Characteristics of Diurnal Variations in Convection and Precipitation over the Southern Tibetan Plateau during Summer
被引:91
作者:
Fujinami, Hatsuki
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机构:
Nagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, Japan
Japan Sci & Technol Agcy, Kawaguchi, Saitama, JapanNagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, Japan
Fujinami, Hatsuki
[1
,2
]
Nomura, Shigeyuki
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机构:
Japan Weather Assoc, Tokyo, JapanNagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, Japan
Nomura, Shigeyuki
[3
]
Yasunari, Tetsuzo
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机构:
Nagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, JapanNagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, Japan
Yasunari, Tetsuzo
[1
]
机构:
[1] Nagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, Japan
[2] Japan Sci & Technol Agcy, Kawaguchi, Saitama, Japan
[3] Japan Weather Assoc, Tokyo, Japan
来源:
SOLA
|
2005年
/
1卷
关键词:
D O I:
10.2151/sola.2005-014
中图分类号:
P4 [大气科学(气象学)];
学科分类号:
0706 ;
070601 ;
摘要:
This study investigated diurnal cycles in convection and precipitation over the complex mountain-valley terrain of the southern Tibetan Plateau (TP) during the mature phase of the summer monsoon. Cloud-cover frequency (CCF) for high cloud increased after 13 LST (07 UTC) over the mountain ranges along 28.5 degrees N and 30.2 degrees N, reaching a maximum near 18 LST (12 UTC). Areas of high CCF subsequently moved towards the valley area along 29.3 degrees N; relatively high CCF persisted there until early morning. Tropical Rainfall Measuring Mission (TRMM) PR data show a nearly identical variation in rainfall frequency. Formation and development of convective-type clouds and phase differences in the diurnal cycle were strongly affected by TP topography. Possible mechanisms for convective enhancement over the southern TP are also discussed.
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页码:49 / 52
页数:4
相关论文
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[1]
Awaka J, 1997, INT GEOSCI REMOTE SE, P1633, DOI 10.1109/IGARSS.1997.608993