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Journal articles on the topic 'Lhasa'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Yasir, Muhammad, Tiesong Hu, and Samreen Abdul Hakeem. "Simulating Reservoir Induced Lhasa Streamflow Variability Using ArcSWAT." Water 12, no. 5 (2020): 1370. http://dx.doi.org/10.3390/w12051370.

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Lhasa River Basin being the socio-economic hotspot of Qinghai-Tibetan Plateau is experiencing an increased hydropower capacity in the form of damming and reservoir construction. The Pangduo hydropower station, commenced in 2013, is one of these developments. Lhasa River discharge is analyzed for spatial variability under the reservoir operation at Pondo and Lhasa gauging station. The Mann–Kendall Trend analysis reveals an increased precipitation and a decreased Lhasa River discharge trend upstream and downstream the reservoir. However, the discharge received at Lhasa gauging station is experie

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2

Zhang, Ming, Wei Yu, Fan Zhi Zeng, Chen Qiu Du, and Xiao Fei Wang. "Analysis of Indoor Air Quality for Residential Buildings in Lhasa, China." Applied Mechanics and Materials 587-589 (July 2014): 453–60. http://dx.doi.org/10.4028/www.scientific.net/amm.587-589.453.

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Adopting the methods of subjective questionnaire and objective test, the indoor air quality (IAQ) of residential buildings in Lhasa were analyzed in summer and winter, and the results were compared with that in Chongqing. Firstly, the data shows that the overall IAQ in Lhasa is better. Excepted total volatile organic compounds (TVOC), the concentration of formaldehyde, carbon dioxide (CO2), PM2.5 are low. Secondly, more than 80% residents accepted the IAQ in Lhasa, which means the satisfaction rate is high. Thirdly, the IAQ in Lhasa is better than that in Chongqing, such that the exceed-standa

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3

Shen, Xiao, Yangshuai Jiang, Yanjie Shang, et al. "A Preliminary Study of Necrophagous Flies (Insecta: Diptera) in the Lhasa Region (Qinghai–Tibet Plateau), China." Journal of Medical Entomology 59, no. 2 (2021): 467–79. http://dx.doi.org/10.1093/jme/tjab187.

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Abstract Lhasa is located on the Qinghai–Tibet Plateau, with an altitude of 3,650 m, and a unique geography. Its climate is dry and cold all year round. Forensic entomological studies of the region are scarce. In this study, the diversity and seasonality of necrophagous flies in eight counties among Lhasa region were determined, and succession of necrophagous flies colonizing on rabbits in the Chengguan area of Lhasa was studied, so as to provide reference data for estimating postmortem interval (PMI) and location of death. In total, 22 species of necrophagous flies, belonging to six families

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4

ZHAN, Chun. "The Structural and Sedimentary Evolution Characteristics of the Lhasa Basin in Xizang Autonomous Region." Chinese Earth Sciences Review 3, no. 3 (2024): 125–31. http://dx.doi.org/10.48014/cesr.20240524001.

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Abstract: The Lhasa Basin is located in the southeast segment of the Gangdise Tectonic Belt, with a unique geological environment, being a typical and common tectonic morphology in the highland areas. By studying the development and evolution characteristics of the Lhasa Basin's tectonic structure, the tectonic evolution of the Lhasa Basin from the early to middle Jurassic onwards is divided into two phases and three stages. The tectonic background of the basin's formation determines the temporal and spatial evolution process of the sedimentary basin. Through investigation and analysis of the

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5

Craig, Sienna R. "Leaving Lhasa Vegas." Anthropology and Humanism 42, no. 2 (2017): 227–29. http://dx.doi.org/10.1111/anhu.12182.

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6

DI, ZHI-YONG, and MING-SHENG ZHU. "One new species of the Genus Scorpiops Peters, 1861 (Scorpiones: Euscorpiidae, Scorpiopinae) from Xizang, China." Zootaxa 2030, no. 1 (2009): 39–48. http://dx.doi.org/10.11646/zootaxa.2030.1.3.

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Scorpiops lhasa sp. n., from China Xizang (Lhasa) is described. S. lhasa is small in size with respect to other species in the genus; external trichobothria on the patella number 17 (5 eb, 2 esb, 2 em, 4 est, 4 et) and ventral trichobothria on the patella number 10 (11 rarely); pedipalp fingers in both sexes are curved; chela narrow and elongated, the ratio between length and width is above 2.6.

