Dialogue with the Millennium-Old Hongjue Temple

Hongjue Temple is located in the central district of Xining City,Qinghai Province.It consists of three main courtyards.After entering the entrance gate and the Buddhist Guardian Hall followed behind,we shall see the front courtyard flanked by two bell and drum towers,the middle courtyard with the grand hall housing the three Buddhas the temple mainly worships,and finally the rear courtyard that contains some meditation rooms and a garden.All these magnificent halls,yards,and the garden together create a peaceful and pure land of sanctity amid the bustling city.

The Simplest Possible Fully Correct Solution of the Clay Millennium Problem about P vs. NP. A Simple Proof That P ≠ NP = EXPTIME

In the current paper, I present probably the simplest possible abstract formal proof that P ≠ NP, and NP = EXPTIME, in the context of the standard mathematical set theory of computational complexity and deterministic Turing machines. My previous publications about the solution of the P vs. NP with the same result NP = EXPTIME, to be fully correct and understandable need the Lemma 4.1 and its proof of the current paper. The arguments of the current paper in order to prove NP = EXPTME are even simpler than in my previous publications. The strategy to solve the P vs. NP problem in the current paper (and in my previous publications) is by starting with an EXPTIME-complete language (problem) and proving that it has a re-formulation as an NP-class language, thus NP = EXPTIME. The main reason that the scientific community has missed so far such a simple proof, is because of two factors 1) It has been tried extensively but in vain to simplify the solutions of NP-complete problems from exponential time algorithms to polynomial time algorithms (which would be a good strategy only if P = NP) 2) It is believed that the complexity class NP is strictly a subclass to the complexity class EXPTIME (in spite the fact that any known solution to any of the NP-complete problems is not less than exponential). The simplicity of the current solution would have been missed if 2) was to be believed true. So far the majority of the relevant scientific community has considered this famous problem not yet solved. The present results definitely solve the 3rd Clay Millennium Problem about P versus NP in a simple, abstract and transparent way that the general scientific community, but also the experts of the area, can follow, understand and therefore become able to accept.

Jiujiang:Poetic Landscape Transmission Millennium Culture

In recent years,Jiujiang has been fully integrated into the construction of the Yangtze River National Cultural Park with the deepening of the construction of“the most beautiful shoreline of the Yangtze River for 100 miles”.

论Millennium预约功能体现的服务理念

Millennium系统是当前世界上最先进的图书馆自动化系统之一,在一定程度上代表了未来图书馆自动化系统的发展方向。文章拟从Millennium系统的预约功能出发,评价其两种预约模式的优缺点,并探讨该系统所蕴含的读者服务理念。

Millennium系统编目模块的应用与问题分析

Millennium系统是美国INNOVATIVE公司开发的一个功能齐全的图书馆集成管理系统,其发展已超过25年历史,在国内外拥有众多用户。我馆于2006年引进该系统,本文结合2年的编目模块实践,从数据套录、统计、数据质量控制等方面,全面论述该系统在我馆编目工作中的应用,同时分析其存在的问题并提出解决的办法。

Millennium安装过程中的有关技术问题探讨

Millennium(INNOPAC)是一个大型的图书馆集成管理软件,它的安装是一个相当繁重和复杂的工作。该文讨论了该软件安装过程中几个值得注意的问题。

Millennium软件安装过程中的导入数据处理

讨论在安装M illenn ium(INNOPAC)这一大型图书馆集成管理软件的过程中,如何处理从旧系统迁移数据时经常会遇到的问题。

MILLENNIUM超乳玻切系统的使用与配合

随着科学技术的进步,显微眼科先进设备及新型材料的增多与应用,给过去许多无法治疗的眼后段疾病患者带来了复明的希望.

