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In order to simplify the simulation,an idealized slope is used. Simulated results with and without orographic effects are compared and analyzed.

结果发现:平坦地面模拟的回波强度、最大降水强度和累积降水都与实况有相当的差距。

Simulations of echo intensity,maximum precipitation without orographic effects are much weaker than observations;and they are much improved and closer to the reality after consideration of orographic effects.

理想地形的对流过程虽然不能模拟出对流群中多单体的生消过程,但最大降水强度和累积降水都比平坦地面的大,更接近实测结果。

From overburden layer s,semipervious layers above depression-cone level drainage consolidation,porous media(geo-formation) compression and water compression,the ground settlement mechanism is analysed during foundation pit dewatering.

从降落漏斗水位以上覆盖层、弱透水层的排水固结过程到多孔介质的压缩、水的压缩三方面分析了深井降水引起地面沉降的机理,得出降水引起地面沉降的压缩层厚度主要为降落漏斗水位以上降深范围内的覆盖层和弱透水层厚度的结论。

he mixture of convective and stratiform clouds is an important precipitation system and also a major object for weather modification studies.

积层混合云是我国的主要降水云系,也是人工影响天气的主要作业对象,从云降水物理的角度来研究云系的形成和发展维系具有重要的意义。

The average rainfall rate of stratiform rain and convective rain has a considerable increase with the intensification of typhoon.

层状云降水和对流性降水的平均雨强均随台风强度加强有较大的增幅。

Results show that stratiform rain occupies more area and contributes more rainfall to the total than convective rain does at the 3 times.

结果表明:三个时次层状云降水在象素数量上及对总降水量的贡献上均比对流性降水大。

Based on observations in northern China, the microphysical process of precipitation formation and the role of ice crystal playing in those processes for three kinds of typical stratiform clouds are analyzed using rain category model.

通过建立层状云雨滴的分档模式,对中国北方常见的三类典型层状云降水形成的微物理过程以及冰粒子在降水形成中的作用进行了数值模拟。

Precipitation of convection will diminish, while that of stratiform clouds will maintain, so the mixture clouds can bring stronger precipitation in a large area.

对流云的降水量不断减小,而层状云的降水不断维持,带来了大面积持续时间很长的降水

The results indicate that the model has certain prediction ability for stratiform precipitation.

利用MM5中增加的双参数显式云物理方案模拟了西北地区一次层状云降水过程,模拟结果显示对小雨的预报评分较高,对中雨以上评分低而且位置有一定偏差,即对层状云降水模拟效果较好。

Its generated mechanism is that poten-tial instability is touched off by the convergent and thermodynamics near theground in the favourable weather controlled by trough of high altitude.Thatmakes effective potential energy release greatly, forming strong convection.Meanwhile, intensive storms with convection are occurred because of the plentyof moisture flowing into the basin and favourable topograph...

吐鲁番盆地的大降水具有降水时间短、强度大、范围小,雨量集中等特点,它的发生机制是在高空低槽控制的有利天气形势下,地面动力辐合作用和热力作用触发了大气中的潜在不稳定结构,使得大气有效位能大量释放,形成强烈的对流;同时,有充沛的水汽输入盆地,在有利地形条件下,产生强对流暴雨。

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