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7

McKay, Alex. "The British Invasion of Tibet, 1903–04." Inner Asia 14, no. 1 (2012): 5–25. http://dx.doi.org/10.1163/22105018-990123777.

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AbstractIn 1903–04, British forces under the command of the Indian Political Officer, Colonel Francis Younghusband, invaded Tibet. After failed negotiations and a series of battles in which Younghusband's modern weaponry vanquished Tibetan forces, the British entered Lhasa and imposed a treaty on the Tibetans. While a fear of Russian influence in Lhasa was the main reason given for the invasion, Tibet's policy of isolating itself from British India was probably a more significant cause. The subsequent withdrawal of the British from Lhasa created a power vacuum which enabled the Chinese to re-e

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8

Xie, Li Sheng, Xin Wu Mi, and Jun Ge. ""Lhasa Hotel" in the Design of Regional Culture." Advanced Materials Research 598 (November 2012): 139–43. http://dx.doi.org/10.4028/www.scientific.net/amr.598.139.

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Qinghai-Tibet Railway will have a historic opportunity on Tibet tourism; tourism has greatly boosted the tourism development of the hotel industry in the region. Our in-depth analysis and study of Lhasa area that ideologies, living habits, aesthetic, moral ethics, regional culture, and through understanding, digesting, and application in the design of the Lhasa hotel. Efforts to make the designs in Lhasa Hotel reflect the quintessence of regional culture of Tibet.

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9

Che, Dong, Mianping Zheng, Yuanyi Zhao, et al. "High Degree of Differentiation and Enrichment of Li, Rb and Cs in Potassic-Ultrapotassic Volcanic Rocks: An Example from the Lhasa Block, Tibet." Minerals 13, no. 3 (2023): 342. http://dx.doi.org/10.3390/min13030342.

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Post-collisional potassic-ultrapotassic volcanic rocks are widely developed in the Lhasa block, Qinghai-Tibet region. In this paper, it was observed for the first time that dilute alkali elements–Li, Rb, and Cs–exhibit supernormal enrichment in the research data of numerous potassic-ultrapotassic volcanic rocks in the Lhasa block. At the same time, there are few studies on the genesis of enrichment. Currently, 568 sets of published volcanic rock data and 8 sets of measured data in the Lhasa block are sorted in detail, and the genesis of dilute alkali element enrichment is explained by means of

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10

Yu, Jiayan, Lingshuo Meng, Yang Chen, Huifang Zhang, and Jianguo Liu. "Ozone Profiles, Precursors, and Vertical Distribution in Urban Lhasa, Tibetan Plateau." Remote Sensing 14, no. 11 (2022): 2533. http://dx.doi.org/10.3390/rs14112533.

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Near-surface ozone is one of the significant issues in the troposphere. Recently, ozone pollution in Lhasa at an altitude of 3600 m has caused attention. The current knowledge of ozone formation in Lhasa city is still minimal. In this work, the profile of VOCs during early summer was investigated, and alkanes were the most critical group of VOCs. The urban areas of Lhasa are under transition conditions and controlled by both VOCs and NOx. Moreover, the most effective way to decrease ozone formation is to reduce the emissions of anthropogenic VOCs and NOx. The vertical distribution of troposphe

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11

Lin, Huiming, Yindong Tong, Long Chen, et al. "Unexpectedly high concentrations of atmospheric mercury species in Lhasa, the largest city in the Tibetan Plateau." Atmospheric Chemistry and Physics 23, no. 7 (2023): 3937–53. http://dx.doi.org/10.5194/acp-23-3937-2023.

