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Готові списки джерел за темами / Bassin du Changjiang (Yangtze) / Статті в журналах

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Статті в журналах з теми "Bassin du Changjiang (Yangtze)"

Автор: Grafiati

Опубліковано: 25 травня 2024

Оновлено: 31 липня 2025

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1

Men, Ke-Pei, and Shu-Dan Zhu. "The Ordered Network Structure and its Prediction for the Big Floods of the Changjiang River Basins." Zeitschrift für Naturforschung A 68, no. 12 (2013): 766–72. http://dx.doi.org/10.5560/zna.2013-0061.

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According to the latest statistical data of hydrology, a total of 21 floods took place over the Changjiang (Yangtze) River Basins from 1827 to 2012 and showed an obvious commensurable orderliness. In the guidance of the information forecasting theory of Wen-Bo Weng, based on previous research results, combining ordered analysis with complex network technology, we focus on the summary of the ordered network structure of the Changjiang floods, supplement new information, further optimize networks, construct the 2D- and 3D-ordered network structure and make prediction research. Predictions show t

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2

Cheung, Richard Ching Wa, Moriaki Yasuhara, Hokuto Iwatani, Chih-Lin Wei, and Yun-wei Dong. "Benthic community history in the Changjiang (Yangtze River) mega-delta: Damming, urbanization, and environmental control." Paleobiology 45, no. 3 (2019): 469–83. http://dx.doi.org/10.1017/pab.2019.21.

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AbstractThe coastal environment of the Changjiang delta has been influenced by recent anthropogenic activities such as dam construction and increased sewage and fertilizer inputs. Previous work examined the compositional shift of marine plankton to assess ecological impacts of these activities on marine ecosystems in the Changjiang discharge area. Here we used benthic marine ostracodes collected in the Changjiang estuary and the adjacent East China Sea in the 1980s and the 2010s, respectively, to investigate temporal changes of the benthic community and controlling factors for the benthic faun

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3

Shankman, David, Barry D. Keim, Tadanobu Nakayama, Rongfang Li, Dunyin Wu, and W. Craig Remington. "Hydroclimate Analysis of Severe Floods in China’s Poyang Lake Region." Earth Interactions 16, no. 14 (2012): 1–16. http://dx.doi.org/10.1175/2012ei000455.1.

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Abstract Poyang Lake in Jiangxi Province is the largest freshwater lake in China and is historically a region of significant floods. Maximum annual lake stage and the number of severe flood events have increased during the past few decades because of levee construction that reduced the area available for floodwater storage. The most severe floods since 1950 occurred during 1954, 1973, 1983, 1995, and 1998. Each of these floods followed El Niño events that influence the Asian monsoon and that are directly linked to rainfall in the Changjiang (Yangtze River) basin. The 1954 flood was the largest

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4

Kubota, Y., R. Tada, and K. Kimoto. "Changes in East Asian summer monsoon precipitation during the Holocene deduced from a freshwater flux reconstruction of the Changjiang (Yangtze River) based on the oxygen isotope mass balance in the northern East China Sea." Climate of the Past 11, no. 2 (2015): 265–81. http://dx.doi.org/10.5194/cp-11-265-2015.

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Abstract. The δ18O of seawater (δ18Ow), an indirect indicator of sea surface salinity (SSS), in the northern East China Sea (ECS) is reconstructed for the Holocene using paired analyses of Mg / Ca ratio and δ18O of planktic foraminiferal tests. According to modern observation, interannual variations in SSS during summer in the northern ECS are mainly controlled by the Changjiang (Yangtze River) discharge, which reflects summer rainfall in its drainage basin. Thus, changes in the summer SSS in the northern ECS are interpreted as reflecting variations in the East Asian summer monsoon (EASM) prec

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5

Huang, Y., W. F. Yang, and L. Chen. "Water resources change in response to climate change in Changjiang River basin." Hydrology and Earth System Sciences Discussions 7, no. 3 (2010): 3159–88. http://dx.doi.org/10.5194/hessd-7-3159-2010.

