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Journal articles on the topic 'Water level changes'

Author: Grafiati

Published: 4 June 2021

Last updated: 16 February 2022

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1

Tabibi, Sajad, and Olivier Francis. "Can GNSS-R Detect Abrupt Water Level Changes?" Remote Sensing 12, no. 21 (November 3, 2020): 3614. http://dx.doi.org/10.3390/rs12213614.

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Global navigation satellite system reflectometry (GNSS-R) uses signals of opportunity in a bi-static configuration of L-band microwave radar to retrieve environmental variables such as water level. The line-of-sight signal and its coherent surface reflection signal are not separate observables in geodetic GNSS-R. The temporally constructive and destructive oscillations in the recorded signal-to-noise ratio (SNR) observations can be used to retrieve water-surface levels at intermediate spatial scales that are proportional to the height of the GNSS antenna above the water surface. In this contribution, SNR observations are used to retrieve water levels at the Vianden Pumped Storage Plant (VPSP) in Luxembourg, where the water-surface level abruptly changes up to 17 m every 4-8 h to generate a peak current when the energy demand increases. The GNSS-R water level retrievals are corrected for the vertical velocity and acceleration of the water surface. The vertical velocity and acceleration corrections are important corrections that mitigate systematic errors in the estimated water level, especially for VPSP with such large water-surface changes. The root mean square error (RMSE) between the 10-min multi-GNSS water level time series and water level gauge records is 7.0 cm for a one-year period, with a 0.999 correlation coefficient. Our results demonstrate that GNSS-R can be used as a new complementary approach to study hurricanes or storm surges that cause abnormal rises of water levels.

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2

Kitagawa, Genshiro, and Norio Matsumoto. "Detection of Coseismic Changes of Underground Water Level." Journal of the American Statistical Association 91, no. 434 (June 1996): 521–28. http://dx.doi.org/10.1080/01621459.1996.10476917.

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3

Elsobeiey, Mohamed. "Advanced spectral analysis of sea water level changes." Modeling Earth Systems and Environment 3, no. 3 (July 31, 2017): 1005–10. http://dx.doi.org/10.1007/s40808-017-0348-2.

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4

LOYDELL, DAVID K. "Early Silurian sea-level changes." Geological Magazine 135, no. 4 (July 1998): 447–71. http://dx.doi.org/10.1017/s0016756898008917.

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Global sea-level fluctuated markedly during the early Silurian, probably as a result of the waxing and waning of ice-sheets in the South American portion of Gondwana. The highest sea-levels of the Silurian are recorded by the Telychian upper crispus–lower griestoniensis and spiralis–lower lapworthi biozones. Other highstands occurred in the early Aeronian, during the convolutus Zone (mid Aeronian), guerichi Zone and late turriculatus Zone (early Telychian), and early Sheinwoodian. Low sea-levels characterized much of the argenteus and sedgwickii zones (Aeronian), the utilis Subzone (late guerichi–early turriculatus zones, early Telychian), the late Telychian (commencing in the mid lapworthi Zone) and, after a period of apparently only small amplitude sea-level fluctuations in the late Sheinwoodian and earliest Homerian, the mid–late Homerian, in particular the early nassa Zone. Facies (and faunal) changes in the Lower Silurian do not support the P and S model of Jeppsson and others, but are consistent with the sea-level changes proposed herein. Mid Telychian marine red beds appear to have been deposited during a minor sea-level fall immediately after a period of very high sea-levels, rather than during a transgressive episode as previously suggested. Comparison of the sea-level curve presented herein with those constructed in the past is hampered by the lack of precision currently possible in the correlation of early Silurian deep water (graptolitic) and shallow water (shelly) sequences. Improving the precision of this correlation should be a priority for future research.

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5

Quinn, Frank H. "Secular Changes in Great Lakes Water Level Seasonal Cycles." Journal of Great Lakes Research 28, no. 3 (January 2002): 451–65. http://dx.doi.org/10.1016/s0380-1330(02)70597-2.

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6

Kohv, Marko, Edgar Sepp, and Lii Vammus. "Assessing multitemporal water-level changes with uav-based photogrammetry." Photogrammetric Record 32, no. 160 (November 20, 2017): 424–42. http://dx.doi.org/10.1111/phor.12214.

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7

Eum, Ho-Sik, Tae-Soon Kang, Soo-Yong Nam, and Won-Moo Jeong. "Wave Modeling considering Water Level Changes and Currents Effects." Journal of Korean Society of Coastal and Ocean Engineers 28, no. 6 (December 31, 2016): 383–96. http://dx.doi.org/10.9765/kscoe.2016.28.6.383.

