中国气象科学研究院2007年度发表SCI（E）、EI、CSCD期刊论文

2007年度中国气象科学研究院共有23个项目获得国家自然科学基金资助，其中包括青年科学基金项目9项，面上项目10项，科学部主任基金2项，重点项目1项以及重大研究计划重点项目1项。     

国家973“我国南方致洪暴雨”项目2008年度工作取得重要进展

2008年是国家重点基础研究发展计划项目“我国南方致洪暴雨监测与预测的理论和方法研究”实施的第4年,也是项目研究工作取得重要进展的一年。2008年,在国家科技部和中国气象局的大力支持下,在项目首席科学家张人禾研究员和项目专家组领导下,经过7个课题负责人的精心组织和合理安排及项目组80多名研究人员的共同努力,我国南方暴雨研究在一些关键科学问题上取得了重要进展,这些进展的取得为本项目圆满完成国家规定的研究任务并实现预期目标奠定了坚实的基础。     

重庆市山洪地质灾害防治气象保障工程项目建设管理与思考

重庆市山洪地质灾害防治气象保障工程是重庆市气象部门"十二五"期间的大型重点建设项目,该文对此项目进行了详细的介绍,通过对项目在建设实施过程中各项管理工作的分析和研究,提出做好项目管理工作的重要性和必要性,为全国各省山洪地质灾害防治气象保障工程的项目建设管理提供了相应的参考。     

规划类清洁发展机制项目开发的政策分析与建议

从规划类清洁发展机制（P-CDM）项目提出的背景出发,介绍了P-CDM项目开发的基本框架,对现阶段开发此类项目在指定国家主管机构审批、开发过程中的技术问题,指定的经营实体审定和减排量销售等方面所面临的困境进行了详细分析。针对上述问题,从政策选择角度,建议进一步完善国家主管机构的管理办法,发挥行业组织和科研机构的优势,解决P-CDM项目开发中存在的技术问题,通过规模效应促进P-CDM项目的市场建设,进一步简化相关的国际规则,以真正降低P-CDM项目开发的交易成本。     

巴彦淖尔紫金有色金属动力系统节能技术改造项目雷击风险评估

巴彦淖尔紫金有色金属有限公司动力系统节能技术改造项目建于内蒙古巴彦淖尔市乌拉特后旗工业园区,利用现行技术规范对该项目进行雷电灾害风险评估,为保证该项目安全可靠实施提供科学的雷电防护设计、风险控制、应急管理等服务。     

从项目融资风险探讨江门市气象科技服务新手段

针对目前气象项目投资来源单一、投资有限而难以达到气象科技服务需求的现状,大胆提出对气象建设项目开展项目融资的理念,并针对项目的融资风险进行客观和科学的分析。     

规划类清洁发展机制项目开发的政策分析与建议

 从规划类清洁发展机制（P-CDM）项目提出的背景出发,介绍了P-CDM项目开发的基本框架,对现阶段开发此类项目在指定国家主管机构审批、开发过程中的技术问题,指定的经营实体审定和减排量销售等方面所面临的困境进行了详细分析。针对上述问题,从政策选择角度,建议进一步完善国家主管机构的管理办法,发挥行业组织和科研机构的优势,解决P-CDM项目开发中存在的技术问题,通过规模效应促进P-CDM项目的市场建设,进一步简化相关的国际规则,以真正降低P-CDM项目开发的交易成本。     

农业气象灾害（干旱和冷害）综合应变防御技术成果转化

该项目属国家科技部“农业科技成果转化资金项目”第一批资助的项目。项目的关键技术是国家科技攻关项目“农业气象灾害防御技术研究”（96—020）的研究成果。申请转化的内容为推广冬小麦干旱综合应变防御集成技术和低温冷害综合防御技术等。项目的创新点是农业干旱综合应变集成防御技术（软硬件相结合）和低温冷害综合防御技术可明显提高防御严重干旱的能力和科学水平，     

