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Статті в журналах з теми "Qinghai-Tibet Plateau"
Wang, Zhiheng, Hongkui Fan, Daikun Wang, Tao Xing, Dongchuan Wang, Qiaozhen Guo, and Lina Xiu. "Spatial Pattern of Highway Transport Dominance in Qinghai–Tibet Plateau at the County Scale." ISPRS International Journal of Geo-Information 10, no. 5 (May 5, 2021): 304. http://dx.doi.org/10.3390/ijgi10050304.
Повний текст джерелаXiao, Qiyun. "Sustainable Development Strategies for Ecotourism in Qinghai-Tibet Plateau Based on SWOT Analysis." British Journal of Environmental Studies 2, no. 2 (September 17, 2022): 08–12. http://dx.doi.org/10.32996/bjes.2022.2.2.2.
Повний текст джерелаDuan, Hanchen, Xian Xue, Tao Wang, Wenping Kang, Jie Liao, and Shulin Liu. "Spatial and Temporal Differences in Alpine Meadow, Alpine Steppe and All Vegetation of the Qinghai-Tibetan Plateau and Their Responses to Climate Change." Remote Sensing 13, no. 4 (February 12, 2021): 669. http://dx.doi.org/10.3390/rs13040669.
Повний текст джерелаGe, Liyan, Zhiqiang Feng, Haibo Yao, and Siwei Liu. "Thoughts on Green Highway Construction in Qinghai-Tibet Plateau." E3S Web of Conferences 233 (2021): 01122. http://dx.doi.org/10.1051/e3sconf/202123301122.
Повний текст джерелаXiao, Qiying. "Approaches to the Development of Ecotourism on the Qinghai-Tibet Plateau: The Aim Being Sustainable Growth." Journal of Humanities and Social Sciences Studies 4, no. 4 (September 18, 2022): 25–29. http://dx.doi.org/10.32996/jhsss.2022.4.4.5.
Повний текст джерелаWang, Dongchuan, Kangjian Wang, Zhiheng Wang, Hongkui Fan, Hua Chai, Hongyi Wang, Hui Long, Jianshe Gao, and Jiacheng Xu. "Spatial-Temporal Evolution and Influencing Mechanism of Traffic Dominance in Qinghai-Tibet Plateau." Sustainability 14, no. 17 (September 4, 2022): 11031. http://dx.doi.org/10.3390/su141711031.
Повний текст джерелаQi, Yinglian, Xiaoyan Pu, Yaxiong Li, Dingai Li, Mingrui Huang, Xuan Zheng, Jiaxin Guo, and Zhi Chen. "Prediction of Suitable Distribution Area of Plateau pika (Ochotona curzoniae) in the Qinghai–Tibet Plateau under Shared Socioeconomic Pathways (SSPs)." Sustainability 14, no. 19 (September 25, 2022): 12114. http://dx.doi.org/10.3390/su141912114.
Повний текст джерелаSONG, Jianlan. "Denisovan from Qinghai-Tibet Plateau." Bulletin of the Chinese Academy of Sciences 34, no. 1 (January 1, 2020): 14–15. http://dx.doi.org/10.3724/sp.j.7101866520.
Повний текст джерелаZhou, Huakun, Xiaoyuan Yang, Chenyu Zhou, Xinqing Shao, Zhengchen Shi, Honglin Li, Hongye Su, et al. "Alpine Grassland Degradation and Its Restoration in the Qinghai–Tibet Plateau." Grasses 2, no. 1 (March 3, 2023): 31–46. http://dx.doi.org/10.3390/grasses2010004.
Повний текст джерелаZou, Yifan, Peng Sun, Zice Ma, Yinfeng Lv, and Qiang Zhang. "Snow Cover in the Three Stable Snow Cover Areas of China and Spatio-Temporal Patterns of the Future." Remote Sensing 14, no. 13 (June 27, 2022): 3098. http://dx.doi.org/10.3390/rs14133098.
