利用卫星图像研究西藏羌塘及邻区的断裂活动性   总被引：18，自引：5，他引：13       下载免费PDF全文

李建华 《地震地质》1998,20(3):10-207

利用１／５０万彩色合成镶嵌的卫星图像,对羌塘块体及邻近大约５０万ｋｍ２地区的断裂活动性进行分析判读。根据断裂的影像特征,将所判读的断裂分成全新世活动、晚更新世活动和第四纪早、中期活动３类。结合本世纪以来的地震活动,分析了主要断裂的活动性。例如位于羌塘盆地以北,全新世明显左行走滑的玛尔盖茶卡－若拉错断裂带上,１９９７年１１月８日发生了玛尼７．５级地震,是该断裂带现代活动的表现  相似文献   

1976年唐山地震发震断裂的活动性研究   总被引：10，自引：5，他引：5       下载免费PDF全文

李建华  郝书俭 《地震地质》1998,20(1):28-33

震后野外考察及航空摄影发现的地裂缝带,说明唐山断裂与１９７６年唐山７．８级大地震的发震构造有密切关系。用卫星遥感信息和浅层地震勘探结果对唐山断裂的活动性做了新的研究。卫星图像解释结果表明：震前一年多时间内,ＮＥ向的唐山断裂被ＮＮＷ向断裂截切而ＮＷＷ向断裂受到牵引,因而显示出右旋走滑的活动形迹。浅层地震勘探结果则证明,唐山断裂是倾向ＮＷ,高倾角的右旋走滑正断层,它断错了全新统（Ｑ４）、晚更新统（Ｑ３）、中更新统（Ｑ２）和早更新统（Ｑ１）地层  相似文献   

遥感技术在南盘江地区油气烃类检测中的应用     

马跃良  何在成 《海相油气地质》1998,3(2):47-54

应用陆地卫星 TM 资料对南盘江地区进行了烃类微渗漏蚀变信息检测研究。岩石土壤地球化学特征分析表明,该区不同程度地存在着“褪红”、“粘土矿化”、“碳酸盐矿化”等烃类蚀变异常现象。选择 FeO/Fe_2O_3作为褪红的成分因子;(K_2O+Na_2O+Al_2O_3)、(K_2O+Na_2O)/Al_2O_3、(K_2O+Na_2O+Al_2O_3)/S∶O_2和 K_2O/Na_2O 等作为粘土矿化的成分因子;CaO+MgO 和 CaO/MgO 作为碳酸盐矿化的成分因子。利用 TM1/TM3、TM1/TM4识别褪红蚀变信息,TM5/TM7、TM5/TM4用干识别粘土矿化和碳酸盐矿化蚀变信息。建立了地球化学—光谱—遥感图像三位一体的遥感找油气模式,根据油气遥感色调异常对南盘江地区进行了评价和分类。  相似文献   

我国卫星总云量与地面总云量分布的对比分析   总被引：44，自引：11，他引：33       下载免费PDF全文

翁笃鸣  韩爱梅 《应用气象学报》1998,9(1):32-37

根据国际卫星云气候学计划（ISCCP）的总云量和地面总云量资料,分析并讨论了两者在我国的空间分布和单站年变化中的相关性和差异性,对比了两种总云量的全国分布形势。结果指出,在总趋势大致相似的前提下,卫星总云量图能更好地揭示青藏高原、塔克拉玛干沙漠以及沿海地区的云气候特征。最后还就青藏高原总云量分布特点作了分析。  相似文献   

1996年8月8日闽西地区特大暴雨过程分析   总被引：3，自引：2，他引：1  

林毅  刘爱鸣 《气象科学》1998,18(2):174-180

本文研究了9601号热带风暴减弱为低压环流后引起突发性大暴雨的成因。结果表明：9610号热带风暴减弱后的低压环流移支福建省南部地区,造成闽西地区湿斜压锋区和不稳定能量明显增强,在低压西侧辐合线所提供的福合上升运动激发下,中尺度对流云团迅速发展,导致远离低压中心的闽西突发大暴雨。闽西特殊的地形对特大暴雨的产生起了组织和增幅作用。另外,还通过逐时数字红外云团图的分析,揭示中尺度对流云团发展演变特征与突发性大暴雨的关系,供日常短时预报参考。  相似文献   

若尔盖等地风能资源评价     

胡毅  青泉  董明琨  何伟贤 《成都信息工程学院学报》1990,(4)

