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163<br />

summer particularly in the Pacific side, indicating that not<br />

only synoptic scale behavior but also finer scale feature may<br />

take an important role by, such as, localized disturbances.<br />

The wind fields are similarly reproduced as air temperature<br />

(figure not shown).<br />

In contrast, precipitation is not reproduced as well as<br />

temperature and wind by the JP10, with averaged correlation<br />

coefficient of 0.3~0.7. Figure 4 shows the same but for<br />

precipitation, with significantly larger number of the<br />

observatories. Interestingly, the seasonality of the scores is<br />

more apparent in precipitation, i.e., summer and Pacific side<br />

precipitation is more difficult, due to sub-grid scale<br />

convective activity and also low quantitative reproducibility<br />

of typhoon and Baiu systems by the model and analysis.<br />

Hazardous snow events<br />

In Figure 5, monthly mean snow water equivalent (SWE)<br />

amount is averaged over all Honshu Island. According to the<br />

hazard record in Japan reported by JMA, there were deadly<br />

severe events in the winters of 1960-61, 62-63, 73-74, 76-77,<br />

80-81, 83-86, and 2005-06. These hazardous events are<br />

captured in this preliminary analysis of JP10 to some extent.<br />

Note that there is no official record before 1960.<br />

Figure 4. Distributions of correlation coefficients of<br />

monthly-long daily precipitation in four seasons.<br />

Number of the observation sites and arithmetic<br />

average of the coefficients of all sites are also shown.<br />

Precipitation<br />

Precip [mm/day]<br />

16<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

Annual<br />

Feb<br />

Apr<br />

Jun<br />

Aug<br />

16<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

Kyushu 2<br />

Kant o 0<br />

DecAll<br />

Surface Air Temperature<br />

Oct<br />

Annual<br />

Feb<br />

Apr<br />

Jun<br />

Aug<br />

Oct<br />

Kyushu<br />

Kant o<br />

DecAll<br />

All<br />

N- Hokkaido<br />

S- Hokkaido<br />

Tohoku<br />

Kant o<br />

Chubu<br />

Kinki<br />

Shikoku<br />

Kyushu<br />

Okinawa<br />

Temperature [C]<br />

30<br />

25<br />

20<br />

15<br />

10<br />

5<br />

0<br />

-5<br />

-10<br />

Annual<br />

Feb<br />

Apr<br />

Jun<br />

Aug<br />

Oct<br />

AMeDAS<br />

DecAll<br />

30<br />

25<br />

20<br />

15<br />

10<br />

5<br />

0<br />

Kyushu-5<br />

Kant o -10<br />

Annual<br />

Feb<br />

Apr<br />

Jun<br />

Aug<br />

Oct<br />

JP10<br />

DecAll<br />

Kyushu<br />

Kant o<br />

Figure 2. Monthly climatology of precipitation and<br />

surface air temperature averaged over the nine<br />

AMeDAS regions.<br />

Figure 5. Same as Figure 3, but for precipitation.<br />

1963/01<br />

1960/12-61/01<br />

74/01<br />

76/12-77/02<br />

80/12-81/01 85/01<br />

84/01-02 86/01<br />

No especially hazardous<br />

event observed<br />

2005/12<br />

Figure 3. Daily variations of surface wind<br />

components, air temperature, and precipitation of<br />

AMeDAS observation (blue) and JP10 (red) in<br />

Okinawa Island.<br />

Figure 6. JP10 monthly mean SWE averaged over<br />

all Honshu Island and historical hazardous snow<br />

events.

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