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11.
青藏铁路沿线闪电活动的时空分布特征 总被引:6,自引:4,他引:2
利用搭载于卫星上的闪电探测仪所获取的8年闪电资料,对青藏铁路沿线闪电活动的时空分布进行了研究。结果表明,青藏铁路沿线的闪电活动呈现出明显的季节变化和日变化。青藏铁路沿线的闪电活动主要发生在4~9月,其中以5~7月最为频繁,到10月份迅速消亡,而且闪电分布在南北向上变化较明显;青藏铁路沿线闪电活动在12:00~16:00(地方时,下同)最易发生。日闪电密度峰值出现在15:00左右。闪电密度的空间分布以那曲为最大,分别向南、北减小。另外,2003年夏季的地面观测资料还表明,那曲地区在傍晚还有一闪电活动峰值。 相似文献
12.
Geomorphic effects observed in the Barranco (creek) de Arás basin are used to characterize the flood. Sediment features allow to qualify the flood as essentially a water flow. Using the critical section method, the peak flood discharge is estimated to be between 400 and 600 m3 s−1. Similar results were obtained using a paleohydraulic formula based on the size of the largest mobilized clasts. Using the rational method with available rainfall data, the discharge for a recurrence interval of 500 years is estimated to be between 150 and 200 m3 s−1. These results agree with predictions obtained using curves of peak discharge versus basin area based on regional data. Several trenches dug on the fan showed that the size of boulders mobilized by the event is larger that those left by previous floods at the same place. When the estimated peak flood discharge is related to the basin area, values between 20 and 30 m3 s−1 km−2 are obtained, demonstrating that the Barranco de Arás flood was most unusual. 相似文献
13.
人工地震测深和天然地震流动观测兼用的轻便数字地震仪系统 总被引:8,自引:1,他引:7
本文介绍一种新的轻便数字地震仪DAS-1。其设计特点是:双微处理器硬件结构;过采样AD转换技术的运用;线性相位和最小相位FIR数字滤波的运用;大容量CMOS快闪存贮器作数据存储介质;GPS授时和内部高精度数字钟相结合的时间服务系统;采集器功耗低于0.65W。该仪器有3个信号输入通道,0 ̄40Hz的带宽和16位字长。它可方便地用于人工地震测深及天然地震流动观测。 相似文献
14.
Between 2001 and 2005, a large debris rock slide occurred on the western slope of the Cordillera de Santa Cruz in the southeast
Andean corner of the Province of San Juan (31°40′ S–70°16′ W). The landslide material accumulated in a downstream gorge as
a natural dam of the Santa Cruz river, forming a large-volume lake. In November 2005, probably as a result of the increasing
pressure of the water volume, this natural dam breached off with a violent and unexpected flash flood. In addition to life-threatening
instances lived by some people downstream, this flood caused great economic loss to main localities of the Department of Calingasta,
as well as considerable damage to one of the most relevant projects of the Province, the Caracoles Hydropower Project dam
on the San Juan river. Considering the high costs of any physical remediation for a natural dam located in this high, remote,
and inaccessible mountain area with no reliable road access, the main protective measures left to be pondered are the installation
of a flash-flood early-warning system connected to downstream localities, along with a program of hydrological monitoring
at the dam-forming area and annual satellital monitoring to verify the evolution of accumulated mass movements. 相似文献
15.
利用卫星上携带的闪电探测仪所获取的8年闪电资料(1995~2002)对青藏高原闪电活动的时空分布以及高原季风期间闪电活动对地面热力学特征的响应进行了研究.结果表明,高原上的平均闪电密度为3fl·a-1·km-2,并在高原中部(32°N, 88°E)出现闪电密度峰值5.1fl·a-1·km-2.闪电活动主要发生在6~8月,并在6月下旬至7月中旬最为活跃.大部分地区的闪电活动日变化峰值出现在14:00~16:00 LT,在中西部的显著高山地区早于这一时刻,而在显著低海拔的塔里木和柴达木盆地晚于这一时刻.夏季季风期间高原上的闪电活动明显依赖于地表的热力学特征,并与地表鲍恩比和感热通量呈明显的线性正相关,相关系数分别为0.7和0.6,鲍恩比有可能作为调整闪电产生效率的量度. 相似文献
16.
盐水闪蒸技术广泛应用于海水淡化及海洋温差能发电,含盐质量分数、给盐液温度和闪蒸压力对闪蒸汽化率和热效率有很大影响。在质量分数为3.5%~20%、给盐液温度为30~95℃和闪蒸压力为1~30 kPa的范围内,对NaCl溶液闪蒸汽化率和热效率等闪蒸效率特性进行了定量计算研究,研究得到了盐水含盐质量分数、给盐液温度和闪蒸压力对闪蒸汽化率以及热效率影响的规律。结果表明,降低含盐质量分数,提高给盐液温度,降低闪蒸压力可提高闪蒸汽化率与热效率;含盐质量分数越高,造成的热损失越大,而提高给盐液温度会增大热损失。 相似文献
17.
本文分析了Adobe Flash技术在网络地图发布前端技术上的优势和应用现状,选择开源Flash地图组件Modest Maps作为开发工具,在其上添加了一些组件模块,以"5.12地震信息显示"为示例,实现了基于Modest Maps的Falsh网络地图发布和简单的空间分析. 相似文献
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20.
Mediterranean flash flood transfer through karstic area 总被引:1,自引:0,他引:1
Vincent Bailly-Comte Hervé Jourde Axel Roesch Séverin Pistre 《Environmental Geology》2008,54(3):605-614
Karstic aquifers influence flash floods propagation in Mediterranean countries. Near Montpellier, Southern France, discharge
data are recorded on the Coulazou River upstream and downstream of the Aumelas Causse. Two gauging stations are used to describe
the hydrodynamics of this binary karstic system. The first station characterizes the non-karstic catchment area. The second
one is representative of the karstic part of the watershed. Records since April 2004 are used to understand how the river
interacts with a karstic aquifer. Hydrograph analysis of three flash flood events is described. Corresponding discharge time
series recorded at the two gauging stations are used to describe the modification of the hydrographs by auto- and crosscorrelations
analyses. Finally, linear system analyses are used to provide the transfer functions of this binary karstic system according
to the three flood events characteristics (initial conditions, volume, spatial distribution of rainfall, etc.). Theses functions
summarize the hydrodynamic behaviour of the system: their shapes are indicative of the dynamics of the storage, the release
and the contribution to surface waters.
相似文献
Vincent Bailly-ComteEmail: |