1980—2020年大湾区海岸线变迁及影响因素分析

海岸线动态变化是全球变化和人类活动共同的反映。本文基于粤港澳大湾区、东京湾和旧金山湾1980—2020年7期Landsat系列遥感影像及Google Earth高分辨率影像, 利用阈值分割, 结合水体指数法、Sobel算子法, 提取各期海岸线。从长度、空间形态、结构和利用程度等多角度分析其岸线变化, 并结合地理探测器对其影响因素进行定性和定量分析。结果显示: 1) 1980—2020年间, 各湾区岸线趋于平直, 其中东京湾海岸线的年均长度变化强度最大, 为0.37%; 2) 40a间各湾区岸线的纵深变化比较稳定, 结构趋于复杂, 形态趋于分散, 其中粤港澳大湾区海岸线的分维差异最小, 形态最分散; 3) 40a间, 各湾区的自然岸线减少, 港口码头岸线和其他人工岸线长度剧烈增长, 其中粤港澳大湾区的生物岸线波动增长, 岸线利用程度指数增幅最大。本文研究结果表明, 气温、波高、潮汐和陆域面积、港口吞吐量是湾区海岸线变化的主要影响因素, 且任意两个影响因素的交互作用大于单一因素的作用。     

时间序列数字滤波后自由度的确定--应用于日长变化与南方涛动指数的相关分析

原始观测时间序列进行数字滤波后，其自由度将大大降低，对各种数字滤波器都可以通过Monte Carlo方法模拟获得对应置信水平的相关系数临界值，从而得到时间序列滤波后的自由度，如果滤波后的频段宽度与Nyquist频率之比为Z，那么对于理想的单边和双边滤波器，时间序列滤波后的自由度为原始值的Z／2和Z倍，非理想滤波器一般不符合此规律。     

Determination of longitudinal dispersivity in an unconfined sandy aquifer

Study of the mobility of contaminants in an aquifer is an important issue for the proper remediation of contaminated groundwater. Determination of associated solute transport parameters therefore is essential for investigation of the extent to which groundwater can be contaminated. This study aimed at determining solute transport parameters for an unconfined sandy aquifer at a laboratory scale through various tracer tests using a conservative solute as a tracer. Tracer tests consisted of both well‐tracer tests (single and double wells) and an aquifer tracer test using a plume‐capturing device such as time domain reflectometry (TDR). The results showed that longitudinal dispersivities estimated from the single and double well‐tracer tests were 2·2 cm and 13·5 cm for a travel distance of 9·3 cm and 13·5 cm from the injection point respectively. These results agreed reasonably well with the results of the aquifer tracer test. The solute transport parameters obtained at multiple points in the aquifer through the aquifer tracer test revealed that the dispersivity length was proportional to the travel distance by a factor of 0·3, which was moderately higher than the value of 0·1 given in the literature. Copyright © 2002 John Wiley & Sons, Ltd.     

Modeling mineral dust emissions from Chinese and Mongolian deserts

The present study investigates the frequency and intensity of mineral dust emissions over the deserts of eastern Asia from 1996 to 2001. Mineral dust emissions are simulated using a physical dust emission scheme over a region extending from 35.5°N to 47°N and from 73°E to 125°E. The input parameters required by the dust emission model are (1) surface features data including aerodynamic roughness length, soil dry size distribution and texture; and (2) meteorological surface data, mainly wind speed, soil moisture and snow cover. The way by which these surface features and meteorological data can be assessed is described and discussed. The influence of soil moisture and snow cover is taken into account and their effects on simulated dust emission are quantified.The simulations reproduce on a daily basis the location and intensity of the severe events of April 1998 and spring 2001 as recorded by the meteorological stations and/or described in various studies. Based on 6 yr of simulations, the main dust source regions are identified and their relative contributions to the total dust emissions are quantified.The seasonal cycle of the dust storms frequency is well reproduced with a maximum in spring. The simulations suggest that it is mainly controlled by the emissions occurring in the Taklimakan desert in latter spring and in summer, and by those occurring in the northern deserts of China in winter. The Taklimakan desert appears to be the most frequent and steady source of dust emissions during the studied period. On the other hand, in the Gobi desert, only a few dust emission events are simulated, but the dust amount emitted during each event is generally very large. In the northern deserts of China, dust emissions are frequent and their intensity is variable.These results show an important annual and inter-annual variability of the emitted dust (between 100 Mt yr^− 1 and 460 Mt yr^− 1), mainly controlled by the occurrence of severe events in the Gobi desert and in the northern deserts of China.     

