东太平洋多金属结核U、Th同位素深度分布特征与生长速率

研究了东太平洋多金属结核中Ｕ、Ｔｈ同位素的深度分布与生长速率。表明,东太平洋多金属结核中的＾２３４Ｕ／＾２３８Ｕ）Ａ．Ｒ．与海水接近,证实了Ｕ的海水来源;２３４Ｕ及２３８Ｕ的活度并不随深度增加而减小,而是在次表层和更深层出现极大值。２３６７站核中＾２３２Ｔｈ的活度在次表层有最大值,之后随深度的增加而降低,反映了结核生长过程中成岩作用的影响;１７９７站南结核中＾２３２Ｔｈ表层有最大值,其它各层的变化     

铁路与欲望——电影《金山》的文化症候阅读

太平洋铁路的修筑,是加拿大民族一国家认同建构过程中的奠基性事件。与此同时,曾经为铁路修筑做出极大贡献与牺牲的华裔劳动力,却无法分享这一北美民族主义的叙述基调,他们被剥夺、受压抑的移民经验则成为北美华裔文化书写的持久性命题。循乎此,电影《金山》（Iron Road,2008）也许可以成为跨文化研究中的一个有趣个案：影片由加拿大一香港一中国内地多方合作完成,共同书写了一部加拿大华裔劳工的“血泪史诗”。我们首先可以将其视为60年代以降,北美少数族裔文化运动的迟滞胜利;然则,考虑到影片事实背后,多国融资的电影事实,加拿大官方资金在其中所占的高额比重,以及影片中的内地与香港演员的角色配置,对于这一文本的讨论,势必要延伸到亚太经济结构中来思考。笔者认为电影《金山》向观者发出了如下信息：面对已然崛起的新一新中国,环太平洋区域中的华人所占据的位置,有待重估。     

用AMSU资料反演西北太平洋海域大气湿度廓线的研究

采用快速辐射传输模式RTTOV对AMSU所有通道进行水汽廓线的敏感性分析, 并根据模式计算结果逐步剔除相关性小的预报通道, 建立两种水汽廓线反演的统计回归模型;之后利用2006年7月NOAA-16卫星AMSU亮温资料, 计算不同算法下的反演系数矩阵, 回归得出大气水汽廓线。反演廓线经与NCEP 廓线比较, 得到0600UTC 和1800UTC 比湿反演的各层偏差(RMS)分别在1.4g/kg 及1.7g/kg 以内。个例分析发现, 反演廓线与NCEP廓线趋势一致; 反演比湿场可定位台风云区及水汽供应输送带, 具有一定的揭示台风结构的能力。     

环太平洋弧形山系探究

论述环太平洋弧形山系的一些主要特征,并从二种类型的板块俯冲——造山作用、太平洋板块的演化进程探讨了环洋山系形成和发展.     

海峡西岸经济区产业空间整合研究

在明确海峡西岸经济区的主体为福建省的基础上,重点分析了福建省区域经济发展现状及后动力机制后,运用产业簇群理论,提出整合设想:按照价值链来布局区域产业集群,形成层次不同的外向空间、承接空间、腹地空间3种形态,构建一个按照“进口(创新)—生产—出口”类似赤松“雁行”产业空间蓝图,全方位、多层次提升闽域整体竞争力,实现海峡西岸经济区经济一体化,使之成为一个独立的经济地区.     

An improvement of the too cold tongue in the tropical Pacific with the development of an ocean-wave-atmosphere coupled numerical model

A common problem in the application of the coupled ocean-atmosphere general circulation models (CGCMs) without flux correction is that the simulated equatorial cold tongue in general tends to be too strong, narrow, and extending too far west. The causes are not well understood yet. One possible reason may be the simulated mixed layer depth (MLD) is too shallow in the tropical Pacific due to insufficient vertical mixing in the OGCM. It is believed that the wave-induced vertical mixing can greatly improve the simulation of the MLD and thermocline structure. In this study, the coupled ocean-atmosphere general circulation model (FGCM-0) incorporated with wave-induced mixing has been employed to simulate the tropical Pacific sea surface temperature (SST). Generally, the wave-induced mixing lowers the SST in the OGCM because the strengthened vertical mixing can bring more cold water upward. However, in the coupled model, the non-uniformity of the space distribution in SST drop generates a horizontal gradient of the sea surface air pressure, and thus yields surface wind field anomaly. The wind anomaly leads to both ocean surface circulation anomaly and downwelling anomaly, which can restrain the overly-westward extension of the cold tongue in the tropical Pacific. Compared with the model results from the original model (FGCM-0), the modeled SST is higher by more than 0.8℃, with a maximum of 1.2℃ in the western Pacific (160—180°E, 0—3°N). The eastern boundary of the isotherm of 26.0℃ also moves from 165°E to 180°E. The overly westward extension of the simulated equatorial cold tongue is suppressed with the incorporation of the wave-induced mixing in the coupled model. The simulated SST shows in general improved results with a maximum improvement of more than 1.0℃. The simulated SST improvement in the north tropical Pacific is much better than that of the south tropical Pacific.     

An improvement of the too cold tongue in the tropical Pacific with the development of an ocean-wave-atmosphere coupled numerical model

A common problem in the application of the coupled ocean-atmosphere general circulation models (CGCMs) without flux correction is that the simulated equatorial cold tongue in general tends to be too strong, narrow, and extending too far west. The causes are not well understood yet. One possible reason may be the simulated mixed layer depth (MLD) is too shallow in the tropical Pacific due to insufficient vertical mixing in the OGCM. It is believed that the wave-induced vertical mixing can greatly improve the simulation of the MLD and thermocline structure. In this study, the coupled ocean-atmosphere general circulation model (FGCM-0) incorporated with wave-induced mixing has been employed to simulate the tropical Pacific sea surface temperature (SST). Generally, the wave-induced mixing lowers the SST in the OGCM because the strengthened vertical mixing can bring more cold water upward. However, in the coupled model, the non-uniformity of the space distribution in SST drop generates a horizontal gradient of the sea surface air pressure, and thus yields surface wind field anomaly. The wind anomaly leads to both ocean surface circulation anomaly and downwelling anomaly, which can restrain the overly-westward extension of the cold tongue in the tropical Pacific. Compared with the model results from the original model (FGCM-0), the modeled SST is higher by more than 0.8℃, with a maximum of 1.2℃in the western Pacific (160—180°E, 0—3°N) . The eastern boundary of the isotherm of 26. 0℃also moves from 165°E to 180°E. The overly westward extension of the simulated equatorial cold tongue is suppressed with the incorporation of the wave-induced mixing in the coupled model. The simulated SST shows in general improved results with a maximum improvement of more than 1.0℃. The simulated SST improvement in the north tropical Pacific is much better than that of the south tropical Pacific.     

Living planktonic foraminifera from the northwestern Pacific Ocean: SSU rDNA sequences and their paleoceanographic significance

Living planktonic foraminifera (PF) samples from the Okinawa Trough of the northwestern Pacific Ocean were taken for DNA analysis. The SSU rDNA sequences of two PF species, Globigerina sp. and Pulleniatina obliquiloculata collected at Station WP01, were obtained and compared with those from the southwestern Pacific Ocean. Only small differences (<0.7%—1.2% for P. obliquiloculata, and 0.3% for Globigerina sp.) were found between samples from the north- and south-western Pacific Ocean areas and this molecular evidence supported that these micropaleontological species are the same species, which implies that the West Pacific Ocean circulation system influences the planktonic foraminiferal gene communication.