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Comprehensive applicability evaluation of four precipitation products at multiple spatiotemporal scales in Northwest China

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Journal of Arid Land 2024年第9期16卷 1232-1254页

作者： WANG Xiangyu XU Min kang shichang LI Xuemei HAN Haidong LI Xingdong School of Mathematics Lanzhou Jiaotong UniversityLanzhou 730070China Key Laboratory of Cryospheric Science and Frozen Soil Engineering Northwest Institute of Eco-Environment and ResourcesChinese Academy of SciencesLanzhou 730000China University of Chinese Academy of Sciences Beijing 100049China Faculty of Geomatics Lanzhou Jiaotong UniversityLanzhou 730070China

Precipitation plays a crucial role in the water cycle of Northwest *** accurate precipitation data is crucial for regional water resource management,hydrological forecasting,flood control and drought ***,the applicability of multi-source precipitation products for long time series in Northwest China has not been thoroughly *** this study,precipitation data from 183 meteorological stations in Northwest China from 1979 to 2020 were selected to assess the regional applicability of four precipitation products(the fifth generation of European Centre for Medium-Range Weather Forecasts(ECMWF)atmospheric reanalysis of the global climate(ERA5),Global Precipitation Climatology Centre(GPCC),Climatic Research Unit gridded Time Series Version 4.07(CRU TS v4.07,hereafter CRU),and Tropical Rainfall Measuring Mission(TRMM))based on the following statistical indicators:correlation coefficient,root mean square error(RMSE),relative bias(RB),mean absolute error(MAE),probability of detection(POD),false alarm ratio(FAR),and equitable threat score(ETS).The results showed that precipitation in Northwest China was generally high in the east and low in the west,and exhibited an increasing trend from 1979 to *** with the station observations,ERA5 showed a larger spatial distribution difference than the other *** overall overestimation of multi-year average precipitation was approximately 200.00 mm and the degree of overestimation increased with increasing precipitation *** multi-year average precipitation of GPCC and CRU was relatively close to that of station *** trend of annual precipitation of TRMM was overestimated in high-altitude regions and the eastern part of Lanzhou with more *** the monthly scale,GPCC performed well but underestimated precipitation in the Tarim Basin(RB=-4.11%),while ERA5 and TRMM exhibited poor accuracy in high-altitude ***5 had a large bias(RB≥120.00%)in winter months

关键词： precipitation products the fifth generation of European Centre for Medium-Range Weather Forecasts(ECMWF)atmospheric reanalysis of the global climate(ERA5) Global Precipitation Climatology Centre(GPCC) Climatic Research Unit gridded Time Series(CRU TS) Tropical Rainfall Measuring Mission(TRMM) applicability evaluation Northwest China

Quantifying glacier surging and associated lake dynamics in Amu Darya river basin using UAV and remote sensing data

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Journal of Mountain Science 2024年第9期21卷 2967-2985页

作者： SAFAROV Mustafo kang shichang MURODOV Murodkhudzha BANERJEE Abhishek NAVRUZSHOEV Hofiz GULAYOZOV Majid FAZYLOV Ali VOSIDOV Firdavs Key Laboratory of Cryospheric Science and Frozen Soil Engineering Northwest Institute of Eco-Environment and ResourcesChinese Academy of SciencesLanzhou 730000China Research Center for Ecology and Environment of Central Asia(Dushanbe) Dushanbe 734063Tajikistan University of Chinese Academy of Sciences Beijing 100049China Xinjiang Institute of Ecology and Geography Chinese Academy of SciencesUrumqi 830011China Mountain Societies Research Institute University of Central AsiaDushanbe 734000Tajikistan State Scientific Institution“Center for Research of Glaciers of the National Academy of Sciences of Tajikistan” Dushanbe 734025Tajikistan Institute of Water Problems Hydropower and Ecology of the National Academy of Sciences of TajikistanDushanbe 734025Tajikistan

