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991.
This paper reviews the progress of population geography in China since the 1980s. The review results suggest that contrary to the common perception of its invisibility and marginalized status in the field, tremendous progress has been made in population geography in China since the 1980s. Population geographers have made significant contribution to the understanding of a wide range of population issues from geographical perspectives, including migration, urbanization, population distribution, the relationships between population, environment and resources, aging, marriage patterns, and migrants’ crimes, although such contribution often did not appear in the geographical circle. Furthermore, population geographers have played an indispensable role in revitalizing population studies in China and forging its links to human geography, occupying an important position in this multi-disciplinary field. Population geographers’ contribution to the areas of migration and urbanization research has been particularly significant, reflected in their leading roles in these areas’ research. The paper demonstrates that as latecomers in the field after more than 20 years of isolation, population geographers in China have gone through a process of catching up and increasing engagement with developments in social sciences and increasing interaction with social scientists since the 1980s, and have benefited greatly from it; however, there is a tendency for population geography to be increasingly alienated from the main stream human geography, a phenomenon similar to but not exactly the same as Anglo-American geography in the late 1990s and early 2000s. The paper argues that population geography is only half way in the course to forge the links between population studies and human geography, and it needs to return to geographical sciences to strike a healthy balance between the field of population studies and that of human geography, and promote its further development in a multi-disciplinary field.  相似文献   
992.
Based on observations of urban mass concentration of fine particulate matter smaller than 2.5 μm in diameter (PM2.5), ground meteorological data, vertical measurements of winds, temperature, and relative humidity (RH), and ECMWF reanalysis data, the major changes in the vertical structures of meteorological factors in the boundary layer (BL) during the heavy aerosol pollution episodes (HPEs) that occurred in winter 2016 in the urban Beijing area were analyzed. The HPEs are divided into two stages: the transport of pollutants under prevailing southerly winds, known as the transport stage (TS), and the PM2.5 explosive growth and pollution accumulation period characterized by a temperature inversion with low winds and high RH in the lower BL, known as the cumulative stage (CS). During the TS, a surface high lies south of Beijing, and pollutants are transported northwards. During the CS, a stable BL forms and is characterized by weak winds, temperature inversion, and moisture accumulation. Stable atmospheric stratification featured with light/calm winds and accumulated moisture (RH > 80%) below 250 m at the beginning of the CS is closely associated with the inversion, which is strengthened by the considerable decrease in near-surface air temperature due to the interaction between aerosols and radiation after the aerosol pollution occurs. A significant increase in the PLAM (Parameter Linking Aerosol Pollution and Meteorological Elements) index is found, which is linearly related to PM mass change. During the first 10 h of the CS, the more stable BL contributes approximately 84% of the explosive growth of PM2.5 mass. Additional accumulated near-surface moisture caused by the ground temperature decrease, weak turbulent diffusion, low BL height, and inhibited vertical mixing of water vapor is conducive to the secondary aerosol formation through chemical reactions, including liquid phase and heterogeneous reactions, which further increases the PM2.5 concentration levels. The contribution of these reaction mechanisms to the explosive growth of PM2.5 mass during the early CS and subsequent pollution accumulation requires further investigation.  相似文献   
993.
为了研究苏州地区大气边界层结构的日变化及季节特征,利用2014年1—7月期间大气颗粒物激光雷达对苏州上空大气气溶胶进行了连续观测。选定2014年1月15日、3月16日、5月7日与7月22日全天的消光系数探测数据,通过优化后的梯度法得到了该地区的大气边界层高度,分析了其日变化特征,并分析了边界层高度与地表的温湿变化之间的相关性。结果表明除1月15日外,边界层的变化与地表温度存在明显的正相关,而与地表的相对湿度存在负相关。同时,对站点微波辐射计观测得到的温湿廓线与边界层内消光系数廓线进行了联合研究。研究结果表明,微波辐射计湿度垂直廓线与激光雷达消光系数廓线探测得到的边界层具有良好的一致性。  相似文献   
994.