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Abstract. The city of Lhasa is located in the central Tibetan Plateau and is the most densely populated area. As the first continuous monitoring of atmospheric mercury (Hg) species in a city in the Tibetan Plateau, our monitoring in Lhasa showed that the concentrations of gaseous elemental Hg (GEM), gaseous oxidized Hg (GOM), and particle-bound Hg (PBM) during the subsequent Indian summer monsoon (S-ISM) period were 2.73 ± 1.48 ng m−3, 38.4 ± 62.7 pg m−3, and 59.1 ± 181.0 pg m−3, respectively. During the westerly circulation (WEC) period, the GEM, GOM, and PBM concentrations were 2.11 ± 2.09 n

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12

Huidong, Su, Liu Yin, Lu Huiting, Wang Dongbo, and Jin Tianian. "Study on Integrated Planning and Management in Lhasa River Basin." E3S Web of Conferences 165 (2020): 03055. http://dx.doi.org/10.1051/e3sconf/202016503055.

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As a political, economic and cultural center of the Tibet Autonomous Region, the Lhasa River needs to take planning and management of the basin. In the past 60 years, the temperature of Lhasa River Basin has been increasing gradually at an annual rate of 0.047 ° C, which leads to the water cycle variation of the river basin and its associated aquatic ecology and environment continue to change and evolve, and ecological environmental protection is affected by more uncertain factors. Based on the assessment of the ecological environment of the Lhasa River Basin, the comprehensive planning sugges

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13

Laskowski, Andrew K., Devon A. Orme, Fulong Cai, and Lin Ding. "The Ancestral Lhasa River: A Late Cretaceous trans-arc river that drained the proto–Tibetan Plateau." Geology 47, no. 11 (2019): 1029–33. http://dx.doi.org/10.1130/g46823.1.

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Abstract Late Cretaceous trench basin strata were deposited in the subduction zone that consumed Neo-Tethyan oceanic lithosphere along the southern margin of the proto–Tibetan Plateau. We conducted detrital zircon (DZ) U-Pb geochronology on six trench basin samples (n = 1716) collected near Dênggar, Tibet (∼500 km west of Lhasa), to assess the provenance of these rocks and reconstruct Late Cretaceous sediment transport pathways. They contained DZ ages that point to a unique source around Lhasa city, north of the Late Cretaceous Gangdese magmatic arc. The modern Lhasa River catchment contains t

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14

Xu, Hai-peng, Yi-chun Zhang, Feng Qiao, and Shu-zhong Shen. "A new Changhsingian brachiopod fauna from the Xiala Formation at Tsochen in the central Lhasa Block and its paleogeographical implications." Journal of Paleontology 93, no. 5 (2019): 876–98. http://dx.doi.org/10.1017/jpa.2019.28.

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AbstractPermian faunal affinity in the Lhasa Block plays a critical role in reconstructing its paleogeographic evolution. Cisuralian and Guadalupian faunas have been described from the Lhasa Block, but very few Lopingian (late Permian) brachiopods have been reported so far. In this paper, a new diverse brachiopod fauna consisting of 17 species of 17 genera and an unidentifiable Orthotetoidea is described from the uppermost part of the Xiala Formation at the Aduogabu section in the central part of the Lhasa Block. The age of this fauna can be assigned to the Changhsingian (late Lopingian) as in

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15

Wu, Zhi Qiang, Hong Zhi Yu, and Shu Hui Wan. "Research and Realization the Method of Pronunciation Conversion for Speech Synthesis of the Lhasa Dialect of Tibetan." Applied Mechanics and Materials 571-572 (June 2014): 858–62. http://dx.doi.org/10.4028/www.scientific.net/amm.571-572.858.

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Pronunciation conversion is the premise to realize the speech synthesis system, besides, the conversion accuracy is directly related to the quality of synthetic speech. By studying the characteristics of Tibetan words and Lhasa pronunciation, currently method of the pronunciation conversion for Tibetan dialect in Lhasa, combination the need of speech synthesis research, designed and realized the pronunciation conversion system that can be applied in the Lhasa dialect of Tibetan speech synthesis. In tests the system is up to 95.3 percent accurate, the results of conversion are basically able to

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16

Gong, Xun. "How many vowels are there in Lhasa Tibetan?" Linguistics of the Tibeto-Burman Area 43, no. 2 (2020): 225–54. http://dx.doi.org/10.1075/ltba.19004.gon.

