混合编程实现电视气象节目中图表的快速处理

随着经济社会的发展,公众对气象信息的需求趋于精细化。通过对电视气象节目中图表要求的分析,介绍了在Windows环境下通过VB编程对气象数据进行处理、分析,以ActiveX的方式调用Matlab、Photoshop等绘图软件二次处理加工,实现气象图表快速生成的思路和方法。利用不同软件的优势和接口技术混合编程可以提升高质量气象图表绘制的自动化程度,使大量气象数据和统计分析结果快速可视化,并通过媒体及时向社会发布,满足公众需求。     

Windows环境下离散点气象要素等值线绘图软件的设计与实现

介绍了用三角网法绘制非规则网格点等值线的基本原理和计算方法及实现过程，并以此方法移植开发了Windows平台下离散点等值线绘图软件，该软件可在东北地区测站要素等值线绘制中使用。     

Windows下VB“面向消息”编程谈

对Windows下VB与C语言混合编程开发Windows应用程序作了一定深度地探讨,对利用“钩子函数”实现VB“面向消息”编程作了详细描述。     

VB和Surfer实现气象等值线的自动绘图

本文主要介绍了在VB环境下利用程序控制Surfer软件,自动绘图气象等值线的方法,成功实现了客户和服务器程序的无缝链接,为开发等值线绘图软件提供了一种简捷、高效的途径。     

基于Windows98的天气图自动填绘软件

基于Windows98平台用Fortran语言开发而成的最新版本的天气图自动填、绘图软件，一改过去DOS环境下的命令行操作方式，通过引入窗口、图标和菜单技术，不仅具有图文并茂的友好操作界面、灵活多样的人机接口方式，而且具有处理资料速度快，填绘图质量好，程度运行稳定可靠等优点。实践证明，它可以满足气象业务台站的使用要求。     

Windows版本NCAR绘图软件包的开发与应用

利用动态链接库技术开发了Windows平台下新版NCAR绘图软件包,可适合各种语言环境下使用,使操作更简单、功能更丰富,满足了当前业务工作的需要。     

Windows版本NCAR绘图软件包的开发与应用

利用动态链接库技术开发了Windows平台下新版NCAR绘图软件包 ,可适合各种语言环境下使用 ,使操作更简单、功能更丰富 ,满足了当前业务工作的需要。     

indows环境下离散点气象要素等值线绘图软件的设计与实现

介绍了用三角网法绘制非规则网格点等值线的基本原理和计算方法及实现过程 ,并以此方法移植开发了Windows平台下离散点等值线绘图软件 ,该软件可在东北地区测站要素等值线绘制中使用。     

Windows环境下离散点气象要素等值线绘图软件的设计与实现

介绍了用三角网法绘制非规则网格点等值线的基本原理和计算方法及实现过程 ,并以此方法移植开发了Windows平台下离散点等值线绘图软件 ,该软件可在东北地区测站要素等值线绘制中使用。     

辽宁省科委日常事务安排管理系统

简要介绍系统结构、功能和编程方案,编程是在Microsoft Windows95环境下,应用数据库开发软件——POWER BUILDER5．0开发成省科委日常事务安排管理系统,在省科委局域网上实现运行、分权限查询的办公自动化系统。     

Native Trees as Biomonitors of Chemical Elements in the Biodiversity Conservation of the Atlantic Forest

The Atlantic Forest, a hotspot in the world with a great diversity of plants and animals, is located in the most industrialized area of Brazil, a potential source of chemical elements for the atmosphere. From its original area about 10% has been preserved mainly through the implementation of conservation units, among which the Parque Estadual Carlos Botelho (PECB) is one of the most representative. Here, leaves of the predominant species in the PECB were analyzed by instrumental neutron activation analysis (INAA) for the establishment of natural backgrounds of As, Ba, Br, Ca, Cd, Ce, Co, Cs, Fe, Hg, K, Na, Rb, Sc, Se, Sr and Zn. Biomonitoring of the Atlantic Forest was realized through the tree community study taking in account the interspecies and the intraspecies variability of chemical concentrations. Results pointed out the low status of pollution based on the concentrations of chemical elements of environmental concerning. However, Br concentrations were higher in the understory species, which could be related to the possible effects of atmospheric pollution or sea influence. In addition, some Hyeronima alchorneoides trees showed to be hyperaccumulators of Co.     

A Brief Introduction to Marine Meteorological Science Experiment Base at Bohe Town,Maoming City,Guangdong Province

<正>With the support of specialized funds for national science institutions,the Guangzhou Institute of Tropical and Marine Meteorology,China Meteorological Administration set up in October 2008 an experiment base for marine meteorology and a number of observation systems for the coastal boundary layer,air-sea flux,marine environmental elements,and basic meteorological elements at Bohe town,Maoming city,Guangdong province,in the northern part of the South China Sea.     

