
The huge underground space of the QinghaiTibet Plateau

Challenges of, Progress in, and Prospects of UltraLong Deep
2024年8月29日 The Qinghai–Tibet Plateau region is undergoing the construction of numerous ultralong deep tunnels in various national strategic water conservancy and hydropower 2021年5月6日 In the Cenozoic, the continual northward subduction of the Indian Plate toward the Eurasian Plate have vertically thickened the crust, which has caused lithospheric Journal of Geophysical Research: Solid Earth2019年10月16日 In this study, we take the Qinghai–Tibet Plateau as a pilot site to illustrate the international geoscience collaboration during this time We first introduce the International The Qinghai–Tibet Plateau: pilot site for international collaboration 2023年12月15日 In this study, through the Second Tibetan Plateau Scientific Expedition and Research and field measurements, the oxygen concentration data and corresponding Surface oxygen concentration on the QinghaiTibet Plateau

Conflict or Coordination? The Spatiotemporal Relationship
2023年9月25日 The QinghaiTibet Plateau (QTP), with an average altitude of over 4,000 m and extensive distribution of glaciers and permafrost, is the source of the nine rivers in Asia, 2021年1月11日 Permafrost extends 40% of the QinghaiTibet Plateau (QTP), a region which contains the headwaters of numerous major rivers in Asia As an aquiclude, permafrost Permafrost Hydrology of the QinghaiTibet Plateau: A Review of 2015年9月7日 The fast uplift, ie, the Qingzang Movement, began since ~36 Ma, evidenced by massive molasse deposits around the plateau margin and the synchronous occurrence of The Qingzang movement: The major uplift of the QinghaiTibetan 2022年6月22日 In this paper, we characterized surface deformation in space and time over the main continuous permafrost area on the QTP, by analyzing 11 ascending and 8 descending Monitoring RegionalScale Surface Deformation of the Continuous

Tectonic evolution of the QinghaiTibet Plateau ScienceDirect
2012年7月7日 The QinghaiTibet Plateau can be divided into three huge orogenic systems, from northeast to southwest: (1) the Qinling–Qilianshan–Kunlunshan, (2) the Qiangtang–Sanjiang, Location maps and landslides in the QinghaiTibet Plateau (QTP) (a) Extent of the study area, location of monitoring stations, and location of landslides associated with permafrost thaw The monitoring network comprises two automatic meteorological stations and one active layer observation station along the QinghaiTibet engineering corridor Formation and evolution of thermokarst landslides in the QinghaiTibet 2021年8月13日 Abstract Lakes can be effective indicators of climate change, and this is especially so for the lakes over the Qinghai–Tibet Plateau (QTP), the highest plateau in the world, which undergoes little direct human influence 100 years of lake evolution over the Qinghai–Tibet structurepopulated areas: case study of the Qinghai‑Tibet Plateau in China
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100 years of lake evolution over the QinghaiTibet Plateau
2021年8月1日 Lakes can be effective indicators of climate change, and this is especially so for the lakes over the Qinghai–Tibet Plateau (QTP), the highest plateau in the world, which undergoes little direct 2023年3月10日 21 Overview of the study area The QinghaiTibet Plateau is located in the west of China (26°00’–39°47’N, 73°19’–104°47’E) and is the largest plateau in China and the highest in the world (Fig 1)The main vegetation landscape is alpine and alpine land, and the main climate type is plateau mountain climate with strong sunshine, and significant seasonal differences in Contamination characteristics, source analysis, and spatial 2024年8月2日 Revealing the response of vegetation on the QinghaiTibet Plateau (QTP) to climate change and human activities is crucial for ensuring East Asian ecological security and regulating the global climate However, the current research rarely explores the timelag effects of climate on vegetation growth, leading to considerable uncertainty in analyzing the driving SpatioTemporal Dynamics of Vegetation and Its Driving MDPI2018年10月25日 Hydrochemical Dynamic Characteristics and Evolution of Underground Brine in the Mahai Salt Lake of the Qaidam Basin QinghaiTibet Plateau Shuya HU, Shuya HU Department of Environmental Science and Engineering, Qingdao Therefore, we selected underground brine from the Mahai Salt Lake, collecting a total of 183 brine samples Hydrochemical Dynamic Characteristics and Evolution of Underground

Accelerating thermokarst lake changes on the Qinghai–Tibetan Plateau
2024年2月5日 The thermokarst lakes on the Qinghai–Tibet Plateau have presented an expansionary trend, and the number of thermokarst lakes in the Beilu River Basin increased by 534, and the size increased by 2022年10月4日 1 Introduction The QinghaiTibet Plateau (TP) is the highest and youngest plateau in the world and one of the most sensitive areas to global climate change (Liu and Chen Citation 2000; Kuang and Jiao Citation 2016)The lake areas in the TP account for more than half of China's total lake area (Zhang et al Citation 2019; Wan et al Citation 2019)Full article: Mapping of lakes in the QinghaiTibet Plateau from 2023年12月15日 The QinghaiTibet Plateau (QTP) is the “third pole” of the Earth 1, with a total area of approximately 25 × 10 6 km 2 and an average elevation of over 4,000 m above sea level 2The air is Surface oxygen concentration on the QinghaiTibet Plateau The Qinghai–Tibet Plateau (QTP) sensu lato (sl) houses an exceptional species diversity in AsiaTo develop a comprehensive understanding of species diversity in this fascinating region, we reviewed recent progress from biogeographic, paleogeographic, paleontological and genomic research of both plants and animals in the QTPslNumerous studies have been conducted to Evolutionary origin of species diversity on the Qinghai–Tibet Plateau

