mjo
- 网络热带大气季节内振荡;季内震荡
mjo-
The IOD has significant influences on the MJO intensity in boreal summer .
IOD对北半球夏季季节内振荡强度存在显著影响。
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In advance , or to the east , of the MJO enhanced activity , winds aloft are westerly .
而在MJO的后面，或者是西面，高空风是向东的，并且降水增强。
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It is shown that the rainfall patterns change from enhanced to suppressed in South China at intraseasonal timescales as the MJO moves from the Indian Ocean to the western Pacific .
结果表明，随着MJO的活跃中心从印度洋进入西太平洋，华南地区的降水由偏多转为偏少。
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It is found that the MJO could also be excited by the only stratiform heating . Meanwhile , the combined role of both cumulus and stratiform heating can enhance the MJO .
如果考虑两者共同的作用，相比于仅考虑积云的情况，能够在很大程度上扩大加热强度的取值范围，从而使热带大气更容易发生MJO。