Trees,forests and water: Cool insights for a hot world

Forest-driven water and energy cycles are poorly integrated into regional, national, continental and global decision-making on climate change adaptation, mitigation, land use and water management. This constrains humanity’s ability to protect our planet’s climate and life-sustaining functions. The substantial body of research we review reveals that forest, water and energy interactions provide the foundations for carbon storage, for cooling terrestrial surfaces and for distributing water resources. Forests and trees must be recognized as prime regulators within the water, energy and carbon cycles. If these functions are ignored, planners will be unable to assess, adapt to or mitigate the impacts of changing land cover and climate. Our call to action targets a reversal of paradigms, from a carbon-centric model to one that treats the hydrologic and climate-cooling effects of trees and forests as the first order of priority. For reasons of sustainability, carbon storage must remain a secondary, though valuable, by-product. The effects of tree cover on climate at local, regional and continental scales offer benefits that demand wider recognition. The forest- and tree-centered research insights we review and analyze provide a knowledge-base for improving plans, policies and actions. Our understanding of how trees and forests influence water, energy and carbon cycles has important implications, both for the structure of planning, management and governance institutions, as well as for how trees and forests might be used to improve sustainability, adaptation and mitigation efforts.     

非轴对称双涡相互作用的研究

在平流动力学的框架内,用准地转正压涡度方程模式实施了19组试验,研究双涡合并的条件及较大尺度涡旋自组织的问题。结果指出:(1)存在着两个影响双涡合并的因素,即初始双涡中心之间的距离和初始涡旋的非轴对称分布。初始两个对称涡旋合并具有明显的临界距离效应,但初始两个非轴对称涡旋能否合并还受到初始涡旋的非对称结构的复杂影响。(2)存在着两类不同的较大尺度涡旋的自组织过程,形成较大尺度涡旋。第一类,初始两个涡旋相同,均呈轴对称分布。双涡作用经历了缓变、快变,以及涡量羽翼的生成、拉伸和发展的过程,合并后呈对称性流型;终态涡内区涡量的堆积来源于两个初始涡,终态涡外区的螺旋带来源于两个初始涡外缘线涡量羽翼的拉伸。第二类,初始两个涡旋不同,一个为椭圆型,一个为偏心型,均呈非轴对称分布。双涡作用中,椭圆涡一边互旋,一边向计算区域中心靠近,同时涡量范围加大,形成了终态涡的内核区;偏心涡一边互旋,一边被不断拉伸,形成了终态涡的螺旋带区;表现出终态涡内区的涡量堆集来源于椭圆涡,终态涡外区螺旋带主要来源于偏心涡的反复拉伸及断裂的特性。     

Atmospheric Dioxin and Furan Deposition in Relation to Land-Use and Other Pollutants: A Survey with Lichens

Polychlorodibenzeno-dioxins and polychlorodibenzeno-furans (PCDD/Fs) are considered among the most toxic compounds on earth. The aim of the present study was to evaluate atmospheric PCDD/F deposition and identify the areas with greater deposition of these compounds in an important industrialized and urbanized region of Portugal, using lichens as biomonitors. For this purpose, samples of the lichen Xanthoria parietina were collected at 60 sampling sites, covering urban, industrial, forestry and agriculture areas, and analyzed for PCDD/Fs, sulfur, nitrogen, zinc, iron, chromium, lead, cobalt, nickel, copper, calcium, manganese, magnesium and potassium. The concentrations of PCDD/Fs in lichens were compared with the other elements and related to land-use and population density. The results obtained through the geostatistical interpolations and after principal component analysis have shown that PCDD/F deposition estimated by lichens is greater near industrial and highly populated urban areas. We found that lichens are suitable biomonitors of PCDD/F atmospheric deposition and can contribute to a better knowledge of air quality in a region, enabling identification of critical pollutant deposition areas.     

日本多主体适应气候变化框架机制及对中国的启示——基于法律政策的视角

通过系统梳理日本适应气候变化法律政策的发展历程,分析日本多主体适应气候变化的框架机制,结合其目前具体的适应实践进展,总结出可供中国借鉴的经验启示。研究发现,日本适应气候变化法律政策的发展经历了由重减缓、轻适应,到上升至国家战略,再到立法这3个阶段,形成了以国家、国立环境研究所、地方公共团体、地区气候变化适应中心、企业和居民为主体的多主体适应框架,从科研成果与决策应用转化、适应信息“共享—反馈—更新”有效循环、建立跨地区合作平台、适应资金支持、实施进度监测管理等5个方面构建了多主体适应气候变化机制。目前日本各适应主体逐步开展适应气候变化实践,但适应工作仍处于初期阶段,适应信息共享体系、跨地区合作细则以及适应政策实施效果评价体系有待进一步完善。结合日本的法律政策经验和中国具体情况,提出了中国应科学定位适应气候变化法律地位、加快立法进程,完善“监测评估—信息共享—适应行动—效果评价”多主体适应框架的机制体制,引导企业采取气候风险管理和适应性商业活动,提高居民的适应认知和适应能力的政策建议。     

Biogenic Volatile Organic Compounds (VOC): An Overview on Emission, Physiology and Ecology