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Abstract. Doubtlessly, global climate change and its impacts have caught increasing attention from all sectors of the society world-widely. Among all those affected aspects, hydrological circle has been found rather sensitive to climate change. Climate change, either as the result or as the driving-force, has intensified the uneven distribution of water resources in the Changjiang (Yangtze) River basin, China. In turn, drought and flooding problems have been aggravated which has brought new challenges to current hydraulic works such as dike or reservoirs which were designed and constructed bas

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6

Hu, Jingwen, Zhengxin Yang, Yuxin Yi, et al. "Possible Origin and Distribution of an Invasive Diatom Species, Skeletonema potamos, in Yangtze River Basin (China)." Water 15, no. 16 (2023): 2875. http://dx.doi.org/10.3390/w15162875.

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Skeletonema potamos is a freshwater diatom that has been widely distributed in North America, Europe, and Australia since the 1980s. However, there have been few previous reports of S. potamos in China. Only recently has S. potamos been frequently found in our extensive ecological surveys in China, and it has sometimes even been the dominant species. This study clarified the morphology, distribution, and origin of S. potamos, as well as the underlying mechanism contributing to its dominance. We examined the samples collected from the Changjiang River (Yangtze River) Basin during 2016–2022 and

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7

Chen, Zhongyuan, and Yiwen Zhao. "Impact on the Yangtze (Changjiang) Estuary from its drainage basin: Sediment load and discharge." Chinese Science Bulletin 46, S1 (2001): 73–80. http://dx.doi.org/10.1007/bf03187240.

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8

Tang, Xianqiang, Rui Li, Ding Han, and Miklas Scholz. "Response of Eutrophication Development to Variations in Nutrients and Hydrological Regime: A Case Study in the Changjiang River (Yangtze) Basin." Water 12, no. 6 (2020): 1634. http://dx.doi.org/10.3390/w12061634.

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Data and literature related to water quality as well as nutrient loads were used to evaluate the Changjiang River (also Yangtze or Yangzi) Basin with respect to its hydrological regime, sediment transport, and eutrophication status. Waterbodies exhibited different eutrophic degrees following the ranking order of river < reservoir < lake. Most of the eutrophic lakes and reservoirs distributed in the upstream Sichuan Basin and Jianghan Plain are located in the middle main stream reaches. During the past decade, the water surface area proportion of moderately eutrophic lakes to total evalua

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9

SATO, Osamu, Takao NAKAGAWA, and Tetsuo HASHIMOTO. "Recent tritium levels in environmental waters collected at the drainage basin of Changjiang (Yangtze river), China." RADIOISOTOPES 38, no. 12 (1989): 529–36. http://dx.doi.org/10.3769/radioisotopes.38.12_529.

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10

Li, Gen, Xingchen T. Wang, Zhongfang Yang, Changping Mao, A. Joshua West, and Junfeng Ji. "Dam-triggered organic carbon sequestration makes the Changjiang (Yangtze) river basin (China) a significant carbon sink." Journal of Geophysical Research: Biogeosciences 120, no. 1 (2015): 39–53. http://dx.doi.org/10.1002/2014jg002646.

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11

Yang, S. L., Z. Shi, H. Y. Zhao, P. Li, S. B. Dai, and A. Gao. "Research Note:Effects of human activities on the Yangtze River suspended sediment flux into the estuary in the last century." Hydrology and Earth System Sciences 8, no. 6 (2004): 1210–16. http://dx.doi.org/10.5194/hess-8-1210-2004.

