长江流域径流量变化过程及其对ENSO和PDO的响应

根据宜昌站、汉口站和大通站的径流量数据,运用M-K检验和小波分析等方法,对1900年以来长江流域径流量的趋势和周期变化进行分析,探究径流量变化对厄尔尼诺?南方涛动（ENSO）和太平洋年代际振荡（PDO）的响应。结果表明：1900 年以来长江流域径流量呈显著的减少趋势,并具有2~8 a的年际周期变化和14~17 a的年代际周期变化。流域径流量与ENSO具有相同的2~8 a周期变化,在El Ni?o发生期,径流量较低,在La Ni?a发生期,径流量较高。14~17 a的周期变化与PDO相关,在暖位相期径流量偏少,在冷位相期径流量偏多。PDO影响着ENSO和径流量之间的相关性,在暖位相期,El Ni?o对径流量的影响增强,在冷位相期,La Ni?a对径流量的影响增强。因此,在分析和预测流域径流量长时间尺度上的变化时要综合考虑ENSO和PDO的影响。     

围绕南海问题的信息权力作用过程与机制研究

2010年以来,南海争端呈现扩大化和复杂化的态势,形成环南海周边国家侵占岛礁、域外国家广泛介入的局面,进而推动南海问题日益走向“国际化”。分析南海问题中的国家（地区）间合作与冲突关系,挖掘南海问题“复杂化”的深层原因,这是理解当前南海局势、避免战略误判的重要支撑。文章借助GDELT新闻媒体数据库,提取2013—2021年有关南海问题的事件数据,利用年代约束聚类方法将南海问题划分为矛盾上升期（2013—2018年）和域外介入期（2019年以后）,并利用社会网络分析方法探讨南海问题中的国家（地区）间合作与冲突关系以及背后的信息生产网络。研究发现：1）矛盾上升期,围绕南海问题的合作与冲突主体主要为环南海国家;2）域外介入期,美国、英国、澳大利亚等域外国家结盟合作并围堵中国,中国在与域内国家紧密合作的同时,却成为冲突关系网络的核心,冲突关系复杂、合作关系萎缩与当前人们对南海问题有所缓和的认知形成矛盾,反映信息权力的作用愈发深远;3）信息生产网络中,美、英、澳等国家主导信息制造和加工过程,表明南海问题成为各信息行为体博弈的角力场。     

国际经济地理学研究的知识图谱分析

基于Web of Science核心数据库收录的1982－2020年7 260篇期刊论文及其参考文献,借助CiteSpace绘制国际经济地理学的知识图谱,梳理该领域的知识基础、研究热点和研究前沿。结果发现：1）知识基础的演进轨迹遵循了新区域主义——制度、社会、文化、演化转向的时序变化,21世纪以来,关系、演化经济地理学下的经典文献成为主要的知识来源。2）研究热点突出,创新和增长始终是研究核心,近年来韧性、全球生产网络、金融地理、全球城市、不平等、企业家精神等成为新的研究热点。3）研究前沿具有较强的问题导向,主要基于西方发达国家的产业发展实践。4）研究空间呈现英美主导的两级格局,大部分国家仍处于边缘地带。5）国际经济地理学呈现明显的数字转向、可持续转型趋势,新冠疫情对学科走向也有一定影响。借鉴国际研究经验,中国经济地理学应加强理论创新并提出具有中国实践特色的理论体系,同时推动多学科之间的交叉融合并加强从社会学视角解读社会经济活动的地理学意义。     

儿童地理学视角下的留守儿童研究述评

文章通过梳理在WOS（Web Of Science）核心数据集、谷歌学术、中国知网（CNKI）等平台筛选出的较高引用率、方法比较规范、与留守儿童主题相关性强的国内外文献159篇,从理论层面总结了儿童地理学研究的新转向：关注儿童与空间的关系,强调儿童在空间使用中的主体性,重视不同情境下儿童地理体验的差异性。并梳理了跨国迁移背景下留守儿童的3个研究主题：从空间视角探讨留守儿童的日常生活实践;从主体性出发探讨儿童在迁移链中的体验;在童年的差异性基础上讨论本土儿童的问题。同时从问题视角和积极视角分析了国内城乡迁移背景下留守儿童的研究主题,指出因现有研究范式中的经验主义和成人中心主义而存在的局限性。尝试勾勒出符合中国情境的留守儿童研究新范式,提出留守儿童的日常生活空间,留守儿童的能动性、异质性和多样性是国内留守儿童研究亟需关注的内容。呼吁学者采用历时和动态的研究设计,充分展现儿童如何理解、体验和应对复杂的流动背景下的日常生活。     