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Abstract Lhasa Tibetan is described in a number of independent research traditions which give different accounts of its phonology. To what extent do these discrepancies reflect real dialectal or idiolectal differences? To what extent do they reflect different analyses of the same system? In this paper, we examine one aspect of Lhasa Tibetan phonology on which different descriptions show substantial discrepancies: vowels. Different descriptions of Lhasa Tibetan transcribe from 8 to more than 16 vowel qualities, ascribing to them different degrees of phonemicity. A detailed comparison of the tra

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17

Xiang, Xin, Tianqi Ao, and Qintai Xiao. "Variation of Runoff and Runoff Components of the Lhasa River Basin in the Qinghai-Tibet Plateau under Climate Change." Atmosphere 13, no. 11 (2022): 1848. http://dx.doi.org/10.3390/atmos13111848.

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Quantitative analysis of changes in Lhasa River runoff components was significant to local water resources management. This study constructed the spatial processes in hydrology (SPHY) model in the Lhasa River Basin and optimized the model’s parameters using the hydrograph partitioning curves (HPC) method. The Lhasa River Basin’s precipitation and temperature were forecasted for 2020 to 2100 using the statistical downscaling model (SDSM) and two scenarios from the fifth generation of the Canadian earth system model (CanESM5) dataset, shared socioeconomic pathways 1-2.6 (SSP1-2.6) and shared soc

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18

Ludlow, F. "THE BIRDS OF LHASA." Ibis 92, no. 1 (2008): 34–45. http://dx.doi.org/10.1111/j.1474-919x.1950.tb01731.x.

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19

Emmer, Michele. "A mathematician in lhasa." Mathematical Intelligencer 25, no. 4 (2003): 67–71. http://dx.doi.org/10.1007/bf02984864.

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20

Pye, Lucian W., and Robert Barnett. "Lhasa: Streets with Memories." Foreign Affairs 85, no. 5 (2006): 178. http://dx.doi.org/10.2307/20032125.

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21

Yang, Jiayi. "Urban Expansion and The Microclimate Characteristics Evolution of Lhasa." Highlights in Science, Engineering and Technology 59 (July 15, 2023): 85–90. http://dx.doi.org/10.54097/hset.v59i.10064.

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Urban expansion is the process of growing urban population and expanding land for residential and productive use. Microclimates are small-scale climates with relatively uniform and changeable climatic characteristics. In the context of climate change on the Tibetan Plateau, the microclimate of Lhasa will respond to urban expansion. With the support of landset8 OLI_TIRS data, this study uses the unsupervised classification method ISO-data algorithm to extract information on construction land and calculate the intensity of urban sprawl. In order to analyze and investigate the evolution of urban

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22

Chen, Jing, Fang Wang, and Jia Ping Liu. "The Research of Folk House Development in Lhasa Area." Applied Mechanics and Materials 357-360 (August 2013): 33–38. http://dx.doi.org/10.4028/www.scientific.net/amm.357-360.33.

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Lhasa region's special natural environment makes a unique form of regional folk house. Because of the external culture influence, the form of traditional folk house is continuous improvement. The traditional independence Tibetan folk house is reducing in the Lhasa city. In this situation, the author and his research team had surveyed and tested different types folk houses in the Lhasa city and surrounding areas. Through comparing the spatial characteristics among the traditional Tibetan folk house, contemporary Tibetan folk house and contemporary unit resident building, and this paper analysis

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23

Lin, Hsiao-Ting. "The 1934 Chinese Mission to Tibet: A Re-examination." Journal of the Royal Asiatic Society 12, no. 3 (2002): 327–41. http://dx.doi.org/10.1017/s1356186302000342.

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AbstractIn the spring of 1934, a Chinese mission led by General Huang Musong, then Deputy Chief of the General Staff of the Guomindang regime, was dispatched to Lhasa with the official purpose of offering condolences to the late 13th Dalai Lama who died in late 1933. Huang's visit to Tibet undoubtedly was the most politically symbolic event in Sino-Tibetan relations since the collapse of the Qing dynasty. He became the most high-profile of Chinese officials to have entered Lhasa since 1911, when the Chinese Republic was created. Before returning to Nanking, Huang left a representative office,

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Sun, Wenjing, Lixing Chen, Baimu Suolang, and Kai Liu. "An Investigation of the Energy-Saving Optimization Design of the Enclosure Structure in High-Altitude Office Buildings." Buildings 14, no. 3 (2024): 645. http://dx.doi.org/10.3390/buildings14030645.