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Abstract. The surface erosion area in the Yangtze River basin increased from 364×103 km2 in the 1950s to 707×103 km2 in 2001 due to a great increase in population. Based on the regression relationship between surface erosion area and population, the surface erosion area was predicted to be about 280×103 km2 at the beginning of the 20th century. The sediment yield, which increased by about 30% during the first six decades of the 20th century, was closely related to the surface erosion area in this river basin. The Yangtze annual suspended sediment flux into the estuary was about 395×106 t a-1 a

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12

Hu, Bangqi, Houjie Wang, Zuosheng Yang, and Xiaoxia Sun. "Temporal and spatial variations of sediment rating curves in the Changjiang (Yangtze River) basin and their implications." Quaternary International 230, no. 1-2 (2011): 34–43. http://dx.doi.org/10.1016/j.quaint.2009.08.018.

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13

Gong, Lebing, Chong-yu Xu, Deliang Chen, Sven Halldin, and Yongqin David Chen. "Sensitivity of the Penman–Monteith reference evapotranspiration to key climatic variables in the Changjiang (Yangtze River) basin." Journal of Hydrology 329, no. 3-4 (2006): 620–29. http://dx.doi.org/10.1016/j.jhydrol.2006.03.027.

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14

Hao, Qiang, Min Tang, Xiangtong Huang, Chi Zhang, Shaohua Dang, and Shouye Yang. "Holocene wildfire regime shifts induced by the enhancement of human activities in the Changjiang (Yangtze River) Basin." CATENA 240 (May 2024): 107998. http://dx.doi.org/10.1016/j.catena.2024.107998.

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15

Yang, Chengfan, Nathalie Vigier, Shouye Yang, Marie Revel, and Lei Bi. "Clay Li and Nd isotopes response to hydroclimate changes in the Changjiang (Yangtze) basin over the past 14,000 years." Earth and Planetary Science Letters 561 (May 2021): 116793. http://dx.doi.org/10.1016/j.epsl.2021.116793.

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16

Chen, Xiqing, Yongqiang Zong, Erfeng Zhang, Jiangang Xu, and Shijie Li. "Human impacts on the Changjiang (Yangtze) River basin, China, with special reference to the impacts on the dry season water discharges into the sea." Geomorphology 41, no. 2-3 (2001): 111–23. http://dx.doi.org/10.1016/s0169-555x(01)00109-x.

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17

Taofa, Zhou, Wu Mingan, Fan Yu, et al. "Geological, geochemical characteristics and isotope systematics of the Longqiao iron deposit in the Lu-Zong volcano-sedimentary basin, Middle-Lower Yangtze (Changjiang) River Valley, Eastern China." Ore Geology Reviews 43, no. 1 (2011): 154–69. http://dx.doi.org/10.1016/j.oregeorev.2011.04.004.

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18

He, Lijun, Yonghong Bi, David Weese, et al. "Genetic Signature of River Capture Imprinted in Schizopygopsis Fish from the Eastern Tibetan Plateau." Genes 15, no. 9 (2024): 1148. http://dx.doi.org/10.3390/genes15091148.

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Some East Asian rivers experienced repeated rearrangements due to Indian–Asian Plates’ collisions and an uplift of the Tibetan Plateau. For the upper Changjiang (Yangtze/Jinsha River), its ancient south-flowing course and subsequent capture by the middle Changjiang at the First Bend (FB) remained controversial. The DNA of freshwater fishes possess novel evolutionary signals of these tectonic events. In this study, mtDNA Cyt b sequences of endemic Schizopygopsis fish belonging to a highly specialized grade of the Schizothoracinae from the eastern Tibetan Plateau were used to infer the palaeo-dr

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19

LI, Daoji. "Oxygen depletion off the Changjiang (Yangtze River) Estuary." Science in China Series D 45, no. 12 (2002): 1137. http://dx.doi.org/10.1360/02yd9110.

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20

Chen, Jingsheng, Feiyue Wang, Xinghui Xia, and Litian Zhang. "Major element chemistry of the Changjiang (Yangtze River)." Chemical Geology 187, no. 3-4 (2002): 231–55. http://dx.doi.org/10.1016/s0009-2541(02)00032-3.