Tephra stratigraphy on the North Icelandic shelf: extending tephrochronology into marine sediments off North Iceland

Tephra stratigraphical and tephrochronological studies of marine core MD99‐2275 on the North Icelandic shelf have revealed 58 new tephra horizons within the last 7050 cal. a BP, bringing the total number of identified tephra layers to 76. So far, over 100 tephra layers have been identified in the entire core spanning the last 15 000 years. The majority of the newly identified tephra layers are basaltic in composition and originate from the most active volcanic systems in Iceland, namely Grímsvötn, Veidivötn‐Bárdarbunga and Katla. A total of 40 tephra layer land–sea correlations have been made within this time period, of which 16 represent absolutely dated tephra markers. In addition, two tephra marker series are revealed in the marine sediments and in the terrestrial tephra stratigraphy, located between c. 2300–2600 and between 5700–5900 years. For the last 15 000 years, 21 tephra markers have been recognized. The marine tephra layer frequency (TLF) reveals two peaks, within the last 2000 years, and between 5000 and 7000 years ago. It shows the same general characteristics as the terrestrial TLF curve in Iceland, which indicates that marine sediments can yield important information about volcanism in Iceland. This is useful in time segments in which terrestrial records are poor or non‐existent. The study contributes to a high‐resolution tephrochronological framework on the North Icelandic shelf, with core MD99‐2275 representing a potential stratotype section in the area, and for the northern North Atlantic–Nordic Seas region, as well as being an important contribution to the Lateglacial–early Holocene volcanic history of Iceland.     

Assessment of code bias variations of BDS triple-frequency signals and their impacts on ambiguity resolution for long baselines

GPS Solutions - Carrier phase ambiguity resolution over long baselines is challenging in BDS data processing. This is partially due to the variations of the hardware biases in BDS code signals and...     

Delineation of different phytoplankton communities in the East China Sea mackerel and carangoid fishing ground

Delineation of phytoplankton communities in this study was based on: 1) cluster analysis by Preston's Equation (1962) and 2) analysis of the number of individuals. Results obtained by these two methods were very similar to that obtained in a previous study (Fig. 1, Gu and Guo, 1982) based on analysis of the number of planktonic species of different ecological nature. Among these three methods, that based on cluster analysis (by which some subcommunities could be recognized) proved to be the best. Contribution No. 1841 from the Institute of Oceanology, Academia Sinica.     

不同约束对GPS观测网平差结果的影响

对卫星轨道和测站坐标的约束程度设计了 4种方案 ,对中国地壳运动观测网络10 18GPS周的基准站观测数据进行了试验研究。结果显示 :松驰轨道和紧约束 IGS站方案的结果与紧约束轨道和 IGS站方案的结果基本一致 ,认为这与先验坐标的精确度较高有关。其他方案之间存在较大的差别。最后讨论了大尺度 GPS监测网数据处理时参考基准的选择问题 ,认为一般情况下 ,应该使用全球解 H文件 ,把平差结果归算到全球参考框架中     

“95.8”川西大暴雨成因分析

通过对“９５．８”大暴雨过程的全面技术总结，揭示了多种尺度系统间相互作用对产生大暴雨过程的贡献，并指出了云团的发生及其发展源于北方冷空气和南方低空急流持续影响所形成的两个中间尺度垂直环流。     

Isolation,purification and characterization of the hydrogen evolution promoting factor of hydrogenase ofSpirulina platensis

A component (s-factor) with obvious promoting effect on hydrogen evolution of hydrogenase has been isolated and extracted from a cell-free preparation ofSpirulina platensis. The effect of the s-factor in the reaction system is similar to that of Na₂S₂O₄, but is coupled with light. The s-factor has the maximum absorption peak at 620 nm in the oxidized state, at 590 nm in the reduced state. The partially purified s-factor showed two bands by SDS-PAGE and is distinctly different from phycocyanin, which has no change of oxidized state and reduced state absorption spectra, and also has no promoting effect on hydrogenase ofSpirulina platensis under the light. The research supported by the NSFC.