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  1. 1581
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    Climatic Cycles and Gradients of the El Niño Core Region in North Peru by Rütger Rollenbeck, Fabian Bayer, Jannes Münchow, Michael Richter, Rodolfo Rodriguez, Nestor Atarama

    Published 2015-01-01
    “…Also, there are regional factors: an extended sea-breeze system, the barrier-effect of the Andes, additional energy input by elevated radiation absorption at the mountain slopes, local wind systems, and the variations of the sea surface temperature. …”
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  3. 1583
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    Spatial and Temporal Distribution of Sand Mining in Poyang Lake and Its Impact on Lake Basin Morphology Based on Remote Sensing Images by LIU Jiahao

    Published 2024-08-01
    “…The results show that: ① sand mining vessels were mainly distributed in the north lake part of Poyang Lake from 2000 to 2006, and the number of sand mining vessels plummeted in 2008 due to the impact of the banning policy, and 2016 was the peak of sand mining activities, in which the policy regulation is the main factor for the change of spatio-temporal distribution and number and scale of sand mining vessels in Poyang Lake from 2000 to 2021; ② the human sand mining activities have affected to a certain extent the hydrological sediment balance of Poyang Lake to a certain extent; ③ sand mining activities led to a decrease in the beach area in the inlet channel of Poyang Lake and Songmen Mountain area, while the net increase in the beach area in the southeast area of Tangyin was about 7.95 km<sup>2</sup>, mainly due to siltation caused by the spreading of sediments from inlet tributaries of the lake. …”
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    Globally scalable glacier mapping by deep learning matches expert delineation accuracy by Konstantin A. Maslov, Claudio Persello, Thomas Schellenberger, Alfred Stein

    Published 2025-01-01
    “…Assessing the spatial, temporal and cross-sensor generalisation shows that our best strategy achieves intersection over union  >0.85 on previously unobserved images in most cases, which drops to  >0.75 for debris-rich areas such as High-Mountain Asia and increases to  >0.90 for regions dominated by clean ice. …”
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  9. 1589

    A dataset of gridded precipitation intensity-duration-frequency curves in Qinghai-Tibet Plateau by Zhihui Ren, Yan-Fang Sang, Peng Cui, Fei Chen, Deliang Chen

    Published 2025-01-01
    “…Abstract The Qinghai-Tibet Plateau (QTP), a high mountain area prone to destructive rainstorm hazards and inducing natural disasters, underscores the importance of developing precipitation intensity-duration-frequency (IDF) curves for estimating extreme precipitation characteristics. …”
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    Influence of Base Rock Deterioration on Tunnel Bottom Structure Damage under Train Excitation by Zi-Qiang Li, Wei-Wei Huang, Zheng Li, Jian-Wen Feng, Hang Zhang, Qi Li

    Published 2023-01-01
    “…In the ground of the preliminary study of the Taihangshan Mountain Tunnel, it was observed that under water-rich conditions, the long rolling of heavy-haul trains would deteriorate the surrounding rock, thereby causing damage to the bottom structure. …”
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  13. 1593

    Vitreous Hemorrhage following High-Altitude Retinopathy by Arjun Shrestha, Rinkal Suwal, Biju Shrestha

    Published 2021-01-01
    “…An apparently healthy 29-year-old boy presented with a history of floater and slight diminution of vision in the left eye after climbing the mountain 4760 meters high. Results. The visual acuity at presentation was 20/20 in the right eye and 20/30 in the left eye. …”
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  14. 1594

    An Analysis of Vegetation Change Trends and Their Causes in Inner Mongolia, China from 1982 to 2006 by Baolin Li, Wanli Yu, Juan Wang

    Published 2011-01-01
    “…In or to the south of Horqin Sandy Land, in the Hetao Plain, and at the northern foothills of the YinshanMountain, the significant NDVI increase trends were mainly caused by the increase of the millet yield per unit of cropland. …”
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  15. 1595

    The zoning of the relative morphotectonic activity of the Kan-Soleghan basin with an emphasis on the location of the Tehran-North Freeway tunnel by sara Kiani, Amir Karam, Nasrin Hoseinaei

    Published 2023-09-01
    “…In this research, morphotectonic indices including river asymmetry index (Af), basin shape (Bs), hypsometric integral (Hi), Stream length index (Sl), mountain front sinusity (Smf), valley width to valley height (Vf), topographic symmetry (Tp) was calculated. …”
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    Rapid Built-up of PM10 in the Ambient Air of the Leeward Side Resulting from Strong Pressure Gradient Force Associated with Density Current by Wei-Kuo Soong, Chung-Hsuang Hung

    Published 2024-07-01
    “…According to the Froude number (above 0.5), the flow in northern Taiwan can pass the terrain, producing subsidence warming in central Taiwan, which is located at the leeward side of the northeastern Central Mountain Range (CMR). In addition, strong winds blew river dusts in the middle of Taiwan under a stable atmosphere and stimulated density current, transporting PM10 to southern Taiwan. …”
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  19. 1599

    Modelling of Chain Process of Debris Flow Blocking River and Induced Flood Disaster in Meizoseismal Area ——A Case of Xiazhuang Gully in Wenchuan County by LUO Yuting, WANG Lijuan, MA Song, TANG Yao

    Published 2023-01-01
    “…After the Wenchuan earthquake,there has been a sharp increase in the frequency of debris flow activity,which is featured by low rainfall threshold,frequent occurrence,wide impact and strong destruction.The hazards mainly include siltation,impact,river blocking and inundation.Among them,the mudslide blocking river shows particularly prominent disaster effect,seriously threatening the improvement of mountain infrastructure,and residents' life and property safety.The research of the dynamic process of river blocking disaster chain of debris flow can provide scientific reference for debris flow hazard prevention and early warning.Based on field surveys,physical tests,remote sensing images and rainfall data for a typical watershed,a numerical simulation was conducted to study the dynamic process of the river blocking disaster chain of debris flow in Xiazhuang Gully.The simulation results show that the debris flow reaches the outlet of the basin at t=120 step;and at t=130 step the debris flow pushes forward and blocks part of the main river;at t=140 and 150 step the debris flow completely blocks the main river,forming a debris-dam with a length,width and thickness of 236.0 m,74.0 m,6.2 m and 312.0 m,79.0 m,and 7.1 m,respectively,which causes the upstream water level to rise,with an inundation depth of the upstream residential area of 3-5 m.By comparing the simulation results with the field measured data,the accuracy of the simulation reaches up to 84.9%,which indicates that the model is of good applicability to simulating the disaster chain process of landslide-debris flow-flood.…”
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  20. 1600

    Physics Features of TRU-Fueled VHTRs by Tom G. Lewis, Pavel V. Tsvetkov

    Published 2009-01-01
    “…The current waste management strategy for spent nuclear fuel (SNF) mandated by the US Congress is the disposal of high-level waste (HLW) in a geological repository at Yucca Mountain. Ongoing efforts on closed-fuel cycle options and difficulties in opening and safeguarding such a repository have led to investigations of alternative waste management strategies. …”
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