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  • 1
    Keywords: Water quality. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (336 pages)
    Edition: 1st ed.
    ISBN: 9780128175248
    Language: English
    Note: Front Cover -- Water Quality in the Third Pole -- Copyright Page -- Contents -- List of contributors -- About the editors -- Preface -- Acknowledgments -- Introduction -- I. Atmosphere -- 1. Chemical components and distributions in precipitation in the Third Pole -- 1.1 Background -- 1.1.1 Third Pole region -- 1.2 Precipitation inorganic chemistry in the Third Pole -- 1.2.1 Monsoon versus nonmonsoon composition of major ions and trace elements in precipitation over the Third Pole -- 1.2.2 Sources and transport mechanisms of major ions and trace elements in the Third Pole -- 1.3 Mercury (Hg) in precipitation over the Third Pole -- 1.3.1 Spatial distribution of total Hg concentration in precipitation and its wet deposition flux -- 1.3.2 Seasonal variation of total Hg concentration and total Hg wet deposition flux -- 1.3.3 Potential sources of Hg in precipitation over the Third Pole region -- 1.4 Carbonaceous matters -- 1.4.1 Carbonaceous matters (dissolved organic carbon) in wet precipitation over the Third Pole -- 1.4.2 Dissolved organic carbon concentration and deposition over the three sites in the Third Pole -- 1.4.3 Dissolved organic carbon sources -- 1.4.4 Source regions of fossil fuel combustion-derived dissolved organic carbon at Nam Co -- 1.4.5 Light absorption characteristics of dissolved organic carbon -- 1.5 Summary -- Acknowledgments -- References -- 2. Chemical components and distributions of aerosols in the Third Pole -- 2.1 Introduction -- 2.2 Carbonaceous species and aerosol composition over Third Pole -- 2.3 Secondary organic aerosol formation, aging, and water-soluble organic carbon/organic carbon ratio -- 2.4 Major ions in aerosols -- 2.5 Mercury and other elements in aerosols over Third Pole -- 2.6 Source and transport mechanism of aerosols to Third Pole -- 2.6.1 Source of aerosols to Third Pole and seasonal variability. , 2.6.2 Transport mechanism of aerosols to Third Pole -- 2.7 Summary and recommendations -- Acknowledgments -- References -- II. Glaciers -- 3. Chemical components and distributions in glaciers of the Third Pole -- 3.1 Background -- 3.2 Major ions -- 3.2.1 Concentration level and spatial distribution -- 3.2.2 Seasonal variation -- 3.2.3 Potential sources -- 3.2.4 Historical change -- 3.3 Trace elements -- 3.3.1 Introduction -- 3.3.2 Concentrations of trace elements -- 3.3.3 Spatial variation -- 3.3.4 Seasonal variation -- 3.3.5 Historical change -- 3.4 Persistent organic pollutants -- 3.4.1 Levels and spatial distribution of polycyclic aromatic hydrocarbons in cryoconites -- 3.4.2 Historical changes to persistent organic pollutants and polycyclic aromatic hydrocarbons -- 3.5 Carbonaceous matter -- 3.5.1 Black carbon and organic carbon -- 3.5.1.1 Spatial distribution -- 3.5.1.2 Historical change of black carbon -- 3.5.1.3 Potential sources of black carbon -- 3.5.1.4 Impact of black carbon and organic carbon on surface snow albedo, radiative forcing, and glacier melt -- 3.5.2 DOC -- 3.5.2.1 Spatial distribution -- 3.5.2.2 DOC deposition and export flux -- 3.5.2.3 DOC characteristics -- DOC light absorption -- DOC fractionation -- DOC bioavailability -- 3.6 Mineral dust and its influence on glacier melt -- 3.6.1 Introduction -- 3.6.2 Spatial-temporal distribution -- 3.6.3 Sources of mineral dust -- 3.6.4 Influences of mineral dust in glacier meltwater -- 3.6.5 Historical change -- 3.7 Summary -- Acknowledgment -- References -- III. Rivers and Springs -- 4. Inorganic components in river waters in the Third Pole -- 4.1 Introduction -- 4.1.1 Background -- 4.1.2 Significance of the study -- 4.2 River catchments -- 4.2.1 Geology of the major river catchments on the Third Pole -- 4.2.1.1 The South Third Pole river system -- Indus -- Ganges. , Yarlung Tsangpo (upstream of the Brahmaputra) -- Nu Jiang (upstream of the Salween) -- Lantsang Jiang (upstream of the