Glaciers in the Pamir region are experiencing rapid melting and receding due to climate change,which has a significant implication for the Amu Darya river ***,surging glaciers,which undergo unpredictable advances,are potentially leading to the obstruction of high-altitude river channels and also glacial lake outburst *** of-703.5±30.0 *** is a substantial increase in the number(from 19 to 75)and area(from 4889.7±0.6 m2 to 15345.5±0.6 m2)of RGS lakes along with supra-glacier ponds based on a comparison of ArcGIS base map in 2011 and high-resolution UAV data in *** M glacier,number of lakes increased from 4 to 22 but the lake area declined from 10715.2±0.6 to 365.6±0.6 *** was noted that the largest lake in 2011 with an area of 10406.4±0.6 m2 at the southeastern portion of the glacier was not observed in 2023 due to *** the glaciers have substantially impacted the river flow(Abdukahor river)by obstructing a significant proportion of river channel in recent years and might cause outburst *** findings enhance the understanding of glacier dynamics and their impacts on the surrounding areas,emphasizing the urgent need for continued monitoring and appropriate management strategies,with a specific focus on surging glaciers and the associated risks.

关键词： UAV Remote sensing Climate change Glacier dynamics Google Earth Engine Pamir

A review of physicochemical properties of dissolved organic carbon and its impact over mountain glaciers

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Journal of Mountain Science 2024年第1期21卷 1-19页

作者： NIU Hewen CHEN Mengxue kang shichang SHUKLA Tanuj QIN Huili GAO Wanni HUANG Shihai ZHANG Fu State Key Laboratory of Cryospheric Sciences/National Field Science Observation and Research Station of Yulong Snow Mountain Cryosphere and Sustainable Development Northwest Institute of Eco-Environment and ResourcesChinese Academy of SciencesLanzhou 730000China School of Politics and International Relations Lanzhou UniversityLanzhou 730000China University of Chinese Academy of Sciences Beijing 10049China Dagu Glacier Scenic and Historic Interest Area Administration Luhua TownHeishui 615715China

Investigating the characteristics and transformation of water-soluble carbonaceous matter in the cryosphere regions is important for understanding biogeochemical process in the earth ***-soluble carbonaceous matter is a heterogeneous mixture of organic compounds that is soluble in aquatic *** its importance,we still lack systematic understanding for dissolved organic carbon(DOC)in several aspects including exact chemical composition and physical interactions with microorganisms,glacier *** review presents the chemical composition and physical properties of glacier DOC deposited through anthropogenic emission,terrestrial,and biogenic *** present the molecular composition of DOC and its effect over snow albedo and associated radiative *** indicate that DOC in snow/ice is made up of aromatic protein-like species,fulvic acid-like materials,and humic acid-like ***-absorbing impurities in surface snow and glacier ice cause considerable albedo reduction and the associated radiative forcing is definitely ***-soluble carbonaceous matter dominated the carbon transport in the high-altitude glacial *** to prevailing global warming and projected increase in carbon emission,the glacial DOC is expected to release,which will have strong underlying impacts on cryosphere *** results of this work have profound implications for better understanding the carbon cycle in high altitude cryosphere regions.A new compilation of globally distributed work is required,including large-scale measurements of glacial DOC over high-altitude cryosphere regions,to overcome and address the scientific challenges to constrain climate impacts of light-absorbing impurities related processes in Earth system and climate models.

关键词： Mountain glaciers Dissolved organic carbon Molecular composition Radiative forcing

Composition， Distribution and Constraint Factors of Fe Isotope(δFe) in the Surface Soils of the Tibetan Plateau

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Journal of Earth Science 2024年

作者： Ting Wei Zhiwen Dong Eric Parteli Xiaoli Liu shichang kang Yaping Shao State Key Laboratory of Cryosphere Sciences， Northwest Institute of Eco-Environment and Resources， Chinese Academy of Sciences Hubei Key Laboratory of Regional Ecology and Environmental Change， School of Geography and Information Engineering， China University of Geosciences Faculty of Physics， University of Duisburg-Essen Institute for Geophysics and Meteorology， University of Cologne

