Geometrodynamical distances to the Galaxy's hydrogen streams     

Shoko Jin  D. Lynden-Bell 《Monthly notices of the Royal Astronomical Society》2008,383(4):1686-1694

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AMI limits on 15-GHz excess emission in northern H ii regions     

A. M. M. Scaife  N. Hurley-Walker  M. L. Davies  P. J. Duffett-Smith  F. Feroz  K. J. B. Grainge  D. A. Green  M. P. Hobson  T. Kaneko  A. N. Lasenby  G. G. Pooley  R. D. E. Saunders  P. F. Scott  D. J. Titterington  E. M. Waldram  J. Zwart 《Monthly notices of the Royal Astronomical Society》2008,385(2):809-822

We present observations between 14.2 and 17.9 GHz of 16 Galactic H  ii regions made with the Arcminute Microkelvin Imager. In conjunction with data from the literature at lower radio frequencies we investigate the possibility of a spinning dust component in the spectra of these objects. We conclude that there is no significant evidence for spinning dust towards these sources and measure an average spectral index of  α= 0.15 ± 0.07  (where   S ∝ν^−α  ) between 1.4 and 17.9 GHz for the sample.  相似文献   

分子云磁场与尘埃导致的偏振   总被引：1，自引：1，他引：0  

石惠  韩金林 《天文学进展》2008,26(4)

磁场对分子云及其中的恒星的形成和演化起到重要的作用.分子云磁场的探测方法主要是谱线塞曼效应、尘埃热辐射的偏振,以及谱线的线偏振观测.利用谱线的塞曼效应可以直接测量视线方向的磁场强度.尘埃热辐射偏振可以有效地示踪磁场方向在天球上的分布.分子云内部的磁场会受到不同物理过程的影响.高分辨率观测可以研究磁场扰动的细节,低分辨率观测可以得到分子云甚至银河系大尺度磁场的宏观信息.只有多波段的观测才能全面地认识分子云磁场与各种物理过程的联系.该文对分子云尘埃热辐射偏振的观测情况做了调研,总结了分子云大尺度磁场的研究现状和发展前景.  相似文献   

小生境遗传算法在地震CT中的应用研究   总被引：3，自引：1，他引：2  

班书昊  杨慧珠 《地球物理学进展》2004,19(1):143-147

针对含单相饱和流体的孔隙介质,综合费马原理、等效孔隙介质理论、Radon变换等,提出了基于地震CT技术求解速度、孔隙度和岩石密度的小生境多参数反演算法．以此为基础,经过改进,形成了物性参数的隔离小生境反演算法．理论分析与实例计算结果表明,该方法简化了波在层状介质中的传播方程,具有一定的实用价值,可以有效解决井间测井地层问题,获得较高精度的地层物性参数;而且模型简单,有精度高、多峰优化等特点,可用于地下层状介质中油气的寻找,满足油气预测与勘探开发的要求．  相似文献   

广汉机场一次非典型辐射平流雾的天气诊断分析     

王钦  曾波  吴俊杰 《成都信息工程学院学报》2013,(5):537-542

为探索广汉机场雾发生发展的机制,确保飞行安全,提高预报准确率,利用广汉机场地面观测资料、Mi—caps系统下的常规观测资料、探空资料和NCEP／NCAR再分析资料,采用天气诊断分析方法,对2012年11月13日-15日广汉机场持续性的辐射平流雾进行分析。结果表明,雾是在稳定的天气背景下形成。夜间地面长波辐射冷却触发了这次雾的形成,而在轻雾转大雾期间,地面长波辐射冷却作用明显减弱,低层暖湿平流则起到了主要作用。与典型辐射平流雾不同的是成雾后,机场由脊前西北气流转为南支槽前西南气流控制,天空中云量的迅速增加使得雾进一步加强。  相似文献   

Anomalously low ozone of 1997 and 2011 Arctic spring: Monitoring results and analysis     

ZHANG Yan  WANG Weihe  LI Xiaojing  ZHANG Xingying  ZHENG Zhaojun  LIU Ruixia 《极地研究(英文版)》2012,23(2):82-86

Total ozone observations from the Total Ozone Unit （TOU） aboard the Chinese second generation polar orbiting mete- orological satellite, Fengyun-3/A （FY-3/A）, revealed that total column ozone over the Arctic declined rapidly from the beginning of March 2011. An extensive region of low column amount formed around mid March; monthly mean total column ozone in March 2011 was about 30% lower than the average observed during 1979-2010. Daily total column density of ozone near the center of low ozone area in mid March was less than 240 Dobson units, about half the total column ozone amount observed during the same period of the prior 10 years. We analyzed total column ozone data from different satellites during 1979-2011. Results show that the Arctic depletion of ozone in spring 2011 was initiated by the cold polar vortex in the lower stratosphere. The March mean total ozone over the Arctic has shown a decreasing trend over the past 32 years, and its variation is strongly correlated with the polar vortex. A similar low ozone process of spring 1997 was compared to that of 2011, but daily variations of total ozone in March over the Northern Hemisphere in 1997 and 2011 have different patterns.  相似文献   

