NHM simulation

Dear all:

Please find out figures attached herewith.

They are results numerical simulation based on GSM 0.5deg (upper left),
NHM 10km (upper right), and NHM 2km (lower left) for 18Z 23 December
(01LT 24 December). MIA-XDR CAPPI(2km) at the corresponding time (01LT
24 December) is shown in the lower right panel, too.

The result of GSM simulation looks successfully showed a large scale
disturbance approaching Sumatera which was also observed by GsMAP in my
last post. Whereas, those calculated by NHM for both 10km and 2km didn't
show any precipitation at all in those domain though the MIA-XDR
observed rain echoes broadly expanded around Padang.

It looks curious that precipitation calculated by HNM
---
http://www.jamstec.go.jp/iorgc/harimau/simulation4/index_s.html
http://www.jamstec.go.jp/iorgc/harimau/simulation4/index_v.html
---
cannot enter the Mentawai Strait though GsMAP, GSM, and MIA-XDR showed
large scale precipitation over the strait. Huuuuum.

~morishu

--
森　修一　Shuichi MORI
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海洋研究開発機構(JAMSTEC)/地球環境変動領域(RIGC)
熱帯気候変動研究プログラム/海大陸気候研究チーム
〒237-0061　神奈川県横須賀市夏島町２−１５
Tel： (046)867-9256（直通） Ｆax：(046)867-9255
e-mail：morishu@jamstec.go.jp
HP：http://www.jamstec.go.jp/seika/pub-j/res/ress/morishu/
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