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| 1 | Detection,Causes and Projection of Climate Change over China:An Overview of Recent Progress显示文摘这篇文章总结中国科学家在过去的五年里进行的研究的主要结果和调查结果。观察到在中国的气候变化与全球一般水准忍受强壮的类似,这被显示出。平均国家的年平均表面气温在过去的 100 年在过去的 50 年和 0.5 0.8 ° C 由 1.1 ° C 增加了,比为一样的时期的全球温度增加稍微高。北中国和冬季在表面空中经历了最大的增加。尽管没有重要趋势在平均国家的年度降水被发现了,内部地区性的规模上的十的可变性和明显的趋势是可检测的与西北的中国和中间、更低的长江盆经历了明显的增加,并且诺思中国严重干旱。一些分析显示出极端天气的那频率和大小,气候事件也在过去的 50 年左右经历了重要变化。地区性的气候的原因的研究通过气候模型和各种各样的 forcings 的考虑的使用变化,温暖最后 50 年能可能被归因于温室气体的增加的大气的集中的表演,当 第20 世纪的第一一半的温度变化可能由于太阳活动时,暴烈的爆发和海面温度变化。在在在东方中国的表面的日照时间和太阳辐射的重要衰落被归因于污染物质的增加的排放。由 NCC 的模型的未来气候的设计(国家气候中心,中国气象学的管理)并且 IAP (大气的物理的研究所,中国科学院),以及 40 个模型海外发展了,显示一个潜力在 第21 世纪的在中国的重要温暖,与最大的温暖设定发生在冬季月内并且在北中国。在改变的排放情形下面,平均国家的年平均温度被投射由 1.5 2.1 ° C 增加 2020,在 2050,并且由在 2100 的 3.9 6.0 ° C 的 2.3 3.3 ° C,与 30 年的一般水准相比 1961 1990。大多数模型在 2100 在中国在年度降水投射 10%12% 增加,与在东北和西北中国是特别地明显的趋势,但是与可能经历一个弄干的趋势的华中的部分。大不确定性在降水,和进一步的研究的设计存在被需要。而且,人为的气候变化将可能在东方亚洲导致更弱的冬季季风和更强壮的夏季风。 | 丁一汇 任国玉 赵宗慈 徐影 罗勇 李巧萍 张锦 | 2007 | Advances in Atmospheric Sciences2007，24，6： | 94 |
| 2 | An Overview of the Semi-arid Climate and Environment Research Observatory over the Loess Plateau显示文摘Arid and semi-arid areas comprise about 30% of the earth’s surface. Changes in climate and climate variability will likely have a significant impact on these regions. The Loess Plateau over Northwest China is a special semi-arid land surface and part of a dust aerosol source. To improve understanding and capture the direct evidence of the impact of human activity on the semi-arid climate over the Loess Plateau, the Semi-Arid Climate and Environment Observatory of Lanzhou University (SACOL) was established in 2005. SACOL consists of a large set of instruments and focuses on: (1) monitoring of long term tendencies in semi- arid climate changes; (2) monitoring of the aerosol effect on the water cycle; (3) studies of interaction between land surface and the atmosphere; (4) improving the land surface and climate models; and (5) validation of space-borne observations. This paper presents a description of SACOL objectives, measurements, and sampling strategies. Preliminary observation results are also reviewed in this paper. | 黄建平 张武 左金清 闭建荣 史晋森 王鑫 常倬林 黄忠伟 杨溯 张北斗 王国印 冯广泓 袁九毅 张镭 左洪超 王式功 符淙斌 丑纪范 | 2008 | Advances in Atmospheric Sciences2008，25，6： | 107 |
| 3 | Fundamental Framework and Experiments of the ThirdGeneration of IAP/LASG World OceanGeneral Circulation Model显示文摘1.IntroductionThefirstbaroclinicoceanicgeneralcirculationmodel(OGCM)developedattheStateKeyLaboratoryofNumericalModelingforAtmosphericSciencesandGeophysicalFluidDynamics(LASG),InstituteofAtmosphericPhysics(IAP)isafour--layermodelwithitshorizontalresol... | 金向泽 张学洪 周天军 | 1999 | Advances in Atmospheric Sciences1999，16，2： | 114 |
| 4 | A Diagnostic Study of the Impact of El Nion on the Precipitation in China显示文摘1.IntroductionEINifioisthemostoutstandinginterannualvariabilityintheocean.Itiswellknownthattheheatsourcedrivingtheatmosphericgeneralcirculationismainlywithinthetropics.EINinooccursinthetropicalPacificandthewarmingoftheoceanduringtheEINinocancoveralar... | 张人禾 | 1999 | Advances in Atmospheric Sciences1999，16，2： | 86 |
| 5 | Climatology and Interannual Variability of the Southeast Asian Summer Monsoon显示文摘ClimatologyandInterannualVariabilityoftheSoutheastAsianSummerMonsoonK.-M.LauLaboratoryforAtmospheres,Code913,NASA-GoddardSpac... | K. M. Lau Song Yang | 1997 | Advances in Atmospheric Sciences1997，14，2： | 123 |