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8

Wrzesiński, Dariusz, and Mariusz Ptak. "Water level changes in Polish lakes during 1976–2010." Journal of Geographical Sciences 26, no. 1 (February 2016): 83–101. http://dx.doi.org/10.1007/s11442-016-1256-5.

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9

Sun, Alexander Y. "Predicting groundwater level changes using GRACE data." Water Resources Research 49, no. 9 (September 2013): 5900–5912. http://dx.doi.org/10.1002/wrcr.20421.

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10

Huszar, Eric, W. Douglass Shaw, Jeffrey Englin, and Noelwah Netusil. "Recreational damages from reservoir storage level changes." Water Resources Research 35, no. 11 (November 1999): 3489–94. http://dx.doi.org/10.1029/1999wr900235.

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11

DEPABLO, M., and A. PACIFICI. "Geomorphological evidence of water level changes in Nepenthes Mensae, Mars." Icarus 196, no. 2 (August 2008): 667–71. http://dx.doi.org/10.1016/j.icarus.2008.04.005.

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12

Colman, Steven M. "Water-level changes in Lake Baikal, Siberia: Tectonism versus climate." Geology 26, no. 6 (1998): 531. http://dx.doi.org/10.1130/0091-7613(1998)026<0531:wlcilb>2.3.co;2.

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13

Bonacci, Ognjen, Cvetanka Popovska, and Violeta Geshovska. "Analysis of transboundary Dojran Lake mean annual water level changes." Environmental Earth Sciences 73, no. 7 (August 23, 2014): 3177–85. http://dx.doi.org/10.1007/s12665-014-3618-6.

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14

Becker, Mélanie, Fabrice Papa, Mikhail Karpytchev, Caroline Delebecque, Yann Krien, Jamal Uddin Khan, Valérie Ballu, et al. "Water level changes, subsidence, and sea level rise in the Ganges–Brahmaputra–Meghna delta." Proceedings of the National Academy of Sciences 117, no. 4 (January 6, 2020): 1867–76. http://dx.doi.org/10.1073/pnas.1912921117.

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Being one of the most vulnerable regions in the world, the Ganges–Brahmaputra–Meghna delta presents a major challenge for climate change adaptation of nearly 200 million inhabitants. It is often considered as a delta mostly exposed to sea-level rise and exacerbated by land subsidence, even if the local vertical land movement rates remain uncertain. Here, we reconstruct the water-level (WL) changes over 1968 to 2012, using an unprecedented set of 101 water-level gauges across the delta. Over the last 45 y, WL in the delta increased slightly faster (∼3 mm/y), than global mean sea level (∼2 mm/y). However, from 2005 onward, we observe an acceleration in the WL rise in the west of the delta. The interannual WL fluctuations are strongly modulated by El Niño Southern Oscillation (ENSO) and Indian Ocean Dipole (IOD) variability, with WL lower than average by 30 to 60 cm during co-occurrent El Niño and positive IOD events and higher-than-average WL, by 16 to 35 cm, during La Niña years. Using satellite altimetry and WL reconstructions, we estimate that the maximum expected rates of delta subsidence during 1993 to 2012 range from 1 to 7 mm/y. By 2100, even under a greenhouse gas emission mitigation scenario (Representative Concentration Pathway [RCP] 4.5), the subsidence could double the projected sea-level rise, making it reach 85 to 140 cm across the delta. This study provides a robust regional estimate of contemporary relative WL changes in the delta induced by continental freshwater dynamics, vertical land motion, and sea-level rise, giving a basis for developing climate mitigation strategies.

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15

Marciniak, Marek, and Anna Szczucińska. "Determination of diurnal water level fluctuations in headwaters." Hydrology Research 47, no. 4 (February 19, 2016): 888–901. http://dx.doi.org/10.2166/nh.2016.039.

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The aim of this paper is to study diurnal fluctuations of the water level in streams draining headwaters and to identify the controlling factors. The fieldwork was carried out in the Gryżynka River catchment, western Poland. The water levels of three streams draining into the headwaters via a group of springs were monitored in the years 2011–2014. Changes in the water pressure and water temperature were recorded by automatic sensors – Schlumberger MiniDiver type. Simultaneously, Barodiver type sensors were used to record air temperature and atmospheric pressure, as it was necessary to adjust the data collected by the MiniDivers calculate the water level. The results showed that diurnal fluctuations in water level of the streams ranged from 2 to 4 cm (approximately 10% of total water depth) and were well correlated with the changes in evapotranspiration as well as air temperature. The observed water level fluctuations likely have resulted from processes occurring in the headwaters. Good correlation with atmospheric conditions indicates control by daily variations of the local climate. However, the relationship with water temperature suggests that fluctuations are also caused by changes in the temperature-dependent water viscosity and, consequently, by diurnal changes in the hydraulic conductivity of the hyporheic zone.

