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71.
印度河文明兴衰和地理环境变迁   总被引:12,自引:1,他引:11  
班武奇 《地理研究》1998,17(3):249-257
历史学界证实,约发端于公元前3000年的印度河文明,历经千年辉煌后,突然衰落了。此文着重探讨了与这一兴衰过程相伴的地理环境变迁问题。初步结论是:印度河流域的热带森林,孕育了古代农业,并成为阶级社会诞生、发展的自然基础。青铜利刃、文明之火,砍尽、烧光了一片又一片原始森林,终于引发了良性生态平衡的崩解,导致难以逆转的沙漠化过程,使一个兴旺的古代社会衰落到死亡的边缘。雅利安人的入侵和其后的漫漫风沙,彻底埋葬了印度河古代文明。  相似文献   
72.
73.

This paper presents the first multi-model ensemble of 10-year, “convection-permitting” kilometer-scale regional climate model (RCM) scenario simulations downscaled from selected CMIP5 GCM projections for historical and end of century time slices. The technique is to first downscale the CMIP5 GCM projections to an intermediate 12–15 km resolution grid using RCMs, and then use these fields to downscale further to the kilometer scale. The aim of the paper is to provide an overview of the representation of the precipitation characteristics and their projected changes over the greater Alpine domain within a Coordinated Regional Climate Downscaling Experiment Flagship Pilot Study and the European Climate Prediction system project, tasked with investigating convective processes at the kilometer scale. An ensemble of 12 simulations performed by different research groups around Europe is analyzed. The simulations are evaluated through comparison with high resolution observations while the complementary ensemble of 12 km resolution driving models is used as a benchmark to evaluate the added value of the convection-permitting ensemble. The results show that the kilometer-scale ensemble is able to improve the representation of fine scale details of mean daily, wet-day/hour frequency, wet-day/hour intensity and heavy precipitation on a seasonal scale, reducing uncertainty over some regions. It also improves the representation of the summer diurnal cycle, showing more realistic onset and peak of convection. The kilometer-scale ensemble refines and enhances the projected patterns of change from the coarser resolution simulations and even modifies the sign of the precipitation intensity change and heavy precipitation over some regions. The convection permitting simulations also show larger changes for all indices over the diurnal cycle, also suggesting a change in the duration of convection over some regions. A larger positive change of frequency of heavy to severe precipitation is found. The results are encouraging towards the use of convection-permitting model ensembles to produce robust assessments of the local impacts of future climate change.

  相似文献   
74.
连云港市城市空气质量预报方法研究   总被引:6,自引:0,他引:6       下载免费PDF全文
姜有山  陈飞  班欣  李军 《气象科学》2007,27(2):220-225
本文利用高空大气探测资料和有限区细网格模式的数值预报产品,分别建立统计预报和数值预报等适合连云港市城市空气质量预报业务发展所需要的客观预报方法,最终利用动态分权法,综合决策集成连云港市城市空气质量预报。结果表明:动态分权法能够有效地提高空气质量的预报准确率。  相似文献   
75.
选取全球52个MGEX测站连续7 d的数据对两种伪距频间偏差(IFB)模型在多系统融合精密单点定位中的性能进行统计分析,第一种IFB模型是对每个GLONASS卫星估计一个IFB参数,第二种模型则是采用频率号的一次线性函数估计IFB参数。结果表明,静态条件下两种伪距IFB模型在E、N、U三个方向上定位精度相当;动态条件下两种模型在E、U方向上精度相当,第二种模型比第一种模型在N方向上定位精度提高21%。相同条件下两种伪距IFB模型的收敛速度相差较小且均能达到指定精度,而第一种伪距IFB模型需要估计更多参数。因此综合考虑定位精度和收敛时间,在进行多系统融合精密单点定位时建议采用第二种模型进行伪距IFB估计。  相似文献   
76.