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Concerning the double carbon national strategy, the energy-saving renovation of old buildings has become one of the most important tasks of energy conservation and emission reduction in construction in China. There are many problems, such as high energy consumption, thermal environment, and poor thermal comfort. Taking Lhasa as an example, this study adopts field research, questionnaire interviews, on-site measurements, numerical simulations, and other methods to propose suitable energy-saving potential excavation points and thermal optimization strategies for office building envelopes in Lhas

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Trinado Jiménez, Carmen Fuensanta. "Análisis del trasvase de los elementos culturales tibetanos en la traducción al español de Voyage d’une Parisienne à Lhasa." Estudios de Traducción 12 (May 27, 2022): 15–24. http://dx.doi.org/10.5209/estr.80001.

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En Voyage d’une Parisienne à Lhasa, Alexandra David-Néel narra el viaje al Tíbet que emprendió disfrazada de peregrino con su hijo adoptivo y que la convirtió en la primera europea en tener acceso a la capital del Tíbet. A lo largo del relato de sus aventuras, David-Néel se esfuerza por transmitir al lector el máximo número posible de elementos culturales. Sin embargo, desde las primeras páginas de la novela, la autora afirma que adapta dichos elementos para que el público francófono pueda comprenderlos. En este trabajo, compararemos Voyage d’une Parisienne à Lhasa con su traducción al español

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Lai, Yang‐Jun, Jian‐Fei Ye, Bing Liu, et al. "Integrating fossil and extant plant communities to calibrate paleoelevation of the Qinghai–Tibet Plateau." Journal of Systematics and Evolution 63, no. 1 (2025): 25–38. https://doi.org/10.1111/jse.13172.

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AbstractThe formation of the Qinghai–Tibet Plateau has long been debated, despite the various proxies used to estimate its paleoelevation. Here, we introduce a novel method to calibrate paleoelevation by comparing the fossil and extant plant communities in the Qinghai–Tibet Plateau. Our estimation confirms that the uplift of the plateau was an episodic and heterochronous process. Specifically, the Lhasa Terrane was already elevated by 1 km before the initial India–Asia collision. During the first orogenic stage, the Qiangtang Terrane rose faster than the Lhasa Terrane, attaining 3 km in the la

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Zhang, Yunjie, Fan Su, Yongjing Song, and Jinkui Lu. "Associations between Physical Fitness Index and Body Mass Index in Tibetan Children and Adolescents in Different High-Altitude Areas: Based on a Study in Tibet, China." International Journal of Environmental Research and Public Health 19, no. 16 (2022): 10155. http://dx.doi.org/10.3390/ijerph191610155.

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Objective: To investigate the relationship between physical fitness index (PFI) and body mass index (BMI) of Tibetan children and adolescents in different high-altitude areas in Tibet, China. Methods: Using the stratified cluster sampling method, 3819 Tibetan children and adolescents from three different high-altitude areas including Nyingchi, Lhasa and Nagqu in the Tibet area of China were given grip strength, standing long jump, sitting forward bend, 50 m running and endurance running tests. One-way analysis of variance was used to compare the physical fitness index in different high-altitud

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Li, Guan Yu, and Hong Zhi Yu. "Large-Vocabulary Continuous Speech Recognition of Lhasa Tibetan." Applied Mechanics and Materials 519-520 (February 2014): 802–6. http://dx.doi.org/10.4028/www.scientific.net/amm.519-520.802.

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The framework of auto speech recognition of Lhasa dialect was established in this paper. Phoneme was chosen as the basic unit for modeling. Then, phonemes set of Lhasa dialect and their Latin transliteration were designed. There were 5568 frequently used monosyllables in the vocabulary. Hidden Markov Models of triphones were established and trained by use of HTK. Word error rate (WER) was 21.81% under the optimal situation.

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Wang, Meimei, Dezhen Kong, Jinhuang Mao, Weijing Ma, and Ramamoorthy Ayyamperumal. "The Impacts of Land Use Spatial Form Changes on Carbon Emissions in Qinghai–Tibet Plateau from 2000 to 2020: A Case Study of the Lhasa Metropolitan Area." Land 12, no. 1 (2022): 122. http://dx.doi.org/10.3390/land12010122.