Mekong River) -- 4.2.1.2 The Central and East Third Pole river system -- The Yangtze River -- Zhajia Tsangpo -- 4.2.1.3 The North-East Third Pole river system -- The Yellow River -- Hei He -- Shule He -- Buha He -- 4.2.1.4 The North-West Third Pole river system -- Amu Darya -- Tarim River -- 4.2.2 Glacial rivers -- 4.2.2.1 Glacial rivers in the South Third Pole -- 4.2.2.2 Glacial rivers in the Central-East Third Pole -- 4.2.2.3 Glacial rivers in the North-East Third Pole -- 4.2.3 Glacial rivers in the North-West Third Pole -- 4.3 Water ionic chemistry in rivers on the Third Pole -- 4.3.1 Spatial variations of the major ions in rivers of the Third Pole -- 4.3.2 Temporal variations of the major ions in rivers of the Third Pole -- 4.4 Characterization of major ions in rivers of the Third Pole -- 4.4.1 Major sources of ions and the controlling factors in rivers of the Third Pole -- 4.5 Dissolved trace elements and water quality assessment in rivers of the Third Pole -- 4.5.1 Dissolved trace elements in rivers of the Third Pole -- 4.5.2 Water quality assessment in the rivers of the Third Pole -- 4.6 Summary and perspectives -- Acknowledgments -- References -- 5. Nutrients and organic carbons in river waters of the Third Pole -- 5.1 Introduction -- 5.2 River catchments -- 5.2.1 The major river catchments on the Tibetan Plateau -- 5.2.2 The glacial river catchments on the Tibetan Plateau -- 5.3 Export of carbon and nitrogen in major rivers of the Tibetan Plateau -- 5.3.1 Export of riverine dissolved organic carbon -- 5.3.2 Export of riverine dissolved organic nitrogen -- 5.3.3 Concentration ratio of riverine dissolved organic carbon and dissolved organic nitrogen in major rivers of the Tibeta. , 5.3.4 Export of organic carbon in glacial rivers of the Tibetan Plateau -- 5.4 Concentrations and spatial distribution of persistent organic pollutants in the water of the Koshi River -- 5.4.1 Sampling region -- 5.4.2 Concentrations of persistent organic pollutants in the Koshi River -- 5.4.3 Spatial distribution of persistent organic pollutants in the Koshi River -- 5.5 Total suspended insoluble particles in rivers of the Third Pole -- 5.5.1 Scenario in the Third Pole -- 5.5.2 Factors and impact of insoluble particles in river water -- 5.5.3 Rivers of the Third Pole region and total suspended solids (insoluble particles) -- 5.5.4 Evolving susceptibility, crisis, and hazards -- 5.6 Summary and perspectives -- Acknowledgments -- References -- 6. Geochemical constituents in hot spring waters in the Third Pole -- 6.1 Introduction -- 6.2 Sampling locations and data sources -- 6.3 Geological setup of the area -- 6.4 Results and discussion -- 6.4.1 Major ion chemistry -- 6.4.2 Dissolved silica -- 6.4.3 Stable water isotopes (δ18O and δD) -- 6.5 Stable carbon isotope (δ13CDIC) in alkalinity -- Acknowledgments -- References -- IV. Lakes -- 7. Inorganic components in lake waters in the Third Pole -- 7.1 Introduction -- 7.2 The composition of major ions in the lakes of the Third Pole region -- 7.3 Mercury and other elements -- 7.3.1 Trace elements in the lakes of the Third Pole -- 7.3.2 Mercury in the lakes of the Third Pole -- 7.3.3 Water quality index and risk assessment -- 7.3.4 Reference dose and hazard quotient for each element in the lake water -- 7.4 Summary -- Acknowledgments -- References -- 8. Nutrients and organic carbons in lake waters of the Third Pole -- 8.1 Introduction -- 8.2 Nutrients -- 8.2.1 Status of lake water nutrients in the Third Pole -- 8.3 Persistent organic pollutants -- 8.3.1 Concentrations. , 8.3.2 Spatial distribution of POPs in Nam Co Lake -- 8.3.3 Air-water gas exchange of POPs in Nam Co Lake -- 8.3.4 Historical variations of POPs in the sediment of Yamzho Yumco Lake -- 8.4 Carbonaceous matter -- 8.4.1 Carbonaceous matters over the Third Pole -- 8.4.2 Sources of carbonaceous matters in the lakes of the Tibetan Plateau -- 8.5 Summary -- Acknowledgments -- References -- Executive summary -- A.1 Atmosphere -- A.2 Glaciers -- A.3 Rivers -- A.4 Lakes -- References -- Author Index -- Subject Index -- Back Cover.