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21

Patra, Sivaji, Congqiang Liu, Siliang Li, Fushun Wang, and Baoli Wang. "Water chemical behavior at Yangtze (Changjiang) River estuary." Chinese Journal of Geochemistry 25, S1 (2006): 269–70. http://dx.doi.org/10.1007/bf02840267.

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22

Zhang, G. L., J. Zhang, S. M. Liu, J. L. Ren, and Y. C. Zhao. "Nitrous oxide in the Changjiang (Yangtze River) Estuary and its adjacent marine area: riverine input, sediment release and atmospheric fluxes." Biogeosciences Discussions 7, no. 3 (2010): 3125–51. http://dx.doi.org/10.5194/bgd-7-3125-2010.

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Abstract. Dissolved nitrous oxide (N2O) was measured in the waters of the Changjiang (Yangtze River) Estuary and its adjacent marine area during five surveys covering the period of 2002–2006. Dissolved N2O concentrations ranged from 6.04 to 21.3 nM, and indicate seasonal variations with high values occurring in summer and spring. Dissolved riverine N2O was observed monthly at station Xuliujing of the Changjiang, and ranged from 12.4 to 33.3 nM with an average of 20.8±7.8 nM. The average annual input of N2O from the Changjiang to the estuary and its adjacent area was estimated to be 15.8×106 mo

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23

Zhang, G. L., J. Zhang, S. M. Liu, J. L. Ren, and Y. C. Zhao. "Nitrous oxide in the Changjiang (Yangtze River) Estuary and its adjacent marine area: Riverine input, sediment release and atmospheric fluxes." Biogeosciences 7, no. 11 (2010): 3505–16. http://dx.doi.org/10.5194/bg-7-3505-2010.

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Abstract. Dissolved nitrous oxide (N2O) was measured in the waters of the Changjiang (Yangtze River) Estuary and its adjacent marine area during five surveys covering the period of 2002–2006. Dissolved N2O concentrations ranged from 6.04 to 21.3 nM, and indicate great temporal and spatial variations. Distribution of N2O in the Changjiang Estuary was influenced by multiple factors and the key factor varied between cruises. Dissolved riverine N2O was observed monthly at station Xuliujing of the Changjiang, and ranged from 12.4 to 33.3 nM with an average of 19.4 ± 7.3 nM. N2O concentrations in th

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24

Wang, Baodong. "Assessment of trophic status in Changjiang (Yangtze) River estuary." Chinese Journal of Oceanology and Limnology 25, no. 3 (2007): 261–69. http://dx.doi.org/10.1007/s00343-007-0261-z.

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25

Cheng, F., X. Song, Z. Yu, and D. Liu. "Historical records of eutrophication in Changjiang (Yangtze) River estuary and its adjacent East China Sea." Biogeosciences Discussions 9, no. 6 (2012): 6261–91. http://dx.doi.org/10.5194/bgd-9-6261-2012.

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Abstract. Two sediment cores from the Changjiang (Yangtze) River estuary and its adjacent East China Sea were collected and studied for eutrophication history using paleoecological records of environmental changes over the last century. A multiproxy approach by using biological and geochemical analyses revealed changes in diatom assemblages, total organic carbon (TOC), total nitrogen (TN) and biogenic silica (BSi) and give an indication of nutrient in status and trends in Changjiang River estuary and its adjacent East China Sea. The diatom assemblages in the two cores generally increased gradu

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26

Wang, Baodong, Qinsheng Wei, Jianfang Chen, and Linping Xie. "Annual cycle of hypoxia off the Changjiang (Yangtze River) Estuary." Marine Environmental Research 77 (June 2012): 1–5. http://dx.doi.org/10.1016/j.marenvres.2011.12.007.

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27

Dai, S. B., and X. X. Lu. "Sediment load change in the Yangtze River (Changjiang): A review." Geomorphology 215 (June 2014): 60–73. http://dx.doi.org/10.1016/j.geomorph.2013.05.027.

