999 resultados para Modèle des boucles de 1 mb
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Vol. 2, pt. 2; v. 3, pt. 1, 3: Unter mitwirkung von prof. dr. Ahrens, dr. Auerbach, dr. Baur ... [u. a.] hrsg. von dr. R. Abegg. Vol. 2, pt. 1; v. 3, pt. 2; v. 4, pt. 1 sect 2: Unter mitwirkung von ... E. Abel ... F. B. Ahrens ... E. Baur ... [u. a.] hrsg. von dr. R. Abegg ... und dr. Fr. Auerbach. Vol. 4, pt. 1, sect. 1, pt. 3-4 : Unter mitwirkung von ... E. Abel ... F. B. Ahrens ... E. Baur ... [u. a.] hrsg. von dr. R. Abegg ... dr. Fr. Auerbach und dr. I. Koppel.
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"The subjoined Syllabary is 'mutatis mutandis' identical with the 'Tabelle für die laute des chinesischen im mandarin-dialecte' submitted by me to the Far-Eastern section of the XIII International congress of Orientalists held at Hamburg in September, 1902." ("Published in the Transactions of the Congress and reprinted in Prof. H. Cordier's report, 'Les etudes chinoises,' 1899-1902, 'Tʼoung pao,' 1903, p. 38-45, and 'Beiträge zur kenntniss des Orients.' vol. 1, München, 1903.")
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VETDOC
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Some issues accompanied by supplements
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Vol.2, pt.2; v.3, pt.1,3: Unter Mitwirkung von Prof. Dr. Ahrens, [et al.] hrsg. von R. Abegg. Vol.2, pt.1; v.3, pt.2; v.4, pt.1, sect.2: Unter Mitwirkung von E. Abel [et al.] hrsg. von R. Abegg und Fr. Auerbach. Vol.4, pt.1, sect.1, pt.3-4: Unter Mitwirkung von E. Abel [et al.] hrsg. von R. Abegg, Fr. Auerbach und I. Koppel.
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Each vol. has also special t.-p.
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Thesis (Ph.D.)--University of Washington, 2016-06
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This paper is concerned with long-term (20+ years) forecasting of broadband traffic in next-generation networks. Such long-term approach requires going beyond extrapolations of past traffic data while facing high uncertainty in predicting the future developments and facing the fact that, in 20 years, the current network technologies and architectures will be obsolete. Thus, "order of magnitude" upper bounds of upstream and downstream traffic are deemed to be good enough to facilitate such long-term forecasting. These bounds can be obtained by evaluating the limits of human sighting and assuming that these limits will be achieved by future services or, alternatively, by considering the contents transferred by bandwidth-demanding applications such as those using embedded interactive 3D video streaming. The traffic upper bounds are a good indication of the peak values and, subsequently, also of the future network capacity demands. Furthermore, the main drivers of traffic growth including multimedia as well as non-multimedia applications are identified. New disruptive applications and services are explored that can make good use of the large bandwidth provided by next-generation networks. The results can be used to identify monetization opportunities of future services and to map potential revenues for network operators. © 2014 The Author(s).
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Cet article examine la complexité du processus d’intégration régionale en Océanie à travers le cas du groupe du Fer de Lance mélanésien (gflm). L’émergence de cette structure subrégionale en 1988 avait pour but d’affirmer la spécificité mélanésienne au cœur du Pacifique Sud. Or, en vingt-cinq années d’existence, le Fer de Lance ne semble pas avoir pleinement réalisé tous les objectifs qu’il s’était initialement fixés. Ses ambitions, politiques en particulier, ne sont qu’en partie réalisées. Quant à la récente présidence fidjienne du Fer de Lance, elle a tenté de donner une nouvelle stature régionale au groupe, mais y est-elle parvenue ? Cet article analyse les défis politiques, intérieurs et extérieurs, que le gflm rencontre depuis sa création et considère ceux qui lui restent à relever. This paper examines the complexities of regional integration in Oceania through the case study of the Melanesian Spearhead Group (MSG). The emergence of a new subregional structure in 1988 aimed to support the development of the Melanesian identity within the South Pacific. However, after twenty-five years of existence, the Spearhead Group does not seem to have reached all its initial objectives. Its political ambition has only partly been achieved. The recent Fijian leadership of the MSG has attempted to give a new regional dimension to the Melanesian group, but has it succeeded? This paper analyses how the subregional group has faced the challenges that emerged from its regional environment as well as from within its own structure. It fnally considers the new challenges ahead for the Melanesian group.
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ex Arabico in Latinum translatus ab Iohanne Hispano et Dominico Gundissalino ; ex codicibus Parisinis, Amploniano, Columbino primum ed. Clemens Baeumker
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Underwater photo-transect surveys were conducted on September 23-27, 2007 at different sections of the reef flat, reef crest and reef slope in Heron Reef. This survey was done by swimming along pre-defined transect sites and taking a picture of the bottom substrate parallel to the bottom at constant vertical distance (30cm) every two to three metres. A total of 3,586 benthic photos were taken. A floating GPS setup connected to the swimmer/diver by a line enabled recording of coordinates of transect surveys. Approximation of the coordinates for each benthic photo was based on the photo timestamp and GPS coordinate time stamp, using GPS Photo Link Software. Coordinates of each photo were interpolated by finding the the gps coordinates that were logged at a set time before and after the photo was captured. The output of this process was an ArcMap point shapefile, a Google Earth KML file and a thumbnail of each benthic photo taken. The data in the ArcMap shapefile and in the Google Earth KML file consisted of the approximated coordinate of each benthic photo taken during the survey. Using the GPS Photo Link extension within the ArcMap environment, opening the ArcMap shapefile will enable thumbnail to be displayed on the associated benthic cover photo whenever hovering with the mouse over a point on the transect. By downloading the GPSPhotoLink software from the www.geospatialexperts.com, and installing it as a trial version the ArcMap exstension will be installed in the ArcMap environment.