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The ecological contribution of the Qinghai–Tibet Plateau has received considerable attention as a result of the increased focus on global climate change and the continuous growth of carbon emissions in all countries. In this study, we proposed a method and measured the carbon emissions from land use in the Lhasa metropolitan area from 2000 to 2020, based on image interpretation data, by exploiting corrected carbon emission factors in different land types from the Qinghai–Tibet Plateau. We studied the impact of construction land form on carbon emissions using the spatial lag model (SLM) and the

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Zhang, Xuepeng, Chunchun Meng, Peng Gou, et al. "Evaluating the Reconstructed All-Weather Land Surface Temperature for Urban Heat Island Analysis." Remote Sensing 16, no. 2 (2024): 373. http://dx.doi.org/10.3390/rs16020373.

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With the continuous improvement of urbanization levels in the Lhasa area, the urban heat island effect (UHI) has seriously affected the ecological environment of the region. However, the satellite-based thermal infrared land surface temperature (LST), commonly used for UHI research, is affected by cloudy weather, resulting in a lack of continuous spatial and temporal information. In this study, focusing on the Lhasa region, we combine simulated LST data obtained by the Weather Research and Forecasting (WRF) model with remote sensing-based LST data to reconstruct the all-weather LST for March,

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Zhang, Heyulu, Tianning Li, Changping Mao, Zhengjin Song, and Wenbo Rao. "Mineralogical and Chemical Characteristics of Sediments in the Lhasa River Basin: Implications for Weathering and Sediment Transport." Water 17, no. 4 (2025): 581. https://doi.org/10.3390/w17040581.

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The Lhasa River, as one of the major rivers on the Tibetan Plateau, is of great value for the study of climate and environmental changes on the Tibetan Plateau. In this paper, the grain size and the mineralogical and geochemical characteristics of the sediments from the Lhasa River were investigated. The results show the following: (1) The average grain size of the Lhasa River sediments is coarse (65.5% sand, 23.6% silt), and the sorting is overall poor; the skewness is mostly positive, and the kurtosis is wide, which reflects the obvious characteristics of river sand deposition. (2) The miner

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Vokurkova, Zuzana. "Grammatical and Lexical Variation of Standard Tibetan Between the Region of Lhasa and the Tibetan Diaspora." Archiv orientální 90, no. 1 (2022): 147–81. http://dx.doi.org/10.47979/aror.j.90.1.147-181.

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In this paper, I deal with differences between the variants spoken in Lhasa and in the Tibetan diaspora. Although they are very similar, one can find various minor differences in the grammar and numerous differences in the lexicon of these two variants of Standard spoken Tibetan. Dissimilarities in the grammar can be illustrated by the use of different variants of case particles or by different verb stems of a verb. Another example of geographical alterations of Standard Tibetan is epistemic verb endings. Certain epistemic types are common for Lhasa and the diaspora, but other types are only u

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Shao, Quan, Yan Zhou, and Pei Zhu. "Spatiotemporal Analysis of Environmental Factors on the Birdstrike Risk in High Plateau Airport with Multi-Scale Research." Sustainability 12, no. 22 (2020): 9357. http://dx.doi.org/10.3390/su12229357.

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The aircrafts’ engine performance deteriorates sharply during the take-off and landing at high plateau airport. This situation increases the take-off or landing distance, aggravating the hidden danger of birdstrikes at high plateau airport. This paper first used GIS to classify and rasterize the bird data and calculated the monthly Birdstrike Risk Index (BRI) within 6, 13, and 25 km radii of Lhasa Airport, based on the bird observation data of Tibet and the birdstrike data of Lhasa Airport from 2015 to 2019. The spatiotemporal relationships between the BRI and the environmental factors around

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Wang, Sishi, Xin Tan, and Fenglei Fan. "Changes in Impervious Surfaces in Lhasa City, a Historical City on the Qinghai–Tibet Plateau." Sustainability 15, no. 6 (2023): 5510. http://dx.doi.org/10.3390/su15065510.