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28

Yao, Qing-Zheng, Zhi-Gang Yu, Hong-Tao Chen, Peng-Xia Liu, and Tie-Zhu Mi. "Phosphorus transport and speciation in the Changjiang (Yangtze River) system." Applied Geochemistry 24, no. 11 (2009): 2186–94. http://dx.doi.org/10.1016/j.apgeochem.2009.09.023.

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29

Jiang, Tao, Hongbo Liu, Yuhai Hu, Xiubao Chen, and Jian Yang. "Revealing Population Connectivity of the Estuarine Tapertail Anchovy Coilia nasus in the Changjiang River Estuary and Its Adjacent Waters Using Otolith Microchemistry." Fishes 7, no. 4 (2022): 147. http://dx.doi.org/10.3390/fishes7040147.

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The estuarine tapertail anchovy, Coilia nasus, is a migratory fish with high economic value in China. We collected fish from the Changjiang River (the Yangtze River) estuary, the Qiantang River estuary, and the southern Yellow Sea, and studied their relationships using otolith elemental and stable isotopic microchemistry signatures to assess the population connectivity of C. nasus. Results show that, in addition to Ca, other elements were present in the otolith core. The δ18O, Na/Ca, Fe/Ca, and Cu/Ca values of the Qiantang population were significantly higher than those of the others, whereas

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30

Wu, Hui, Bing Deng, Rui Yuan, et al. "Detiding Measurement on Transport of the Changjiang-Derived Buoyant Coastal Current." Journal of Physical Oceanography 43, no. 11 (2013): 2388–99. http://dx.doi.org/10.1175/jpo-d-12-0158.1.

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Abstract Measuring the transport of the Changjiang (also known as the Yangtze) River–derived buoyant coastal current, that is, the Min–Zhe Coastal Current, is of great importance for understanding the fate of terrestrial materials from this large river into the open ocean, but it is usually difficult to achieve because of the energetic tidal currents along the Chinese coast. In February 2012, a detiding cruise survey was carried out using the phase-averaging method. For the first time, this coastal current has been quantified with in situ data and has been shown to have a volume transport of 0

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31

Große, Fabian, Katja Fennel, Haiyan Zhang, and Arnaud Laurent. "Quantifying the contributions of riverine vs. oceanic nitrogen to hypoxia in the East China Sea." Biogeosciences 17, no. 10 (2020): 2701–14. http://dx.doi.org/10.5194/bg-17-2701-2020.

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Abstract. In the East China Sea, hypoxia (oxygen ≤ 62.5 mmol m−3) is frequently observed off the Changjiang (or Yangtze River) estuary covering up to about 15 000 km2. The Changjiang is a major contributor to hypoxia formation because it discharges large amounts of freshwater and nutrients into the region. However, modeling and observational studies have suggested that intrusions of nutrient-rich oceanic water from the Kuroshio Current also contribute to hypoxia formation. The relative contributions of riverine vs. oceanic nutrient sources to hypoxia have not been estimated before. Here, we co

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32

Tseng, Y. F., J. Lin, M. Dai, and S. J. Kao. "Joint effect of freshwater plume and coastal upwelling on phytoplankton growth off the Changjiang River." Biogeosciences 11, no. 2 (2014): 409–23. http://dx.doi.org/10.5194/bg-11-409-2014.

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Abstract. The Changjiang (Yangtze) River discharges vast amount of unbalanced nutrients (dissolved inorganic nitrogen and phosphorus with N / P ratio > 80 in general) into the East China Sea in summer. To study nutrient dynamics and P-stress potential for phytoplankton, a cruise was conducted in the Changjiang plume during summer 2011. With 3-D observations of nutrients, chlorophyll a (Chl a), and bulk alkaline phosphatase activity (APA), we concluded that the Changjiang Diluted Water and coastal upwelling significantly influenced the horizontal and vertical heterogeneities of phytoplankton

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33

Pei, Shaofeng, Zhiliang Shen, and Edward A. Laws. "Nutrient Dynamics in the Upwelling Area of Changjiang (Yangtze River) Estuary." Journal of Coastal Research 253 (May 2009): 569–80. http://dx.doi.org/10.2112/07-0948.1.