Cryostructures and ground ice content in icerich permafrost area
2021年5月13日 Permafrost is an important part of the cryosphere, playing an integral role in the hydrologic cycle, ecology, and influencing human activity Melting of ground ice can drastically change landscapes and associated thaw subsidence may induce instability of infrastructure The terrain conditions on the QinghaiTibet Plateau are complex, and the spatial distribution of 2020年10月26日 The Qinghai–Tibet Plateau is a unique but fragile ecosystem, and its landscape services are vital components to the sustainability in this specific polar region This study sought to understand the landscape service relationships, their dynamics and influencing factors, and achieve a sustainable landscape management in the Qinghai–Tibet PlateauRelationships of multiple landscape services and their influencing In this paper, the basic climate characteristics of winter, summer and annual mean surface temperatures were analyzed by using 86 stations during period from founding to 2001 over the Tibetan Plateau, and the spatial anomaly structure and time evolution tendency have been analysed systematically through principal component analysis, a periodic function and a THE TIMESPACE VARIETY CHARACTERISTICS OF THE2021年11月24日 The Qinghai–Tibet Plateau, which is the source area for the Yellow River, Yangtze River, and Lancang River, is known as the great water tower of Asia (Zhang et al 2013; Huang et al 2020)The abundant water resources of this plateau not only have an important role in the sustainable economic development of the plateau region but also have a strategic Spatiotemporal variation and periodic evolution characteristics
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(PDF) Effect of the Asian Water Tower over the QinghaiTibet Plateau
2019年8月7日 From the perspective of regional and global atmospheric moisture circulation, this paper summarizes the unique thermal and dynamic mechanisms present in the Qinghai–Tibet Plateau (QTP) and their 2020年12月12日 1 Introduction Frozen ground is an important component of the cryosphere, which exerts strong influences on regional ecology, hydrology and infrastructure engineering (W Wang et al, 2018; Westermann et al, 2015)The QinghaiTibet Plateau (QTP) is underlain by typical highaltitude permafrost region, which is undergoing more dramatic climatic warming Simulation of the Present and Future Projection of Permafrost on PDF On Nov 1, 2021, Jian‐Quan Liu and others published Plant diversity and ecology on the Qinghai–Tibet Plateau which share more functional trait space due to environmental filtering or Plant diversity and ecology on the Qinghai–Tibet PlateauThe Qinghai–Tibet Plateau (QTP) sensu lato (sl) houses an exceptional species diversity in AsiaTo develop a comprehensive understanding of species diversity in this fascinating region, we reviewed recent progress from biogeographic, paleogeographic, paleontological and genomic research of both plants and animals in the QTPslNumerous studies have been conducted to Evolutionary origin of species diversity on the Qinghai–Tibet Plateau
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SentinelBased Inventory of Thermokarst Lakes and Ponds Across
Thermokarst lakes and ponds (hereafter referred to as thaw lakes) play an important role in the permafrost regions by regulating hydrology, ecology, and biogeochemistry However, detailed quantitative information on thaw lake extent and distribution remains poorly resolved across the entire permafrost regions on the QinghaiTibet Plateau (QTP)2017年6月23日 The QinghaiTibet Plateau (QTP) is the largest geographical unit with the highest elevation on earth where grassland ecosystems dominate over 50% of whole plateau area 1It is also an important Spatiotemporal dynamics of grassland 2019年1月1日 on the QinghaiTibet Plateau of about 2 m in average (Mu et al 2015 ), the organic carbon stored in permafrost layer (2 – 3m ) i n the upper 3 m was estimated to be 109 (45 – 173) Pg (Fig Assessment of frozen ground organic carbon pool 2021年10月25日 The QinghaiTibet Plateau (QTP) is the largest alpine permafrost region in the world (Yang et al, 2019) The permafrost area is estimated to be as large as 106 × 10 6 km 2 on the QTP, which occupies Sentinel‐Based Inventory of Thermokarst Lakes and
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Ecological Progress on the QinghaiTibet Plateau Ministry of
2018年7月18日 Located in Southwest China, the QinghaiTibet Plateau covers the entire Tibet Autonomous Region and Qinghai Province, in addition to parts of Sichuan, Yunnan, Gansu and Xinjiang It is about 26 million sq km in area and most of it lies at an altitude of more than 4,000 m above sea level2012年11月1日 Background and aims The warming of the planet in recent decades has caused rapid, widespread permafrost degradation on the Qinghai–Tibet Plateau These changes may significantly affect soil moisture content and nutrient supply, thereby affecting ecosystem structure and function This study aimed to describe the dynamic changes in thaw depth, assess the Linking thaw depth with soil moisture and plant community 2015年9月7日 Thirtyfive years ago, the idea of a young QinghaiTibetan Plateau was proposed based on a comprehensive investigation on the QinghaiTibetan Plateau This hypothesis suggested that the plateau began to rise from a planation surface (relict surface) that was less than 1000 m high formed during the Miocene to Pliocene The fast uplift, ie, the Qingzang The Qingzang movement: The major uplift of the QinghaiTibetan Plateau Tibetan Plateau, or QinghaiTibet Plateau as it called in China (simplified Chinese:青藏高原), is the highest plateau in the world with an average altitude of 4,500m, and was reputed as “the roof of the world” and “the world’s third pole” Located in Central Asia, it covers an area of 2,500,000,000 square kilometers, which is also the largest plateau in ChinaQinghaiTibet Plateau: the World's Highest Plateau Top China
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Effects of grassland degradation on ecological stoichiometry of
2020年6月20日 On the QinghaiTibet Plateau (QTP), “Spacefortime” substitution is an alternative approach to study longterm phenomena in ecology (Pickett, 1989; Blois et al, 2013) It has been used widely and successfully, especially in systems that experience strong successional dynamics (Pickett, 1989)In order to study the space distribution of Grain Number per spike (GNS) and its relationship with the environmental factors in the QinghaiTibet Plateau, 83 data samples from different ecological areas were selected for GNS inverstigation Meanwhile, the seeds of highland barley were harvested and planted in the farm of Xizang Agriculture and Animal Husbandry College; the Space Distribution of Highland Barley GNS and its Relationship 2020年5月18日 Permafrost on the Qinghai–Tibet Plateau (QTP) has undergone degradation as a result of recent climate change This may alter the thermo‐hydrological processes and unlock soil organic carbon Changing climate and the permafrost environment on the Qinghai–Tibet 2023年3月1日 Land degradation has become a catastrophic global environmental issue The current status of land degradation and changing trends of land remain unclear on the QinghaiTibet Plateau (QTP)Integrated assessments of land degradation on the QinghaiTibet plateau

