拟线性双曲型方程组的奇性

考虑一类拟线性退化特征双曲型方程组Cauchy问题,利用特征线法和局部延拓法证明了其经典解的整体存在性.结果表明,对于具退化特征双曲型方程组Cauchy问题在一定条件下存在整体经典解.     

带权Burger方程的初边值问题的整体光滑解

考虑带权Ｂｕｒｇｅｒ方程的初边值问题,构造性地证明了整体光滑解的存在性．     

基于GPS/GIS/RS集成技术的物流监控管理

阐述全球定位系统GPS（Global Position System)，地理信息系统GIS（Geographical Information System)，遥感RS（Remote Sensing)技术（简称3S）的基本特征，相互关系及其集成基本方式，并针对现代物流管理状况和发展趋势，借助3S技术集成的优势，探讨性研究3S技术集成在物流监控管理，其应用前景广阔。     

二维阻尼Gross-Pitaevskii(GP)方程的整体解

考察一类描述吸引Bose Einstein凝聚(BEC)的二维阻尼Gross Pitaevskii(GP)方程iφt=-Δφ+｜x｜2φ-｜φ｜2φ+ia｜φ｜4φ,t≥0,x∈R2,a<0.借鉴文献(CommunMathPhys,1983,87:567～576.)关于经典Schr dinger方程研究的思想和结果,建立GP方程与一个经典的非线性数量场方程的对应关系,得到方程的整体解存在的一个充分条件.     

一类总体极值问题的进化计算法

给出一类总体极值问题的进化计算方法 ,研究了进化计算随机搜索的机制特征     

具功能反应的食饵与捕食者两种群模型的极限环

研究了具功能反应的食饵与捕食者两种群模型：{dx/dt=x(θ1 θ2x-θ3x^2-y),dy/dt=y(-1 x).讨论了该系统平衡点的性态，并证明了权限环的存在性与惟一性及其全局稳定性。     

一类带记忆边界条件的抛物型方程的爆破问题

本文讨论了一类带记忆边界条件的半线性抛物型方程的爆破问题.利用上下解方法,结合积分估计本文给出了方程的解在有限时刻爆破或整体存在的充分条件,并证明了某些条件下解的爆破只能在边界上发生.     

Interdecadal trend turning of global terrestrial temperature and precipitation during 1951–2002

A grid-by-grid counting of interdecadal trend turning (ITT) of annual mean surface air temperature (SAT) and total precipitation at 67,359 terrestrial grids in the period 1951–2002 is presented. An analysis of the last ITTs of SAT and total precipitation in the period, in the context of both occurrence time and linear trends after the breakpoint, indicates that a warming trend has become highly significant across most of the world in the late 20th Century. Most terrestrial grids have recorded an ITT of total precipitation in either the 1970s or 1980s, and 45.7% of the terrestrial grids in the study have seen a decreasing trend in total annual precipitation after the breakpoint, with the remaining 54.3% having experienced an increasing trend. Basically, global terrestrial regions have experienced either an increasingly warm and dry climate or an increasingly warm and wet climate. An analysis of ITT of regional mean SAT and total precipitation in 22 regions shows the northern American continent has become increasingly warm and dry after the last inter-decadal breakpoint. Meanwhile, the African continent has become increasingly warm and wet, with both Europe and most of Asia having the same trend. Southern South America and the west of Australia have experienced an opposite trend in climate, becoming increasingly cold and wet.     

Unrami?ed extensions of quadratic ?elds

Let K be a global quadratic ?eld, then every unrami?ed abelian extension of K is proved to be absolutely Galois when K is a number ?eld or under some natural conditions when K is a function ?eld. The absolute Galois group is also determined explicitly.     

Interdecadal trend turning of global terrestrial temperature and precipitation during 1951-2002

A grid-by-grid counting of interdecadal trend turning (ITT) of annual mean surface air temperature (SAT) and total precipitation at 67,359 terrestrial grids in the period 1951-2002 is presented. An analysis of the last ITTs of SAT and total precipitation in the period, in the context of both occurrence time and linear trends after the breakpoint, indicates that a warming trend has become highly significant across most reagent of the world in the late 20th Century. Most terrestrial grids have recorded an ITT of total precipitation in either the 1970s or 1980s, and 45.7% of the terrestrial grids in the study have seen a decreasing trend in total annual precipitation after the breakpoint, with the remaining 54.3% having experienced an increasing trend. Basically, global terrestrial regions have experienced either an increasingly warm and dry climate or an increasingly warm and wet climate. An analysis of ITT of regional mean SAT and total precipitation in 22 regions shows that the Northern American continent has become increasingly warm and dry after the last interdecadal breakpoint. Meanwhile, the African continent has become increasingly warm and wet, with both Europe and most of Asia having the same trend. Southern South America and the West of Australia have experienced an opposite trend in climate, becoming increasingly cold and wet.