > 10 y event Jaun et al.: A probabilistic view on the August 2005 floods in the upper Rhine catchment, to be submitted

11 Conclusions & Outlook Operational ensemble runoff forecast are established for MAP D-PHASE Seems to provide reliable information about the forecast uncertainty and early indication for flood events  Verification over an extended period needed

12 Part II Most recent COSMO-LEPS Verification Results:
12-h sum of precipitation from SYNOP messages, COSMO-LEPS domain Brier Skill Score for 1, 5, 10, 25 mm Climatological event frequency estimated from data from

13 BSS for precipitation > 1 mm/12h
night-time precipitation daytime precipitation No skill lead-time

14 BSS for precipitation > 5 mm/12h
lead-time

15 BSS for precipitation > 10 mm/12h
lead-time

16 BSS for precipitation > 25 mm/12h
lead-time

17 Large spatial variability of the skill
BSS for precipitation > 1 mm/12h MAM 2006 (+42h)

18 Station Sion: BSS for precipitation > 1 mm/12h
lead-time

19 “No skill station”: Sion
12-h precipitation sum > 1mm MAM 2006:

20 Station Sion: BSS for postprocessed precipitation > 1 mm/12h
Very simple post-processing: p’=0.5p lead-time

21 Conclusions For low precipitation thresholds skill up to forecast day 5 for all seasons No skill for high threshold 25mm/12h for all seasons In spring and summer higher skill for night-time precipitation than for daytime High spatial variability There is potential to improve precip. forecast in Alpine region with post-processing  sophisticated method Talk/Poster of F. Fundel


Download ppt "Verification of COSMO-LEPS and coupling with a hydrologic model"

Similar presentations


Ads by Google