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Bibliography, Ancient TL, Vol. 35, No. 2, 2017

Bibliography

_____________________________________________________________________________________________________

Compiled by Sebastien Huot From 15th May 2017 to 1st December 2017

Various geological applications

- aeolian

Arbogast, A.F., Luehmann, M.D., William Monaghan, G., Lovis, W.A., Wang, H., 2017. Paleoenvironmental and geomorphic significance of bluff-top dunes along the Au Sable River in Northeastern Lower Michigan,

USA. Geomorphology 297, 112-121, http://dx.doi.org/10.1016/j.geomorph.2017.09.017.

Guedes, C.C.F., Giannini, P.C.F., Sawakuchi, A.O., DeWitt, R., Paulino de Aguiar, V.Â., 2017. Weakening of northeast trade winds during the Heinrich stadial 1 event recorded by dune field stabilization in tropical Brazil. Quaternary Research 88, 369-381, http://dx.doi.org/10.1017/qua.2017.79.

Ho, L.-D., Lüthgens, C., Wong, Y.-C., Yen, J.-Y., Chyi, S.-J., 2017. Late Holocene cliff-top dune evolution in the Hengchun Peninsula of Taiwan: Implications for palaeoenvironmental reconstruction. Journal of Asian

Earth Sciences 148, 13-30, http://dx.doi.org/10.1016/j.jseaes.2017.08.024.

Hu, G., Yu, L., Dong, Z., Lu, J., Li, J., Wang, Y., Lai, Z., 2018. Holocene aeolian activity in the Zoige Basin, northeastern Tibetan Plateau, China. Catena 160, 321-328, http://dx.doi.org/10.1016/j.catena.2017.10.005.

Huntley, D.H., Hickin, A.S., Lian, O.B., 2016. The pattern and style of deglaciation at the Late Wisconsinan
Laurentide and Cordilleran ice sheet limits in northeastern British Columbia. Canadian Journal of Earth

Sciences 54, 52-75, http://dx.doi.org/10.1139/cjes-2016-0066.

Long, H., Shen, J., Chen, J., Tsukamoto, S., Yang, L., Cheng, H., Frechen, M., 2017. Holocene moisture variations over the arid central Asia revealed by a comprehensive sand-dune record from the central Tian Shan, NW China. Quaternary Science Reviews 174, 13-32,

http://dx.doi.org/10.1016/j.quascirev.2017.08.024.

Nartišs, M., Kalińska-Nartiša, E., 2017. An aeolian or a glaciolacustrine record? A case study from Mieļupīte,

Middle Gauja Lowland, northeast Latvia. Geologos 23, 15, http://dx.doi.org/10.1515/logos-2017-0002.
Zeng, F., Liu, X., Li, X., E, C., 2017. Aquatic species dominate organic matter in Qinghai Lake during the
Holocene: Evidence from eolian deposits around the lake. Journal of Earth Science 28, 484-491,

http://dx.doi.org/10.1007/s12583-016-0926-x.

- alluvial fan

Mouslopoulou, V., Begg, J., Fülling, A., Moraetis, D., Partsinevelos, P., Oncken, O., 2017. Distinct phases of eustatic and tectonic forcing for late Quaternary landscape evolution in southwest Crete, Greece. Earth Surface Processes and Landforms 5, 511-527, http://dx.doi.org/10.5194/esurf-5-511-2017.

65

Bibliography, Ancient TL, Vol. 35, No. 2, 2017

- coastal (in broad term)

Bampton, M., Kelley, A., Kelley, J., Jones, M., Bigelow, G., 2017. Little Ice Age catastrophic storms and the destruction of a Shetland Island community. Journal of Archaeological Science 87, 17-29,

http://dx.doi.org/10.1016/j.jas.2017.08.003.

Brill, D., May, S.M., Shah-Hosseini, M., Rufer, D., Schmidt, C., Engel, M., 2017. Luminescence dating of cyclone-induced washover fans at Point Lefroy (NW Australia). Quaternary Geochronology 41, 134-150,

http://dx.doi.org/10.1016/j.quageo.2017.03.004.