利用我国160个测站1951—2013年冬季月平均气温资料和1951—2016年间冬季太平洋年代际振荡(PDO:Pacific Decadal Oscillation)指数资料,分析了两者在年际和年代际时间尺度上的相关关系,探讨了PDO对我国冬季气温影响的可能物理过程。结果发现:PDO与我国冬季气温年际变化不显著;在冬季期间,PDO对我国气温的影响是滞后的;PDO与我国冬季气温年代际变化存在密切关系,当PDO处于年代际正(负)位相时,我国气温普遍偏高(低);PDO年代际分量对我国的影响机制为:当PDO指数位于年代际正(负)位相时段,海平面气压场上西伯利亚高压减弱(增强),500 hPa高度场东亚大槽强度减弱(增强),200 hPa纬向风场东亚北支急流减弱(增强),这些都有利于我国冬季气温偏高(低)。  相似文献   
995.
996.
Hurricane Isabel made landfall along the North Carolina coast on September 18, 2003 (UTC 17:00) and the storm surge exceeded 2.0 m in many areas of the Chesapeake Bay and in the York River estuary. River flooding occurred subsequently, and the peak river discharge reached 317 and 104 m3 s−1 in the Pamunkey and Mattaponi rivers, respectively. The York River estuary experienced both storm surge and river flooding during the event and the estuary dynamics changed dramatically. This study investigates the hydrodynamics of the York River estuary in response to the storm surge and high river inflows. A three-dimensional model was used to investigate the changes of estuarine stratification, longitudinal circulation, salt flux mechanisms, and the recovery time required for the estuary to return to its naturally evolved condition without the storm. Results show that the salt flux was mainly caused by advection, which was induced by the barotropic gradient during the storm event. The net salt flux increased by a factor of 30 during the rise of the storm surge. However, the large amount of salt transported into the estuary was quickly transported out of the estuary as the barotropic gradient reversed during the descent of the storm surge. Subsequent high freshwater inflow influenced the estuarine circulation substantially. The estuary changed from a partially mixed estuary to a very stratified estuary for a prolonged period. The model results show that it will take about 4 months for the estuary to recover to its naturally evolved salinity distribution after the impacts of the storm surge and freshwater pulse.  相似文献   
997.
沙洲并陆与长江口北部岸线的演变   总被引:4,自引:0,他引:4  
凌申 《台湾海峡》2001,20(4):484-489
全新世以来,长江口北岸南通-扬州南部经历了“浅海-陆地”的成陆过程。4ka,B.P.前,本区为一漏斗形的浅水海湾,河口拦门沙极为发育.4ka.B.P。以来,沙洲并岸,河口陆地淤长,长江口北部岸线呈东南延伸之势。  相似文献   
998.
缢蛏滤除率与颗粒选择性的实验研究   总被引:5,自引:0,他引:5  
利用4种不同大小的单细胞藻类作为饵料研究缢蛏(Sinonovacula constricta)的滤除率以及缢蛏对不同大小料颗粒的选择性。实验结果表明:3种规格缢蛏对4种单细胞藻类的滤除率表现出相同的变化规律,即随藻类规格的增大,缢蛏的滤除率亦逐渐变大,并且大规格缢蛏的滤除率变化最显著;在饵料颗粒选择性的实验中,小规格缢蛏对大规格(ESD=8.83),藻类具有较高的选择性,中规格缢蛏对藻类的选择性不明显,而大规格缢蛏则对小规格(ESD=4.46)藻类具较高的选择性。  相似文献   
999.
海湾扇贝性腺发育的初步研究   总被引:10,自引:0,他引:10  
1992年7月-11月在青岛胶州五号码头养殖海区采集海湾扇贝,定期取样,测壳长、水温,并对性腺进行切片观察,以研究其性腺发育。观察表明,海湾扇贝性腺由3部分构成:滤泡、生殖管和生殖输送管。  相似文献   
1000.
夏季风场对长江冲淡水扩展影响的数值模拟   总被引:7,自引:3,他引:7  
建立一个σ坐标系下三维非线性斜压陆架模式,研究长江冲淡扩展的动力机制。数值试验再现了夏季长江冲淡水转向东北的现象,夏季风场对长江冲淡水扩展的影响,取决于风速的大小和动向,风速为3m/s的南风,对冲淡水向北扩展的影响比较明显,而当南风风速达到6m/s时,则起着十分显著的作用,西南风加强了冲淡水向东扩展,但对南北向的扩展影响甚微,东南风抑了冲淡水向东扩散,并使之偏向西北,明确阐明了夏季风场对冲淡水扩展  相似文献   
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