刘彬  王学求 《地学前缘》2016,23(5):291-300
白山钼矿位于东天山康古尔-黄山韧性剪切带三岔口-白山斑岩铜钼矿带中,为典型的斑岩型钼矿。本文以白山钼矿床深部花岗斑岩体为研究对象,对其进行了精确的锆石SIMS U-Pb定年以及锆石原位Hf同位素分析,旨在确定白山钼矿床深部斑岩体的形成时代以及岩石成因,进而分析其形成时的动力学背景。本文获得的白山钼矿床深部斑岩体锆石SIMS U-Pb年龄为(229.7±3.2) Ma,这一结果与前人获得的辉钼矿Re-Os等时线年龄225~229 Ma基本一致,因此可以代表成矿岩体的形成年龄为晚三叠世。锆石原位Hf同位素组成特征显示,εHf(t)均显示正值,为+8.3~+12,地壳模式年龄(TCDM)为556~758 Ma。结合前人研究成果及区域地质演化历史,可以确定白山钼矿床深部斑岩体形成于晚三叠世陆内伸展环境,由新生下地壳部分熔融形成。  相似文献   
77.
北京石花洞洞穴滴水中硫酸根浓度的时空变化及其意义   总被引:6,自引:3,他引:3  
硫是环境地球化学循环中重要的元素之一,是区域及全球性环境变化的重要驱动因子。本文通过对石花洞洞穴4个滴水点(JG,SH,PL1和PL2)硫酸根浓度近3个水文年的分析测定(BL点观测近两年),结果表明:响应降雨快的滴水点(SH和JG点)滴水SO42-浓度升高幅度最明显,且滴水SO42-浓度与滴率成指数关系;滞后响应降雨的观测点滴水SO42-浓度雨季升高幅度不明显,但在长期观测期间有明显增加的趋势;对降雨没有响应的滴水点,其SO42-浓度低且雨季没有明显变化。通过分析表明,在快速响应降水的滴水点,滴水硫酸根浓度大幅升高可能在一定程度上影响滴水pH值,这也可能是导致雨季时,快速下渗进入洞穴的滴水碳酸钙饱和度降低,从而抑制滴水沉积的一个不可忽略的因素。   相似文献   
78.
Three long-term fixed acoustic Doppler current profilers were first used for investigating the vertical structure of tidal currents in Xuliujing Section of Changjiang River Estuary. Moreover, three different periods(spring, summer and fall) were also considered for investigating seasonal variations. The semi-diurnal tides were the most energetic, with along-channel speed of up to 80 cm/s for M2 constituent, which dominates at all stations with percent energy up to 65%–75% during seaso...  相似文献   
79.
河北文安地震与云南盐津地震震害比较分析   总被引:4,自引:1,他引:3  
2006年7月4日在河北省文安县发生5.1级地震,未造成人员伤亡和较大的经济损失;而22日在云南省盐津县发生的同样震级的地震却造成22人死亡,经济损失达3亿多元。本文对比分析了这两次5.1级地震的人员伤亡和震害情况,探讨了我国东部地区与西南部地区地震灾害的异同。  相似文献   
80.
Changes in thawed depth of frozen soil caused by diurnal and seasonal temperature fluctuations are commonly found in high altitude and latitude regions of the world. These changes significantly influence hydrologic and erosion processes. Experimental data are necessary to improve the understanding and modeling of the phenomenon. Laboratory experiments were conducted in Beijing to assess the impacts of thawed soil depth, slope gradient, and flow rate on soil erosion by concentrated meltwater flow over an underlying frozen soil layer. Soil samples from watershed were filled in flumes, saturated before being frozen. After the soil was completely frozen, flumes were taken out of storage to thaw the frozen soil from top to the designed depths. Meltwater flow was simulated using a tank filled with water and icecubes at approximately 0°C. The erosion experiments involved four thawed soil depths of 1, 2, 5, and 10 cm; three slope gradients of 5°, 10°, and 15°; and three flow rates of 1, 2, and 4 l/min; and seven rill lengths of 0.5, 1, 2, 3, 4, 5, and 6 m. Sediment‐laden water samples were collected at the lower end of the flume for determination of sediment concentration. The results showed that sediment concentration increased exponentially with rill length to approach a maximum value. The sediment concentrations were closely correlated with thawed soil depth, flow rate, and slope gradient. Shallower thawed depths delivered more sediments than deeper thawed depths. Slope gradient was the primary factor responsible for severe erosion. The effect of flow rate on sediment concentration which decreased with increasing slope gradient, was not as significant as that of slope gradient. Results from these experiments are useful for understanding the effect of thawed soil depth on erosion process in thawed soils subject to freezing and for estimating erosion model parameters. Copyright © 2017 John Wiley & Sons, Ltd.  相似文献   
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