地貌分形理论模型的数值模拟

利用简单分形模型和分数布朗运动模型，分别对分形地貌研究中的多度域分形曲线和外营力作用下地貌剖线自仿射分形进行了模拟计算。模拟结果显示，不同机制作用下的地貌形态分维值差异不大的时候，从分维结构图上无法获得相应的多度域分维值，这时需要借助其它手段进行分析；不同起伏的地表形态可以具有相同的分维值，夷平作用并不改变由地表侵蚀作用形成的分维值，表现出外营力作用的相对稳定性，要全面描述曲线的起伏特性需要引入渡越长度。     

Absence of initial singularities in superstring cosmology

In a universe whose elementary constituents are point particles there does not seem to be any obvious mechanism for avoiding the initial singularities in physical quantities in the standard model of cosmology. In contrast in string theory these singularities can be absent even at the level where spacetime is treated classically. This is a consequence of the basic degrees of freedom of strings in compact spaces, which necessitate a reinterpretation of what one means by a very small universe. We discuss the basic degrees of freedom of a string at the classical and quantum level, the minimum size of strings (string uncertainty principle), the t-duality symmetry, and string thermodynamics at high energy densities, and then describe how these considerations suggest a resolution of the initial singularity problem. An effort has been made to keep this writeup self-contained and accessible to non-string theorists.     

平面贴片天线的研究

介绍了半波谐振贴片的理论,并利用HFSS分别对采用微带和同轴两种方式馈电的中心频率为12GHZ的平面贴片天线进行了仿真.仿真结果表明:当改变微带与同轴传输线馈电位置时,对于微带馈电方式,要实现单频点,取贴片的长边中点效果较好;如果偏离该中心点,将具有双频点特性.而采用同轴馈电时,所研究的几个馈电点位置中也是贴片长边中点相对较好,如偏离该中心点,频率将偏离中心频率.     

低对比度扩展目标跟踪算法

针对如太阳表面米粒结构和太阳黑子这类低对比度扩展目标，研究了互相关因子和绝对差分两种跟踪算法的有效性，并给出了根据所采集的图像进行后处理所得到的小整体倾斜信号，此外还比较了去除整体倾斜前后的太阳表面米粒结构长曝光像的对比度。     

Measurements of attenuation and absorption lengths with the KASCADE experiment

The attenuation of the electron shower size beyond the shower maximum is studied with the KASCADE extensive air shower (EAS) experiment in the primary energy range of about 10¹⁴–10¹⁶ eV. Attenuation and absorption lengths are determined by applying different approaches, including the method of constant intensity, the decrease of the flux of EASs with increasing zenith angle, and its variation with ground pressure. We observe a significant dependence of the results on the applied method. The determined values of the attenuation length ranges from 175 to 196 g/cm² and of the absorption length from 100 to 120 g/cm². The origin of these differences is discussed emphasizing the influence of intrinsic shower fluctuations.     

Displacement and transport of marked pebbles,cobbles and boulders during floods in a steep mountain stream

In a small experimental catchment of the Dolomites (Rio Cordon, 5 km²) field observations have been carried out on the movement of various sized bed material particles. Displacement length of 860 marked pebbles, cobbles and boulders (0·032 < D < 0·512 m) has been measured along the river bed during individual snowmelt and flood events in the periods 1993–1994 and 1996–1998. Floods were grouped into two categories. The first includes ‘ordinary’ events, which are characterized by peak discharges with a return period of 1–5 years and by an hourly bedload rate not exceeding 20 m³ h^?1. The second refers to ‘exceptional’ events with a return period of 50–60 years. A flood of this latter type occurred on 14 September 1994, with a peak discharge of 10·4 m³ s^?1 and average hourly bedload rate of 324 m³ h^?1. The variation according to grain size of total displacement length L_i depends on the degree of mobilization of the individual fractions of the bed surface: L_i is independent of D_i for smaller, fully mobile grain sizes and decreases rapidly with D_i for larger fractions in a state of partial transport. Sustained selective transport without a supply of sediment from upstream leads to the development of a stable coarse armoured surface through progressive winnowing of finer material from the bed surface. With supply unlimited conditions for transport, both the occurrence of extreme events and the duration of a sequences of ‘ordinary’ floods play an important role in the degree of mobilization of the individual fractions of the bed. Copyright © 2004 John Wiley & Sons, Ltd.