Dillenburg, S.R., Barboza, E.G., Rosa, M.L.C.C., Caron, F., Sawakuchi, A.O., 2017. The complex prograded
Cassino barrier in southern Brazil: Geological and morphological evolution and records of climatic, oceanographic and sea-level changes in the last 7–6ka. Marine Geology 390, 106-119,

http://dx.doi.org/10.1016/j.margeo.2017.06.007.

Massuanganhe, E.A., Berntsson, A., Risberg, J., Westerberg, L.-O., Christiansson, M., Preusser, F., Bjursäter,
S., Achimo, M., 2018. Palaeogeography and dynamics of the deltaic wetland of Save River, Mozambique. Palaeogeography, Palaeoclimatology, Palaeoecology 489, 64-73,

http://dx.doi.org/10.1016/j.palaeo.2017.09.021.

Nooren, K., Hoek, W.Z., Winkels, T., Huizinga, A., Van der Plicht, H., Van Dam, R.L., Van Heteren, S., Van
Bergen, M.J., Prins, M.A., Reimann, T., Wallinga, J., Cohen, K.M., Minderhoud, P., Middelkoop, H., 2017. The Usumacinta–Grijalva beach-ridge plain in southern Mexico: a high-resolution archive of river discharge and precipitation. Earth Surface Processes and Landforms 5, 529-556, http://dx.doi.org/10.5194/esurf-5-529-

2017.

Rémillard, A.M., St-Onge, G., Bernatchez, P., Hétu, B., Buylaert, J.-P., Murray, A.S., Lajeunesse, P., 2017.
Relative sea-level changes and glacio-isostatic adjustment on the Magdalen Islands archipelago (Atlantic Canada) from MIS 5 to the late Holocene. Quaternary Science Reviews 171, 216-233,

http://dx.doi.org/10.1016/j.quascirev.2017.07.015.

Simms, A.R., DeWitt, R., Zurbuchen, J., Vaughan, P., 2017. Coastal erosion and recovery from a Cascadia subduction zone earthquake and tsunami. Marine Geology 392, 30-40,

http://dx.doi.org/10.1016/j.margeo.2017.08.009.

- coastal (estuary)

Rossi, V., Amorosi, A., Sarti, G., Mariotti, S., 2017. Late Quaternary multiple incised valley systems: An unusually well-preserved stratigraphic record of two interglacial valley-fill successions from the Arno Plain (northern Tuscany, Italy). Sedimentology 64, 1901-1928, http://dx.doi.org/10.1111/sed.12379.

- colluvial

Veit, H., Trauerstein, M., Preusser, F., Messmer, T., Gnägi, C., Zech, R., Wüthrich, L., 2017. Late Glacial/Early
Holocene slope deposits on the Swiss Plateau: Genesis and palaeo-environment. CATENA 158, 102-112,

http://dx.doi.org/10.1016/j.catena.2017.06.012.

Zhao, Q., Thomsen, K.J., Murray, A.S., Wei, M., Song, B., 2017. Single-grain quartz OSL dating of debris flow deposits from Men Tou Gou, south west Beijing, China. Quaternary Geochronology 41, 62-69,

http://dx.doi.org/10.1016/j.quageo.2017.06.001.

- earthquake (and fault related)

Bergen, K.J., Shaw, J.H., Leon, L.A., Dolan, J.F., Pratt, T.L., Ponti, D.J., Morrow, E., Barrera, W., Rhodes, E.J.,
Murari, M.K., Owen, L.A., 2017. Accelerating slip rates on the Puente Hills blind thrust fault system beneath metropolitan Los Angeles, California, USA. Geology 45, 227-230, http://dx.doi.org/10.1130/g38520.1.

66

Bibliography, Ancient TL, Vol. 35, No. 2, 2017

Charreau, J., Saint-Carlier, D., Dominguez, S., Lavé, J., Blard, P.-H., Avouac, J.-P., Jolivet, M., Chen, Y.,
Wang, S., Brown, N.D., Malatesta, L.C., Rhodes, E., 2017. Denudation outpaced by crustal thickening in the eastern Tianshan. Earth and Planetary Science Letters 479, 179-191,

http://dx.doi.org/10.1016/j.epsl.2017.09.025.

Druzhinina, O., Bitinas, A., Molodkov, A., Kolesnik, T., 2017. Palaeoseismic deformations in the Eastern Baltic region (Kaliningrad District of Russia). Estonian Journal of Earth Sciences 66, 119–129,

http://dx.doi.org/10.3176/earth.2017.09.

