5 , there is extremely difference of the locally climatic meridional circulations , as well as there is obviously different seasonal changes
2.
6 , the zonal difference and seasonal change of locally anomalous meridional circulation are great . the meridional circulation anomaly over the pacific ocean relates closely with the el nino / la nina events
3.
In terms of the real data , the mass stream function is calculated by two methods , results indicate that both methods fit well with the need for calculating the climate and its anomaly of the mean meridional circulation
4.
The seasonal variation of the mean meridional circulation and the double - level structure of the hadley circulation are analyzed by the two methods . the paper also studies the zonal difference of the anomalous meridional circulation and the impacts of el nino / la nina events on the local meridional circulation anomaly . conclusions are drawn as follows : 1 , the hadley circulations in both hemisphere and the position of their joint uprising branch move wholly with the heat equation , with most north in july and most south in january
5.
The main factors affecting the precipitation in the first stage of rainy season in fujian province are pacific sst in preceding june , the western pacific subtropical high area index in preceding may , the asia polar vortex area index in preceding september , the eurasian meridional circulation index in preceding april to june , the 500hpa height in northwest asia in preceding spring . the main factors affecting the precipitation in the second stage of rainy season in fujian province are pacific sst in preceding july and august , the northern hemisphere polar vortex area index in january in same term , the pacific polar vortex intensity index in preceding september , the 500hpa height in south europe in preceding summer
6.
All these results confirm the important of wind in meridional circulation and heat transport . based on mom2 model , a rectangular basin model with ideal w ind stress and other ideal conditions is designed to study the main processes and dynamical mechanism in setting the depth of cross - equator flow . the effects of horizontal diffusivity , seasonal variations of
7.
4 ) during the meiyu , the precipitation in middle and lower reaches of yangtze river has the relationship with southern hemisphere circulation in early april and may . when the meridional circulation in middle and high latitude of south pacific in april and may is rather obvious and the south pole eddy is rather strong , the precipitation in middle and lower reaches of yangtze river may be bigger than ever
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