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  • 2
    Publication Date: 2023-05-12
    Keywords: Ammonium; Belukha_core01; Calcium cation; Chloride anion; DATE/TIME; Depth, relative; ELEVATION; Event label; Glacier; Himalaya; Holtedahl_core05; ICEDRILL; Ice drill; Ice thickness, glacier; Latitude of event; Lomonosov_core97; Longitude of event; MtEverest_core02; Nitrate ion; Penetration depth; Russia; Sulfate anion; Svalbard; Vestfonna_core95
    Type: Dataset
    Format: text/tab-separated-values, 43 data points
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  • 3
    Publication Date: 2023-11-22
    Keywords: Abbreviation; Age; Datum level; DEPTH, ice/snow; Difference; Event label; Glacier; Himalaya; Holtedahl_core05; ICEDRILL; Ice drill; Latitude of event; Lomonosov_core97; Longitude of event; MtEverest_core02; Svalbard; Vestfonna_core95; Year of eruption
    Type: Dataset
    Format: text/tab-separated-values, 180 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Zhang, Guoqing; Xie, Hongjie; Kang, Shichang; Yi, Donghui; Ackley, Stephen F (2011): Monitoring lake level changes on the Tibetan Plateau using ICESat altimetry data (2003-2009). Remote Sensing of Environment, 115(7), 1733-1742, https://doi.org/10.1016/j.rse.2011.03.005
    Publication Date: 2023-12-13
    Description: In this study, ICESat altimetry data are used to provide precise lake elevations of the Tibetan Plateau (TP) during the period of 2003-2009. Among the 261 lakes examined ICESat data are available on 111 lakes: 74 lakes with ICESat footprints for 4-7 years and 37 lakes with footprints for 1 -3 years. This is the first time that precise lake elevation data are provided for the 111 lakes. Those ICESat elevation data can be used as baselines for future changes in lake levels as well as for changes during the 2003-2009 period. It is found that in the 74 lakes (56 salt lakes) examined, 62 (i.e. 84%) of all lakes and 50 (i.e. 89%) of the salt lakes show tendency of lake level increase. The mean lake water level increase rate is 0.23 m/year for the 56 salt lakes and 0.27 m/year for the 50 salt lakes of water level increase. The largest lake level increase rate (0.80 m/year) found in this study is the lake Cedo Caka. The 74 lakes are grouped into four subareas based on geographical locations and change tendencies in lake levels. Three of the four subareas show increased lake levels. The mean lake level change rates for subareas I, II, III, IV, and the entire TP are 0.12, 0.26, 0.19, -0.11, and 0.2 m/year, respectively. These recent increases in lake level, particularly for a high percentage of salt lakes, supports accelerated glacier melting due to global warming as the most likely cause.