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16

Kimaro, T. A., and R. Fidelis. "Impacts of Lake Victoria Level Fluctuations to Livelihoods Missungwi District Case Study." Tanzania Journal of Engineering and Technology 30, no. 2 (December 31, 2007): 98–109. http://dx.doi.org/10.52339/tjet.v30i2.403.

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Lake Victoria experienced drastic levels changes in 2005 causing great inconveniences to lakeside communities. Thisstudy investigated effects of these changes on livelihoods through questionnaire surveys, focused group discussions,interviews and analysis of fish catches, diseases, crops, and lake levels data. Results indicate recession of levels hadvarious socio-economic impacts. The changes caused severe water shortage due to drying up of shallow wells and aremarkable increase in prevalence of schistosomiasis because of increased utilization of lake water. There was noevidence for impact of level changes on malaria and diarrhea. Decline of water levels caused decline in fish catches dueto retreat of water from breeding sites. However receding waters created a new land for cultivation which helped toboost Maize and sweet potatoes production. The results emphasize on ensuring stability of lake levels to avoid negativeimpacts on livelihoods and to maintain ecological integrity of the lake.

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17

Goldsmith, Victor, and Michael Gilboa. "MEDITERRANEAN SEA LEVEL CHANGES FROM TIDAL RECORDS." Coastal Engineering Proceedings 1, no. 20 (January 29, 1986): 17. http://dx.doi.org/10.9753/icce.v20.17.

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Of the more than 90 tide gage records in the Mediterranean, 10 representative gages were analyzed for indications of sea level rise (SLR). No definitive trend of regional sea level rise has been discerned for this area. The lack of SLR may be partially attributed to local effects on sea level such as seasonal water temperature and wind differences, and to local tectonics. The extent of these seasonal changes is in the order of tens of cms/year, and varies greatly from year to year, probably masking the trends of long-term SLR of mm/yr.

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18

Deniz, O., and M. Z. Yildiz. "The ecological consequences of level changes in Lake Van." Water Resources 34, no. 6 (November 2007): 707–11. http://dx.doi.org/10.1134/s0097807807060127.

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19

Alemayehu, Tamiru, Tenalem Ayenew, and Seifu Kebede. "Hydrogeochemical and lake level changes in the Ethiopian Rift." Journal of Hydrology 316, no. 1-4 (January 2006): 290–300. http://dx.doi.org/10.1016/j.jhydrol.2005.04.024.

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20

GE, Hua, and Chunyan DENG. "Analysis of changes of relationship between water level and discharge and its causes at the tail of Fuhe River in recent 70 years." E3S Web of Conferences 206 (2020): 03030. http://dx.doi.org/10.1051/e3sconf/202020603030.

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Based on the measured day-averaged water level and discharge data of the tail reach of Fuhe River, the changes of hydrological situation in recent 70 years was analysed in this paper. The results show that the relationship between the water level and discharge at the tail of Fuhe River has been greatly changed, and the water level at the same discharge was significantly reduced. These changed were not related to the runoff changes, but mainly affected by the changes of river bed and downstream boundary water level.

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21

Duong Thi, Toan, and Duc Do Minh. "Riverbank Stability Assessment under River Water Level Changes and Hydraulic Erosion." Water 11, no. 12 (December 10, 2019): 2598. http://dx.doi.org/10.3390/w11122598.

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The dominant mechanism of riverbank cantilever failure is soil erosion of the bank toe and near bank zone. This paper demonstrates that the shape of the riverbank cantilever failure depends on the properties of the soil and the fluctuation of the river water level (RWL). With a stable RWL, a riverbank with higher resistance force leads to failure with larger and deeper overhang erosion width. When RWL rises, a less cohesive soil bank will be eroded over a larger width and riverbank failure will occur earlier. With a low rate of rising RWL, riverbank failure may happen in a type of mass failure. With a high rate of rising RWL, a riverbank will fail in a type of overhang riverbank failure, with the soil erosion rate being the main affected factor.