基于整体最小二乘的稳健点云数据平面拟合   总被引：3，自引：0，他引：3  

官云兰  刘绍堂  周世健  张立亭  鲁铁定 《大地测量与地球动力学》2011,31(5):80-83

针对点云数据平面拟合方法没有完整考虑测量数据中的误差及系数阵中误差的情况,提出稳健整体最小二乘点云数据平面拟合方法。该法以整体最小二乘法为基础,在考虑全部观测量存在误差的情况下,通过一定的准则删除数据中的粗差或异常值,从而获得稳健的平面参数估值。实验中,分别利用最小二乘法、特征值法和稳健整体最小二乘拟合法对仿真点云数据和真实点云数据进行平面拟合,结果显示该法能克服异常值的影响,得到可靠的平面参数估值,具有稳健性。  相似文献   

利用多元LBP特征自动提取城市道路边界     

刘如飞  马新江  卢秀山  王旻烨  王鹏 《遥感学报》2022,26(3):541-554

车载移动测量系统可采集高精度道路三维点云数据,为道路边界自动化提取提供了支撑.为解决车载激光点云中城市道路边界点云提取困难问题,本文引入局部二值模式LBP(Local Binary Pattern),针对各类城市道路边界特征,设计了高度LBP、高程离散度LBP和空间形状LBP3种改进算子;构建多元LBP特征语义识别模型...  相似文献   

湖南杏枫山金矿区首次发现高品位的钨矿体   总被引：3，自引：0，他引：3  

彭建堂 《地质论评》2019,65(3):664-670

湖南隆回县杏枫山金矿床位于雪峰山弧形构造隆起带的中段,白马山岩体南缘,是一产于新元古界浅变质岩中的石英细脉型金矿,目前已开采了30余年。最近,笔者在该金矿区新发现了矽卡岩和高品位的钨矿体,这类矽卡岩型钨矿床,明显不同于雪峰山一带广泛分布的石英脉型钨矿床。该区矽卡岩在矿区非常发育,主要呈层状、似层状产出,与地层呈整合接触;白钨矿主要是以条带状、脉状充填于矽卡岩之中,少量分布于含金的石英脉中;该区钨矿石的品位高,所有中段矿石WO_3平均含量均在0.5%以上,部分中段可达到3.0%以上。初步研究显示,该区矽卡岩为一还原性矽卡岩,结合其层状产出特征,可推断杏枫山为一品位高、资源潜力大的钨矿床。杏枫山金矿区矽卡岩和钨矿体的发现,不仅具有十分重要的经济价值和社会效益,而且对认识湘中地区岩浆岩的演化与钨、金成矿,也很有价值。  相似文献   

Reducing discrepancies in ground and satellite-observed eruption heights   总被引：2，自引：2，他引：0  

Andrew Tupper  Rick Wunderman   《Journal of Volcanology and Geothermal Research》2009,186(1-2):22

The plume height represents a crucial piece of evidence about an eruption, feeding later assessment of its size, character, and potential impact, and feeding real-time warnings for aviation and ground-based populations. There have been many observed discrepancies between different observations of maximum plume height for the same eruption. A comparison of maximum daily height estimates of volcanic clouds over Indonesia and Papua New Guinea during 1982–2005 shows marked differences between ground and satellite estimates, and a general tendency towards lower height estimates from the ground. Without improvements in the quality of these estimates, reconciled among all available methods, warning systems will be less effective than they should be and the world's record of global volcanism will remain hard to quantify. Examination of particular cases suggests many possible reasons for the discrepancies. Consideration of the satellite and radar cloud observations for the 1991 Pinatubo eruptions shows that marked differences can exist even with apparently good observations. The problem can be understood largely as a sampling issue, as the most widely reported parameter, the maximum cloud height, is highly sensitive to the frequency of observation. Satellite and radar cloud heights also show a pronounced clumping near the height of the tropopause and relative lack of eruptions reaching only the mid-troposphere, reinforcing the importance of the tropopause in determining the eruption height in convectively unstable environments. To reduce the discrepancies between ground and satellite estimates, a number of formal collaboration measures between vulcanological, meteorological and aviation agencies are suggested.  相似文献