This overview compiles the actual knowledge of the biogenic emissions of some volatile organic compounds (VOCs), i.e., isoprene, terpenes, alkanes, alkenes, alcohols, esters, carbonyls, and acids. We discuss VOC biosynthesis, emission inventories, relations between emission and plant physiology as well as temperature and radiation, and ecophysiological functions. For isoprene and monoterpenes, an extended summary of standard emission factors, with data related to the plant genus and species, is included. The data compilation shows that we have quite a substantial knowledge of the emission of isoprene and monoterpenes, including emission rates, emission regulation, and biosynthesis. The situation is worse in the case of numerous other compounds (other VOCs or OVOCs) being emitted by the biosphere. This is reflected in the insufficient knowledge of emission rates and biological functions. Except for the terpenoids, only a limited number of studies of OVOCs are available; data are summarized for alkanes, alkenes, carbonyls, alcohols, acids, and esters. In addition to closing these gaps of knowledge, one of the major objectives for future VOC research is improving our knowledge of the fate of organic carbon in the atmosphere, ending up in oxidation products and/or as aerosol particles.     

Assessment of Temperature Extremes in China Using RegCM4 and WRF

This study assesses the performance of temperature extremes over China in two regional climate models(RCMs),RegCM4 and WRF, driven by the ECMWF's 20 th century reanalysis. Based on the advice of the Expert Team on Climate Change Detection and Indices(ETCCDI), 12 extreme temperature indices(i.e., TXx, TXn, TNx, TNn, TX90 p, TN90 p,TX10 p, TN10 p WSDI, ID, FD, and CSDI) are derived from the simulations of two RCMs and compared with those from the daily station-based observational data for the period 1981–2010. Overall, the two RCMs demonstrate satisfactory capability in representing the spatiotemporal distribution of the extreme indices over most regions. RegCM performs better than WRF in reproducing the mean temperature extremes, especially over the Tibetan Plateau(TP). Moreover, both models capture well the decreasing trends in ID, FD, CSDI, TX10 p, and TN10 p, and the increasing trends in TXx, TXn, TNx, TNn, WSDI, TX90 p,and TN90 p, over China. Compared with observation, RegCM tends to underestimate the trends of temperature extremes,while WRF tends to overestimate them over the TP. For instance, the linear trends of TXx over the TP from observation,RegCM, and WRF are 0.53?C(10 yr)^-1, 0.44?C(10 yr)^-1, and 0.75?C(10 yr)^-1, respectively. However, WRF performs better than RegCM in reproducing the interannual variability of the extreme-temperature indices. Our findings are helpful towards improving our understanding of the physical realism of RCMs in terms of different time scales, thus enabling us in future work to address the sources of model biases.     

气候变化知识传播之思考

本文试图从经典的大众传播学基本理论和模式入手,梳理现有气候变化知识产品的编制方式、主要传播途径和相关实践经验,以期为未来气候变化信息传播研究和实践提供参考。分析表明,气候变化知识传播过程应遵循信息传播的基本规律,并充分考虑气候变化知识自身所具有的复杂性和交叉性特点;在信息采集方面,应注重知识的科学性、系统性、准确性和权威性;在展示方式方面,应注重内容的可读性、趣味性、精练性和通俗性;在传播途径方面,除传统的大众媒介外,还需要注重利用新兴的互联网、社交媒体等平台,发挥人际关系网络作用;在国家经济社会发展的新形势下,需要进一步加强气候变化知识传播的理论、模式和实践等方面的创新性研究。     

Dominant cloud microphysical processes of a torrential rainfall event in Sichuan,China

High-resolution numerical simulation data of a rainstorm triggering debris flow in Sichuan Province of China simulated by the Weather Research and Forecasting (WRF) Model were used to study the dominant cloud microphysical processes of the torrential rainfall. The results showed that: (1) In the strong precipitation period, particle sizes of all hydrometeors increased, and mean-mass diameters of graupel increased the most significantly, as compared with those in the weak precipitation period; (2) The terminal velocity of raindrops was the strongest among all hydrometeors, followed by graupel’s, which was much smaller than that of raindrops. Differences between various hydrometeors’ terminal velocities in the strong precipitation period were larger than those in the weak precipitation period, which favored relative motion, collection interaction and transformation between the particles. Absolute terminal velocity values of raindrops and graupel were significantly greater than those of air upward velocity, and the stronger the precipitation was, the greater the differences between them were; (3) The orders of magnitudes of the various hydrometeors’ sources and sinks in the strong precipitation period were larger than those in the weak precipitation period, causing a difference in the intensity of precipitation. Water vapor, cloud water, raindrops, graupel and their exchange processes played a major role in the production of the torrential rainfall, and there were two main processes via which raindrops were generated: abundant water vapor condensed into cloud water and, on the one hand, accretion of cloud water by rain water formed rain water, while on the other hand, accretion of cloud water by graupel formed graupel, and then the melting of graupel formed rain water.