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Underwater georeferenced photo-transect surveys were conducted on December 10-15, 2011 at various sections of the reef at Lizard Island, Great Barrier Reef. For this survey a snorkeler or diver swam over the bottom while taking photos of the benthos at a set height using a standard digital camera and towing a GPS in a surface float which logged the track every five seconds. A standard digital compact camera was placed in an underwater housing and fitted with a 16 mm lens which provided a 1.0 m x 1.0 m footprint, at 0.5 m height above the benthos. Horizontal distance between photos was estimated by three fin kicks of the survey diver/snorkeler, which corresponded to a surface distance of approximately 2.0 - 4.0 m. The GPS was placed in a dry-bag and logged the position as it floated at the surface while being towed by the photographer. A total of 5,735 benthic photos were taken. A floating GPS setup connected to the swimmer/diver by a line enabled recording of coordinates of each benthic photo (Roelfsema 2009). Approximation of coordinates of each benthic photo was conducted based on the photo timestamp and GPS coordinate time stamp, using GPS Photo Link Software (www.geospatialexperts.com). Coordinates of each photo were interpolated by finding the GPS coordinates that were logged at a set time before and after the photo was captured. Benthic or substrate cover data was derived from each photo by randomly placing 24 points over each image using the Coral Point Count for Microsoft Excel program (Kohler and Gill, 2006). Each point was then assigned to 1 of 78 cover types, which represented the benthic feature beneath it. Benthic cover composition summary of each photo scores was generated automatically using CPCE program. The resulting benthic cover data of each photo was linked to GPS coordinates, saved as an ArcMap point shapefile, and projected to Universal Transverse Mercator WGS84 Zone 55 South.
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Underwater georeferenced photo-transect surveys were conducted on October 3-7, 2012 at various sections of the reef and lagoon at Lizard Island, Great Barrier Reef. For this survey a snorkeler swam while taking photos of the benthos at a set distance from the benthos using a standard digital camera and towing a GPS in a surface float which logged the track every five seconds. A Canon G12 digital camera was placed in a Canon underwater housing and photos were taken at 1 m height above the benthos. Horizontal distance between photos was estimated by three fin kicks of the survey snorkeler, which corresponded to a surface distance of approximately 2.0 - 4.0 m. The GPS was placed in a dry bag and logged the position at the surface while being towed by the photographer (Roelfsema, 2009). A total of 1,265 benthic photos were taken. Approximation of coordinates of each benthic photo was conducted based on the photo timestamp and GPS coordinate time stamp, using GPS Photo Link Software (www.geospatialexperts.com). Coordinates of each photo were interpolated by finding the GPS coordinates that were logged at a set time before and after the photo was captured. Benthic or substrate cover data was derived from each photo by randomly placing 24 points over each image using the Coral Point Count for Microsoft Excel program (Kohler and Gill, 2006). Each point was then assigned to 1 of 79 cover types, which represented the benthic feature beneath it. Benthic cover composition summary of each photo scores was generated automatically using CPCE program. The resulting benthic cover data of each photo was linked to GPS coordinates, saved as an ArcMap point shapefile, and projected to Universal Transverse Mercator WGS84 Zone 55 South.
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Wind- induced exposure is one of the major forces shaping the geomorphology and biota in coastal areas. The effect of wave exposure on littoral biota is well known in marine environments (Ekebon et al., 2003; Burrows et al., 2008). In the Cabrera Archipelago National Park wave exposure has demostrated to have an effect on the spatial distribution of different stages of E.marginatus (Alvarez et al., 2010). Standarized average wave exposures during 2008 along the Cabrera Archipelago National park coast line were calculated to be applied in studies of littoral species distribution within the archipelago. Average wave exposure (or apparent wave power) was calculated for points located 50 m equidistant on the coastline following the EXA methodology (EXposure estimates for fragmented Archipelagos) (Ekebon et al., 2003). The average wave exposures were standardized from 1 to 100 (minimum and maximum in the area), showing coastal areas with different levels of mea wave exposure during the year. Input wind data (direction and intensity) from 2008 was registered at the Cabrera mooring located north of Cabrera Archipelago. Data were provided by IMEDEA (CSIC-UIB, TMMOS http://www.imedea.uib-csic.es/tmoos/boyas/). This cartography has been developed under the framework of the project EPIMHAR, funded by the National Park's Network (Spanish Ministry of Environment, Maritime and Rural Affairs, reference: 012/2007 ). Part of this work has been developed under the research programs funded by "Fons de Garantia Agrària i Pesquera de les Illes Balears (FOGAIBA)".