| 6 | The Influence of ENSO on the Summer Climate Change in China and Its Mechanism显示文摘The influence of ENSO on the summer climate change in China and its mechanism from the observed data is discussed. It is discovered that in the developing stage of ENSO, the SST in the western tropical Pacific is colder in summer, the convective activities may be weak around the South China Sea and the Philippines. As a consequence, the subtropical high shifted southward. Therefore, a drought may be caused in the Indo-China peninsula and in the South China. Moreover, in midsummer the subtropical high is weak over the Yangtze River valley and Huaihe River valley, and the flood may be caused in the area from the Yangtze River valley to Huaihe River valley. On the contrary, in the decaying stage of ENSO. the convective activities may be strong around the Philippines, and the subtropical high shifted northward, a drought may be caused in the Yangtze River valley and Huaihe River valley. | 黄荣辉 吴仪芳 | 1989 | Advances in Atmospheric Sciences1989，6，1： | 269 |
| 7 | A Daily Temperature Dataset over China and Its Application in Validating a RCM Simulation显示文摘This paper describes the construction of a 0.5°×0.5°daily temperature dataset for the period of 1961- 2005 over China's Mainland for the purpose of climate model validation. The dataset is based on the in- terpolation from 751 observing stations in China and comprises 3 variables: daily mean,minimum,and maximum temperature.The'anomaly approach'is applied in the interpolation.The gridded climatology of 1971-2000 is first calculated and then a gridded daily anomaly for 1961-2005 is added to the climatologY to obtain the final dataset.Comparison of the dataset with CRU (Climatic Research Unit) observations at the monthly scale shows general agreement between the two datasets.The differences found can be largely attributed to the introduction of observations at new stations.The dataset shows similar interannual vari- ability as does CRU data over North China and eastern part of the Tibetan Plateau,but with a slightly larger linear trend. The dataset is employed to validate the simulation of three extreme indices based on daily mean,minimum,and maximum temperature by a high-resolution regional climate model. Results show that the model reproduces these indices well.The data are available at the National Climate Center of China Meteorological Administration,and a coarser resolution(1°×1°)version can be accessed via the World Wide Web. | 徐影 高学杰 沈艳 许崇海 石英 F.GIORGI | 2009 | Advances in Atmospheric Sciences2009，26，4： | 145 |
| 8 | The Interannual Variability of East Asian Winter Monsoon and Its Relation to the Summer Monsoon显示文摘Based on the NCEP / NCAR reanalysis data the interannual variability of the East Asian winter monsoon (EAWM) is studied with a newly defined EAWM intensity index. The marked features for a strong (weak) winter monsoon include strong (weak) northerly winds along coastal East Asia, cold (warm) East Asian continent and surrounding sea and warm (cold) ocean from the subtropical central Pacific to the tropical western Pacific, high (low) pressure in East Asian continent and low (high) pressure in the adjacent ocean and deep (weak) East Asian trough at 500 hPa. These interannual variations