Gong, Z., Sun, J., Zhang, Z., Fu, B., Jia, Y., 2017. Optical dating of an offset river terrace sequence across the
Karakax fault and its implication for the late Quaternary left-lateral slip rate. Journal of Asian Earth Sciences

147, 415-423, http://dx.doi.org/10.1016/j.jseaes.2017.07.013.

He, Z., Ma, B., Long, J., Zhang, H., Liang, K., Jiang, D., 2017. Recent ground fissures in the Hetao basin, Inner

Mongolia, China. Geomorphology 295, 102-114, http://dx.doi.org/10.1016/j.geomorph.2017.07.008.

Olszak, J., 2017. Late Pleistocene dip-slip faulting along the Dunajec Fault, West Carpathians: Insights from alluvial sediments. Geomorphology 295, 749-757, http://dx.doi.org/10.1016/j.geomorph.2017.08.006.

Personius, S.F., Briggs, R.W., Maharrey, J.Z., Angster, S.J., Mahan, S.A., 2017. A paleoseismic transect across the northwestern Basin and Range Province, northwestern Nevada and northeastern California, USA.

Geosphere 13, 782-810, http://dx.doi.org/10.1130/GES01380.1.

Philip, G., Suresh, N.P., Jayangondaperumal, R., 2017. Late Pleistocene-Holocene strain release by normal faulting along the Main Boundary Thrust at Logar in the northwestern Kumaon Sub Himalaya, India.

Quaternary International, http://dx.doi.org/10.1016/j.quaint.2017.05.022.

Poujol, A., Ritz, J.-F., Vernant, P., Huot, S., Maate, S., Tahayt, A., 2017. Which fault destroyed Fes city
(Morocco) in 1755? A new insight from the Holocene deformations observed along the southern border of Gibraltar arc. Tectonophysics 712-713, 303-311, http://dx.doi.org/10.1016/j.tecto.2017.05.036.

Rossetti, D.F., Valeriano, M.M., Gribel, R., Cohen, M.C.L., Tatumi, S.H., Yee, M., 2017. The imprint of Late
Holocene tectonic reactivation on a megafan landscape in the northern Amazonian wetlands.

Geomorphology 295, 406-418, http://dx.doi.org/10.1016/j.geomorph.2017.07.026.

Warrell, K.F., Cox, R.T., Hatcher Jr., R.D., Vaughn, J.D., Counts, R., 2017. Paleoseismic Evidence for Multiple

Mw≥6 Earthquakes in the Eastern Tennessee Seismic Zone during the Late Quaternary. Bulletin of the

Seismological Society of America 107, 1610-1624, http://dx.doi.org/10.1785/0120160161.
Weissl, M., Hintersberger, E., Lomax, J., Lüthgens, C., Decker, K., 2017. Active tectonics and geomorphology of the Gaenserndorf Terrace in the Central Vienna Basin (Austria). Quaternary International 451, 209-222,

http://dx.doi.org/10.1016/j.quaint.2016.11.022.

Yang, H., Yang, X., Huang, X., Li, A., Huang, W., Zhang, L., 2018. New constraints on slip rates of the
Fodongmiao-Hongyazi fault in the Northern Qilian Shan, NE Tibet, from the 10Be exposure dating of offset terraces. Journal of Asian Earth Sciences 151, 131-147, http://dx.doi.org/10.1016/j.jseaes.2017.10.034.

- fluvial

Bhattacharya, F., Shukla, A.D., Patel, R.C., Rastogi, B.K., Juyal, N., 2017. Sedimentology, geochemistry and
OSL dating of the alluvial succession in the northern Gujarat alluvial plain (western India) - A record to evaluate the sensitivity of a semiarid fluvial system to the climatic and tectonic forcing since the late Marine

Isotopic Stage 3. Geomorphology 297, 1-19, http://dx.doi.org/10.1016/j.geomorph.2017.08.046.

