985 resultados para Zhu Jiang


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Contient : I萬日略經說Wan ri lüe jing shuo ; IITian zhu jiang sheng yan xing ji lüe

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Évangiles expliqués des dimanches et des principales fêtes de l'année.Par le P. Emmanuel Diaz junior, Jésuite (1574-1659 ; noms Chinois Yang Ma nuo Yan xi) ; préface de l'auteur (1636) ; publié avec l'autorisation du P. Francisco Furtado, Jésuite (1587-1653 ; noms Chinois Fu Fan ji Ti zhai). Réédition de l'église Ling bao à Pékin (1739).14 livres.

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Évangiles expliqués des dimanches et des principales fêtes de l'année.Par le P. Emmanuel Diaz junior, Jésuite (1574-1659 ; noms Chinois Yang Ma nuo Yan xi) ; préface de l'auteur (1636) ; publié avec l'autorisation du P. Francisco Furtado, Jésuite (1587-1653 ; noms Chinois Fu Fan ji Ti zhai). Réédition de l'église Ling bao à Pékin (1739).14 livres.

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Vie illustrée de Notre-Seigneur.Introduction du P. Aleni (1637) ; figure du Christ ; plan de Jérusalem et 56 gravures (28 feuillets doubles). Édition de l'église Jing jiao de Jin jiang.

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Traité sur l'incarnation de Notre-Seigneur.Par le P. Aleni ; publié avec l'autorisation du P. Diaz.2 livres.

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Mode of access: Internet.

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Acrossocheilus malacopterus n. sp. is described from the Yuan Jiang (Red River) and Zhu Jiang basins in I South China. It is separated from other congeners by a combination of the following characters: an inconspicuously stripped body, 16 circumpeduncular scales, 47-49 lateral line scales, depth of caudal peduncle 7.8-9.3% SL, snout length 37.9-41.7% SL, dorsal-fin length 18.7-21.0% SL and last simple dorsal-fin ray slender with 8-10 fine serrations along posterior margin.

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yLinichthys, new genus, is proposed for Barbodes laticeps Lin and Zhang, 1986. It can be separated from all other genera of Asian Barbinae in having a shallow depression extending along the median portion of the upper lip. Linichthys is superficially very similar to the type species of a monotypic Chinese cyprinid cavefish genus, Typhlobarbus nudiventris, in having an elongate and somewhat compressed body form, a truncate distal margin of the dorsal fin, and a soft and smooth last unbranched dorsal-fin ray, all of them being atypical for most of Asian barbins. The two genera differ in size of the eye and the number of rows of pharyngeal tooth. Although the same body form and/or structure of the dorsal fin are also shared with some species currently placed in other genera of Asian barbins, the recognition of Linichthys is warranted because of their marked differences in other characters. A redescription is also provided for the type species of the monotypic genus, Linichthys laticeps. It is known only from the upper and middle Zhu Jiang basin and the upper Chang Jiang basin in the city of Guiyang, Guizhou Province, South China.

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Qianlabeo striatus gen. et sp. nov. is described from a stream tributary to the Beipan Jiang of the upper Zhu Jiang (Pearl River) drainage in Matou, Anshun County, Guizhou Province, China. This monotypic genus is mainly characterized by its oromadibular morphology, namely an upper lip only present in and fully adnate to the side of the upper jaw, not covered by the pendulous rostral fold; the median portion of the upper jaw lacking an upper lip but bearing a thin, flexible and cornified cutting edge that is fully covered by the pendulous rostral fold; a postlabial groove prolonged, extended anteromedially close to the anteromost point of the midline of the lower lip but not to meet with its counterpart. The type species of this genus, Q. striatus has a longitudinal dark stripe along the side of the body.

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Mesoscale eddy plays an important role in the ocean circulation. In order to improve the simulation accuracy of the mesoscale eddies, a three-dimensional variation (3DVAR) data assimilation system called Ocean Variational Analysis System (OVALS) is coupled with a POM model to simulate the mesoscale eddies in the Northwest Pacific Ocean. In this system, the sea surface height anomaly (SSHA) data by satellite altimeters are assimilated and translated into pseudo temperature and salinity (T-S) profile data. Then, these profile data are taken as observation data to be assimilated again and produce the three-dimensional analysis T-S field. According to the characteristics of mesoscale eddy, the most appropriate assimilation parameters are set up and testified in this system. A ten years mesoscale eddies simulation and comparison experiment is made, which includes two schemes: assimilation and non-assimilation. The results of comparison between two schemes and the observation show that the simulation accuracy of the assimilation scheme is much better than that of non-assimilation, which verified that the altimetry data assimilation method can improve the simulation accuracy of the mesoscale dramatically and indicates that it is possible to use this system on the forecast of mesoscale eddies in the future.

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Contient : I天主降生言行紀略Tian zhu jiang sheng yan xing ji lüe ; II ; IIIWan ri lüe jing shuo ; IV ; VWan ri lüe jing shuo. Tian zhu jiang sheng yan xing ji lüe

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Contient : IWan ri lüe jing shuo ; IITian zhu jiang sheng yan xing ji lüe

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Contient : ISheng hao jing ; IITian zhu jing ; IIITian shen chao bai sheng mu jing ; IVXin jing ; VTian zhu shi jie ; VISheng jiao hui si gui ; VII天主事情問荅Tian zhu shi qing wen da ; VIII人讐有三Ren chou you san ; IX十誡問荅Shi jie wen da ; X悔罪問荅Hui zui wen da ; XIHui zui jing ; XII天學警言Tian xue jing yan