Повний текст джерелаДисертації з теми "Qinghai-Tibet Plateau"
Wang, Yun Summer, and 王筠. "Love to the eternity : eco-tourism design along Qinghai-Tibet railway." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2014. http://hdl.handle.net/10722/207151.
Повний текст джерелаpublished_or_final_version
Architecture
Master
Master of Landscape Architecture
Rui, Yichao. "Soil Carbon, Nitrogen and Phoshorus Dynamics in Response to Warming and Grazing in Alpine Meadow Ecosystem of the Tibet plateau." Thesis, Griffith University, 2013. http://hdl.handle.net/10072/366008.
Повний текст джерелаThesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Biomolecular and Physical Sciences
Science, Environment, Engineering and Technology
Full Text
Wang, Baolai. "Some aspects of plateau permafrost, Qinghai-Xizang (Tibet) Plateau, China, and a comparison with the Mackenzie Delta region, Canada." Thesis, University of Ottawa (Canada), 1993. http://hdl.handle.net/10393/6840.
Повний текст джерелаZhang, Xuemei. "The Structural Model of the Lithosphere-asthenosphere System in the Qinghai-Tibet and its adjacent Areas from Surface Wave Tomography." Doctoral thesis, Università degli studi di Trieste, 2010. http://hdl.handle.net/10077/3622.
Повний текст джерелаThe Qinghai-Tibet Plateau lies at the continent-continent collision between the Indian and Eurasian plates. Because of their interaction the shallow and deep structures are very complicated with different tectonic units. The force system forming the tectonic patterns and driving tectonic movements is exerted together by the deep part of the lithosphere and the asthenosphere. In the recent decades, many deep explorations have been performed and a series of important results about the collision models of Indian and Eurasian plates and their deep structures have been gained, but the studies on the fine structure of the lithosphere-asthenosphere system are still a few. In order to get knowledge about their formation and evolution, dynamic process, layers coupling and exchange of material and energy, it is important to study the 3-D velocity structures, the material properties and physical state of the lithosphere-asthenosphere system. Based on the Rayleigh wave dispersion theory, we study the 3-D velocity structures, including the crust, of the lithosphere-asthenosphere system in the Qinghai-Tibet Plateau and its adjacent areas. In the study area (20ºN - 50ºN, 70ºE - 110ºE) we collect long period and broad-band seismic data from the global and regional seismic networks surrounding the area: G (Geoscope), IC (NCDSN) , II/IU (GSN), KZ (Kazakhstan), XA (Bhutan), XR (INDEPTH II&III), YA (2003MIT-China), and YL (Himalayan Nepal Tibet Experiment) during the period of 1966-2007. After making instrumental correction and proper band-pass filtering, group velocities dispersion of fundamental mode of Rayleigh waves are measured using the frequency-time analysis (FTAN). Cluster averaging is applied to similar ray paths and, in such a way, a set of dispersion curves, in the period range from 8 s to 150 s is obtained along 791 paths. A 2-Dsurface-wave tomography method capable to evaluate the average lateral resolution, proposed by Yanovskaya, is applied to calculate the lateral variations in the group velocity distribution at the different periods. The lateral heterogeneity resolution has been estimated to be about 200 km in most of the study area. To be consistent with the resolution level, the group velocity maps, at different periods, are discretized in cells of 2o×2o. The most conspicuous low group velocity anomaly, in the period range from 25 s to 40 s appears in whole Qinghai-Tibet Plateau, while the Indian Plate and the Yangtze craton are characterized by high group velocity anomalies. At the intermediate periods (50 - 80 s) the most dominant feature is the NW-SE directed low velocity anomaly in the Qinghai-Tibet Plateau. At the long ii periods the velocity anomaly is comparable with the anomaly at the lower periods. The determination of the shear-wave velocity distribution versus depth from a surface wave dispersion curve is a severely non-linear problem. The non-linear Hedgehog inversion method (Panza, 1981) is applied to the surface wave tomography cellular dispersion curves to obtain shear wave velocity-depth models of the crust and upper mantle. The non-linear inversion does not depend upon the initial model. Since the Hedgehog is a non-linear procedure, the inversion is multi-valued, i.e., a set of