67

Bibliography, Ancient TL, Vol. 35, No. 2, 2017

Chamberlain, E.L., Wallinga, J., Reimann, T., Goodbred Jr, S.L., Steckler, M.S., Shen, Z., Sincavage, R., 2017.
Luminescence dating of delta sediments: Novel approaches explored for the Ganges-Brahmaputra-Meghna Delta. Quaternary Geochronology 41, 97-111, http://dx.doi.org/10.1016/j.quageo.2017.06.006.

Daley, J., Croke, J., Thompson, C., Cohen, T., Macklin, M., Sharma, A., 2017. Late Quaternary channel and floodplain formation in a partly confined subtropical river, eastern Australia. Journal of Quaternary Science

32, 729-743, http://dx.doi.org/10.1002/jqs.2930.

Foster, M.A., Anderson, R.S., Gray, H.J., Mahan, S.A., 2017. Dating of river terraces along Lefthand Creek, western High Plains, Colorado, reveals punctuated incision. Geomorphology 295, 176-190,

http://dx.doi.org/10.1016/j.geomorph.2017.04.044.

Gliganic, L.A., Cohen, T.J., Meyer, M., Molenaar, A., 2017. Variations in luminescence properties of quartz and feldspar from modern fluvial sediments in three rivers. Quaternary Geochronology 41, 70-82,

http://dx.doi.org/10.1016/j.quageo.2017.06.005.

Hughes, K., Croke, J., 2017. How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? Journal of Quaternary Science 32, 744-759,

http://dx.doi.org/10.1002/jqs.2956.

Jia, L., Hu, D., Wu, H., Zhao, X., Chang, P., You, B., Zhang, M., Wang, C., Ye, M., Wu, Z., Liang, X., 2017.
Yellow River terrace sequences of the Gonghe–Guide section in the northeastern Qinghai–Tibet: Implications for plateau uplift. Geomorphology 295, 323-336,

http://dx.doi.org/10.1016/j.geomorph.2017.06.007.

Kasse, C., Van Balen, R.T., Bohncke, S.J.P., Wallinga, J., Vreugdenhil, M., 2017. Climate and base-level controlled fluvial system change and incision during the last glacial–interglacial transition, Roer river, the Netherlands – western Germany. Netherlands Journal of Geosciences 96, 71-92,

http://dx.doi.org/10.1017/njg.2016.50.

Kothyari, G.C., Shukla, A.D., Juyal, N., 2017. Reconstruction of Late Quaternary climate and seismicity using fluvial landforms in Pindar River valley, Central Himalaya, Uttarakhand, India. Quaternary International

443, Part B, 248-264, http://dx.doi.org/10.1016/j.quaint.2016.06.001.

Kumar, A., Srivastava, P., 2017. The role of climate and tectonics in aggradation and incision of the Indus River in the Ladakh Himalaya during the late Quaternary. Quaternary Research 87, 363-385,

http://dx.doi.org/10.1017/qua.2017.19.

Kumar, A., Srivastava, P., Meena, N.K., 2017. Late Pleistocene aeolian activity in the cold desert of Ladakh: A record from sand ramps. Quaternary International 443, 13-28,

http://dx.doi.org/10.1016/j.quaint.2016.04.006.

Machado, M.J., Medialdea, A., Calle, M., Rico, M.T., Sánchez-Moya, Y., Sopeña, A., Benito, G., 2017.
Historical palaeohydrology and landscape resilience of a Mediterranean rambla (Castellón, NE Spain): Floods and people. Quaternary Science Reviews 171, 182-198,

http://dx.doi.org/10.1016/j.quascirev.2017.07.014.

Ngangom, M., Bhandari, S., Thakkar, M.G., Shukla, A.D., Juyal, N., 2017. Mid-Holocene extreme hydrological events in the eastern Great Rann of Kachchh, western India. Quaternary International 443, Part B, 188-199,

http://dx.doi.org/10.1016/j.quaint.2016.10.017.

Olszak, J., 2017. Climatically controlled terrace staircases in uplifting mountainous areas. Global and Planetary

Change 156, 13-23, http://dx.doi.org/10.1016/j.gloplacha.2017.07.013.

Resmi, M.R., Achyuthan, H., Jaiswal, M.K., 2017. Middle to late Holocene paleochannels and migration of the
Palar River, Tamil Nadu: Implications of neotectonic activity. Quaternary International 443, 211-222,

http://dx.doi.org/10.1016/j.quaint.2016.05.002.

