Department of Atmospheric Science, Chinese Culture University, Taipei, Taiwan

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The abrupt increase of winter rainfalls in early 1980s in Northern Taiwan and the weakening of the East Asian winter monsoon. Department of Atmospheric Science, Chinese Culture University, Taipei, Taiwan Advisor: Chih-wen Hung Student: Pei-ken Kao. ?. (shaded). (contour). mm. - PowerPoint PPT Presentation

Transcript of Department of Atmospheric Science, Chinese Culture University, Taipei, Taiwan

Department of Atmospheric Science, Chinese Culture University, Taipei, Taiwan

Advisor: Chih-wen HungStudent: Pei-ken Kao

?

mm

(shaded) (contour)

Gray line: DJF, V<0, interannual variationof wind speed

Black line: DJF,interannual variationof wind speed

Thickness line:11 years running mean

surface wind

winter rainfall

interannual variation

Taipei DJF rain days >=30mm/day rain days Total rain days

Black bars: decadal variation Gray bars: interannual variation

plain stations hill and coastal stations

winter rainfall

interannual variation

Red box:plain stations green box:

hill or coast stations

northeasterly monsoonal wind rainfall pattern frontal rainfall pattern

1997-2005 DJF

1990~1961P

P

hill and coastal stations

plainstations

latterperiod

early period

E: El NinoL: La Nina

mm

latter minus early period

°C

latter minus early period

kg/g

latter minus early period

conceptual model

END

Data8 CWB conventional surface stations and 377

ARMTS daily data(洪, 2007; Hung, 2008; Chen et al., 1999).

JMA surface weather map, 1997-2005.ERA40 re-analysis data (Uppala et al., 2005),

2.5°×2.5°, 1958-2003, monthly data.HadISST, 1.0°×1.0°, 1870-2007, monthly

data(Rayner et al., 2003). CRU rainfall data, 0.5°×0.5°, 1901-2002,

monthly data(Mitchell and Jones, 2005).

Only front

V > 0 + front

V > 0 + no front

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