Title: The observational dataset most RT
1The observational dataset most RTs are waiting
for the WP5.1 daily high-resolution gridded
datasets
2Why?
- developing daily high-resolution gridded
observational datasets for Europe? - Evaluation of the ENSEMBLES simulation/prediction
system - Scenario construction
- Impact assessment
- Analysis of climate extremes
3Project partners
- KNMI, Lisette Klok Albert Klein Tank
- MeteoSwiss, Evelyn Zenklusen Michael Begert
- University of East Anglia, Malcolm Haylock Phil
Jones - University of Oxford, Nynke Hofstra Mark New
4Overview
- Variables and grid
- Stations and series
- Homogeneity
- Interpolation
- Data availability
5Variables and grid
- daily observations
- Tmax, Tmin, Tmean, RR, mslp, snow depth
- regular 0.25 degree grid and/or an equal area
grid - 1960-2004 or present
Domain
6Station locations
- Data sources
- ECAD
- EMULATE
- STARDEX
- GSN
- GHCN - daily
- MAP project
- MARS
2033 stations
7Series
- 1831 precipitation
- 1384 Tmax
- 1388 Tmin
- 1244 Tmean
- 317 mslp
- 180 snow depth
- quality controlled
- updated with SYNOP data
8Homogeneity results of the absolute test
following the method of Wijngaard et al., 2004
Homogeneous for periods gt 10 years absolute test Homogeneous for periods gt 40 years absolute test
Precipitation 78 35
Temperature 64 20
Air pressure 80 41
Snow depth 89 77
9Homogeneity results of the relative test
- Vera-QC (Begert et al., in preparation)
- Only complete series
- Period 1960-2000
- Number of break-points detected
- 0(?)
- 1(?)
- 2(?)
- 3(?)
- gt4(?)
- undefined (?)
10Homogeneity results of the relative test
Homogeneous for periods gt 10 years absolute test Homogeneous for periods gt 40 years absolute test Homogeneous over 1960 2000 relative test
Precipitation 78 35 32
Temperature 64 20 Tmean 23 Tmax 22 Tmin 12
Air pressure 80 41 9
Snow depth 89 77 -
11Homogeneity results of the relative test
C
C
C
Frequency distribution of shift dimensions for
temperature
12Interpolation methods
- Natural Neighbour Interpolation
- Angular Distance Weighting
- Thin Plate Splines
- Kriging
- Conditional Interpolation (only rainfall)
13Selection of best method and validation
- Cross validation
- Remove one station and interpolate to location of
that station - Compare results with observed values and
calculate skill scores (e.g. RMSE, LEPS) - Comparison with grids from high resolution
station series - E.g. UK 55 km rainfall, Switzerland rainfall and
Norway - Compare results with gridded datasets and
calculate skill scores
14Interpolation results
LEPS skill scores averaged across all methods
15Uncertainties in the interpolation results
- Still looking for appropriate method to determine
uncertainties - Will be in the form of uncertainty bands around
the interpolated value - Different uncertainty bands for every grid for
every day
16Data availability
- Gridded datasets (September 2007)
- http//www.ensembles-eu.org/ gtgt RT5 site
- Daily station series (if public!)
- http//eca.knmi.nl
17(No Transcript)