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Impervious surface cover reflects the urban environment and urban expansion. Lhasa City is a historical city and one of the most populous on the Qinghai–Tibetan Plateau, and has been experiencing rapid urbanization in recent years. Analyzing the impervious surface distribution can reveal urban development characteristics and provide data for sustainable urban planning to protect the heritage. This study explored the spatial and temporal changes and expansion patterns of impervious surfaces in different zones of Lhasa City. Impervious surface maps (2014 and 2021) were extracted from Gaofen-1 im

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Yao, Qiyan, Kaijun Li, Zhiqiang Wang, Wumeng Yang, and Hong Bin. "Optimization Study of Non-motorized left Turn at Intersections based on Webster's Timing Method." Highlights in Science, Engineering and Technology 78 (December 26, 2023): 10–16. http://dx.doi.org/10.54097/t5mkgk65.

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Lhasa tourism drives Lhasa's economic development and also brings a considerable burden to Lhasa's transportation, so solving the problem of traffic congestion caused by the increase of non-motorized traffic flow at the intersection in Lhasa is of great significance to the development of Lhasa's transportation. In order to solve the problem of non-motorized vehicles turning left at the intersection and alleviate the traffic pressure in Lhasa, this paper constructs a multi-phase signal timing optimization scheme based on the Webster timing method model, and takes the intersection of Dangre Midd

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Wang, Ying Ying, Yan Feng Liu, and Deng Jia Wang. "Numerical Simulation Analysis on Residential Building Indoor Thermal Environment of Intermittent Heating in Lhasa Based on DeST." Advanced Materials Research 462 (February 2012): 215–20. http://dx.doi.org/10.4028/www.scientific.net/amr.462.215.

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The aim of this paper is to analyze whether the intermittent heating mode is feasible for residential buildings in Lhasa, the thermal parameters of each palisade structure and the influence law of intermittent heating mode on the indoor thermal environment. In this paper, the DeST energy consumption simulation software that is compiled by Tsinghua University was used to simulate and analyze a residential building in Lhasa city. The results show that: It is completely feasible to carry out intermittent heating in Lhasa area. Considering the indoor temperature reduction should not be too large d

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Basnyat, Buddha. "Acetazolamide for tourists to Lhasa." Wilderness & Environmental Medicine 9, no. 3 (1998): 191. http://dx.doi.org/10.1580/1080-6032(1998)009[0191:afttl]2.3.co;2.

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Wangmo, Tsoja, Norsang Gelsor, Jens Havskov, Nima Puntsog, and Baima Tsering. "Lhasa seismicity during 2004-2006." Journal of Nepal Geological Society 38 (September 25, 2008): 9–14. http://dx.doi.org/10.3126/jngs.v38i0.31475.

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The Tibetan Plateau is an active seismic region due to the collision between Indian and Eurasian plates. We have set up a new seismic network in the heart of the Tibetan Plateau, in the Lhasa region, to detect seismic activities. The measured data show that Lhasa is a seismically active region where at least 716 earthquakes were detected and a total of 218 events of magnitude greater than 2.0 occurred in the period between January 2004 and July 2006. Out of them, 11 earthquakes had a magnitude greater than 5.0. A high seismic activity was observed along the Dangshung fault zone.

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39

Cathcart, Adam. "Tibet in Agony: Lhasa 1959." Chinese Historical Review 28, no. 2 (2021): 204–6. http://dx.doi.org/10.1080/1547402x.2021.1990538.

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40

Meredith Hess, Julia. "Tibet in Agony: Lhasa 1959." Canadian Journal of History 53, no. 3 (2018): 597–98. http://dx.doi.org/10.3138/cjh.ach.53.3.br41.

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41

Narayanan, Raviprasad. "Railway to Lhasa: An Assessment." Strategic Analysis 29, no. 4 (2005): 739–45. http://dx.doi.org/10.1080/09700161.2005.12050290.

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42

Grunfeld, A. Tom. "Lhasa. Streets With Memories (review)." China Review International 13, no. 2 (2007): 349–51. http://dx.doi.org/10.1353/cri.2008.0040.

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43

Qiogya. "What Really Happened In Lhasa." China Report 24, no. 3 (1988): 383–85. http://dx.doi.org/10.1177/000944558802400308.

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Muhtar, Amina. ""Little Lhasa," Tibetans in Exile." SAIS Review of International Affairs 31, no. 1 (2011): 153–66. http://dx.doi.org/10.1353/sais.2011.0008.

