透视大学校园洋节热背后的西方价值观渗透

当今大学校园里的"洋节"热,根源是西方社会的文化和价值观的渗透。这就需要教育工作者对大学生的思想成长给予足够的重视和关注,从加强爱国主义教育、民族传统文化教育和社会主义核心价值观教育几个方面努力,提高当代大学生的政治思想觉悟。

商业营销视角下“洋节热”的冷思考

在商业营销环境下,"洋节"被包装成了集娱乐、狂欢和购物为一体的节日文化盛宴,"洋节热"现象愈发引起社会关注。本文从商业营销视角梳理"洋节"在中国的发展脉络,然后拨开商业喧嚣的表象,辩证理性地分析"洋节热"现象的影响,提出通过推销文化创意产品、创作优质的艺术作品、增添时尚的文化元素等方式搭乘商业文明的快车弘扬中国优秀传统节日文化的冷静思考。

对“洋节热”现象的反思——打铁还需自身硬

近年来"洋节热"和"传统节日冷"现象引起了学界和普通民众层面的重视和广泛讨论,结论不一。这实则是在全球化和社会转型双重作用下的文化自觉的表现。节日作为一种社会文化现象,其内在功能渗透于社会的方方面面,并通过作用于人影响一国发展。可以以传统节日为落脚点,加强宣传教育、注重形式方法、调动社会各阶层的力量,达到在世界文化交融中保持中国特色、弘扬传统文化的效用。

关于“洋节热”现象的思考

本文从文化研究角度对“洋节热”这一现象进行了解读。文章主要从亚文化和大众文化的视角分析了“洋节热”现象。“洋节热”首先是作为一种亚文化产生的，后来由于受到商业化和青年心理的影响，成为一种大众文化形式。最后探讨了对“洋节热”应持的态度：既要保持中国传统特色，又要避免狭隘的民族主义。

跨文化传播中网络媒体所扮演的角色——以“洋节热”现象为例

现今,跨文化传播活动大量借助于网络媒介,东西方文化交流日益深入",洋节热"就是文化"西进"的结果。在这个过程中,网络新媒体发挥了巨大的推动的作用,但同时网络跨文化交流的缺点也暴露出来。在文化竞争与融合的时代,民族传统文化应保持一种宽容进取的姿态,并有效地利用网络资源进行跨文化传播。

浅析中国“洋节热”的原因——以东西方情人节为例

洋节热近年来引发了大家广泛的热议,通过对中西方情人节为例进行比较,笔者发现洋节热的原因除了大家普遍认为的外来文化的入侵之外,还有着更加深层次的原因,那就是中西方节日形式对于现代人吸引力的差异以及满足现代人需求能力的差异。要想使得中国的传统节日重放光彩,需要各种媒体加大对传统节日的宣传,使得传统节日重新回到人们的视线当中,另外传统节日的内容和形式都应当要顺应时代不断发展创新。

《共产党宣言》文化观视域下“洋节”热探析

《共产党宣言》蕴含着丰富的文化思想。本文以马克思、恩格斯在《共产党宣言》中的文化观视角分析当下中国"洋节"热现象,从"洋节"热的成因、政府态度以及立足于《共产党宣言》理论基础上分析当下"洋节"热现象,使人们以更开放和辩证的态度审视当下"洋节"热现象并坚定文化自信和防止文化殖民主义。

过洋节现象与大学生传统节日文化教育对策探析

针对大学校园出现“洋节热”现象，提出了中国节才是我们节日的主旋律，大学生应该树立正确的节庆观。认为中华传统节日文化蕴涵着宝贵的教育资源，对培养大学生成人成才具有重要作用。认为高校作为从事高等教育的社会组织机构，在保护、传承传统节日文化方面，肩负着自己的特殊历史使命，应采取有效途径，切实加强对大学生传统节日文化的教育工作。

