| 1. | Substantial increases are found in heavy precipitation events
极端降水事件确实是在增加。 |
| 2. | Climatic trends of different intensity heavy precipitation events concentration in china
中国强降水过程时空集中度气候趋势 |
| 3. | At a given location , heavy precipitation is usually pulsing at intervals of a few hours
雨带接近及经过的时候，风势疾劲，甚至会有狂风。 |
| 4. | At a given location , heavy precipitation is usually pulsing at intervals of a few hours
雨带接近及经过的时候，风势疾劲，甚至会有狂风。 |
| 5. | B ) . the scattering areas of the data above contracted for the heavy precipitation of more than 5mm / h
对于较强逐时降水，卫星资料在不同地区其范围有不同程度的收缩，具有更好的预报指示意义。 |
| 6. | The rainbands rotate in the same sense as the storm circulation and tend to sweep through an area one after another . at a given location , heavy precipitation is usually pulsing at intervals of a few hours
雨带随著风暴环流方向旋转，一条接著一条地扫过某一区域，受影响的地方有间歇性的大雨。 |
| 7. | ( 2 ) the increase of rainfall is closely associated with the increase of the disturbance wind which often can be found before the increase of rainfall , so the increase of the nonlinear subcritical symmetric instability can make the rainfall increase . ( 3 ) heavy precipitation often occurs between the south of axis of upper jet at 200hpa and the north of axis of low jet at 850hpa
( 3 )降水区和暴雨中心主要位于200hpa高空急流轴南侧和85ohpa低空急流轴北侧之间;非线性亚临界对称不稳定与高空急流关系密切，它可能触发高空急流核的形成;它与低空急流关系也很密切，它的出现可能引起低空急流的出现。 |
| 8. | In the final stage of the liangzhu culture , warm - humid climate , heavy precipitation and rising temperature led to sea - level rising , rivers running impeded , water areas large , in addition that the sites in the last stage of the liangzhu culture were mostly located in low - lying areas , which had liangzhu ancients suffered a unparalleledbig flood disaster resulting in the cultural decline
良渚文化末期，气候暖湿，温度增加，导致海平面上升，入海河流宣泄不畅，水域面积扩大，加之良渚文化晚期遗址多分布在地势低洼地区，因此良渚先民遭受了一场大洪水灾难，遂使良渚文化迅速衰落。 |
| 9. | Heavy precipitation often forms in the place between the source of high - disturbance wind field at 200hpa , especially of low - disturbance wind field at 850hpa . ( 2 ) the temporal and spatial scale about e - reflection index of nonlinear subcritical symmetric instability disturbance is 5 - 8hours and 200 - 300km respectively
非线性亚临界对称不稳定使线性对称稳定的大气变为不稳定。降水区和暴雨中心主要位于高层200hpa和中层500hpa扰动风场极大值南侧与低层850hpa扰动风场极大值北侧之间。 |