赴丹麦Risoe DTU参加培训交流总结

《可再生能源项目——中国风能发展项目》是经中华人民共和国和丹麦王国两国政府共同协商,本着增强两国间在可再生能源和加强发展合作方面的联系,寻求更多可再生能源发展合作契机,于2005年11月签定、决定实施的项目,     

大型新建项目防雷检测服务工作体会

随着我国城市化进程的加快,大型新建项目越来越多,如何规范化的做好大型新建项目的防雷检测服务工作,对我们提出了更高的要求。本文介绍我们在大型新建项目检测服务过程中的工作经验。     

COMPARATIVE ANALYSIS OF VARIOUS DATA OF AIR–SEA TEMPERATURE DIFFERENCE AND ITS VARIATION ACROSS SOUTH CHINA SEA IN THE PAST 35 YEARS

Using the International Comprehensive Ocean-Atmosphere Data Set(ICOADS) and ERA-Interim data, spatial distributions of air-sea temperature difference(ASTD) in the South China Sea(SCS) for the past 35 years are compared,and variations of spatial and temporal distributions of ASTD in this region are addressed using empirical orthogonal function decomposition and wavelet analysis methods. The results indicate that both ICOADS and ERA-Interim data can reflect actual distribution characteristics of ASTD in the SCS, but values of ASTD from the ERA-Interim data are smaller than those of the ICOADS data in the same region. In addition, the ASTD characteristics from the ERA-Interim data are not obvious inshore. A seesaw-type, north-south distribution of ASTD is dominant in the SCS; i.e., a positive peak in the south is associated with a negative peak in the north in November, and a negative peak in the south is accompanied by a positive peak in the north during April and May. Interannual ASTD variations in summer or autumn are decreasing. There is a seesaw-type distribution of ASTD between Beibu Bay and most of the SCS in summer, and the center of large values is in the Nansha Islands area in autumn. The ASTD in the SCS has a strong quasi-3a oscillation period in all seasons, and a quasi-11 a period in winter and spring. The ASTD is positively correlated with the Nio3.4 index in summer and autumn but negatively correlated in spring and winter.     

Could the Recent Taal Volcano Eruption Trigger an El Ni?o and Lead to Eurasian Warming?

正The Taal Volcano in Luzon is one of the most active and dangerous volcanoes of the Philippines. A recent eruption occurred on 12 January 2020(Fig. 1a), and this volcano is still active with the occurrence of volcanic earthquakes. The eruption has become a deep concern worldwide, not only for its damage on local society, but also for potential hazardous consequences on the Earth's climate and environment.     

IMPACT OF ATMOSPHERIC LOW-FREQUENCY OSCILLATION ON THE IMMIGRATION OF NILAPARVATA LUGENS(STL) IN HUNAN AND JIANGXI PROVINCES

Various features of the atmospheric environment affect the number of migratory insects, besides their initial population. However, little is known about the impact of atmospheric low-frequency oscillation(10 to 90 days) on insect migration. A case study was conducted to ascertain the influence of low-frequency atmospheric oscillation on the immigration of brown planthopper, Nilaparvata lugens(Stl), in Hunan and Jiangxi provinces. The results showed the following:(1) The number of immigrating N. lugens from April to June of 2007 through 2016 mainly exhibited a periodic oscillation of 10 to 20 days.(2) The 10-20 d low-frequency number of immigrating N. lugens was significantly correlated with a low-frequency wind field and a geopotential height field at 850 h Pa.(3) During the peak phase of immigration, southwest or south winds served as a driving force and carried N. lugens populations northward, and when in the back of the trough and the front of the ridge, the downward airflow created a favorable condition for N. lugens to land in the study area. In conclusion, the northward migration of N. lugens was influenced by a low-frequency atmospheric circulation based on the analysis of dynamics. This study was the first research connecting atmospheric low-frequency oscillation to insect migration.     

