海洋与湖沼1993年总目录第24卷

第1期均匀水底上二维随机波面的二阶谱·································……孙孚、丁平兴、余宙文(1)杭州湾潮波三维数值模拟....········..··········································……李身铎、顾思美(7)渤海局部海域风暴潮漫滩的数值模拟··········································……史峰岩、孙文心(16)用实测海水透明度数据和NOAA卫星数据计算黄海悬浮体含量···············…     

著名鱼类学和淡水生态学家刘建康教授

刘建康（LinJiankang）鱼类学和淡水生态学家。汉族。1917年9月1日出生，籍贯江苏省吴江。1938年毕业于苏州东吴大学生物系，获理学学士学位。1947年毕业于加拿大麦基尔大学研究生院，获哲学博士学位。现任中国科学院水生生物研究所研究员，名誉所长。曾任该所淡水生态与生物技术开放研究实验室（国家重点实验室）首届主任。我国首批博士学位研究生导师。1980年当选为中国科学院学部委员，生物学部常委。目前担任我国“人与生物圈”国家委员会委员，中国海洋湖沼学会副理事长，《海洋与湖沼》学报、师国海洋湖沼学报》和《生态学报惯性编等…     

A Scientist of Oceanic Geology – Prof. Qin Yunshan

QinYunshan,SeniorScientist,InstituteofOceanology,AcademiaSinica.Male,borninShandongProvinceonJulle1,1933.GraduatedfromBeijingCollegeofGeologyin1956.DirectoroftheInstituteofOceanology,AcademiaSinica;DirectoroftheChineseSocietyofOceanologyandLimnology,Editorof"GeologyofBohaiSea"(SciencePress,1985)and"GeologyofEastChinaSea"(SciencePress,1988).HepublishedinvariousChineseandwor1djournalsmoretban50papers,suchas"PrimarystudyonthereliefandsedimenttypeofthecontinentalshelfofChina"(Ocean…     

青年海洋地质学家──李乃胜

李乃胜，男，1957年7月出生，山东寿光人。于1981年毕业于青岛海洋大学，1985年在中国科学院海洋研究所研究生毕业。1993-1994年，在美国TexasA＆M大学客座研修。现任中国科学院海洋研究所研究员，自1995年为所领导成员之一。兼任中国海洋湖沼学会青年工作委员会主任，中国海洋地质学会理事，美国地球物理联合会（AGU）会员。主要从事海洋地球物理学与海底构造学调查研究，研究海域主要是西北太平洋边缘海，如黄海、东海、南海、菲律宾海等等。曾多次主持国家科技攻关、国家自然科学基金及中科院院长择优基金主持项目，也曾本持中日合作…     

四川运动及其在中国之分布

中国中生代末期之造山运动发生于白垩纪之末或白垩纪与第三纪之间,并非如翁文灏氏所说燕山乙墓发生于上下白垩纪之间,此期运动我们称之为四川运动,其时期与北美之拉惹米运动相当。四川运动之强烈程度难各地互有差异,但分布则最广泛,遍及各省。四川运动在四川省表现最为强烈,在云南、西康、贵州、陕西南部,甘肃中部,宁夏、察哈尔、热河等省都县最重要的造山运勤,台湾省之始新统前造山运动尚不能定其确期,可能亦是这一幕,在其他各省,虽有时不是最重要的造山运动,但其影响则都曾见到。     

中国地质调查局、中国地质科学院2015年度地质科技十大进展新鲜出炉

中国地质调查局、中国地质科学院2015年度地质科技十大进展评选于2015年12月23—24日在北京召开, 评选工作由中国地质调查局组织, 中国地质科学院具体实施。经来自国土资源部、科技部、中国科学院、国家自然科学基金委员会等多家单位的38位院士、专家和用户代表投票,“神狐及其邻近海域天然气水合物资源勘查取得重大突破”等十项成果脱颖而出, 入选2015年度地质科技十大进展。本次评选的“地质科技十大进展”集中代表了2015年度中国地质调查和地学研究的重要进展, 这些地质科技成果在解决资源环境问题和基础地质问题、实现转化应用和有效服务、推动科学理论创新和技术方法进步、促进人才成长和团队建设等方面成效显著, 发挥出科技支撑引领找矿突破、服务生态文明建设的作用, 对社会各界了解我国地质行业为国民经济发展所作的贡献、对提高地质行业的社会认知度起到积极作用。     

基于DEM的单窗算法及山区地表长波净辐射的计算

地表温度和长波净辐射是地表能量平衡中两个重要的能量项。首先对单窗算法应用于山区的可行性进行了分析,然后依据DEM和大气温度、湿度轮廓线对地表气温和湿度进行空间上的插值。在计算出每个像元上的气温值和湿度值基础上求算出单窗算法所需要的两个主要的大气参数分布图——大气平均作用温度分布图和大气透过率分布图,从而将单窗算法推广应用于地形起伏悬殊的山区,以计算各个高程上的地表温度。通过建立基于DEM的山地热辐射传输模型,计算每个像元来自于周围地形的热辐射分量,引用大气向下长波辐射公式计算其分量,并依据长波辐射平衡方程计算山区各个像元的长波净辐射。     

Empirical evaluation of microtremor H/V spectral ratio

The objective of this work is to perform a purely empirical assessment of the actual capabilities of the horizontal-to-vertical (H/V) spectral ratio technique to provide reliable and relevant information concerning site conditions and/or site amplification. This objective has been tackled through the homogeneous (re)processing of a large volume of earthquakes and ambient noise data recorded by different research teams in more than 200 sites located mainly in Europe, but also in the Caribbean and in Tehran. The original recordings were first gathered in a specific database with information on both the sites and recorded events. Then, for all sites close to an instrumented reference, average site-to-reference spectral ratios (“spectral ratio method” (SSR)) were derived in a homogeneous way (window selection, smoothing, signal-to-noise ratio threshold, averaging), as well as H/V ratios (“HVSRE–RF”) on earthquake recordings. H/V ratios were also obtained from noise recordings at each site (either specific measurements, or extracted from pre- or post-event noise windows). The spectral curves resulting from these three techniques were estimated reliable for a subset of 104 sites, and were thus compared in terms of fundamental frequency, amplitude and amplification bandwidth, exhibiting agreements and disagreements, for which interpretations are looked for in relation with characteristics of site conditions. The first important result consists in the very good agreement between fundamental frequencies obtained with either technique, observed for 81% of the analyzed sites. A significant part of the disagreements correspond to thick, low frequency, continental sites where natural noise level is often very low and H/V noise ratios do not exhibit any clear peak. The second important result is the absence of correlation between H/V peak amplitude and the actual site amplification measured on site-to-reference spectral ratios. There are, however, two statistically significant results about the amplitude of the H/V curve: the peak amplitude may be considered as a lower bound estimate of the actual amplification indicated by SSR (it is smaller for 79% of the 104 investigated sites), and, from another point of view, the difference in amplitude exhibits a questioning correlation with the geometrical characteristics of the sediment/basement interface: large SSR/HV differences might thus help to detect the existence of significant 2D or 3D effects.