GE Millennium MG SPECT故障检修1例

机器在做心脏断层采集的时候．Detector 2#有时没有计数．在采集计算机上Stop后．计算机显示屏上显示“Loading Calibration Data”．将整个SPECT关机后重新开机．此时Detector 2#自检不能通过。总是显示“Detector 2 Calibration Radial Axis Err-or”．导致整个机器自检不能通过．无法采集患者影像．

基于Millennium系统的图书清点工作探讨

介绍了利用Millennium系统实现馆藏图书清点的两种方法,并对两种清点方法进行了比较。

GE Millennium VG图像链简介与故障维修

SPECT是通过记录患者体内的放射性核素分布来显像的。要形成一幅图像,必须经过数据采集、处理、传输和图像重建等过程,这是由机器内部一系列功能单元和PCB板协同完成的,

Robot Millennium在应用型高校材料力学教学中的辅助作用

文章针对材料力学中的假设和概念,通过实例说明在应用型高校的材料力学课程的学习中引入商业软件Robot Millennium,利用其强大的绘图能力和计算速度,可以简化计算和绘图的过程,不但能够帮助学生理解,还能够使应用型高校的学生直观地了解到力学概念和假设在实际中的应用依据和例子,提高教学效率并提升教学质量。

Strengthening International Cooperation in the New Millennium

Attheturnofthenewmillennium,IwouldliketoextendthebestwishestoallChineseandforeignfriendsofeconomicandtradecircles,onbehalfofChinaCouncilforthePromotionofInternationalTrade(CCPIT)andChinaChamberofInternationalCommerce(CCOIC).CCPIThasbeendedicatedtopro...

Regional-scale Surface Air Temperature and East Asian Summer Monsoon Changes during the Last Millennium Simulated by the FGOALS-gl Climate System Model

The spatial patterns and regional-scale surface air temperature （SAT） changes during the last millennium,as well as the variability of the East Asian summer monsoon （EASM） were simulated with a low-resolution version of Flexible Global Ocean-Atmosphere-Land-Sea-ice （FGOALS-gl） model.The model was driven by both natural and anthropogenic forcing agents.Major features of the simulated past millennial Northern Hemisphere （NH） mean SAT variations,including the Medieval Climate Anomaly （MCA）,the Little Ice Age （LIA） and the 20th Century Warming （20CW）,were generally consistent with the reconstructions.The simulated MCA showed a global cooling pattern with reference to the 1961-90 mean conditions,indicating the 20CW to be unprecedented over the last millennium in the simulation.The LIA was characterized by pronounced coldness over the continental extratropical NH in both the reconstruction and the simulation.The simulated global mean SAT difference between the MCA and LIA was 0.14°C,with enhanced warming over high-latitude NH continental regions.Consistencies between the simulation and the reconstruction on regional scales were lower than those on hemispheric scales.The major features agreed well between the simulated and reconstructed SAT variations over the Chinese domain,despite some inconsistency in details among different reconstructions.The EASM circulation during the MCA was stronger than that during the LIA The corresponding rainfall anomalies exhibited excessive rainfall in the north but deficient rainfall in the south.Both the zonal and meridional thermal contrast were enhanced during the MCA.This temperature anomaly pattern favored a stronger monsoon circulation.

Variation of Surface Temperature during the Last Millennium in a Simulation with the FGOALS-gl Climate System Model

A reasonable past millennial climate simulation relies heavily on the specified external forcings, including both natural and anthropogenic forcing agents. In this paper, we examine the surface temperature responses to specified external forcing agents in a millennium-scale transient climate simulation with the fast version of LASG IAP Flexible Global Ocean-Atmosphere-Land System model （FGOALS-gl） developed in the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics （LASG/IAP）. The model presents a reasonable performance in comparison with reconstructions of surface temperature. Differentiated from significant changes in the 20th century at the global scale, changes during the natural-forcing-dominant period are mainly manifested in the Northern Hemisphere. Seasonally, modeled significant changes are more pronounced during the wintertime at higher latitudes. This may be a manifestation of polar amplification associated with sea-ice-temperature positive feedback. The climate responses to total external forcings can explain about half of the climate variance during the whole millennium period, especially at decadal timescales. Surface temperature in the Antarctic shows heterogeneous and insignificant changes during the preindustrial period and the climate response to external forcings is undetectable due to the strong internal variability. The model response to specified external forcings is modulated by cloud radiative forcing （CRF）. The CRF acts against the fluctuations of external forcings. Effects of clouds are manifested in shortwave radiation by changes in cloud water during the natural-forcing-dominant period, but mainly in longwave radiation by a decrease in cloud amount in the ant hropogenic- forcing-dominant period.

