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21.
区域暴雨增强数值预报业务系统及其预报效果分析 总被引:3,自引:7,他引:3
该文介绍了区域暴雨增强数值预业务系统的设计思想,主体结构及主要的关键技术,并总结了该系统业务试验的情况和效果。该系统以YH模式为基础,对其从坐标系、水平和垂直分辨率及物理过程等方面进行了改进,并结合实时资料处理系统,图形处理等形成了一个比较完整的数值预报业务体系。 相似文献
22.
对复杂地形条件下嵌套细网和数据模式进行了改进和发展,使之成为水平格距为50km,垂直分层为11层的高分辨率模式。同时对其物理过程如积云对流参数化、边界层物理等也进行了改进,并将该模式程序优化为能在计算机工作站和微机上进行业务运行的数值预报系统。 相似文献
23.
本文针对国家重点牵引力动力实验室的机车车辆整车滚动振动试验台的特点,探讨了一套适合试验台安装和养护的精密测量方法,实践证明,这套方法能满足试验台安装所需的精度要求。 相似文献
24.
利用矿泉水的水文地质、水化学特征、环境同位素水文地质学和国际WATCH水/岩平衡计算机程序等新理论、新方法,可以推算出雪峰矿泉水的形成年龄和补给与迳流条件,计算出水的循环深度,以及主要成分的迁移系数,从而有机地研究矿泉水的水文地球化学机制,探讨矿泉水形成的水文地球化学成因模式。 相似文献
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Antarctic krill (Euphasia superba Dana) is a key organism of the Antarctic marine ecosystem and a potential fishery resoure. Its ecology was the major biological
project in the First Chinese Antarctic Expedition (1985). Acoustic observations and IKMT tows were madecin waters north and
west of Antarctic Peninsula. Environmental factors were also observed. Analyses of the population structure, i.e. the sex
percentage distribution and other data obtained show that among the 3,640 individuals of determinable sex, only 38.1% were
males and that the larger the body length the smaller the percentage of males, for example, male percentage dropped to 8.3%
for size group >55 mm. The population's relations to environmental factors are also discussed.
Contribution No. 1711 from the Institute of Oceanology, Academia Sinica. 相似文献
28.
本文基于MODIS NDVI时问序列数据集,运用Sen+Mann-Kendall趋势检验、Hurst指数和相关分析等方法,对湖南省2000—2018年植被的时空变化特征、演化趋势可持续性及其与气候因子的相关性进行了研究.结果表明:①湖南省植被覆盖整体较高,并具有明显的季节变化特征;研究区植被与气温的相关性要强于降水.②近19年湖南省植被NDVI整体呈上升态势,增速为8.6%/10 a(P<0.001),其中显著和极显著上升的地区分别占10.3%、57.3%;主要分布在湘中与湘西北的林地、耕地区域;降低的地区主要分布在长株潭等城市建设用地区域及洞庭湖平原的局部耕地区域.③未来湖南省植被变化可能向退化的恶性方向发展的面积占80.1%. 相似文献
29.
Although the residual layer has already been noted in the classical diurnal cycle of the atmospheric boundary layer,its effect on the development of the convective boundary layer has not been well studied. In this study, based on 3-hourly20 th century reanalysis data, the residual layer is considered as a common layer capping the convective boundary layer. It is identified daily by investigating the development of the convective boundary layer. The region of interest is bounded by(30°–60° N, 80°–120° E), where a residual layer deeper than 2000 m has been reported using radiosondes. The lapse rate and wind shear within the residual layer are compared with the surface sensible heat flux by investigating their climatological means, interannual variations and daily variations. The lapse rate of the residual layer and the convective boundary layer depth correspond well in their seasonal variations and climatological mean patterns. On the interannual scale, the correlation coefficient between their regional averaged(40°–50°N, 90°–110° E) variations is higher than that between the surface sensible heat flux and convective boundary layer depth. On the daily scale, the correlation between the lapse rate and the convective boundary layer depth in most months is still statistically significant during 1970–2012. Therefore, we suggest that the existence of a deep neutral residual layer is crucial to the formation of a deep convective boundary layer near the Mongolian regions. 相似文献
30.
Peiyue Li Hui Qian Jianhua Wu Hongwei Liu Xinsheng Lyu Hongbo Zhang 《Environmental Earth Sciences》2014,71(1):293-299
Global curve-fitting method (GCFM) is regarded as an effective approach in hydrogeological parameter estimation, as it integrates and uses pumping data and water recovery data of a transient pumping test for parameter estimation. The impacts of pumping duration on hydrogeological parameter estimation by GCFM were investigated in the present study using 2 in situ pumping tests and 24 simulated transient pumping tests. Empirical formulas for determining the optimal pumping duration were derived. The study results suggest that pumping duration will have impacts on the accuracy of hydrogeological parameter estimation. When pumping duration is longer than a certain period, relative errors of hydrogeological parameter estimation keep relatively stable within an acceptable limit. Therefore, it is unnecessary to continue the pumping for a very long time after the groundwater level has become stable. When the change rate of drawdown over time (γ) in an observation well located within a distance of 100 m to the pumping well reaches 0.134, the pumping can be stopped. If there are more than one observation wells in a pumping test, the smallest γ value should be selected to determine the optimal pumping duration. This research is meaningful in the instruction of pumping tests, and will reduce test costs greatly. 相似文献