Iron isotopes， represented by δ56Fe， serve as valuable tools for constraining the surface iron processes and as potent tracers for studying the biogeochemical cycle of iron. Nevertheless， our comprehension of iron isotopes in the land surface processes of the Tibetan Plateau （TP） remains limited. In this study， we present the results of iron isotopic composition (δ56Fe) in the surface soils of the TP， encompassing both glacial and non-glacial regions characterized by rugged and flat topographies. Our findings reveal that soil δ56Fe values ranged from -0.01±0.05‰ to 0.14±0.01‰， with the highest values observed in eastern locations （0.14‰） and the lowest appeared in the northeast （-0.1‰）. On a global scale， the δ56Fe values observed in Tibetan soils exhibited relatively small variability compared to reservoirs marked by significant iron isotope fractionation. By contrast， the range of TP soils measured here was slightly larger than that of the Chinese Loess. Furthermore， we discerned noticeable spatial variations in δ56Fe across the large-scale region of TP， indicating a gradual increase trend from the northeast to the south and from the west to the east. These regional disparities in δ56Fe likely arise from a combination of constraining factors， including differences in mineralogy， lithological variations， organic matter content， and variations in chemical weathering intensity. This study is pivotal in advancing our understanding of land surface iron isotope δ56Fe dynamics and its role in the biogeochemical cycle within the TP region.

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Himalayas as a global hot spot of springtime stratospheric intrusions:Insight from isotopic signatures in sulfate aerosols

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Research in Cold and Arid Regions 2024年第1期16卷 5-13页

作者： Kun Wang shichang kang Mang Lin PengFei Chen ChaoLiu Li XiuFeng Yin Shohei Hattori Teresa L.Jackson JunHua Yang YiXi Liu Naohiro Yoshida Mark HThiemens State Key Laboratory of Cryospheric Science Northwest Institute of Eco-Environment and ResourcesChinese Academy of Sciences(CAS)LanzhouGansu 730000China State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryCASGuangzhouGuangdong 510640China University of Chinese Academy of Sciences Beijing 100049China International Center for Isotope Effects Research(ICIER) School of Earth Sciences and EngineeringNanjing UniversityNanjingJiangsu 210023China Frontiers Science Center for Critical Earth Material Cycling State Key Laboratory for Mineral Deposits ResearchSchool of Earth Sciences and EngineeringNanjing UniversityNanjingJiangsu 210023China Department of Chemical Science and Engineering School of Materials and Chemical TechnologyTokyo Institute of Technology4259 Nagatsuta-choMidori-kuYokohamaKanagawa 226-8502Japan Department of Chemistry and Biochemistry University of California San DiegoLa JollaCA 92093-0021USA Earth-Life Science Institute Tokyo Institute of TechnologyMeguro-kuTokyo 152-8551Japan National Institute of Information and Communications Technology KoganeiTokyo 184-8795Japan

Downward transport of stratospheric air into the troposphere(identified as stratospheric intrusions)could potentially modify the radiation budget and chemical of the Earth's surface *** the highest and largest plateau on earth,the Tibetan Plateau including the Himalayas couples to global climate,and has attracted widespread attention due to rapid warming and cryospheric *** studies recognized strong stratospheric intrusions in the Himalayas but are poorly understood due to limited direct evidences and the complexity of the meteorological dynamics of the third ***^(35)S is a radioactive isotope predominately produced in the lower stratosphere and has been demonstrated as a sensitive chemical tracer to detect stratospherically sourced air mass in the planetary boundary ***,we report 6-month(April–September 2018)observation of^(35)S in atmospheric sulfate aerosols(^(35)SO_(4)^(2-))collected from a remote site in the Himalayas to reveal the stratospheric intrusion phenomenon as well as its potential impacts in this *** the sampling campaign,the^(35)SO_(4)^(2-)concentrations show an average of 1,070±980 atoms/m^(3).In springtime,the average is 1,620±730 atoms/m^(3),significantly higher than the global existing data measured so *** significant enrichments of^(35)SO_(4)^(2-)measured in this study verified the hypothesis that the Himalayas is a global hot spot of stratospheric intrusions,especially during the springtime as a consequence of its unique geology and atmospheric *** combined with the ancillary evidences,e.g.,oxygen-17 anomaly in sulfate and modeling results,we found that the stratospheric intrusions have a profound impact on the surface ozone concentrations over the study region,and potentially have the ability to constrain how the mechanisms of sulfate oxidation are affected by a change in plateau atmospheric properties and *** study provides new observational constraints on stra