equally probable model is accepted, which is consistent, within the chosen parametrization, with the experimental errors. An ensemble of acceptable models is found and in order to summarize and define the geological meaning of the results, it is often necessary to identify a representative model. Physical and mathematical reasons can be used to define the criteria that allow us to select a unique solutions. The Local Smoothness Optimization (LSO) (Panza et al., 2007;Boyadzhiev et al., 2008) fixes the solution as the one which minimizes the norm between neighbouring cells. Applying the first iteration of LSO, the Starting Cell (SC) is chosen such that satisfies the analogous objective criterion: the cell with the minimal divergence between the accepted solutions. Staring from the SC, the LSO takes, as representative model, the solution that has the smallest distance (difference in the velocity) in l2 with respect to the models of the neighbouring cells. The LSO method is a smoothness criteria, which can avoid the introduction of heterogeneities that can arise from a subjective choice. However, in the Qinghai-Tibet Plateau and its vicinity, the heterogeneity is too severe to apply LSO to the whole study area, because its deep structure is very complicated. It is appropriate to obtain representative models by LSO method in local regions, each with different starting cell (SC). Since the Hedgehog non-linear inversion and the local smoothing algorithm provide us only a mathematical solution, the representative models are chosen, considering a priori geophysical and geological information. The top and bottom of the lithosphere and asthenosphere are recognized from the velocity values and velocity contrast between the layers. These thicknesses are helpful to study the structural differences between the Qinghai-Tibet Plateau and its adjacent areas and among different geologic units of the plateau. Taking into account also previous investigations, the following conclusions are reached from the distributions of the S-wave velocities in the crust and the upper mantle and thicknesses of the crust, lithosphere and asthenosphere. (1) The crust is very thick in the Qinghai-Tibet Plateau, and varies from 60 km to iii 80 km. The lithospheric thickness in the Qinghai-Tibet Plateau is smaller (125-160 km) than in the adjacent areas. The asthenosphere is relatively thick, varies from 100 km to 200 km, and the thickest area lies in the western Qiangtang block (QT). India, located to the south of the Main Boundary thrust, has a thinner crust (32-42 km), a thicker lithosphere of 190 km and a rather thin asthenosphere of only about 80 km. Sichuan and Tarim basins have the crust thickness less than 50 km. Their lithospheres are thicker than the Qinghai-Tibet Plateau, and their asthenospheres are thinner. (2) The uppermost mantle of the Indian Plate is subducted almost horizontally beneath the Himalaya block (HM) and the Lhasa block (LS), and the subduction is delimited by the Bangong-Nujiang suture belt (BNS). The Indian lithospheric lid is also subducted with a large-angle beneath the Eurasian Plate before the Yalung-Zangbo suture belt (YZS). The low velocity lower crust and asthenosphere, detected in central Qinghai-Tibet Plateau, show that in the Qiangtang block (QT) the temperature is high, well in agreement with the active Cenozoic volcanism in the area. We also think that the underplating of the asthenosphere may thin the lithosphere and that the buoyancy might be the main mechanism of deep dynamics of the uplift of the Qinghai-Tibet hinterland. (3) Inside the plateau two blocks can be recognized, divided by an NNE striking boundary running between 90ºE ~ 92ºE. The shear-wave velocities of the crust and the thicknesses of the lithosphere and asthenosphere in the eastern Qinghai-Tibet Plateau are different from those in the western one. The width of the boundary between the eastern Qinghai-Tibet Plateau and the western one may be 2° ~ 3°. (4)The continental surface loss by the kinematic shortening is not compensated by the increment of the crust thickness due to the collision of Indian Plate and Eurasian Plate. Therefore we may deduce that the crustal material is laterally extruded along a channel between the Jinshajiang suture belt (JSJS) and Banggong-Nujiang suture belt (BNS), and rotated around the eastern Himalayan Syntaxes because of the obstacle of the Yangze block. The source of the lateral extrusion may be in the Qiangtang block (QT).