are shown to be closely connected to the SST anomaly in the tropicaI Pacific, both in the western and eastern Pacific. The results suggest that the strength of the EAWM is mainly innuenced by the processes associated with the SST anomaly over the tropical Pacific. The EAWM generally becomes weak when there is a positive SST anomaly in the tropical eastern Pacific (E1 Nino), and it becomes strong when there is a negative SST anomaly (La Nina). Moreover, the SST anomaly in the South China Sea is found to be closely related to the EAWM and may persist to the following summer. Both the circulation at 850 hPa and the rainfall in China confirm the connection between the EAWM and the following East Asian summer monsoon. The possibIe reason for the recent 1998 summer flood in China is briefly discussed too. | 陈文 Han-F.Graf 黄荣辉 | 2000 | Advances in Atmospheric Sciences2000，17，1： | 146 |
| 9 | Interaction between Anomalous Winter Monsoon in East Asia and EI Nino Events显示文摘Based on a series of data analyses, the intimate relations between anomalous winter monsoon in East Asia and El Nino arc studied in this paper.Anomalistic circulation in the Northern Hemisphere caused by El Nino event can lead to enhancing the Ferre! cell and the westerlies in the mid-latitudes as the Hadley cell and result in the location of the front zone in East Asia to the north. These are unfavourable for the cold wave breaking out southward in East Asia. Therefore, there ate warmer weather and weaker winter monsoon in East Asia in El Nino winter.There are stronger and frequent cold waves in East Asia during the wintertime prior to the occurrence of El Nino event. They will induce stronger winter monsoon in East Asia. Thus, the weakened trade wind and enhanced cumulus convection in the equatorial middle-western Pacific area caused by the stronger winter monsoon will play an important role in the occurrence of El Nino event. Therefore, the anomalously strong winter monsoon in East Asia during | 李崇银 | 1990 | Advances in Atmospheric Sciences1990，7，1： | 94 |
| 10 | Changes of Extreme Events in Regional Climate Simulations over East Asia显示文摘使用ResCM2区域气候模式,嵌套澳大利亚CSIRO R21L9全球海气耦合模式,进行了温室效应(二氧化碳加倍)对东亚(主要是中国区域)极端气候事件影响的数值试验。控制试验的结果表明,区域模式能够较好地模拟中国区域的极端气候事件。对温室效应引起的它们的变化进行了信度检验,分析结果表明,温室效应将引起日最高和最低气温增加,日较差减小;使得高温天气增多,低温日数减少。降水日数和大雨日数在一些地区将增加。同时还会引起影响中国的台风活动的变化。 | 高学杰 赵宗慈 Filippo Giorgi | 2002 | Advances in Atmospheric Sciences2002，19，5： | 119 |
| 11 | Western North Pacific Tropical Cyclone Database Created by the China Meteorological Administration显示文摘This paper describes the access to, and the content, characteristics, and potential applications of the tropical cyclone(TC) database that is maintained and actively developed by the China Meteorological Administration, with the aim of facilitating its use in scientific research and operational services. This database records data relating to all TCs that have passed through the western North Pacific(WNP) and South China Sea(SCS) since 1949. TC data collection has expanded over recent decades via continuous TC monitoring using remote sensing and specialized field detection techniques,allowing collation of a multi-source TC database for the WNP and SCS that covers a long period, with wide coverage and many observational elements. This database now comprises a wide variety of information related to TCs, such as historical or real-time locations(i.e., best track and landfall), intensity, dynamic and thermal structures, wind strengths, precipitation amounts, and frequency. This database will support ongoing research into the processes and patterns associated with TC climatic activity and TC forecasting. | Xiaoqin LU Hui YU Ming YING Bingke ZHAO Shuai ZHANG Limin LIN Lina BAI Rijin WAN | 2021 | Advances in Atmospheric Sciences2021，38，4： | 96 |