    Keywords: Argog_Co; Baqan_Co; Cedo_Caka; Chaoyang_Co; Co_Nag; Co_Ngoin; Co_Nyi; Co_Rabamgodang; Con_Arimar; Darab_Co; Date/time end; Date/time start; Dawa_Co; Deyu_Co; Dogai_Coring; Dorsoidong_Co; ELEVATION; Elevation 2; Event label; Gopug_Co; Goren_Co; Gyado_Co; Gyarab_Co; Gyaring_Lake; Gyeze_Caka; Har_Lake; Himalaya; Hoh_Sai_Lake; Hoh_Xil_Lake; Hulu_Lake; ICESat satellite data; International Polar Year (2007-2008); IPY; Jang_Co; Kekao_Lake; Kunggyu_Co; Kushuihuan_Lake; Kyobxang_Co; Lagkor_Co; Lake; Lakes_Tibet; Lake type; Latitude of event; Lixi_Oidaim_Co; Longitude of event; Longwei_Co; Mapam_Yumco; Marye_Co; Meriqancomari; MULT; Multiple investigations; Nam_Co; Namka_Co; Ngangla_Ringco; Ngangzi_Co; Number; Number of years; Peiku_Co; Pibi_Lake; Puma_Yumco; Qagain_Co; Qinghai_Lake; Ringco_Ogma; Ringinyubu_Co; Sector; Selin_Co; Serbug_Co; Standard deviation; Suang_Lake; Tangra_Yumco; Taro_Co; Tibetan Plateau; Urru_Co; Water level change; Waxunggabma_Co; Weishan_Lake; Xianhe_Lake; Xijir_Ulan_Lake; Xogor_Co; Yamzhog_Yumco; Yangain_Canco; Yinbo_Lake; Yurbao_Co; Yuye_Lake; Zhangne_Co; Zhari_Namco; Zige_Tangco
    Type: Dataset
    Format: text/tab-separated-values, 814 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Moore, John C; Beaudon, Emilie; Kang, Shichang; Divine, Dmitry V; Isaksson, Elisabeth; Pohjola, Veijo A; van de Wal, Roderik S W (2012): Statistical extraction of volcanic sulphate from nonpolar ice cores. Journal of Geophysical Research, 117(D3), D03306, https://doi.org/10.1029/2011JD016592
    Publication Date: 2023-12-13
    Description: Ice cores from outside the Greenland and Antarctic ice sheets are difficult to date because of seasonal melting and multiple sources (terrestrial, marine, biogenic and anthropogenic) of sulfates deposited onto the ice. Here we present a method of volcanic sulfate extraction that relies on fitting sulfate profiles to other ion species measured along the cores in moving windows in log space. We verify the method with a well dated section of the Belukha ice core from central Eurasia. There are excellent matches to volcanoes in the preindustrial, and clear extraction of volcanic peaks in the post-1940 period when a simple method based on calcium as a proxy for terrestrial sulfate fails due to anthropogenic sulfate deposition. We then attempt to use the same statistical scheme to locate volcanic sulfate horizons within three ice cores from Svalbard and a core from Mount Everest. Volcanic sulfate is 〈5% of the sulfate budget in every core, and differences in eruption signals extracted reflect the large differences in environment between western, northern and central regions of Svalbard. The Lomonosovfonna and Vestfonna cores span about the last 1000 years, with good extraction of volcanic signals, while Holtedahlfonna which extends to about AD1700 appears to lack a clear record. The Mount Everest core allows clean volcanic signal extraction and the core extends back to about AD700, slightly older than a previous flow model has suggested. The method may thus be used to extract historical volcanic records from a more diverse geographical range than hitherto.
    Keywords: International Polar Year (2007-2008); IPY
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
    Publication Date: 2023-02-08
    Description: Retreating Arctic sea ice under rapid warming is projected to continue. A new transarctic route, the Northeast Passage (NEP), may open in the near future, with considerable impacts on global shipping transportation. Comprehensive research on the past changes in sea ice in September and future accessibility along the NEP is essential. In this investigation, an unstructured-grid model was used for accurate fitting to the irregular coastal boundary, and accessibility was assessed under two different shared socioeconomic pathways (SSPs) and two vessel classes with the Arctic transportation accessibility model from 2021−2050. Significant warming was presented in the deep layer in the Arctic seas along the NEP in recent decades (1988−2016), with a distinct band on the outer edge of the abyssal zone. The positive anomaly of seawater temperature moved westward and increased notably in coastal areas, which made sea ice disappear, and the area was dominated by the negative anomaly in the last decade. The NEP is projected to be navigable for open water ships in September from 2021 to 2025, which would extend to August−October during 2025−2050 under both SSP2-4.5 and SSP5-8.5. In addition, Polar Class 6 ships would be capable of crossing the NEP from August to December during 2021−2025 and from July to December during 2026−2050. The Vilkitsky Strait and Dmitrii Laptev Strait, which are close to the coast, have higher accessibility than the Shokalskiy Strait and Sannikov Strait, especially in the next five years.
    Type: Article , PeerReviewed
    Format: text
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  • 7
    Publication Date: 2015-08-12
    Print ISSN: 0022-1430
    Electronic ISSN: 1727-5652
    Topics: Geography , Geosciences
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  • 8
    Publication Date: 2012-10-06
    Print ISSN: 0022-1430
    Electronic ISSN: 1727-5652
    Topics: Geography , Geosciences
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  • 9
    Publication Date: 2013-04-17
    Print ISSN: 0022-1430
    Electronic ISSN: 1727-5652
    Topics: Geography , Geosciences
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