68

Bibliography, Ancient TL, Vol. 35, No. 2, 2017

Rosenwinkel, S., Landgraf, A., Schwanghart, W., Volkmer, F., Dzhumabaeva, A., Merchel, S., Rugel, G.,
Preusser, F., Korup, O., 2017. Late Pleistocene outburst floods from Issyk Kul, Kyrgyzstan? Earth Surface Processes and Landforms 42, 1535-1548, http://dx.doi.org/10.1002/esp.4109.

Salcher, B.C., Frank-Fellner, C., Lomax, J., Preusser, F., Ottner, F., Scholger, R., Wagreich, M., 2017. Middle to Late Pleistocene multi-proxy record of environmental response to climate change from the Vienna Basin, Central Europe (Austria). Quaternary Science Reviews 173, 193-210,

http://dx.doi.org/10.1016/j.quascirev.2017.08.014.

Sant'Anna, L.G., Soares, E.A.d.A., Riccomini, C., Tatumi, S.H., Yee, M., 2017. Age of depositional and weathering events in Central Amazonia. Quaternary Science Reviews 170, 82-97,

http://dx.doi.org/10.1016/j.quascirev.2017.06.015.

Singh, A.K., Pattanaik, J.K., Gagan, Jaiswal, M.K., 2017. Late Quaternary evolution of Tista River terraces in
Darjeeling-Sikkim-Tibet wedge: Implications to climate and tectonics. Quaternary International 443, 132-

142, http://dx.doi.org/10.1016/j.quaint.2016.10.004.

Thokchom, S., Bhattacharya, F., Durga Prasad, A., Dogra, N.N., Rastogi, B.K., 2017. Paleoenvironmental implications and drainage adjustment in the middle reaches of the Sabarmati river, Gujarat: Implications towards hydrological variability. Quaternary International 454, 1-14,

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  • The Extent and Composition of Disaster Relief After China's 1823 Flood: New Archival Evidence

    The Extent and Composition of Disaster Relief After China's 1823 Flood: New Archival Evidence

    The extent and composition of disaster relief after China's 1823 flood: New archival evidence Ni Yuping History Department, Tsinghua University Martin Uebele Faculty of Arts, University of Groningen Abstract: In 1823, large parts of China were drowned in one of the heaviest floods of the whole Qing dynasty (1644-1911), but detailed data on its impact and government responses have so far been scattered. Due to a recent reorganization of China’s First Historical Archives, however, this paper is able to provide new evidence about the flood’s impact as well as the extent and composition of central government disaster relief. This matters especially because many scholars believe that because of this flood, China entered into the “Daoguang Depression” providing the background for China’s “lost century” in connection with interior and exterior security issues such as the First Opium War (1839-42), and the Taiping rebellion (1850-64). Our evidence thus may help to understand if these combined challenges exceeded state capacity when modernization would have required internal reform more than ever. We find that in the 17 provinces for which we have data at least 20 percent of all counties were flooded, half of them seriously. The combination of tax relief, water works and direct payments grew proportionally with the share of counties affected by the flood and totaled to about 26 million taels of silver, more than half of annual fiscal revenue of the Qing state. Key words: Daoguang Depression, disaster relief, China, 19th century, state capacity 1. Introduction No matter if from the perspective of meteorological, disaster or economic history, the year of 1823 (the third year of the Daoguang emperor’s rule) was an all-important node.
  • Recent Anthropogenic Curtailing of Yellow River Runoff and Sediment Load Is Unprecedented Over the Past 500 Y

    Recent Anthropogenic Curtailing of Yellow River Runoff and Sediment Load Is Unprecedented Over the Past 500 Y