XXI Ciclo
1974
Bosch, Anna [Verfasser], and Thomas [Akademischer Betreuer] Scholten. "Quantification of soil CO2 emissions under the influence of climate change on the Qinghai-Tibet Plateau based on freely accessible data / Anna Bosch ; Betreuer: Thomas Scholten." Tübingen : Universitätsbibliothek Tübingen, 2017. http://d-nb.info/1165578069/34.
Повний текст джерелаBosch, Anna Verfasser], and Thomas [Akademischer Betreuer] [Scholten. "Quantification of soil CO2 emissions under the influence of climate change on the Qinghai-Tibet Plateau based on freely accessible data / Anna Bosch ; Betreuer: Thomas Scholten." Tübingen : Universitätsbibliothek Tübingen, 2017. http://d-nb.info/1165578069/34.
Повний текст джерелаMatuszak, Sabine Verfasser], Alexandra [Akademischer Betreuer] Müllner-Riehl, Adrien [Akademischer Betreuer] Favre, and Georg [Akademischer Betreuer] [Zizka. "Evolution of Mountain Plants in the region of the Qinghai-Tibet Plateau and beyond / Sabine Matuszak. Betreuer: Alexandra Müllner-Riehl ; Adrien Favre. Gutachter: Alexandra Müllner-Riehl ; Georg Zizka." Frankfurt am Main : Universitätsbibliothek Johann Christian Senckenberg, 2016. http://d-nb.info/1092187448/34.
Повний текст джерелаCotte, Nathalie. "Détermination des variations latérales de la lithosphère par l'analyse des ondes de surface enregistrées par des réseaux régionaux." Phd thesis, Grenoble 1, 2000. http://tel.archives-ouvertes.fr/tel-00703264.
Повний текст джерелаPan, Xicai [Verfasser]. "Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau / put forward by Xicai Pan." 2011. http://d-nb.info/1013101065/34.
Повний текст джерелаHuuang, Yung-Ruei, and 黃勇叡. "Lake level changes in Qinghai-Tibet Plateau from Cryosat-2 altimeter: validation by results from repeat altimeter missions and satellite images." Thesis, 2017. http://ndltd.ncl.edu.tw/handle/3777j2.
Повний текст джерела國立交通大學
土木工程系所
105
The mean elevation of the Qinghai-Tibet Plateau (QTP) exceeds 4000 m. Lake levels in the QTP are less affected by human activities than elsewhere, and may better reflect the state of contemporary climate change. Here ground-based lake level measurements are rare. Repeat altimeter missions, particularly TOPEX and ERS series of altimetry, have provided long-term observations of lake levels in the QTP, but their large cross-track distances allow only few lakes to be monitored. In contrast, the Cryosat-2 altimeter, equipped with the new sensor SIRAL (interferometric / synthetic aperture radar altimeter), provides a much finer spatial coverage than repeated missions, and can detect water level changes over a large number of lakes in the QTP. In this study, Cryosat-2 data are used to determine lake level changes in the QTP (75˚E-100˚E, 28˚N-37.5˚N), where Cryosat-2 provides data over 60 lakes and SARAL / AltiKa over 32 lakes from 2013 to 2016. Over a lake, Cryosat-2 in different cycles can pass through different spots, making the numbers of observations non-uniform and requiring corrections for lateral variations in geoidal undulation. Four cases are used to cope with these: (1) neglecting inconsistency in data volume and geoid-based lake slope (2) considering data volume, (3) considering lake slope only, (4) considering both data volume and lake slope. Because Cryosat-2 is available only from 2010 to 2016, Jason-2 data are used to fill gaps between the time series of Cryosat-2 and ICESat (2003-2009) to obtain >10 years of lake level changes.The Cryosat-2 result is then compared with the result from the SARAL to determine the best case. The Cryosat-2 result shows dramatic lake level changes in Lakes Kusai, Zhuoaihu and Salt in 2011.Landsat satellite imagery is used to assist the determination of volume changes over these lakes..