传统节日文化的现代困境及其出路

完全成长于开放时代的当代青年,他们对西方节日的推崇和对传统节日的冷落,一定程度反映了国民对传统文化与西方文化的价值取向。本文从社会政治、经济及观念层面上分析传统节日式微的原因,并对"洋节"热现象作针对性透析,以此提出,只有融合西方节日一些符合时代要求的因素,才能寓教于节,实现传统节日的现代意义。

Seasonal variability of zonal heat advection in the mixed layer of the tropical Pacific

Zonal heat advection （ZHA） plays an important role in the variability of the thermal structure in the tropical Pacific Ocean, especially in the western Pacific warm pool （WPWP）. Using the Simple Ocean Data Assimilation （SODA） Version 2.02/4 for the period 1958-2007, this paper presents a detailed analysis of the climatological and seasonal ZHA in the tropical Pacific Ocean. Climatologically, ZHA shows a zonal- band spatial pattern associated with equatorial currents and contributes to forming the irregular eastern boundary of the WPWP （EBWP）. Seasonal variation of ZHA with a positive peak from February to July is most prominent in the Nifio3.4 region, where the EBWP is located. The physical mechanism of the seasonal cycle in this region is examined. The mean advection of anomalous temperature, anomalous advection of mean temperature and eddy advection account for 31%, 51%, and 18% of the total seasonal variations, respectively. This suggests that seasonal changes of the South Equatorial Current induced by variability of the trade winds are the dominant contributor to the anomalous advection of mean temperature and hence, the seasonality of ZHA. Heat budget analysis shows that ZHA and surface heat flux make comparable contributions to the seasonal heat variation in the Nifio3.4 region, and that ZHA cools the upper ocean throughout the calendar year except in late boreal spring. The connection between ZHA and EBWP is further explored and a statistical relationship between EBWP, ZHA and surface heat flux is established based on least squares fitting.

Super Typhoon Activity over the Western North Pacific and Its Relationship with ENSO

This paper analyzes the characteristics of super typhoons （STYs） over the western North Pacific （WNP） from 1965 to 2005 and describes the seasonal variability of STY activity. The relation between STY activity and the E1 Nifio-Southern Oscillation （ENSO） as well as the possible reason for the influence of the ENSO on STY activity are also investigated. The results showed that about one fifth of the tropical cyclones （TCs） over the WNP could reach the rank of STY. Most STYs appeared from July to November while there was a highest ratio between number of STYs and total number of TCs in November. Most STYs appeared east of the Philippine Sea. In E1 Nino years, affected by sea surface temperature （SST）, monsoon trough and weak vertical wind shear, TC formation locations shifted eastward and there were more STYs than in La Nifia years when the affecting factors changed.

Does a monsoon circulation exist in the upper troposphere over the central and eastern tropical Pacific?

Considering the central and eastern tropical Pacific （CETP） has important climate impacts, and its seasonal variability is also thought to be important, the authors used the monsoon investigation method named ＇dynamical normalized seasonality＇, which can precisely describe the wind vector direction over time, to analyze the upper-tropospheric circulation over the region. The authors discovered that there is a clear reversal of seasonal changes between winter and summer wind, just like the classic monsoon. Accordingly, the authors propose the new concept of the upper- troposphere monsoon over the CETP. The results extend the classical lower-troposphere monsoon region into the upper troposphere.

Effects of air-sea coupling on the eastward propagating boreal winter intraseasonal oscillation over the tropical Indian Ocean

The effects of air-sea coupling over the tropical Indian Ocean（TIO） on the eastward propagating boreal winter intraseasonal oscillation（MJO） are investigated by comparing a fully coupled and a partially decoupled Indian Ocean experiment using the SINTEX-F coupled model.Air-sea coupling over the TIO significantly enhances the intensity of the eastward propagations of the MJO along the5°-10°S zonal areas.The zonal asymmetry of the SST anomaly（SSTA） is responsible for the enhanced eastward propagation.A positive SSTA appears to the east of the MJO convection,which results in the boundary layer moisture convergence and positively feeds back to the MJO convection.In addition,the air-sea interaction effect on the eastward propagation of the MJO is related to the interannual variations of the TIO.Air-sea coupling enhances（reduces） the eastward-propagating spectrum during the negative Indian Ocean dipole mode and positive Indian Ocean basin mode.Such phase dependence is attributed to the role of the background mean westerly in affecting the wind-evaporation-SST feedback.Air-sea coupling（decoupling） enhances（reduces） the zonal asymmetry of the low-level specific humidity,and thus the eastward propagation spectrum of the MJO.