    Recent anthropogenic curtailing of Yellow River runoff and sediment load is unprecedented over the past 500 y Yu Liua,b,c,d,1, Huiming Songa,b,e, Zhisheng Ana,b,e,1, Changfeng Suna,b, Valerie Trouetf, Qiufang Caia,b,c, Ruoshi Liud, Steven W. Leavittf, Yi Songa, Qiang Lia,b,e, Congxi Fanga, Weijian Zhoua,b, Yinke Yangg, Zhao Jina,b, Yunqiang Wanga,b, Junyan Suna, Xingmin Muh, Ying Leia, Lu Wanga, Xuxiang Lid, Meng Rena, Linlin Cuia, and Xueli Zenga aThe State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, 710061 Xi’an, China; bCAS Center for Excellence in Quaternary Science and Global Change, Chinese Academy of Sciences, 710061 Xi’an, China; cOpen Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology, 266061 Qingdao, China; dSchool of Human Settlements and Civil Engineering, Xi’an Jiaotong University, 710049 Xi’an, China; eInterdisciplinary Research Center of Earth Science Frontier, Beijing Normal University, 100875 Beijing, China; fLaboratory of Tree-Ring Research, The University of Arizona, Tucson, AZ 85721; gSchool of Environmental Science and Engineering, Chang’an University, 710054 Xi’an, China; and hState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences & Ministry of Water Resources, 712100 Yangling, China Contributed by Zhisheng An, May 29, 2020 (sent for review December 26, 2019; reviewed by Achim Bräuning and Hongyan Liu) The Yellow River (YR) is the fifth-longest and the most sediment- load of the YR has declined by ∼90% over the past 60 y (10), laden river in the world.
  • The Need for Integrated Management for the Endangered Miyun Resevoir

    The Need for Integrated Management for the Endangered Miyun Resevoir

    Quenching Beijing’s Thirst: The Need for Integrated Management for the Endangered Miyun Resevoir By Christoph Peisert and Eva Sternfeld Miyun reservoir, a large reservoir northeast of Beijing municipality, is the Chinese capital’s most important source of drinking water. For many years the Beijing municipal government has made great efforts to protect the reservoir and its catchment area. However, successful implementation has been hampered by numerous user conflicts. This paper investigates the origin and various types of conflicts, which include inter-provincial, city-county disputes, as well as conflicts between county government and local residents living in the water protection zone. The magnitude of these conflicts and continued deteriorating quality of the reservoir underline the need for integrated watershed management approaches as stipulated in the 2002 revised Water Law, and the adoption of a water economy that includes the costs for water protection and compensation for those required to carry out watershed protection activities. he large Miyun reservoir, built during the Great Natural Determinants of the Beijing Water Crisis Leap Forward period (1958-1960) in the Beijing municipality is located in the dry northeast Tnortheast of Beijing municipality, is a critical edge of the North China Plain bordering the Mongolian source of drinking water for the 14 million people living Plateau in central Hebei province. Since the last in this booming metropolis. Considering the huge administrative reforms in 1958, the Chinese capital population reliant on the catchment for drinking water, and its rural hinterland were expanded to cover a total Miyun reservoir is one of the most important water area of 16,800 square kilometers (km2) with about protection areas in the world.
  • IWHR Annual Report 2018

    IWHR Annual Report 2018

    Printed on recycled paper ANNUAL REPORT IWHR China Institute of Water Resources and Hydropower Research 中国水利水电科学研究院 ANNUAL REPORT IWHR China Institute of Water Resources and Hydropower Research 中国水利水电科学研究院 ANNUAL REPORT IWHR China Institute of Water Resources and Hydropower Research 中国水利水电科学研究院 WELCOME MESSAGE Annual Report 2018 CHINA INSTITUTE OF WATER RESOURCES AND HYDROPOWER RESEARCH The year 2018 is undoubtedly an unusual year for IWHR as it originality recognized by national and provincial prizes. Covering 18 research disciplines marks the 40th anniversary of China’s adoption of Reform and and 93 research directions now, IWHR has established 4 national and 8 ministerial research Opening-up Policy and the 60th anniversary of IWHR, which centers, 1 state key laboratory and 2 ministerial key laboratories, representing China’s is more special to the Institute itself. In Chinese culture, 60 largest research center and training base of water resources and hydropower with the most decades is called a Jiazi which means a cycle of development complete disciplines and best research conditions. and is therefore of special significance. During the sixty years of development, IWHR people have worked with all our efforts Over the 60 years, IWHR has always been aiming high with global vision. As China keeps to pursue the prosperity of the nation and happiness of the rising, IWHR has accelerated its international cooperation and exchange and made people, bearing this in mind as our mission and responsibility remarkable achievement. IWHR has established cooperative relationship with over 100 as we went ups and down with the country. We have proudly foreign academic organizations and overseas research institutes and universities.
  • LCSH Section Y