Interactions of the Westerlies and Asian Summer
2022年11月9日 Located at a climate junction, the northeastern QinghaiTibetan Plateau (QTP) is a sensitive zone for the interaction of the westerlies and ASM In the current work, we present a new loess data set from the northeastern QTP 2011年12月15日 Study of the characteristics of the crustal magnetic anomaly in the QinghaiTibet Plateau and the adjacent areas helps better understand the lithospheric structure and evolution, as well as the regional geodynamic processes Here we analyze the distribution laws of the crustal magnetic anomaly and its vertical gradient, the decay characteristics of the Characteristics of the crustal magnetic anomaly and regional 2012年12月6日 The areal extent of permafrost in China has been reduced by about 186 % during the last 30 years Due to the combined influences of climate warming and human activities, permafrost has been degrading extensively, with marked spatiotemporal variability Distribution and thermal regimes of permafrost and seasonal freezethaw processes are closely related to Permafrost and groundwater on the QinghaiTibet Plateau and in 2024年10月21日 Plateau of Tibet, vast high plateau of southwestern China It encompasses all of the Tibet Autonomous Region and much of Qinghai province and extends into western Sichuan province and southern Uygur Autonomous Region of Xinjiang The region lies between the Kunlun Mountains and its associatedPlateau of Tibet Himalayas, Plateau Region, Plateau Lakes

Protecting rare and endangered species under climate change on
2018年12月10日 The QinghaiTibet Plateau is the highest and biggest plateau, (Parmesan et al, 1999) and the redistributions of species pose a huge challenge for the static boundary of current protected area (PA) networks (Chen, Hill This index was measured in geographic space using a defined spatial neighborhood according to Equation 1 A large number of paleolandslide deposits exist in the Southeastern margin of the Qinghai–Tibet Plateau Once these deposits are destroyed, the disaster chain will cause huge damage to life and property and have an impact on local geomorphic evolution Diverse models are applied to analyze different geological problems of paleolandslide deposits, which can produce the Stability evaluation and potential damage of a giant paleo 2024年9月9日 "The strongest net carbon sink effect along the QinghaiTibet Plateau occurs at an altitude of 4,000 meters," said Wei Da, a researcher at the institute who coauthored a study published in the Proceedings of the National Academy of Sciences, a peerreviewed journal of the academy in the United StatesQinghaiTibet Plateau research offers insight into effects of 2022年9月12日 These areas are generally low in terrain and hence receive water from the upstream region In 2015, the precipitation of the QinghaiTibet Plateau was low due to the El Niño effect, and the supply of water provision services decreased Some areas in the southwest of the QinghaiTibet Plateau exhibit a negative dynamic water surplus (figure 4)Is the 'water tower' reassuring? Viewing water security of Qinghai

Chronology and tectonic significance of Cenozoic faults in the
2013年9月1日 The Liupanshan Arcuate Tectonic Belt (LATB) is located at the northeastern margin of the Qinghai–Tibet Plateau Major strikeslip and thrust faults in the Liupanshan area are prominent Cenozoic