关键词： Himalayas Stratospheric intrusions Cosmogenic^(35)SO_(4)^(2-) Ozone Atmospheric oxidation

Characteristics of carbonaceous aerosols analyzed using a multiwavelength thermal/optical carbon analyzer: A case study in Lanzhou City

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Science China Earth Sciences 2019年第2期62卷 389-402页

作者： Yulan ZHANG shichang kang State Key Laboratory of Cryospheric Sciences Northwest Institute of Eco-Environmental Resources Chinese Academy of Sciences Geoscience Innovation and Innovation Center of the Tibetan Plateau Chinese Academy of Sciences University of Chinese Academy of Sciences

Characteristics of atmospheric carbonaceous aerosols in Lanzhou City from December 2014 to November 2015 are analyzed using a multiwavelength thermal/optical carbon analyzer. Results reveal that average concentrations of black carbon (BC) and organic carbon in atmospheric aerosols at Lanzhou are 6.7 and 25.4 μg m^(-3), respectively, showing obvious seasonality (higher in winter and lower in summer). This is consistent with findings in cities of northern China. Primary organic aerosols and secondary organic aerosols respectively account for approximately 60% and 17% of carbonaceous aerosols. No significant seasonality is found for secondary organic carbon, indicating that its potential sources do not vary significantly throughout the study period. The mass absorption cross-section (MAC_(632nm)) of BC is 7.1 m^2g^(-1), slightly higher than that of immediately emitted BC. MAC values of BC at different wavelengths vary drastically; they are higher for ultraviolet and visible light (8.5–10.2 m^2g^(-1)) than for near-infrared light (4.9–5.7 m^2g^(-1)). The aerosol absorption optical depth generally declines from the near-infrared to the near-ultraviolet region. The values are higher in winter than in summer, thus showing there are different contributions of BC deposition in different seasons. Brown carbon (BrC) has an ?ngstr?m absorption exponent (AAE) value of approximately 2.75, which is similar to the AAE value of BrC generated by diesel combustion (2.3). The contribution of BrC to light absorption is as much as 34% at a wavelength of 635 nm. This study demonstrates that the multiwavelength thermal/optical carbon analyzer can quantify absorption properties of BrC in atmospheric aerosols. This can enhance understanding of carbonaceous aerosols and provide key parameters for simulations of climate models.

关键词： Carbonaceous aerosol Black carbon Organic carbon Brown carbon Multiwavelength thermal/optical carbon analyzer

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表碛覆盖型冰川参数提取方法研究进展

冰川冻土 2024年第1期46卷 347-362页

作者：周卫永许民韩惠韩海东康世昌兰州交通大学测绘与地理信息学院甘肃兰州730070 中国科学院西北生态环境资源研究院冰冻圈科学国家重点实验室甘肃兰州730000 地理国情监测技术应用国家地方联合工程研究中心甘肃兰州730070 甘肃省地理国情监测工程实验室甘肃兰州730070 中国科学院大学北京100049 中国科学院西北生态环境资源研究院国家冰川冻土沙漠科学数据中心甘肃兰州730000

表碛的存在影响了大气与冰川间的能量传输过程,一方面,促进了冰面湖(塘)、冰崖的发育;另一方面,改变了冰川的消融过程和水文模式。利用表碛各项属性和物理参数模型化气候-表碛-冰川间的相互作用和反馈过程能够正确认识表碛覆盖型冰川变... 详细信息