The Upper Mixed Layer during Coastal Upwelling Events on the Northern Portugal Shelf

The upper mixed layer (UML) depth obtained from temperature is very close to that from density:the maximum is about 15m. This indicates that temperature is a good indicator of mixed layer during measurements. When the surface heat flux is balanced by a cross-shore heat flux, the surface mixed layer depth obtained from the WM model (Weatherly and Martin, 1978),hPRT, is roughly the same as observed. The mixed layer depth calculated from the PWP model (Price, Weller and Pinkel, 1986) is close to the depth obtained from thermistor chain temperature data. The results show that both the WM model and PWP model can provide a good estimate of stratification in the study area during the cruise. The value of log( h/u3) is about 9.5 in the study area, which shows that the study area is strongly stratified in summer. Observations on the northern Portugal shelf reveal high variability in stability, giving rise to semi-diurnal, semi-monthly and diurnal oscillations, and long term variations. The fortnightly oscillations are highlighted by post-springs and post-neaps. The stirring of spring tide is reinforced by strong wind mixing which brings about complete vertical homogeneity everywhere. The semi-diurnal periodic stratification is very pronounced because the major axis of the tidal ellipse is orientated acrossshore, even though the tidal current is weak in this area, the maximum stratification is observed around the middle of ebb, and, the water at this time is much warmer. The diurnal oscillation results from the upper ocean response to heating and wind mixing when solar heating warms and stabilizes the upper ocean. There is a clear relationship between upper mixed layer depth and wind-stress magnitude at subtidal frequencies. Stronger winds result in a deeper surface mixed layer. Typically, the surface mixed layer depth lags the wind stress by 6 -12 h.

ON THE CHARACTERISTICS OF PROPAGATION OF INTRASEASONAL OSCILLATIONS AND THEIR OBSERVED ASSOCIATION WITH TROPICAL SYNOPTIC WAVES IN THE ASIAN-WESTERN PACIFIC REGION IN BOREAL SUMMER

Using the daily average outgoing longwave radiation and NCEP/NCAR reanalysis data in boreal summer(Mays to Octobers)from 1979 to 2007,the propagating characteristics of convection intraseasonal oscillations(ISOs)in the Asian-western Pacific(AWP)region and the relationship between tropical synoptic waves and ISOs are examined by means of finite-domain wavenumber-frequency energy spectrum analysis and lagged linear regression technique.The results are shown as follows.(1)The AWP ISOs propagate both eastward and westward,showing seasonality and regionality.The ISOs propagate eastward with a period of 30 to 60 days over equatorial regions in the whole AWP region,while the westward propagation occurs over 10 to 20°N western Pacific or in the late summers(August,September and October) with periods of 20 to 40 days.The ISOs eastward propagation mainly occurs in primary summers while the westward propagation enhances in late summers.(2)Deep ISO convections associate with westerly and cyclonic circulation anomalies that first form in the Indian Ocean,propagate eastward to the dateline in the Pacific and then turn northwestward.The ISOs convections show northwestward propagating characteristics in the western North Pacific.(3)The ISOs link with the tropical synoptic waves closely.Both convection signals,though with different spatio-temporal scale,enhance simutaneously in the northwestern Pacific,and the ISOs facilitate the forming of a cluster of tropical cyclones(TCs),while a cluster of TCs convection becomes one portion of the northwestward ISOs.