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34

Zhou, Jian-yin, Min Wang, Zheng-bing Chen, Jin-qiong Zhao, and Chun-yan Hu. "Evolution Trend of the Changjiang (Yangtze) Estuary with reduced incoming sediment." IOP Conference Series: Earth and Environmental Science 371 (December 13, 2019): 032048. http://dx.doi.org/10.1088/1755-1315/371/3/032048.

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35

Beardsley, R. C., R. Limeburner, H. Yu, and G. A. Cannon. "Discharge of the Changjiang (Yangtze River) into the East China Sea." Continental Shelf Research 4, no. 1-2 (1985): 57–76. http://dx.doi.org/10.1016/0278-4343(85)90022-6.

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36

Wu, Jiaxue, Yonghong Wang, and Heqin Cheng. "Bedforms and bed material transport pathways in the Changjiang (Yangtze) Estuary." Geomorphology 104, no. 3-4 (2009): 175–84. http://dx.doi.org/10.1016/j.geomorph.2008.08.011.

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37

Wang, Baodong. "Cultural eutrophication in the Changjiang (Yangtze River) plume: History and perspective." Estuarine, Coastal and Shelf Science 69, no. 3-4 (2006): 471–77. http://dx.doi.org/10.1016/j.ecss.2006.05.010.

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38

Dai, Zhijun, Xuefei Mei, Stephen E. Darby, Yaying Lou, and Weihua Li. "Fluvial sediment transfer in the Changjiang (Yangtze) river-estuary depositional system." Journal of Hydrology 566 (November 2018): 719–34. http://dx.doi.org/10.1016/j.jhydrol.2018.09.019.

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39

Yanling, Liang. "Preliminary study of the aquatic Oligochaeta of the Changjiang (Yangtze) River." Hydrobiologia 155, no. 1 (1987): 195–98. http://dx.doi.org/10.1007/bf00025651.

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40

Guo, Shujin, and Xiaoxia Sun. "Concentrations and distribution of transparent exopolymer particles in a eutrophic coastal sea: a case study of the Changjiang (Yangtze River) estuary." Marine and Freshwater Research 70, no. 10 (2019): 1389. http://dx.doi.org/10.1071/mf18211.

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Transparent exopolymer particles (TEPs) contribute to carbon export and can represent a significant part of the carbon pool, most notably in eutrophic systems. This study represents the first investigation of the concentrations and distribution of TEPs in the Changjiang (Yangtze River) estuary, one of the most eutrophic coastal seas in the world. The concentration of TEPs was determined on a seasonal basis (spring, summer and autumn), and the distribution patterns of TEPs were studied with respect to physical, chemical and biological conditions. Spatially, TEP concentrations exhibited a signif

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41

Liblik, Taavi, Yijing Wu, Daidu Fan, and Dinghui Shang. "Wind-driven stratification patterns and dissolved oxygen depletion off the Changjiang (Yangtze) Estuary." Biogeosciences 17, no. 10 (2020): 2875–95. http://dx.doi.org/10.5194/bg-17-2875-2020.

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Abstract. Multiple factors have been accused of triggering coastal hypoxia off the Changjiang Estuary, and their interactions lead to high yearly variation in hypoxia development time window and distribution extent. Two oceanographic cruises, conducted in July 2015 and August–September 2017, were complemented by river discharge, circulation simulation, remotely sensed wind, salinity and sea level anomaly data to study the dissolved oxygen (DO) depletion off the Changjiang Estuary from synoptic to interannual timescales. Intensification of the Chinese Coastal Current and Changjiang Diluted Wate

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42

Yuan, Xiong, Xiong Haojun, Wen Nan, Yao Yuan, and Tong Yuan. "Evaluation of the suitability of urban waterfront landscape recreation: A case study of the Changjiang waterfront in Yichang." E3S Web of Conferences 625 (2025): 03003. https://doi.org/10.1051/e3sconf/202562503003.

