西南印度洋海温异常影响亚洲夏季风爆发的数值试验

利用中国科学院大气物理研究所的9层大气环流模式(IAP9—AGCMⅡ)作了西南印度洋海温月异常对亚洲夏季风爆发影响的数值试验。试验结果表明，当该海域1—3月份的海温出现异常增暖时，印度夏季风和东亚夏季风的爆发均较平常晚，反之，二者的建立均较平常早；该海域1—3月份的海温异常对亚洲季风区的降水也有明显的影响。     

冠脉循环的血流动力学分析

冠状动脉疾病作为最常见的心血管疾病严重威胁人类的生命．而对冠脉循环的认识与对该种疾病的诊治具有重要的作用．本文就冠状血管的形态计量学、动物实验和数学建模及计算机仿真这几个方面，回顾了冠脉循环的血流动力学分析方法的进展，论述了冠脉循环中血压和血液的分布及其影响因素以及研究的发展方向．     

2003 vs 2002: A large amplitude wintertime temperature anomaly reversion event and its anomalous atmospheric circulation

It is revealed that there happened a large amplitude wintertime temperature anomaly reversion event (LTAR) in Northern Hemisphere high latitude regions and South Australia for the year 2003 versus 2002, with the most notable change in Eurasia, eastern North America, North Pacific, and South Australia. The accompanying atmospheric general circulation anomalies are analyzed and the dominant changes in the circulation are found out. The anomalous cyclonic eddies over the north Pacific and the anomalous anticyclonic eddies over North Europe that cooperate each other are mostly linked with the event. Both anomalous eddy systems are connected with the remote teleconnection patterns respectively. The research also suggests the existence of a cross-equator teleconnection pattern, namely, the Northern Pacific-Western Pacific-Australia teleconnection pattern (NPWPA). It is not only related to LTAR, but also associated with the temperature transition from cold episode to warm episode in the year 2003 versus 2002 during December-January-February.     

Change in the tilting of the ridgeline surface of the subtropical anticyclone and the predictability of the onset of the Asian summer monsoon

The NCEP/NCAR reanalysis data are used to study the relationships among the change in the tilting of the ridgeline surface of the subtropical anticyclone, the establishment of the so-called "seasonal transition axis (STA)" and the onset of the Asian summer monsoon. It is shown that the monsoon onset is characterized by the overturning of the meridional temperature gradient (MTG) in the vicinity of the ridgeline surface. A MTG index is then constructed to investigate the predictability of the Asian summer monsoon onset conceptually. Data diagnoses show that if the initial MTG is known and the meridional gradient across the ridgeline surface of the local temperature tendency can be estimated, a late or early onset of the summer monsoon can be qualitatively predicted in advance.     

玻色-爱因斯坦凝聚体中的三角涡旋格子

 讨论了玻色-爱因斯坦凝聚体中的三角涡旋格子,从磁光阱里玻色-爱因斯坦凝聚体波函数满足的Gross-Pitaevskii方程求出三角格子的解,并简要解释了相关实验观察结果.     

一类特殊静态查找问题的解决方法

查找就是在按某种数据结构形式存储的数据集合中 ,找出满足指定条件的结点 .为了确定指定条件的结点存在与否 ,称为静态查找 .就实际问题中存在的局部范围内有序问题采用了小范围循环列表查找的方法 ,对传统的静态查找算法加以改进 ,使程序运行的效率大大提高     

青藏高原：全球气候变化的驱动机与放大器──Ⅲ．青藏高原隆起对气候变化的影响

新生代出现的几次重大气候变化事件与青藏高原形成过程中经历的几次强烈构造运动在发生年代上的良好对应关系表明两者存在紧密的联系．或许正是青藏高原的隆起导致了气候的巨大变化和现代东亚季风的形成及加强．高大的高原对大气系统有两个重要影响，热力作用和动力作用．它们在亚洲冬季形成蒙古高压、夏季形成印度低压，从而导致东亚季风出现．青藏高原越高，其对大气的作用越显著，形成的蒙古高压、印度低压和东亚季风越强大．因此，东亚季风的形成和加强是青藏高原隆起的结果．东亚季风的加强和高原动力作用使西风带波动增加，造成冰期极地冷空气不断南侵、气候波动变大．青藏高原抬升和季风造成的化学风化增强还使大气ＣＯ２含量降低、气候变冷．因此，青藏高原隆起是控制新生代气候变化的重要因素．     

从粗线条长距离的物理学发展到21世纪中国的科技前途

本文首先对物理学,特别是近代物理学的起源、发展过程及其影响进行了阐述。文中述及近代物理学起源于17世纪,经过一百多年(1666～1800)的发展,在欧洲近代的科学观念开始萌芽,并逐渐开花、结果。到19世纪近代物理学有了长足进步,并大大刺激了工业的发展。19世纪末20世纪初,由于相对论、广义相对论和量子力学的创立,使整个物理学出现了革命性的进展。此后,从1930年开始物理学进入了一个新的纪元,以固体物理学和液体物理学、原子和分子物理学、核物理学、基本粒子物理学为标志的近代物理学蓬勃兴起。本文认为,物理学的发展与技术的发展,是一连锁循环,而技术的发展与经济的发展又是一连锁循环。因而世界各国竞相重视,大量投资于物理学尖端的研究。本文后部分对中国科技的发展进行了回顾和展望,指出中国古代科学技术在世界上处于领先地位,但1600年后中国科技发展长期停滞,落后于西方科技300年。最后,本文对新中国成立后科学技术的突飞猛进作了高度评价,并预言21世纪中国将成为世界科技强国。     

计算浅水环流的波方程模式

对计算浅水环流的波方程模式进行了研究，指出了波方程模式的解在什么条件下满足质量守恒；并证明了空间离散误差不会影响该模式对非物理短波干扰的衰减，所以波方程模式具有较好的抑制短波振荡的特性。     

Uplift of the Tibetan Plateau and environmental changes

Major progress, problems, and challenges of recent investigation of the Tibetan Plateau uplift processes and resulting environmental changes are reviewed and summarized briefly, which especially covers the National Tibetan Research Projects of the Chinese Eighth (1992-1996) and Ninth (1997-2001) "Five-Year Projects". The Tibetan Plateau uplift is a complicated multiple cyclic process. The Gangdise and Himalayas began to uplift in the Middle Eocene and Early Miocene respectively, while the main part of the Plateau merely underwent corresponding passive deformation and secular denudation, resulting in two planation surfaces. The third and also the strongest uplift involved the whole Plateau and its marginal mountains commenced at 3.6 Ma. Successive Kunlun-Huanghe movement at 1.1-0.6 Ma and Gonghe movement at 0.15 Ma raised the Plateau to its present height. The Asian monsoonal system and Asian natural environment formed in response to these tectonic uplifts.