青藏高原感热加热对7月份大气环流和亚洲夏季风影响的数值试验

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青藏高原感热加热对7月份大气环流和亚洲夏季风影响的数值试验

胡江林, 朱乾根

文章导航 > 热带气象学报 > 1993 > (1): 78-84

胡江林, 朱乾根. 青藏高原感热加热对7月份大气环流和亚洲夏季风影响的数值试验[J]. 热带气象学报, 1993, (1): 78-84.

引用本文:

胡江林, 朱乾根. 青藏高原感热加热对7月份大气环流和亚洲夏季风影响的数值试验[J]. 热带气象学报, 1993, (1): 78-84.

Hu Jianglin, Zhu Qiangen. NUMERICAL EXPERIMENTS WITH EFFECTS OF SENSIBLE HEATING OF THE TIBETAN PLATEAU ON JULY ATMOSPHERIC GENERAL CIRCULATION AND SUMMER MONSOON IN ASIA[J]. Journal of Tropical Meteorology, 1993, (1): 78-84.

Citation:

Hu Jianglin, Zhu Qiangen. NUMERICAL EXPERIMENTS WITH EFFECTS OF SENSIBLE HEATING OF THE TIBETAN PLATEAU ON JULY ATMOSPHERIC GENERAL CIRCULATION AND SUMMER MONSOON IN ASIA[J]. Journal of Tropical Meteorology, 1993, (1): 78-84.

胡江林, 朱乾根. 青藏高原感热加热对7月份大气环流和亚洲夏季风影响的数值试验[J]. 热带气象学报, 1993, (1): 78-84.

引用本文:

胡江林, 朱乾根. 青藏高原感热加热对7月份大气环流和亚洲夏季风影响的数值试验[J]. 热带气象学报, 1993, (1): 78-84.

Hu Jianglin, Zhu Qiangen. NUMERICAL EXPERIMENTS WITH EFFECTS OF SENSIBLE HEATING OF THE TIBETAN PLATEAU ON JULY ATMOSPHERIC GENERAL CIRCULATION AND SUMMER MONSOON IN ASIA[J]. Journal of Tropical Meteorology, 1993, (1): 78-84.

Citation:

Hu Jianglin, Zhu Qiangen. NUMERICAL EXPERIMENTS WITH EFFECTS OF SENSIBLE HEATING OF THE TIBETAN PLATEAU ON JULY ATMOSPHERIC GENERAL CIRCULATION AND SUMMER MONSOON IN ASIA[J]. Journal of Tropical Meteorology, 1993, (1): 78-84.

青藏高原感热加热对7月份大气环流和亚洲夏季风影响的数值试验

胡江林¹,
朱乾根²

1.
武汉中心气象台, 武汉430074
2.
南京气象学院

基金项目: 气候动力学和气候预测理论研究项目

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出版历程
- 收稿日期: 1992-01-21
- 修回日期: 1992-07-27

NUMERICAL EXPERIMENTS WITH EFFECTS OF SENSIBLE HEATING OF THE TIBETAN PLATEAU ON JULY ATMOSPHERIC GENERAL CIRCULATION AND SUMMER MONSOON IN ASIA

Hu Jianglin¹,
Zhu Qiangen²

1.
Wuhan Meteorological Central Station, Wuhan, 430074
2.
Nanjing institute of Meteorology

摘要: 利用OSU的两层大气环流模式进行了有无青藏高原感热加热的对比数值试验,结果显示,青藏高原的非绝热加热对夏季大气环流的影响具有全球性,尤其对形成亚洲夏季风是必不可少的因子。去掉青藏高原感热加热,印度夏季风不存在,东亚副热带夏季风也被严重削弱,而南海—西太平洋热带夏季风活跃.
- 加热 /
- 环流 /
- 季风
Abstract: Comparative numerical experiments using OSU 2-level atmospheric general circulation model was done with/without the sensible heating of the Tibetan Plateau.It is shown that the diabatic heating there affects global general circulation in summer and particularly serves as an indispensible factor for the generation of Asian summer monsoon.If there is no such heating, there will be no more Indian summer monsoon and the subtropical East Asian summer monsoon will be significantly reduced, while the tropical South China Sea-West Pacific monsoon will be more active instead.
- Heating /
- General circulation /
- Monsoon

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HTML全文浏览量: 0
PDF下载量: 950
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