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The shoreline resources in the middle and lower reaches of the Yangtze River are abundant and have great value for development and utilization. With the rapid development of the economy and society, the development and utilization of waterfront resources have problems such as unreasonable layout of local areas, low utilization efficiency, and serious resource waste. It is urgent to achieve the rational utilization and effective protection of waterfront resources through scientific planning. This article starts from the perspective of landscape recreation, and constructs a suitability evaluatio

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Kubota, Y., R. Tada, and K. Kimoto. "Quantitative reconstruction of East Asian summer monsoon precipitation during the Holocene based on oxygen isotope mass-balance calculation in the East China Sea." Climate of the Past Discussions 10, no. 2 (2014): 1447–92. http://dx.doi.org/10.5194/cpd-10-1447-2014.

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Abstract. The δ18O of seawater (δ18Ow), an indirect indicator of sea surface salinity, in the northern East China Sea (ECS) was reconstructed for the last 7 kyr using paired Mg/Ca ratio and δ18O of planktic foraminiferal tests. According to modern observation, interannual variations in sea surface salinity during summer in the northern part of the ECS are mainly controlled by the discharge from the Changjiang (Yangtze River), which reflects summer rainfall in the drainage area of the Changjiang. Thus, changes in the summer sea surface salinity in the northern ECS are interpreted as reflecting

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Duan, Zongqi, Qingsong Liu, Xuefa Shi, Zhengquan Yao, Jianxing Liu, and Kai Su. "Reconstruction of high-resolution magnetostratigraphy of the Changjiang (Yangtze) River Delta, China." Geophysical Journal International 204, no. 2 (2015): 948–60. http://dx.doi.org/10.1093/gji/ggv497.

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Dai, Zhijun, James T. Liu, and Yunbo Xiang. "Human interference in the water discharge of the Changjiang (Yangtze River), China." Hydrological Sciences Journal 60, no. 10 (2015): 1770–82. http://dx.doi.org/10.1080/02626667.2014.944182.

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Nian, Xiaomei, Weiguo Zhang, Zhanghua Wang, Qianli Sun, Jing Chen, and Zhongyuan Chen. "Optical dating of Holocene sediments from the Yangtze River (Changjiang) Delta, China." Quaternary International 467 (February 2018): 251–63. http://dx.doi.org/10.1016/j.quaint.2018.01.011.

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Hori, Kazuaki, Yoshiki Saito, Quanhong Zhao, and Pinxian Wang. "Architecture and evolution of the tide-dominated Changjiang (Yangtze) River delta, China." Sedimentary Geology 146, no. 3-4 (2002): 249–64. http://dx.doi.org/10.1016/s0037-0738(01)00122-1.

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Hori, Kazuaki, Yoshiki Saito, Quanhong Zhao, et al. "Sedimentary facies and Holocene progradation rates of the Changjiang (Yangtze) delta, China." Geomorphology 41, no. 2-3 (2001): 233–48. http://dx.doi.org/10.1016/s0169-555x(01)00119-2.

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Lou, Yaying, Zhijun Dai, Yuying He, Xuefei Mei, and Wen Wei. "Morphodynamic couplings between the Biandan Shoal and Xinqiao Channel, Changjiang (Yangtze) Estuary." Ocean & Coastal Management 183 (January 2020): 105036. http://dx.doi.org/10.1016/j.ocecoaman.2019.105036.

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Weihua, Li, He-Qin Cheng, Li Jiufa, and Dong Ping. "Temporal and spatial changes of dunes in the Changjiang (Yangtze) estuary, China." Estuarine, Coastal and Shelf Science 77, no. 1 (2008): 169–74. http://dx.doi.org/10.1016/j.ecss.2007.09.006.

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