ISSUES THAT ARE OF IMPORTANCE FOR THE INTERNATIONAL COMMISSION ON RADIOLOGICAL PROTECTION AS THE MILLENNIUM APPROACHES

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When and how will the Millennium Silk Road witness 1.5 °C and 2 °C warmer worlds?

Western China and central Asia are positioned centrally along the Millennium Silk Road,which is regarded as a core region bridging the East and the West.Understanding the potential changes in climate over this core region is important to the successful implementation of the so-called＇Belt and Road Initiative＇（a $1 trillion regional investment in infrastructure）.In this study,both mean and extreme climate changes are projected using the ensemble mean of CMIP5 models.The results show a warming of ～1.5,2.9,3.6,and 6.0 ℃ under RCP2.6,4.5,6.0,and 8.5,respectively,by the end of the twenty-first century,with respect to the 1986-2005 baseline period.Meanwhile,the annual mean precipitation amount increases consistently across all RCPs,with an increase by ～14% with respect to 1986-2005 under RCP8.5.The warming over the Millennium Silk Road region reaches 1.5 ℃ before 2020 under all the emission scenarios.The 2020s （2030s） see a 2 ℃ warming under the RCP8.5 （RCP4.5） scenario.Global warming that is 0.5 ℃ lower （i.e.a warming of 1.5 ℃） could result in the avoidance of otherwise significant impacts in the Silk Road core region-specifically,a further warming of 0.73 ℃ （with an interquartile range of 0.49%-0.94 ℃） and an increase in the number of extreme heat days by 4.2,at a cost of a reduced increase of 2.72% （0.47%-3.82%） in annual precipitation.The change in consecutive dry days is region-dependent

Interannual Climate Variability Change during the Medieval Climate Anomaly and Little Ice Age in PMIP3 Last Millennium Simulations

In this study, we analyzed numerical experiments undertaken by 10 climate models participating in PMIP3（Paleoclimate Modelling Intercomparison Project Phase 3） to examine the changes in interannual temperature variability and coefficient of variation（CV） of interannual precipitation in the warm period of the Medieval Climate Anomaly（MCA） and the cold period of the Little Ice Age（LIA）. With respect to the past millennium period, the MCA temperature variability decreases by 2.0% on average over the globe, and most of the decreases occur in low latitudes. In the LIA, temperature variability increases by a global average of 0.6%, which occurs primarily in the high latitudes of Eurasia and the western Pacific. For the CV of interannual precipitation, regional-scale changes are more significant than changes at the global scale, with a pattern of increased（decreased） CV in the midlatitudes of Eurasia and the northwestern Pacific in the MCA（LIA）. The CV change ranges from-7.0% to 4.3%（from -6.3% to 5.4%）, with a global average of -0.5%（-0.07%） in the MCA（LIA）.Also, the variability changes are considerably larger in December–January–February with respect to both temperature and precipitation.

Erratum to “The Riemann Hypothesis-Millennium Prize Problem” [Advances in Pure Mathematics 6 (2016) 915-920]

The original online version of this article (Durmagambetov, A.A. (2016) The Riemann Hypothesis-Millennium Prize Problem. Advances in Pure Mathematics, 6, 915-920. 10.4236/apm.2016.612069) unfortunately contains a mistake. The author wishes to correct the errors in Theorem 2 of the result part.