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22

Laumann, Tron, and Bjørn Wold. "Reactions of a calving glacier to large changes in water level." Annals of Glaciology 16 (1992): 158–62. http://dx.doi.org/10.3189/1992aog16-1-158-162.

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Austdalsvatn in western Norway was regulated in 1988 as a reservoir for a hydropower development. From a pre-1988 water level of 1157 m a.s.l. the new water level will vary more or less annually from 1170 to 1200 m a.s.l. The outlet glacier Austdalsbreen calves into this reservoir. About 1600 m up-valley from its terminus the glacier flows over a bedrock riegel that is, at its lowest point, ∼ 15 m above the projected maximum lake level of 1200 m. As a result of the increase in water level, the surface velocity near the front has increased from about 0.07 to 0.13 m d−1.Calculations suggest that the glacier terminus will retreat about 750 m in 50 years. The measured response of the glacier terminus for the first three years is in good agreement with the simulations.

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23

Laumann, Tron, and Bjørn Wold. "Reactions of a calving glacier to large changes in water level." Annals of Glaciology 16 (1992): 158–62. http://dx.doi.org/10.1017/s0260305500004997.

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Austdalsvatn in western Norway was regulated in 1988 as a reservoir for a hydropower development. From a pre-1988 water level of 1157 m a.s.l. the new water level will vary more or less annually from 1170 to 1200 m a.s.l. The outlet glacier Austdalsbreen calves into this reservoir. About 1600 m up-valley from its terminus the glacier flows over a bedrock riegel that is, at its lowest point, ∼ 15 m above the projected maximum lake level of 1200 m. As a result of the increase in water level, the surface velocity near the front has increased from about 0.07 to 0.13 m d−1.Calculations suggest that the glacier terminus will retreat about 750 m in 50 years. The measured response of the glacier terminus for the first three years is in good agreement with the simulations.

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24

Mower, Ethan B., and Leandro E. Miranda. "Evaluating changes to reservoir rule curves using historical water-level data." International Journal of River Basin Management 11, no. 3 (September 2013): 323–28. http://dx.doi.org/10.1080/15715124.2013.823979.

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25

Alsdorf, D. E., L. C. Smith, and J. M. Melack. "Amazon floodplain water level changes measured with interferometric SIR-C radar." IEEE Transactions on Geoscience and Remote Sensing 39, no. 2 (2001): 423–31. http://dx.doi.org/10.1109/36.905250.

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26

Casco, María Adela. "Epilithic algal strategies in a reservoir with periodic water-level changes." SIL Proceedings, 1922-2010 26, no. 2 (December 1997): 458–62. http://dx.doi.org/10.1080/03680770.1995.11900756.

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27

King, Chi-Yu. "Characteristics of a Sensitive Well Showing Pre-Earthquake Water-Level Changes." Pure and Applied Geophysics 175, no. 7 (April 3, 2018): 2411–24. http://dx.doi.org/10.1007/s00024-018-1855-4.

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28

Krejci, T., T. Koudelka, and M. Broucek. "Numerical modelling of consolidation processes under the water level elevation changes." Advances in Engineering Software 72 (June 2014): 166–78. http://dx.doi.org/10.1016/j.advengsoft.2013.08.005.

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29

Fathian, Farshad, and Babak Vaheddoost. "Modeling the volatility changes in Lake Urmia water level time series." Theoretical and Applied Climatology 143, no. 1-2 (October 4, 2020): 61–72. http://dx.doi.org/10.1007/s00704-020-03417-8.

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30

Zhu, Jianting, Michael Young, John Healey, Richard Jasoni, and John Osterberg. "Interference of river level changes on riparian zone evapotranspiration estimates from diurnal groundwater level fluctuations." Journal of Hydrology 403, no. 3-4 (June 2011): 381–89. http://dx.doi.org/10.1016/j.jhydrol.2011.04.016.

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31

Choi, Mi-Jin, and Sang-Hyeon Lee. "Impact of Non-point Source Runoff on Water Resource Quality according to Water-Level Changes." Journal of Environmental Science International 24, no. 8 (August 31, 2015): 1045–53. http://dx.doi.org/10.5322/jesi.2015.24.8.1045.

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32

Liu, Xia, Katrin Teubner, and Yuwei Chen. "Water quality characteristics of Poyang Lake, China, in response to changes in the water level." Hydrology Research 47, S1 (September 23, 2016): 238–48. http://dx.doi.org/10.2166/nh.2016.209.