| 12 | Quick Measurement of CH_4, CO_2 and N_2O Emissions from a Short-Plant Ecosystem显示文摘Combining improved injector, gas line and valve-driving models, a gas chromatograph (GC) equippedwith Hydrogen Flame Ionization Detector (FID) and Electron Capture Detector (ECD), can measureCH4, CO2, and N2O simultaneously in an air sample in four minutes. Test results show that the systemhas high sensitivity, resolution, and precision; the linear response range of the system meets the requirementof flux measurements in situ. The system is suitable for monitoring fluxes of the main greenhouse gases ina short-plant field since it is easy to use, efficacious, and constant and reliable in collecting data. | 王跃思 王迎红 | 2003 | Advances in Atmospheric Sciences2003，20，5： | 122 |
| 13 | An Eddy-Permitting Oceanic General Circulation Model and Its Preliminary Evaluation显示文摘An eddy-permitting, quasi-global oceanic general circulation model, LICOM (LASG/IAP (State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics) Climate System Ocean Model), with a uniform grid of 0.5? × 0.5? is established. Forced by wind stresses from Hellerman and Rosenstain (1983), a 40-yr integration is conducted with sea surface temperature and salinity being restored to the Levitus 94 datasets. The evaluation of the annual mean climatology of the LICOM control run shows that the large-scale circulation can be well reproduced. A comparison between the LICOM control run and a parallel integration of L30T63, which has the same framework but a coarse resolution, is also made to con?rm the impact of resolution on the model performance. On account of the reduction of horizontal viscosity with the enhancement of the horizontal resolution, LICOM improves the simulation with respect to not only the intensity of the large scale circulations, but also the magnitude and structure of the Equatorial Undercurrent and South Equatorial Current. Taking advantage of the ?ne grid size, the pathway of the Indonesian Through?ow (ITF) is better represented in LICOM than in L30T63. The transport of ITF in LICOM is more convergent in the upper layer. As a consequence, the Indian Ocean tends to get warmer in LICOM. The poleward heat transports for both the global and individual basins are also signi?cantly improved in LICOM. A decomposed analysis indicates that the transport due to the barotropic gyre, which primarily stands for the barotropic e?ect of the western boundary currents, plays a crucial role in making the di?erence. | 刘海龙 张学洪 李薇 俞永强 宇如聪 | 2004 | Advances in Atmospheric Sciences2004，21，5： | 68 |
| 14 | 亚洲季风环流在20世纪70年代末之后的减弱(英文)显示文摘全球大气环流自20世纪70年代末之后的转变可以很清楚地在大气温度、风场等的变化上得到发现。子波分析的结果证实这次转变的时间尺度在20年以上。本文的研究着重揭示:在对流层中层,亚洲中纬度区域的转变趋势同全球平均的转变趋势相反;更重要的是,在这次转变之后亚洲和非洲的季风环流变弱了,同时热带东太平洋区的贸易风环流也变弱了。而在降水的变化中也可以发现这次转变。 | 王会军 | 2001 | Advances in Atmospheric Sciences2001，18，3： | 80 |
