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61.
62.
通过对库尔勒机场1991—2000年出现沙尘天气的统计分析,总结出了库尔勒地区沙尘天气的天气、气候特征及预报指标;确定了预报沙尘天气的隶属函数,并对其进行了历史回报。 相似文献
63.
提出了在异构系统实现负载平衡的区域分解算法和实现负载平衡的计算方法,利用它的负反馈性质解决了异构系统处理机计算速度测量误差造成的负载测量不准问题,并对处理机速度变化,速度测量误差、处理机数量、网格点计算量的分布等因素的影响进行了计算,结果表明本方法具有很强的平衡负载能力和较强的适应性;根据计算结果提出了解决模式网格点计算量不易测量问题的解决方案,并用扩散方程和模拟物理过程进行试验,试验表明这种方法是可行的,平衡负载的效果十分显著。 相似文献
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本文介绍利用NOAA极轨气象卫星AVHRR资料监测森林草原火点的原理和方法。对甘肃省1992年10月至1996年12月监测到的火点进行时空统计,分析了火灾监测中可能产生的误差原因,并提出相应改进措施。 相似文献
66.
Observations show that the sequences of microsecond-scale pulses are produced in cloud flashdischarge processes.In the present work we report on measurements of larger bipolar pulses(LBP)of the radiation fields which are classified into four types according to their waveshapes andpolarities of initial peak.Either positive or negative pulse contains two kinds of waveshapes:onewith a smooth rise and the other with 2 or 3 fast-rising pulse superimposed on the initial half cycle.The pulse waveshape characteristics in both time and frequency domains are as follows.Among2908 samples there are 45% of the positive polarity and 55% of the negative polarity.The positivepulses tend to have distinctly smaller values than negative pulses in rise time,half width and zero-crossing time of the initial peak.The peaks of positive pulse spectra tend to occur at a higherfrequency than those of negative pulses.Despite differences above,positive and negative pulseshave a similar total duration. 相似文献
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68.
The ability of seismological criteria to identify earthquakes from underground explosions depends partly on the orientation of the earthquake source. Well-determined double-couple moment tensor solutions for a large number of earthquakes have been published in the Harvard centroid moment tensor (CMT) and United Slates Geological Survey (USGS) catalogues. Statistical analyses of these catalogues indicate that the distribution of the orientation of earthquake mechanisms is not random. The distribution of the T axes shows significant clustering around the downward vertical, indicating that a larger number of earthquake mechanisms radiate compressional P -wave energy to teleseismic distances from near the maximum of the radiation pattern than is predicted if earthquake sources are randomly oriented double couples. The clustered T axes correspond to compressional dip-slip mechanisms, and it is this type of mechanism which is believed to cause both the m b : M s (the ratio of body-wave to surface-wave magnitude) and first-motion criteria to misidentify an earthquake as an explosion. 相似文献
69.
本文对西南极菲尔德斯形变网GPS监测数据的误差特性进行分析,利用数理统计原理检验了数据中的系统误差,提出了削弱这类系统误差的方法。该方法有3个特点:1.以监测网中两个稳定点为基准;2.对监测网数据进行尺度因子改正与坐标变换迭代计算;3.归算后监测网点位结构不变。经改化处理后的数据,基本上消除了系统误差的影响。 相似文献
70.
Hazard mapping based on macroseismic data considering the influence of geological conditions 总被引:1,自引:0,他引:1
The object of this study is to consider directly the influence of regional geological conditions on the assessment of seismic hazard. It is assumed that macroseismic data at individual locations contain, in an average way, the influence of geological conditions.A Data Base referring to 199 historical (5) and instrumental (194, in the 1947–1993 period) events with macroseismic information in 1195 locations of Portugal was built. For any given seismic event, whenever macroseismic information was available at a location (town, village, etc.), an EMS-92 intensity value was estimated. To each one of those locations a geological unit, representing the most common type of soil, was assigned, based on the Geological Portuguese Map at a scale 1:500 000; the geological units were grouped into three categories: soft, intermediate and hard soils.The Data Base was used to determine the attenuation laws in terms of macroseismic intensity for the three different geological site conditions, using multiple linear regression analysis. The reasonability of the laws was tested by (i) checking residual distributions and (ii) comparing the map of isoseismals of important earthquakes with the isoseismals generated by the attenuation curves derived for each one of the three different soil classes, taking into consideration the soil class of each site. The main results of attenuation modeling are: high dispersion on macroseismic intensity data; all the models predict intensity values, for short hypocentral distances, lower than the ones observed; and for some important analyzed earthquakes and for the observed range of distances, the models confirm the expectancy that macroseismic intensity increases from hard to soft soil.The approach to obtain the hazard assessment at each location consisted in the use of the attenuation law specifically derived for the class of soil of that particular location. This method, which considers the influence of the regional geology, was illustrated with the mapping of hazard for the country for several return periods. Comparison with previous maps not taking into consideration the regional geological conditions emphasizes the importance of this new parameter. It can be concluded that (i) soil segmentation is clearly the cause for hazard increase in the region to the north of Lisbon, especially at sites with soft and intermediate soils as the ones in lower Tagus valley; the maximum increase on hazard is, in any case, less than one degree; (ii) when geological conditions are disregarded in the attenuation regression analysis, hazard pattern is similar to the one obtained for the case of hard soil everywhere. 相似文献