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As one of the few remaining lakes that are freely connected with the Yangtze River, Poyang Lake exhibits large annual water level (WL) fluctuations. In this study, weekly samples were collected at the north end of Poyang Lake from September 2011 to December 2012, and we investigated the mechanism of limnological responses to fluctuations in the WL. The study covers three seasons that were associated with WL fluctuations ranging from 8 to 19 m. Spearman's rank correlations and multivariate non-metric multidimensional scaling analyses indicated that low and high WL periods differed in a number of water quality characteristics. The low WL period coincided with the non-growing season and was associated with the peak concentrations of nitrogen, the highest turbidity (Turb), and the lowest water temperature. The high WL period was mainly characterized by enhanced chlorophyll a concentration. Spearman's rank correlations revealed positive relationships between the WL and the concentrations of NO3-N and PO4-P and negative relationships between the WL and the Turb, total nitrogen, total phosphorus, NO2-N, and NH4-N concentrations. All results support the conclusion that the large WL fluctuations are the principal drivers for physicochemical variables in this floodplain lake ecosystem.

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33

Li, Qiang. "Influence of Water Level on Cynodon dactylon Population in Water-Level-Fluctuating Zone of the Three Gorges Reservoir." Applied Mechanics and Materials 295-298 (February 2013): 1857–61. http://dx.doi.org/10.4028/www.scientific.net/amm.295-298.1857.

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To research influence of water level changes on vegetations restoration in water-level-fluctuating zone of the Three Gorges Reservoir, Cynodon dactylon in Changshou area was respectively investigated in 2008 and 2009. The results show that germination rate in 2009 is 45.3% lower than that in 2008. Total rhizome length and total node number of rhizomes in 2009 significantly increase by 303.5% and 411.1%, respectively. However, stem length, node number, leaf width and leaf number of ramets decrease by 60.1%, 55.1%, 28.6% and 33.8%, respectively. Meanwhile, total buds number, germinated buds number and buds number to rhizome length ratio in 2009 increase by 500.7%, 228.5% and 50.9%, respectively. Compared with 2008, fresh mass of ramats, rhizomes and roots reduce respectively 65.6%, 23.4% and 70.0%, and their dry mass reduce respectively 65.9%, 18.8% and 64.5%. Therefore, water level changes accelerate rhizomes extension and the formation of buds and ramets, and inhibite ramets growth.

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34

Ptak, Mariusz, Mariusz Sojka, and Bogusław Nowak. "CHANGES IN PROSNA WATER LEVELS (BOGUSŁAW PROFILE) IN 1973-2017." Zeszyty Naukowe Uniwersytetu Zielonogórskiego / Inżynieria Środowiska 171, no. 51 (October 15, 2018): 47–59. http://dx.doi.org/10.5604/01.3001.0012.8359.

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The paper presents long-term changes in water levels of Prosna, one of the main rivers in Wielkopolska, i.e. the region which is widely regarded as one of the least abundant in water in Poland. It was established that during the last 40 years the average annual water levels of Prosny showed a downward trend at the level of 7.8 cm-dec-1 and were statistically significant at the level of p=0.05 and also p=0.01. In all months a decrease in the water level was noted, although it was statistically significant in seven cases. The highest decrease in average monthly water levels (statistically significant, p=0.05) occurred in August and December and progressed at a rate of 13.2 and 12.3 cm-dec-1. The consequence of the ongoing trend may be, among others, worsening of ichthyofauna living conditions or worse quality of Prosny's water.

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35

Juschus, Olaf, Maksim Pavlov, Georg Schwamborn, Frank Preusser, Grigory Fedorov, and Martin Melles. "Late Quaternary lake-level changes of Lake El'gygytgyn, NE Siberia." Quaternary Research 76, no. 3 (November 2011): 441–51. http://dx.doi.org/10.1016/j.yqres.2011.06.010.

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AbstractLake El'gygytgyn is situated in a 3.6 Ma old impact crater in northeastern Siberia. Presented here is a reconstruction of the Quaternary lake-level history as derived from sediment cores from the southern lake shelf. There, a cliff-like bench 10 m below the modern water level has been investigated. Deep-water sediments on the shelf indicate high lake levels during a warm Mid-Pleistocene period. One period with low lake level prior to Marine Oxygen Isotope Stage (MIS) 3 has been identified, followed by a period of high lake level (10 m above present). In the course of MIS 2 the lake level dropped to − 10 m. At the end of MIS 2 the bench was formed and coarse beach sedimentation occurred. Subsequently, the lake level rose rapidly to the Holocene level. Changes in water level are likely linked to climate variability. During relatively temperate periods the lake becomes free of ice in summer. Strong wave actions transport sediment parallel to the coast and towards the outlet, where the material tends to accumulate, resulting in lake level rise. During cold periods the perennial lake ice cover hampers any wave activity and pebble-transport, keeping the outlet open and causing the lake level to drop.