A COMPARATIVE ANALYSIS OF ATMOSPHERIC AND OCEANIC CONDITIONS BEFORE THE OCCURRENCE OF TWO TYPES OF EL NIO EVENTS

The atmospheric and oceanic conditions before the onset of EP El Ni?o and CP El Ni?o in nearly 30 years are compared and analyzed by using 850 hPa wind, 20℃ isotherm depth, sea surface temperature and the Wheeler and Hendon index. The results are as follows: In the western equatorial Pacific, the occurrence of the anomalously strong westerly winds of the EP El Ni?o is earlier than that of the CP El Ni?o. Its intensity is far stronger than that of the CP El Ni?o. Two months before the El Ni?o, the anomaly westerly winds of the EP El Ni?o have extended to the eastern Pacific region, while the westerly wind anomaly of the CP El Ni?o can only extend to the west of the dateline three months before the El Ni?o and later stay there. Unlike the EP El Ni?o, the CP El Ni?o is always associated with easterly wind anomaly in the eastern equatorial Pacific before its onset. The thermocline depth anomaly of the EP El Ni?o can significantly move eastward and deepen. In addition, we also find that the evolution of thermocline is ahead of the development of the sea surface temperature for the EP El Ni?o. The strong MJO activity of the EP El Ni?o in the western and central Pacific is earlier than that of the CP El Ni?o. Measured by the standard deviation of the zonal wind square, the intensity of MJO activity of the EP El Ni?o is significantly greater than that of the CP El Ni?o before the onset of El Ni?o.     

Analysis of Atmospheric Boundary Layer Height Characteristics over the Arctic Ocean Using the Aircraft and GPS Soundings

正ERRATUM to: Atmospheric and Oceanic Science Letters, 4(2011), 124-130 On page 126 of the printed edition (Issue 2, Volume 4), Fig. 2 was a wrong figure because the contact author made mistake giving the wrong one. The corrected edition has been updated on our website. The editorial office is sincerely sorry for any     

Index to Vol.31

正AN Junling;see LI Ying et al.;(5),1221—1232AN Junling;see QU Yu et al.;(4),787-800AN Junling;see WANG Feng et al.;(6),1331-1342Ania POLOMSKA-HARLICK;see Jieshun ZHU et al.;(4),743-754Baek-Min KIM;see Seong-Joong KIM et al.;(4),863-878BAI Tao;see LI Gang et al.;(1),66-84BAO Qing;see YANG Jing et al.;(5),1147—1156BEI Naifang;     

Information for Contributors

正Journal of Meteorological Research is an international academic journal in atmospheric sciences edited and published by Acta Meteorologica Sinica Press,sponsored by the Chinese Meteorological Society.It has been acting as a bridge of academic exchange between Chinese and foreign meteorologists and aiming at introduction of the current advancements in atmospheric sciences in China.The journal columns include Articles.Note and Correspondence,and research letters.Contributions from all over the world are welcome.     

前寒武纪气候演化中的三个重要科学问题

自地球形成至寒武纪将近40亿年（距今46亿～5.4亿年,通常称为前寒武纪）的气候演变是一个具有特殊难度和挑战性的研究领域,同时也是基础和前沿的研究领域。文章选择了前寒武纪气候演化中的三个重要科学问题进行综述：大气演化、两次全球性的冰川期以及暗弱太阳问题。关于大气演化,本文首先描述了大气成分的演化历史,然后简述了影响大气成分演化的三个基本过程：大气逃逸、两次大气氧含量突然增加、碳酸盐-硅酸盐循环及其对气候系统的负反馈作用。两次全球性的冰川期分别发生在古元古代（距今24亿～21亿年）和新元古代（距今8亿～5.8亿年）,文章简述了其成因以及相关的气候模拟结果。暗弱太阳问题是地球历史气候演化的一个经典问题,论文简要地综述了一些最新的研究成果和观点。