Книги з теми "Qinghai-Tibet Plateau"
Gongjian, Wu, Xiao Xuchang, and Li Tingdong, eds. Yadong to Golmud Transect: Qinghai-Tibet Plateau, China. Washington, D. C.: American Geophysical Union, 1991. http://dx.doi.org/10.1029/gt003.
Повний текст джерелаMianping, Zheng. An Introduction to Saline Lakes on the Qinghai—Tibet Plateau. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1.
Повний текст джерелаCheng, Mien-pʻing. An introduction to saline lakes on the Qinghai-Tibet Plateau. Dordrecht: Kluwer Academic Publishers, 1997.
Знайти повний текст джерелаWang, Wenying, and Jürgen Hövermann. Reports on the northeastern part of the Qinghai-Xizang (Tibet) plateau. Beijing: Science Press, 1987.
Знайти повний текст джерелаSino-W. German Scientific Expedition (1981). Reports on the northeastern part of the Qinghai-Xizang (Tibet) Plateau. Edited by Hövermann Jürgen and Wang Wen-ying. Beijing, China: Science Press, 1987.
Знайти повний текст джерела1918-, Péwé Troy Lewis, ed. Origin and character of loesslike silt in the southern Qinghai-Xizang (Tibet) Plateau, China. Washington: U.S. G.P.O., 1995.
Знайти повний текст джерелаQing Zang Gaoyuan she hui jing ji shi: The social and economic history of Qinghai-Tibet Plateau. Beijing: She hui ke xue wen xian chu ban she, 2019.
Знайти повний текст джерелаChengfa, Chang, Royal Society (Great Britain), and Zhongguo ke xue yuan, eds. The geological evolution of Tibet: Report of the 1985 Royal Society-Academia Sinica Geotraverse of the Qinghai-Xizang Plateau. London: Royal Society, 1988.
Знайти повний текст джерелаQing Zang Gaoyuan zhen xi ye sheng dong wu: Precious and rare wildlife in the Qinghai-Tibet Plateau. Chengdu: Sichuan min zu chu ban she, 2010.
Знайти повний текст джерелаYongshou, Qi, Liu Fenggui, Liao Lisheng, and Hou Guangliang, eds. Qing Zang Gaoyuan lü you kai fa yan jiu: The study on tourism development of Qinghai-Tibet Plateau. Beijing: Ke xue chu ban she, 2013.
Знайти повний текст джерелаЧастини книг з теми "Qinghai-Tibet Plateau"
Chang, Chen-Fa, Yu-Sheng Pan, and Yi-Ying Sun. "The Tectonic Evolution of Qinghai-Tibet Plateau: A Review." In Tectonic Evolution of the Tethyan Region, 415–76. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2253-2_18.
Повний текст джерелаMianping, Zheng. "Introduction." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 1–17. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_1.
Повний текст джерелаMianping, Zheng. "Biomineralization of Boron and Other Halotolerant Organisms." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 200–210. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_10.
Повний текст джерелаMianping, Zheng. "Division of Minerogenic Zones and Prediction of Resource Potential." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 211–30. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_11.
Повний текст джерелаMianping, Zheng. "Prospects of Development of Resources of Saline Lakes and their Environmental Protection." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 231–36. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_12.
Повний текст джерелаMianping, Zheng. "Saline Lakes and Lake Districts." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 18–22. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_2.
Повний текст джерелаMianping, Zheng. "Evolution of Cenozoic Lake Basins and the Formation of Saline Lakes." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 23–54. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_3.
