天主降生言行紀略Tian zhu jiang sheng yan xing ji lüe.

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

天主降生聖經直解Tian zhu jiang sheng sheng jing zhi jie.

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.

天主降生聖經直解Tian zhu jiang sheng sheng jing zhi jie.

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.

天主降生出像經解Tian zhu jiang sheng chu xiang jing jie.

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.

天主降生引義Tian zhu jiang sheng yin yi.

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

Si shu guan zhu jiang yi.

Mode of access: Internet.

Chinois 6716

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

Chinois 6718

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

聖教要訓Sheng jiao yao xun.

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

The Holocene temperature conundrum

A recent temperature reconstruction of global annual temperature shows Early Holocene warmth followed by a cooling trend through the Middle to Late Holocene [Marcott SA, et al., 2013, Science 339(6124):1198–1201]. This global cooling is puzzling because it is opposite from the expected and simulated global warming trend due to the retreating ice sheets and rising atmospheric greenhouse gases. Our critical reexamination of this contradiction between the reconstructed cooling and the simulated warming points to potentially significant biases in both the seasonality of the proxy reconstruction and the climate sensitivity of current climate models.

Data assimilation and its applications

In data assimilation, one prepares the grid data as the best possible estimate of the true initial state of a considered system by merging various measurements irregularly distributed in space and time, with a prior knowledge of the state given by a numerical model. Because it may improve forecasting or modeling and increase physical understanding of considered systems, data assimilation now plays a very important role in studies of atmospheric and oceanic problems. Here, three examples are presented to illustrate the use of new types of observations and the ability of improving forecasting or modeling.

Pearl River Estuary Region : North, Guangdong Sheng, China, 1749 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Carte de l'entrée de la riviere de Canton : dressée sur les observations les plus récentes, par N.B., Ingr. ordre. de la Marine ; J.V. Schley direx. It was published by Pierre de Hondt in 1749. Scale [ca. 1:475,000]. Covers the Zhujiang Kou region, Guangdong Sheng, China. Map in French and Dutch.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Asia North Lambert Conformal Conic coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, selected buildings and fortification, shoreline features, and more. Relief shown pictorially.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Pearl River Estuary Region : South, Guangdong Sheng, China, 1749 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Carte des isles qui sont a l'embouchure de la riviere de Canton : dressée sur les observations des navigateurs, par N.B., Ingr. ordre. de la Marine ; J.V. Schley, direx. It was published by Pierre de Hondt in 1749. Scale [ca. 1:500,000]. Covers the Zhujiang Kou region, Guangdong Sheng, China. Map in French and Dutch. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Asia North Lambert Conformal Conic coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, selected buildings and fortification, shoreline features, and more. Relief shown pictorially.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Molecular dynamics simulations of the hydrophobin SC3 at a hydrophobic/hydrophilic interface

Hydrophobins are small (similar to 100 aa) proteins that have an important role in the growth and development of mycelial fungi. They are surface active and, after secretion by the fungi, self-assemble into amphipathic membranes at hydrophobic/hydrophilic interfaces, reversing the hydrophobicity of the surface. In this study, molecular dynamics simulation techniques have been used to model the process by which a specific class I hydrophobin, SC3, binds to a range of hydrophobic/ hydrophilic interfaces. The structure of SC3 used in this investigation was modeled based on the crystal structure of the class II hydrophobin HFBII using the assumption that the disulfide pairings of the eight conserved cysteine residues are maintained. The proposed model for SC3 in aqueous solution is compact and globular containing primarily P-strand and coil structures. The behavior of this model of SC3 was investigated at an air/water, an oil/water, and a hydrophobic solid/water interface. It was found that SC3 preferentially binds to the interfaces via the loop region between the third and fourth cysteine residues and that binding is associated with an increase in a-helix formation in qualitative agreement with experiment. Based on a combination of the available experiment data and the current simulation studies, we propose a possible model for SC3 self-assembly on a hydrophobic solid/water interface.

Qiu jiang ji zhu : 6 juan /

Block print.