| 15 | Interannual Meridional Displacement of the East Asian Upper-tropospheric Jet Stream in Summer显示文摘On the interannual timescale, the meridional displacement of the East Asian upper-tropospheric jet stream (EAJS) is significantly associated with the rainfall anomalies in East Asia in summer. In this study, using the data from the National Centers for Environmental Prediction-Department of Energy (NCEP/DOE) reanalysis-2 from 1979 to 2002, the authors investigate the interannual variations of the EAJS's meridional displacement in summer and their associations with the variations of the South Asian high (SAH) and the western North Pacific subtropical high (WNPSH), which are dominant circulation features in the upper and lower troposhere, respectively. The result from an EOF analysis shows that the meridional displacement is the most remarkable feature of the interannual variations of the EAJS in each month of summer and in summer as a whole. A composite analysis indicates that the summer (June-JulyAugust, JJA) EAJS index, which is intended to depict the interannual meridional displacement of the EAJS, is not appropriate because the anomalies of the zonal wind at 200 hPa (U200) in July and August only, rather than in June, significantly contribute to the summer EAJS index. Thus, the index for each month in summer is defined according to the location of the EAJS core in each month. Composite analyses based on the monthly indexes show that corresponding to the monthly equatorward displacement of the EAJS, the South Asian high (SAH) extends southeastward clearly in July and August, and the western North Pacific subtropical high (WNPSH) withdraws southward in June and August. | 林中达 陆日宇 | 2005 | Advances in Atmospheric Sciences2005，22，2： | 79 |
| 16 | A Heavy Sea Fog Event over the Yellow Sea in March 2005: Analysis and Numerical Modeling显示文摘在这篇论文,在 2005 年 3 月 9 日发生在黄海上的一个波涛汹涌的海雾事件被调查。与在它的成熟阶段的几百公里的空间规模,海雾补丁在一些地点沿着山东半岛海岸把可见性归结为 100 m 或少得多。在岛和海岸的卫星图象,表面观察和 soundings,和从日本气象学机构(JMA ) 的分析被用来描述并且分析这个事件。分析显示这海雾能作为使雾凉下来的移流被分类。包括雾区域和它的运动的这海雾的主要特征被大气的研究 Mesoscale 模型(MM5 ) 的第五产生的宾夕法尼亚州的大学 / 公民中心相当复制。模型结果建议这个事件的形成和进化能是被构画出:(1 ) 低级空气的南方的温暖 / 潮湿的移流与大约 600 m 的厚度导致了强壮的 sea-surface-based 倒置;(2 ) 当倒置从更温暖的东方海搬到更冷的黄海时,当海雾响应由混合的骚乱冷却并且弄湿成长了时,热内部边界层(TIBL ) 逐渐地在倒置的底形成了;(3 ) 当 TIBL 向北方移动了,(4 ) 强壮的在北方的寒冷和干旱风破坏了 TIBL 并且驱散海雾,海雾发展了。这研究的主要调查结果是海雾响应相对坚持的南方的温暖 / 潮湿的风和冷海面形成,并且由风切变混合的那骚乱是为使海洋的层凉下来并且弄湿的主要机制。另外,敏感实验的学习显示确定的数字建模提供一答应在黄海而是它上的海雾的预言的途径可能是更有效的认为整体数字因为极端敏感,当模特儿为输入建模。 | 高山红 林行 沈飙 傅刚 | 2007 | Advances in Atmospheric Sciences2007，24，1： | 68 |
| 17 | Influence of the Atlantic Multidecadal Oscillation on the Winter Climate of East China显示文摘大西洋 Multidecadal 摆动(AMO ) ,诺思大西洋海面温度(SST ) 的多十的变化,与 65 80 年和 0.4 ° C 的一个振幅的一个时期展出摆动。观察合成分析表明温暖的阶段 AMO 在华东被连接到更温暖的冬季,与在这个区域的北方的提高的降水和在南方的减少的降水,在多十的时间规模上。模式在冷阶段 AMO 期间被颠倒。当一强迫华东的多十的冬季气候被调查大气的反应在大气的总环流大气环流模型(AGCM ) 的一个大整体温暖 AMO SST 异例探索, AMO 是否行动,试验。从三 AGCM 的结果是一致的并且建议 AMO 温暖在华东赞成更温暖的冬季。这影响通过在从中间的纬度诺思大西洋延长到中间的纬度欧亚大陆的半球宽的领域导致否定表面气压异例被认识到。这些否定表面异例赞成高变弱蒙古的寒冷,并且因此导致更弱的东方亚洲冬季季风。 | 李双林 Gary T.BATES | 2007 | Advances in Atmospheric Sciences2007，24，1： | 72 |
| 18 | Characteristics and Variations of the East Asian Monsoon System and Its Impacts on Climate Disasters in China显示文摘在结构的特征的研究和东方亚洲季风(电动会计记帐机) 的时间空间的变化的最近的进展系统和在中国的严重气候灾难上的这个系统的影响被考察。以前的研究在电动会计记帐机区域改进了我们水平、垂直的结构的基本特征和 EAM 系统和水汽运输的年度周期的理解。许多研究证明了 EAM 系统是亚洲澳大利亚人的季风系统的一个相对独立的分系统,并且那在那里存在有南方的 tripole 模式分布在的明显的伪二年的摆动内部电动会计记帐机系统的年变化。基本物理过程的进一步的分析,内部、外部,那影响 EAM 系统的可变性当 atmosphere-ocean-land 联合了系统,显示 EAM 系统可以被看,在这篇论文指了电动会计记帐机气候系统。进一步,纸讨论在这个系统的各种各样的部件之中的相互作用和关系怎么能在东亚上沿着西的喷气通过东亚太平洋(EAP ) 电视连接模式和南方的 upper-tropospheric 风异例的电视连接模式被描述。如此的推理建议分别地,在 Yangtze 和 Huaihe 河山谷的严重洪水和在诺思中国的延长干旱的出现被连接到背景内部 EAM 气候系统的年度、内部的十的可变性。而且,与电动会计记帐机系统有关的突出的科学问题和它在中国的气候灾难上的影响也被讨论。 | 黄荣辉 陈际龙 黄刚 | 2007 | Advances in Atmospheric Sciences2007，24，6： | 76 |
