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The relative water content in tilth layer could still be kept over 60% in the continuous 11.2~47.1d without precipitation after a precipitation made the relative water content in tilth layer got over 80%.

使耕层相对含水量达到80%以上的一次降水过后,连续11.2~47.1 d无降水,耕层相对含水量尚可维持在60%以上。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.the results show that The relativity of Precipitation and macroeconomics topographer is good in time scale.

研究发现,在时间尺度上,降水与宏观地形因素有良好的相关性;在空间尺度上,降水与海拔高度有较好的相关性。

On the basis of this, the role of condensational latent heat release is studied emphatically and a conceptual model of mutual positive feedback mechanism between the growing of meso-α-scale cyclone on MeiYu front and its accompanying intensifying precipitation due to stable condensational heating is posed, i. e. condensational heating generates negative allobar, divergent wind kinetic energy promotes meso-α-scale cyclone growing, and simultaneously, updraft motion is also reinforced, precipitation continues intensifying.

并在此基础上着重对凝结潜热释放的作用进行了研究,提出了一种由稳定性凝结加热作用而导致的梅雨锋上α中尺度气旋发展与降水增强之间相互正反馈机制的概念模型即凝结加热可以产生负变压,变压风动能通过转变为旋转风动能促进中气旋发展,同时上升运动得到增强,降水增幅。

Before establishment of SEASM, if southerly moisture transportation through the meridional moisture channel is very strong, the convection activity becomes more active around the IndochinaPeninsula and the rainy season begins earlier in Yunnan corresponsively.

当这一水汽通道中南风水汽输送在季风建立前异常偏强时,相应地中南半岛附近的对流也增强,对应着云南的雨季开始偏早,初夏降水偏多,反之则初夏降水偏少。

The achievements have been made such as the records revealed by climatic proxies,show the instability of the East Asian monsoon climates and warm phases; a short term warm event and a cold reversal before the termination of the penultimate; cold Henrich fingerprint in lake sediments of the Tibetan Plateau; the instability of oxygen isotope stage 5e and Holocene climates; the spatial variability of East Asian monsoon precipitation during the Younger Dryas and the increased variability of the recent centennial East Asian monsoon precipitation.

发现在倒数第二次冰期结束前一次持续时间非常短暂的气候温暖事件和寒冷回返事件,发现我国青藏高原湖相沉积物中保存了Henrich寒冷事件的烙印、氧同位素阶段5e和全新世的不稳定性,Yonger Dryas东亚季风降水的空间变率以及最近100年东亚季风降水变率增大等。

Then we elementarily find that the assimilation of the real-time data in high layer and surface i...

初步的结果显示,同化高空和地面实况资料后对模式的初始场有明显的改进、对暴雨过程的降水落区和强度有不同程度的正反馈,更接近实况的降水

This method improves the computational accuracy, embodies the precipitation changes with topographty and the distributive incontinuity of precipitation, and solves the problem of the precision of the spatial interpolation of precipitation under complicated topographty condition.

该方法提高了计算的准确性,体现了降水随地形的变化以及在空间分布上的不连续性,有效解决了复杂地形条件下降水空间插值精度不高的问题。

Summer monsoon precipitation in 1998 is simulated with different soil temperature and solar short wave radiation parameterization schemes using the improved p-σ nine level hybrid coordinate model.It is found that the improved soil temperature calculation method together with Lacis and Hansen short wave radiation parameterization has a good simulation for precipitation.

利用改进后的p-σ 9层混合坐标系模式,采用不同的土壤温度与太阳短波辐射参数化方案,对1998年夏季风降水进行模拟,发现改进的土壤温度计算法和改进的Lacis和Hansen 短波辐射参数化方法相结合能较好地模拟降水

The effects of meterological factors on the growth quantity of Larix leptolepis were different analyzed by step-by-step regression and correlation coefficient analysis.

采用多元逐步回归方法和关联分析法得出的气候因素对日本落叶松生长量影响的排序次序是有差异的,但基本结论具有共同性:影响重要的气象因子不管是上年夏季的降水量,还是上年9~10月相对湿度都与降水有关,表明该地区日本落叶松生长量与降水状况和春季地温有密切关系。

When the spatial pattern is meridionally anti-symmetric, in the north-warm/south-cold years, an anticyclonic anomaly circulation exists over the warm pool at 850hPa, the easterly near 15°N and the westerly near the equator are greatly strengthened, while the center of the 200 hPa anticyclonic circulation moves to the East Asia, and the Hadley circulation is affected evidently, so the summer rainfall may be above normal in the middle and lower reaches of the Yangtze River, and vice versa.

当SSTA为南北反对称分布时,北暖南冷年850hPa暖池区上空为一反气旋偏差环流,15°N附近东风气流和赤道附近西风气流增强,200hPa反气旋偏差环流中心移到东亚大陆上空,长江中下游地区为上升气流,降水明显增多,华北地区为下沉气流,降水减少;冷异常年则相反。

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