本文用平均风速和最大风速法对若尔盖等三地的韦伯分布参数k、c进行估算,并用韦伯分布计算风能的指标。计算表明:若尔盖、红原属风能可利用区,用风力发电是有利用价值的;阿坝属风能贫乏地区。  相似文献   

Dynamics of a satellite orbiting a planet with an inhomogeneous gravitational field     

J. F. Palacián 《Celestial Mechanics and Dynamical Astronomy》2007,98(4):219-249

We study the dynamics of a satellite (artificial or natural) orbiting an Earth-like planet at low altitude from an analytical point of view. The perturbation considered takes into account the gravity attraction of the planet and in particular it is caused by its inhomogeneous potential. We begin by truncating the equations of motion at second order, that is, incorporating the zonal and the tesseral harmonics up to order two. The system is formulated as an autonomous Hamiltonian and has three degrees of freedom. After three successive Lie transformations, the system is normalised with respect to two angular co-ordinates up to order five in a suitable small parameter given by the quotient between the angular velocity of the planet and the mean motion of the satellite. Our treatment is free of power expansions of the eccentricity and of truncated Fourier series in the anomalies. Once these transformations are performed, the truncated Hamiltonian defines a system of one degree of freedom which is rewritten as a function of two variables which generate a phase space which takes into account all of the symmetries of the problem. Next an analysis of the system is achieved obtaining up to six relative equilibria and three types of bifurcations. The connection with the original system is established concluding the existence of various families of invariant 3-tori of it, as well as quasiperiodic and periodic trajectories. This is achieved by using KAM theory techniques.  相似文献   

Study of temperature and precipitation variations in Italy based on surface instrumental observations   总被引：1，自引：0，他引：1  

Tiziano Colombo  Vinicio Pelino  Stefania Vergari  Paolo Cristofanelli  Paolo Bonasoni 《Global and Planetary Change》2007,57(3-4):308-318

In this paper we present a study concerning the climatic behaviour of two principal observables, temperature and precipitation as obtained from the measurements carried out at 50 Italian meteorological stations, since 1961. Analyses of WMO Climate Normals (CliNo) from 1961 to 1990 have been performed dividing the 50 Italian stations in three different classes: mountain (11 stations), continental (17) and coastal areas (21).The comparison of the CliNo 1961–1990 with the trend of temperature and precipitation for the period 1991–2000 showed a sharp significant increase of summer temperatures over Italy starting from 1980. This phenomenon was particularly evident for mountain stations, where a significant temperature increase has been recorded also during the autumn. Moreover, the analysis of precipitation data permitted to point out that, starting from 1980, mountain stations have been affected by a significant increase of precipitation events during autumn and winter, while for the rest of the Italian territory a reduction of precipitations has been recorded during early spring.  相似文献   

SOFTWARE REVIEWS     

《The Professional geographer》1990,42(3):386-390

AMOS—Analysis of MOment Structures . James Arbuckle CLIMATEDATA–Summary of the Day . (Version 1.10). HYDRODATA–U.S.G.S. Daily Values (Version 2.0). The MAP SETS (includes EUROPEAN MAPSET, US MAPSET and WORLD MAPSET). James Taylor  相似文献   

Envisat and SARAL/AltiKa Observations of the Antarctic Ice Sheet: A Comparison Between the Ku-band and Ka-band     

Frédérique Rémy  Thomas Flament  Aurélie Michel  Denis Blumstein 《Marine Geodesy》2015,38(3):510-521

The AltiKa altimeter onboard SARAL is a joint CNES/ISRO mission launched in February 2013 that has the same 35 days repeat orbit of the previous European altimeters, Envisat, and ERS-1/2. SARAL/AltiKa is thus a unique opportunity to extend the repeat observations of this orbit that have been surveyed since 1991. However, the altimeter operates in Ka-band, which is higher than the previous frequencies, and offers new paths of investigation. The penetration depth is theoretically reduced from around 10 m in Ku-band to less than 1 m in Ka-band, such that the volume echo originates from the near subsurface. Second, the sharper antenna aperture leads to a narrower leading edge that reduces the impact of the ratio between surface and volume echoes of the height retrieval. Indeed, the spatial and temporal observations of AltiKa at cross-over points and along-track indicate that the impact of backscatter changes on the height decreasesfrom 0.3 m/dB for the Ku-band to only 0.05 m/dB for the Ka-band. Therefore, the height measurement is stable over time. Moreover, the volume echo in the Ka-band results from the near subsurface layer and is mostly controlled by ice grain size, unlike the Ku-band.  相似文献