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36

Qian, MIN, and ZHAN Lasheng. "Characteristics of low-water level changes in Lake Poyang during 1952 -2011." Journal of Lake Sciences 24, no. 5 (2012): 675–78. http://dx.doi.org/10.18307/2012.0505.

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37

Jing, YAO, LI Yunliang, LI Mengfan, and ZHANG Qi. "The influence of bathymetry changes on low water level of Lake Poyang." Journal of Lake Sciences 29, no. 4 (2017): 955–64. http://dx.doi.org/10.18307/2017.0419.

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38

Wang, Xianwei, Peng Gong, Yuanyuan Zhao, Yue Xu, Xiao Cheng, Zhenguo Niu, Zhicai Luo, Huabing Huang, Fangdi Sun, and Xiaowen Li. "Water-level changes in China's large lakes determined from ICESat/GLAS data." Remote Sensing of Environment 132 (May 2013): 131–44. http://dx.doi.org/10.1016/j.rse.2013.01.005.

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39

Červeňanská, Michaela, Dana Baroková, and Andrej Šoltész. "Modeling the groundwater level changes in an area of water resources operations." Pollack Periodica 11, no. 3 (December 2016): 83–92. http://dx.doi.org/10.1556/606.2016.11.3.8.

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40

Bian, Xuecheng, Hongguang Jiang, and Yunmin Chen. "Preliminary Testing on High-speed Railway Substructure Due to Water Level Changes." Procedia Engineering 143 (2016): 769–81. http://dx.doi.org/10.1016/j.proeng.2016.06.124.

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41

Rudnicki, J. W., J. Yin, and E. A. Roeloffs. "Analysis of water level changes induced by fault creep at Parkfield, California." Journal of Geophysical Research: Solid Earth 98, B5 (May 10, 1993): 8143–52. http://dx.doi.org/10.1029/93jb00354.

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42

Lavoie, Martin, and Pierre J. H. Richard. "Postglacial water-level changes of a small lake in southern Québec, Canada." Holocene 10, no. 5 (July 2000): 621–34. http://dx.doi.org/10.1191/095968300672141865.

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43

Wang, Chi-yuen, and Yeeping Chia. "Mechanism of water level changes during earthquakes: Near field versus intermediate field." Geophysical Research Letters 35, no. 12 (June 19, 2008): n/a. http://dx.doi.org/10.1029/2008gl034227.

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44

Reis, Selcuk, and Haci Murat Yilmaz. "Temporal monitoring of water level changes in Seyfe Lake using remote sensing." Hydrological Processes 22, no. 22 (October 30, 2008): 4448–54. http://dx.doi.org/10.1002/hyp.7047.

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45

Rühle, Franziska Anna, Nadine Zentner, and Christine Stumpp. "Changes in water table level influence solute transport in uniform porous media." Hydrological Processes 29, no. 6 (April 11, 2014): 875–88. http://dx.doi.org/10.1002/hyp.10200.

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46

Matsumoto, Norio. "Regression analysis for anomalous changes of ground water level due to earthquakes." Geophysical Research Letters 19, no. 12 (June 19, 1992): 1193–96. http://dx.doi.org/10.1029/92gl01042.

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47

Alsdorf, Douglas E., John M. Melack, Thomas Dunne, Leal A. K. Mertes, Laura L. Hess, and Laurence C. Smith. "Interferometric radar measurements of water level changes on the Amazon flood plain." Nature 404, no. 6774 (March 2000): 174–77. http://dx.doi.org/10.1038/35004560.

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孔, 兰. "Research on Changes of Peak Water Level in the Pearl River Estuary." Journal of Water Resources Research 01, no. 05 (2012): 315–19. http://dx.doi.org/10.12677/jwrr.2012.15048.

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Danard, M. B., and T. S. Murty. "Atmospheric pressure changes due to volcanic eruptions and possible water level fluctuations." Natural Hazards 1, no. 1 (1988): 15–26. http://dx.doi.org/10.1007/bf00168219.

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Karaman, Abdullah, Philip Carpenter, and Colin Booth. "Type-curve analysis of water-level changes induced by a longwall mine." Environmental Geology 40, no. 7 (May 1, 2001): 897–901. http://dx.doi.org/10.1007/s002540100254.

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