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Danish Meteorological Institute - DMI

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<strong>Danish</strong> <strong>Meteorological</strong> <strong>Institute</strong><br />

<strong>Danish</strong> Climate Centre Report 07-03<br />

ECA Daily Normalized Prec. 1961−1990<br />

NCEP Daily Normalized Prec. 1961−1990<br />

ERA 40 Daily Normalized Prec. 1961−1990<br />

10 −1<br />

10 −2<br />

10 −3<br />

10 −4<br />

10 −1<br />

10 −2<br />

10 −3<br />

10 −4<br />

10 −1<br />

10 −2<br />

10 −3<br />

10 −4<br />

Wet day fraction: 30.8%<br />

Wet day precipitation average: 6.15 mm<br />

All day precipitation average: 1.89 mm<br />

R1 BI<br />

R2 IP<br />

R3 FR<br />

R4 ME<br />

R5 SC<br />

R6 AL<br />

R7 MD<br />

R8 EA<br />

0 40 80 120 160 200 240 280<br />

Bin [mm day −1 ]<br />

Wet day fraction: 39.5%<br />

Wet day precipitation average: 5.70 mm<br />

All day precipitation average: 2.25 mm<br />

R1 BI<br />

R2 IP<br />

R3 FR<br />

R4 ME<br />

R5 SC<br />

R6 AL<br />

R7 MD<br />

R8 EA<br />

0 40 80 120 160 200 240 280<br />

Bin [mm day −1 ]<br />

Wet day fraction: 36.3%<br />

Wet day precipitation average: 4.03 mm<br />

All day precipitation average: 1.46 mm<br />

R1 BI<br />

R2 IP<br />

R3 FR<br />

R4 ME<br />

R5 SC<br />

R6 AL<br />

R7 MD<br />

R8 EA<br />

0 40 80 120 160 200 240 280<br />

Bin [mm day −1 ]<br />

Figure 4.3: Normalised precipitation distribution for ERA40 (bottom panel) and NCEP/NCAR<br />

(middle panel) reanalysis data together with ECA observational data (top panel) for the period<br />

1961-1990 for the eight European sub-regions.<br />

To compare the climate change in different climatological areas, nine European sub-regions are<br />

defined as given by the boxes in Figure 4.2 (see Figure 4 in Christensen and Christensen (2007) and<br />

Table 4.2). After removing data for all ocean grid points, daily precipitation for each model and for<br />

each of the European PRUDENCE sub-regions were extracted. Because we want to be able to<br />

compare the model data to observations, we define dry days as days with precipitation less than<br />

1 mm, and remove these from the precipitation data. The observations of weak intensity<br />

precipitation is not always reliable, and it has earlier been found that low intensity precipitation does<br />

not contribute significantly to the total amount of precipitation (Dai, 2001). PDFs were then<br />

calculated from the remaining daily data for each region and model through three steps. First the<br />

data were binned into bins of 1 mm width starting at 1 mm. Then each bin’s frequency of events was<br />

multiplied by the bin average to get the precipitation amount. The binned data were finally<br />

www.dmi.dk/dmi/dkc07-03 page 9 of 43

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