Intensity of the Trough over the Bay of Bengal and Its Impact on the Southern China Precipitation in Winter

In this study, the intensity of the trough over the Bay of Bengal (BBT) and its association with the southern China precipitation, the Madden-Julian Oscillation (MJO) and the Rossby wave propagation along the African-Asian subtropical Jet stream (AASJ) are investigated on the intraseasonal time scale. The results show that the intensity of the BBT affects the southern China precipitation more directly and to a greater degree than the MJO. The peak amplitude of the BBT tended to occur in phase-3 of the MJO. The strong BBT was substantially modulated by the Rossby wave propagation along the AASJ, which was triggered by the anomalous upstream circulation similar to the pattern of the North Atlantic Oscillation (NAO). Therefore, from the perspective of medium- and extended-range weather forecasts, the NAO- like pattern may be regarded as a precursory signal for the strong BBT and thus the southern China precipitation.

ABRUPT CHANGES OF THE WESTERN PACIFIC SUBTROPICAL HIGH AND ITS INTERANNUAL VARIATION DURING LATE SPRING AND EARLY SUMMER

The 500-hPa geopotential height data used in this paper are from NCEP/NCAR data set for the period from 1979 to 1996 (from March to July). Using pentad average, we define the intensity, westernmost ridge point and mean latitude of the subtropical high ridge. Then the wavelet transform and EOF analysis are performed. It is found that there mainly exist three interseasonal abrupt change processes, which correspond to the onset time of the South China Sea Summer Monsoon (SCSSM), the beginning and the end of the Mei-yu respectively. The interannual variation of the subtropical high in late spring and early summer presents quasi-4-year and 8-year periods.

Typical Surface Seasonal Circulation in the Indian Ocean Derived from Argos Floats

This study investigates the surface circulation in the Indian Ocean using Argos float data over the period 1979-2011.The Argos observations manifest some new phenomena.The climatological annual mean circulation shows that the surface current becomes much stronger after turning around in shore in the western Indian Ocean.In the tropical Indian Ocean,the Great Whirl(GW) to the east of Somalia develops quickly in spring(April-May) as the monsoon reverses to move northward,becoming strongest in summer(June-September) and disappearing in autumn(October-November).The west end of the Agulhas retroflection can reach 18°E,and it exhibits a seasonal variation.At approximately 90°E,the Agulhas Return Current combines with the eastward South Atlantic Current and finally joins the Antarctic Circumpolar Current.

RELATIONSHIPS BETWEEN PRECEDING PACIFIC SEA SURFACE TEMPERATURES AND SUBTROPICAL HIGH INDEXES OF MAIN RAINING SEASONS

With correlation analysis and factor analysis methods, the effects of preceding Pacific SSTs on subtropical high indexes of main raining seasons are discussed. The results of correlation analysis show that the effects of SSTs on five subtropical high indexes differ in seasons and regions. The variation of SSTs mostly affects the area and intensity indexes of the subtropical high, followed by the western ridge index, and the effect on the ridge line index is more remarkable than on the north boundary index. The results of factor analysis reveals that the first common factor of SST of each season reflected mainly the inverse relation of SSTs variation between the central and eastern part of equatorial Pacific and the western Pacific, which correlates better with the subtropical high indexes in the main raining seasons than other common factors of SST. The analysis of interdecadal variation indicated that the variation of SSTs was conducive to the emergence of the La Ni?a event before the end of 1970s, such that in the summer the subtropical high is likely to be weaker and smaller and located eastward and northward. After the 1980s, the opposite characteristics prevailed.

关于高校“洋节”现象的再思考——兼论校园文化的塑造

随着全球化的推进,中西方文化的交流日益增多,外来文化对本土文化带来强烈的冲击,尤其是“洋节”现象的盛行引发了广泛的关注和讨论。该文全面剖析高校中“洋节”现象产生的原因包括文化交流、英语教育普及、社会氛围、青少年追求快乐本性等,对此高校作为管理者,应客观看待、取其精华、适当转化,培养积极向上的校园文化。