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van Rozendaal, Erik L. M., Martin A. Ott, and Hans W. Scheeren. "A LHASA analysis of taxol." Recueil des Travaux Chimiques des Pays-Bas 113, no. 5 (1994): 297–303. http://dx.doi.org/10.1002/recl.19941130507.

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46

Macário, Fernanda Cunha Boer, Karen Pierin Silvestre, and Stella Helena Sakata. "Displasia coxofemoral em cão de raça lhasa apso / Canine hip dysplasia in lhasa apso." Brazilian Journal of Animal and Environmental Research 4, no. 1 (2021): 77–80. http://dx.doi.org/10.34188/bjaerv4n1-009.

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47

Lei, Ming, Jian-Lin Chen, Ji-Feng Xu, Yun-Chuan Zeng, and Qiu-Wei Xiong. "Late Cretaceous magmatism in the NW Lhasa Terrane, southern Tibet: Implications for crustal thickening and initial surface uplift." GSA Bulletin 132, no. 1-2 (2019): 334–52. http://dx.doi.org/10.1130/b31915.1.

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Abstract Crustal thickening and uplift of southern Tibet have been widely associated with India-Asia continental collision during the Cenozoic. However, recent studies indicated that the crust of the northwestern (NW) Lhasa Terrane was thickened during the late Mesozoic. Here we report geochronological and geochemical data for the Gaerqiong diorite porphyries (GPs) and Xiongma plutons (XPs) in the NW Lhasa terrane, southern Tibet. Zircon U-Pb dating suggests that these intrusive rocks were generated at ca. 85 and ca. 88 Ma, respectively. The GPs are characterized by high MgO, Cr, and Ni conten

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Wang, Yi-Gang, and Dong-Li Sun. "The Triassic and Jurassic paleogeography and evolution of the Qinghai–Xizang (Tibet) Plateau." Canadian Journal of Earth Sciences 22, no. 2 (1985): 195–204. http://dx.doi.org/10.1139/e85-017.

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The Kunlun, Qilian, and Qinling mountains already existed in embryonic form as coastal ranges in Triassic times. Marine conditions predominated to the south. The southern coastline is demarcated by the northern margin of the Tertiary Siwalik sediments. The paleo-landmass of Longmenshan–Sichuan–Yunnan separated this sea from that of southwest China. By Jurassic times, the coastline of the Eurasian continent within what is now China had already moved southwards to a line along the Kunlun and Hengduan mountains.Mainly on the basis of differences between continental and oceanic crust, several diff

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Qi, Bing, Miao Yu, and Yunyuan Li. "Multi-Scenario Prediction of Land-Use Changes and Ecosystem Service Values in the Lhasa River Basin Based on the FLUS-Markov Model." Land 13, no. 5 (2024): 597. http://dx.doi.org/10.3390/land13050597.

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The quantitative evaluation and prediction of ecosystem service value (ESV) in the Lhasa River Basin can provide a basis for ecological environment assessment and land-use optimization and adjustment in the future. Previous studies on the ESV in the Lhasa River Basin have focused mainly on static assessment and evolution analysis based on historical data, and have not considered future development trends. Moreover, most of the current driving factors selected in land use and ESV prediction studies are homogeneous, and do not reflect the geographical and cultural characteristics of the study ar

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Zhu, Zhicai, Qingguo Zhai, Peiyuan Hu, et al. "Closure of the Bangong–Nujiang Tethyan Ocean in the central Tibet: Results from the provenance of the Duoni Formation." Journal of Sedimentary Research 89, no. 10 (2019): 1039–54. http://dx.doi.org/10.2110/jsr.2019.55.

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ABSTRACT The closure of the Bangong–Nujiang Tethyan Ocean (BNTO) and consequent Lhasa–Qiangtang collision is vital to reasonably understanding the early tectonic history of the Tibetan Plateau before the India-Eurasia collision. The timing of the Lhasa–Qiangtang collision was mainly constrained by the ophiolite and magmatic rocks in previous studies, with only limited constraints from the sedimentary rocks within and adjacent to the Bangong–Nujiang suture zone. In the middle segment of the Bangong–Nujiang suture zone, the Duoni Formation, consisting of a fluvial delta sequence with minor andes

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