基于组合算法的水下地形匹配技术          下载免费PDF全文

龙涛  王虎彪  边少锋  纪兵 《海洋测绘》2021,41(3):24-27

利用地形信息辅助惯性系统导航,能有效地约束误差的累积,匹配算法作为地形辅助导航的核心,不同的算法在匹配精度和时间上各有特点.为了改善单一算法的缺陷,以水下地形辅助导航应用为背景,根据这些算法的特性,提出了一种将TERCOM算法和SITAN算法进行组合的方案,综合了两种算法的特性,引入可靠性比值,并在地形条件差异较大的两...  相似文献   

耦合气溶胶气候模式FGOALS-f3-L模拟青藏高原地区气溶胶特性          下载免费PDF全文

Min Zhao  Tie Dai  Hao Wang  Bian He  Qing Bao  Yimin Liu  Guangyu Shi 《大气和海洋科学快报》2021,14(2):60-66

基于新耦合气溶胶气候模式FGOALS-f3-L模拟分析了2002-2011年青藏高原地区气溶胶时空分布特征.结果表明:青藏高原地区,沙尘,硫酸盐,碳质气溶胶(包括黑碳,有机碳和混合碳)地表质量浓度分别占比为53.6％,32.2％,14.2％;在拉萨站点,模拟的气溶胶地表质量浓度被低估,尤其是黑碳和有机碳气溶胶;模拟的气...  相似文献   

非定常过程对大气边界层的内参数与风廓线的影响(二)          下载免费PDF全文

赵鸣  钟世远  卞新棣 《气象学报》1988,46(2):210-218

本文用大气边界层运动方程的数值积分研究了当边界层顶风向不变但风速变化时对大气边界层的内参数u_*/A(u_*为摩擦速度,A为上界风速)和α角(地面风与上界风向的交角)的影响。设上界处风速随时间指数增加及减少,最后趋于定常。在大气正、斜压时,u_*/A及α角的时间变化均是振幅衰减的振荡,最后趋于定常时相应的值。在时间变化过程中的任一时刻,内参数值与当上界条件取该时刻上界风时的定常解结果有一定的差别,严格说,定常时的内参数值并不能直接用于当上界风非定常时。本文还考虑了上界风速非定常对风廓线的影响。  相似文献   

Stochastic mechanics-based Bayesian method calibrating the constitutive parameters of the unified model for clay and sand with CPTU data     

Fu  Yanbin  Ma  Chengtao  Bian  Yuewei  Lv  Guiyang  Hu  Yu  Wang  Changhong 《Acta Geotechnica》2022,17(10):4577-4598

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新疆泥火山发育区场地震陷灾害机理探讨          下载免费PDF全文

许世阳  柴少峰  尹光华  王平  蒲小武 《地震工程学报》2021,43(1):63-69

粒度组分是影响黄土震陷的重要因素之一.通过采集新疆艾其沟泥火山泥质碎屑喷出样品和泥火山发育区域出露的沉积剖面泥质碎屑样品,利用激光粒度分析测试的实验方法对样品进行粒度测试,分别对样品中值(Md)、均值(Mz)、标准偏差(σφ)、偏度(SK1)、峰度(KG)等粒度参数进行分析.研究结果显示:艾其沟泥火山泥质沉积物粒度组分...  相似文献   

The Cretaceous volcanic succession around the Songliao Basin,NE China: relationship between volcanism and sedimentation     

Pujun Wang  Yanguang Ren  Xuanlong Shan  Shaobo Sun  Chuanbiao Wan  Weihua Bian 《Geological Journal》2002,37(2):97-115

With volume ratio of 8:1:1.5 amongst acidic, intermediate and basaltic rocks, the Cretaceous volcanics around the Songliao Basin are a series of high‐K or medium‐K, peraluminous or metaluminous, calc‐alkaline rocks, lacking typical basalts and peralkaline members of typical rift‐related types. Their eruption ages range between 133 and 127 Ma, 124 and 122 Ma and 117 and 113 Ma respectively. They are high in total (Rare earth element) REE contents (96.1–326 ppm), enriched in LREE and depleted in HREE (LREE/HREE = 4.6–13.8), with negative Eu and Ce anomalies (Eu/Eu* = 0.04–0.88; Ce/Ce* = 0.60–0.97). They have enriched large‐ion lithophile elements (e.g. K, Ba, Th) and depleted high field strength elements (e.g. Nb, Ti and Y), suggesting a subduction‐related tectonic setting. The volcanic activities migrated from south to north, forming a successively northward‐stepping volcanic series and showing a feature significantly different from the overlying sedimentary sequence striking northeast. Thus, an overlap basin model was proposed. Accompanied by opening of the basin, the volcanogenic succession was formed at the block‐faulting stage (131–113 Ma) owing to the closure of the Mongolia–Okhotsk ocean in the Jurassic and early Cretaceous, while the overlying sedimentary sequence was unconformably deposited at the spreading stage (Albian–Maastrichtian) owing to the oblique subduction of the Pacific plate under the Eurasian plate. The volcanic succession constitutes the lower unit of basin filling and is the forerunner of further basin spreading. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献