| 19 | An Overview of Research and Forecasting on Rainfall Associated with Landfalling Tropical Cyclones显示文摘The ability to forecast heavy rainfall associated with landfalling tropical cyclones (LTCs) can be improved with a better understanding of the mechanism of rainfall rates and distributions of LTCs. Research in the area of LTCs has shown that associated heavy rainfall is related closely to mechanisms such as moisture transport, extratropical transition (ET), interaction with monsoon surge, land surface processes or topographic effects, mesoscale convective system activities within the LTC, and boundary layer energy transfer etc.. LTCs interacting with environmental weather systems, especially the westerly trough and mei-yu front, could change the rainfall rate and distribution associated with these mid-latitude weather systems. Recently improved technologies have contributed to advancements within the areas of quantitative precipitation estimation (QPE) and quantitative precipitation forecasting (QPF). More specifically, progress has been due primarily to remote sensing observations and mesoscale numerical models which incorporate advanced assimilation techniques. Such progress may provide the tools necessary to improve rainfall forecasting techniques associated with LTCs in the future. | 陈联寿 李英 程正泉 | 2010 | Advances in Atmospheric Sciences2010，27，5： | 74 |
| 20 | Temporal and Spatial Characteristics of Extreme Hourly Precipitation over Eastern China in the Warm Season显示文摘Based on hourly precipitation data in eastern China in the warm season during 1961-2000,spatial distributions of frequency for 20 mm h 1 and 50 mm h 1 precipitation were analyzed,and the criteria of short-duration rainfall events and severe rainfall events are discussed.Furthermore,the percentile method was used to define local hourly extreme precipitation;based on this,diurnal variations and trends in extreme precipitation were further studied.The results of this study show that,over Yunnan,South China,North China,and Northeast China,the most frequent extreme precipitation events occur most frequently in late afternoon and/or early evening.In the Guizhou Plateau and the Sichuan Basin,the maximum frequency of extreme precipitation events occurs in the late night and/or early morning.And in the western Sichuan Plateau,the maximum frequency occurs in the middle of the night.The frequency of extreme precipitation (based on hourly rainfall measurements) has increased in most parts of eastern China,especially in Northeast China and the middle and lower reaches of the Yangtze River,but precipitation has decreased significantly in North China in the past 50 years.In addition,stations in the Guizhou Plateau and the middle and lower reaches of the Yangtze River exhibit significant increasing trends in hourly precipitation extremes during the nighttime more than during the daytime. | 张焕 翟盘茂 | 2011 | Advances in Atmospheric Sciences2011，28，5： | 72 |
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