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Then the main circulation of the atmosphere, secondary circulation (monsoon, air masses, front, cyclone), local circulation (sea breeze, land breeze, mountain wind, valley wind), violent weather, typhoon, agricultural meteorological disaster, process of microclimate formation on farm land, climate of Taiwan and China will be explained chapter by chapter.

本课程先介绍各种气象要素(如日射,日照,温度,气压,风,云,雾,降水,蒸发等),其次对於大气主环流,次环流,局部环流(海风,陆风,山风,谷风),剧烈天气,台风,农业气象灾害,农地微气候形成过程,台湾及中国之气候加以逐章阐述。

Sensible and latent heat fluxes from the plateau surface are of great importance in the Asian monsoon system.

高原地表的感热和潜热通量在亚洲季风系统中有很重要的作用。

Mimimum area of 3000m2 in monsoon evergreen broadleaved forest was suggested according to species-area relationship of Logarithmic at this scale.

表明样地植物群落可能处于非平衡状态,栖息地异质性对群落物种多样性影响不大。

Both observations and model research attest local monsoon in Luzon Strait is not the critical dynamics factor to Kuroshio loop.

观测和数值模式研究都发现吕宋海峡局地季风风场在吕宋海峡黑潮流套的形成中不起决定作用。

The impacts of SSTA on the onset of SCS summer monsoon can be achieved by restricting zonal and meridional cell.

海温异常对南海夏季风的影响可以通过制约纬圈和经圈环流而达到。

The monsoon circulation can be decomposed into the zonal circulation and the meridional circulation.

季风环流可以分解为经向环流和纬向环流。

In summary, moisture variability in ACA and northern Tibetan Plateau has showed major difference from monsoon evolution on various timescales in the Holocene. It is thus proposed that there is a westerlydominated climate model in midlatitude Asia during the modern interglacial period.

据此我们提出,亚洲中部西风带控制区在现代间冰期从数千年到年代际的各个时间尺度上均存在不同于季风区的湿度变化模式,称之为现代间冰期气候变化的西风模式。

The midlatitude Asian continent can be roughly divided into two distinct climatic regions: the humid easternsouthern part of Asia mainly controlled by monsoon circulation and inland arid Asia (including the coldarid northern Tibetan Plateau) in the western part dominated by the midlatitude westerlies.

中纬度亚洲地区存在主要受季风环流影响的东南部湿润地区和主要受西风环流控制的内陆干旱区(包括青藏高原北部高寒干旱区,简称西风区)。

Research has shown that deep tillage with a moldboard plough in the monsoon season can overcome this problem.

研究表明,用有壁犁在季风季节深耕可解决这一问题。

This benefit was obtained by using a moldboard plough to prepare the soil in the pre-monsoon period in June.

这种好处由6月季风季节之前用有壁犁整地翻耕得到,然后土地在季风季节休闲直到11月种麦。1983年有壁犁耕翻(30厘米深)的效果与深松犁(45厘米深)、凿形犁(25厘米深)和农民的播种机(10厘米深)加以比较,只有有壁犁的效果明显好于播种机(Khan等,1986)(图1)图1。

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