    LCSH Section Y

    Y-Bj dialects Yabakei (Japan) Yacatas Site (Mexico) USE Yugambeh-Bundjalung dialects BT Valleys—Japan BT Mexico—Antiquities Y-cars Yabakei (Japan) Yaccas USE General Motors Y-cars USE Yaba Valley (Japan) USE Xanthorrhoea Y chromosome Yabarana Indians (May Subd Geog) Yachats River (Or.) UF Chromosome Y UF Yaurana Indians BT Rivers—Oregon BT Sex chromosomes BT Indians of South America—Venezuela Yachats River Valley (Or.) — Abnormalities (May Subd Geog) Yabbie culture UF Yachats Valley (Or.) BT Sex chromosome abnormalities USE Yabby culture BT Valleys—Oregon Y Fenai (Wales) Yabbies (May Subd Geog) Yachats Valley (Or.) USE Menai Strait (Wales) [QL444.M33 (Zoology)] USE Yachats River Valley (Or.) Y-G personality test BT Cherax Yachikadai Iseki (Haga-machi, Tochigi-ken, Japan) USE Yatabe-Guilford personality test Yabby culture (May Subd Geog) USE Yachikadai Site (Haga-machi, Tochigi-ken, Y.M.C.A. libraries [SH380.94.Y32] Japan) USE Young Men's Christian Association libraries UF Yabbie culture Yachikadai Site (Haga-machi, Tochigi-ken, Japan) Y maze Yabby farming This heading is not valid for use as a geographic BT Maze tests BT Crayfish culture subdivision. Y Mountain (Utah) Yabby farming UF Yachikadai Iseki (Haga-machi, Tochigi-ken, BT Mountains—Utah USE Yabby culture Japan) Wasatch Range (Utah and Idaho) YABC (Behavioral assessment) BT Japan—Antiquities Y-particles USE Young Adult Behavior Checklist Yachinaka Tate Iseki (Hinai-machi, Japan) USE Hyperons Yabe family (Not Subd Geog) USE Yachinaka Tate Site (Hinai-machi, Japan) Y-platform cars Yabem (Papua New Guinean people) Yachinaka Tate Site (Hinai-machi, Japan) USE General Motors Y-cars USE Yabim (Papua New Guinean people) This heading is not valid for use as a geographic subdivision.
  • Attribution of Runoff Variation in the Headwaters of the Yangtze River

    Attribution of Runoff Variation in the Headwaters of the Yangtze River

    International Journal of Environmental Research and Public Health Article Attribution of Runoff Variation in the Headwaters of the Yangtze River Based on the Budyko Hypothesis Junlong Liu , Jin Chen *, Jijun Xu, Yuru Lin, Zhe Yuan and Mingyuan Zhou Changjiang Scientific Research Institute of Changjiang Water Resources Commission, Wuhan 430010, China * Correspondence: [email protected] Received: 30 May 2019; Accepted: 11 July 2019; Published: 13 July 2019 Abstract: Quantifying the contributions of climate change and human activities on runoff changes is of great importance for water resource management, sustainable water resource utilization, and sustainable development of society. In this study, hydrological and climatic data from hydrological and meteorological stations in the headwaters of the Yangtze River (YRHA) from 1966 to 2013 were used to quantitatively attribute the runoff change to the impacts of climate change and human activities separately. Firstly, the change trends in precipitation, runoff depth and potential evapotranspiration were analyzed by the Mann-Kendall test method. Three methods, secondly, including ordered clustering, Mann-Kendall and cumulative anomaly curve were adopted to detect the change points of runoff at Zhimenda hydrological station and partition the whole study period into two sub-periods at the change point (base and impacted periods). Then, the elasticity coefficient method based on the Budyko hypothesis was applied to calculate elasticity coefficients of runoff to precipitation, potential evapotranspiration and land use/cover during the two periods, and to evaluate the contributions of climate change and human activities. Results indicated that during 1966–2013, runoff depth, precipitation and potential evapotranspiration all showed a significant increasing trend, 1 1 1 with increasing rates of 7.26 mm decade− , 18.725 mm decade− and 7.228 mm decade− , respectively.