表碛的存在影响了大气与冰川间的能量传输过程,一方面,促进了冰面湖(塘)、冰崖的发育;另一方面,改变了冰川的消融过程和水文模式。利用表碛各项属性和物理参数模型化气候-表碛-冰川间的相互作用和反馈过程能够正确认识表碛覆盖型冰川变化的过程和机理,有助于准确估算和预测冰川物质平衡,进而判断冰川未来演变趋势。本文系统总结和对比了识别表碛范围、提取冰川流速以及获取表碛物理参数的各种技术手段,介绍了表碛覆盖影响下冰川消融模型的原理和应用情况,同时还对这些方法或模型的局限性和发展趋势进行了讨论。表碛覆盖型冰川所处山区地形起伏大、地表变化复杂,为遥感方法识别表碛范围和提取冰川流速带来了诸多困难,如现有表碛识别方法仍无法克服固有干扰因素的影响,而流速提取方法需具备较强抗干扰能力,且配对影像时间基线需尽可能短。当前表碛覆盖型冰川相关研究中关键参数、数据存在大量空缺的状况有望在将来得到改善,冰川动力学过程和表碛动态变化的模型描述将更为精细,冰川物质平衡、径流量等指标的评估和预测也将更为真实准确。

关键词：表碛覆盖型冰川表碛参数提取冰川流速提取冰川物质平衡能量平衡模型

Seasonal features of aerosol particles recorded in snow from Mt. Qomolangma (Everest) and their environmental implications

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Journal of Environmental Sciences 2009年第7期21卷 914-919页

作者： CONG Zhiyuan kang shichang QIN Dahe Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing 100085 China State Key Laboratory of Cryospheric Science Chinese Academy of Sciences Lanzhou 730000 China Graduate University of the Chinese Academy of Sciences Beijing 100049 China

To assess the seasonality of aerosol deposition and anthropogenic effects on central Himalayas, a 1.85-m deep snow pit was dug on the northern slope of Mt. Qomolangma （Everest）. Based on the morphology and energy dispersive X-ray （EDX） signal, totally 1500 particles were classed into 7 groups： soot; aluminosilicates; fly ash; calcium sulfates; Ca/Mg carbonates; metal oxides; and biological particles and carbon fragments. The size distribution and number fractions of different particle groups exhibited distinct seasonal variations between non-monsoon and monsoon periods, which are clearly related to the differences in air mass pathways. Specifically, the relative abundance of soot in non-monsoon period （25%） was much higher than that in monsoon period （14%）, indicating Mt. Qomolangma region received more anthropogenic influence in non-monsoon than monsoon period.

关键词： Mt. Qomolangma seasonality SEM-EDX aerosol particle

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北极海冰变化及其影响

自然杂志 2024年第5期46卷 330-336页

作者：陈金雷康世昌中国科学院西北生态环境资源研究院冰冻圈科学与冻土工程全国重点实验室兰州730000

在全球变暖背景下,北极冰冻圈正在发生显著变化。近几十年来,北极海冰总体呈退缩状态,面积减少、厚度减薄、体积减小,预计到21世纪中叶夏季,海冰将完全消失。北极海冰的减少对生态系统、大气环流、海洋环流、中纬度天气气候以及社会经... 详细信息

在全球变暖背景下,北极冰冻圈正在发生显著变化。近几十年来,北极海冰总体呈退缩状态,面积减少、厚度减薄、体积减小,预计到21世纪中叶夏季,海冰将完全消失。北极海冰的减少对生态系统、大气环流、海洋环流、中纬度天气气候以及社会经济发展等均产生影响。北极海冰变化及其影响研究可为北极可持续发展提供重要支撑,同时也可增加中国在北极的话语权,保障中国在北极的权益。

关键词：全球变暖北极海冰变化影响