Повний текст джерелаMianping, Zheng. "Hydrochemistry and Mineral Associations of Saline Lakes." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 55–78. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_4.
Повний текст джерелаMianping, Zheng. "Classification of Saline Lakes and Types of Mineral Deposit." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 79–84. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_5.
Повний текст джерелаMianping, Zheng. "Tectonogeochemistry and Regional Geochemistry." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau, 85–122. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_6.
Повний текст джерелаТези доповідей конференцій з теми "Qinghai-Tibet Plateau"
Li, Zhongqiu. "Effects of Qinghai-Tibet Railway and Highway on Plateau Picas." In 2012 International Conference on Biomedical Engineering and Biotechnology (iCBEB). IEEE, 2012. http://dx.doi.org/10.1109/icbeb.2012.189.
Повний текст джерелаYang, Y., Z. Feng, D. Liu, and J. Zhang. "The Spatial-temporal Change of Grassland in Qinghai-Tibet Plateau." In 2006 IEEE International Symposium on Geoscience and Remote Sensing. IEEE, 2006. http://dx.doi.org/10.1109/igarss.2006.795.
Повний текст джерелаQin, Yinghong. "Estimate the Permafrost Degradation at Muli Coalfield, Qinghai-Tibet Plateau." In 14th Conference on Cold Regions Engineering. Reston, VA: American Society of Civil Engineers, 2009. http://dx.doi.org/10.1061/41072(359)19.
Повний текст джерелаFeng, Cangxu, Jun Liu, Xiao Cui, and Lei Zhang. "Monitoring of Qinghai–Tibet plateau hydrothermal circulation with heat pulse." In 2013 International Conference on Biomedical Engineering and Environmental Engineering. Southampton, UK: WIT Press, 2014. http://dx.doi.org/10.2495/icbeee130641.
Повний текст джерелаWang, Ge, and Lin Han. "Progress of Research on Qinghai-Tibet Plateau Satellite Remote Sensing." In 2012 2nd International Conference on Remote Sensing, Environment and Transportation Engineering (RSETE). IEEE, 2012. http://dx.doi.org/10.1109/rsete.2012.6260667.
Повний текст джерелаXie, Zhenhong, Qigang Jiang, and Hao Wu. "Carbon cycle review of the permafrost in Qinghai-Tibet Plateau." In 2011 19th International Conference on Geoinformatics. IEEE, 2011. http://dx.doi.org/10.1109/geoinformatics.2011.5980869.
Повний текст джерелаCaiJi, Zhuoma, Guo Luo, Dayuan Xue, and Yuhuan Du. "The Spatial Analysis of Monastery on the Qinghai-Tibet Plateau." In 2015 Information Technology and Mechatronics Engineering Conference. Paris, France: Atlantis Press, 2015. http://dx.doi.org/10.2991/itoec-15.2015.9.
Повний текст джерелаZhang, Xuefei, Yixian Tang, Hong Zhang, Chao Wang, Bo Zhang, and Fan Wu. "Permafrost Subsidence Monitoring of Qinghai-Tibet Plateau using Sentinel-1 Data." In 2019 SAR in Big Data Era (BIGSARDATA). IEEE, 2019. http://dx.doi.org/10.1109/bigsardata.2019.8858504.
Повний текст джерелаTang, Panpan, Zhen Li, Jianmin Zhou, Bangsen Tian, and Juan Xu. "Coherence based analysis of distributed scatterers in the Qinghai-Tibet Plateau." In IGARSS 2013 - 2013 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2013. http://dx.doi.org/10.1109/igarss.2013.6723034.
Повний текст джерелаYan, J. P. "Research on land degradation and management countermeasures in Qinghai-Tibet plateau." In The 2015 International Conference on Sustainable Development (ICSD2015). WORLD SCIENTIFIC, 2016. http://dx.doi.org/10.1142/9789814749916_0048.
Повний текст джерела