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1

Dizon, Neil, Jeffrey Hogan, and Scott Lindstrom. "Circumcentered reflections method for wavelet feasibility problems." ANZIAM Journal 62 (January 9, 2022): C98—C111. http://dx.doi.org/10.21914/anziamj.v62.16118.

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We introduce a two-stage global-then-local search method for solving feasibility problems. The approach pairs the advantageous global tendency of the Douglas–Rachford method to find a basin of attraction for a fixed point, together with the local tendency of the circumcentered reflections method to perform faster within such a basin. We experimentally demonstrate the success of the method for solving nonconvex problems in the context of wavelet construction formulated as a feasibility problem. References F. J. Aragón Artacho, R. Campoy, and M. K. Tam. The Douglas–Rachford algorithm for convex
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2

YOĞURTÇUOĞLU, BARAN, CÜNEYT KAYA, MATTHIAS F. GEIGER, and JÖRG FREYHOF. "Revision of the genus Seminemacheilus, with the description of three new species (Teleostei: Nemacheilidae)." Zootaxa 4802, no. 3 (2020): 477–501. http://dx.doi.org/10.11646/zootaxa.4802.3.5.

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The nemacheilid genus Seminemacheilus is revised. Six species are recognised, three of them described herein as new. All species are endemic to Central Anatolia. Seminemacheilus lendlii from the Sakarya River drainage and the endorheic Lake Aksehir and Eber basins, S. ispartensis from Lake Eğirdir basin and S. ahmeti from Sultan Sazlığı are valid species. Although Seminemacheilus lendlii and S. ispartensis have almost identical COI sequences, they are distinguished by the shape of the caudal peduncle and the presence of scales on the caudal peduncle in S. ispartensis (vs. absent in S. lendlii)
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3

Doadrio, Ignacio, Silvia Perea, and Ahmed Yahyaoui. "Two new species of Atlantic trout (Actinopterygii, Salmonidae) from Morocco." Graellsia 71, no. 2 (2015): e031 (26 pp.). https://doi.org/10.3989/graellsia.2015.v71.142.

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Four trout species of the genus <em>Salmo</em> Linnaeus, 1758 have been traditionally recognized in Morocco: <em>S. macrostigma</em> Duméril, 1858; <em>S. pallaryi</em> Pellegrin, 1924; <em>S. pellegrini</em> Werner, 1931 and <em>S. akairos</em> Delling &amp; Doadrio, 2005. Two of these species are mainly distributed in Mediterranean (<em>S. macrostigma</em>) and Atlantic (<em>S. pellegrini</em>) river basins while the other two species are restricted to isolated lakes in the Atlas Mountains, one of them to Ifni Lake (<em>S. akairos</em>) and the other, probably extinct, to Sidi Ali Lake (<em>
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4

Nunes, Gilliard, Ricardo T. Minoti, and Sergio Koide. "Mathematical Modeling of Watersheds as a Subsidy for Reservoir Water Balance Determination: The Case of Paranoá Lake, Federal District, Brazil." Hydrology 7, no. 4 (2020): 85. http://dx.doi.org/10.3390/hydrology7040085.

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Paranoá Lake, Federal District (DF), Brazil, is one of the most important urban lakes in the country and it receives inputs from basins with different characteristics, from natural and preserved to intensely urbanized and agricultural areas. The study of the hydrological processes in these basins, as well as the water balance in each of them, is fundamental for planning current and future water uses in Paranoá Lake. Using an extensive database (35 years) and the Soil and Water Assessment Tool (SWAT) model, we modelled five sub-basins. The outflow rates of the model for each sub-basin served as
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5

Spaulding, W. Geoffrey, Douglas B. Sims, and Korey T. Harvey. "Lake Ivanpah: An overlooked pluvial lake in the southern Great Basin, U. S. A." Quaternary Science Reviews 254 (February 2021): 106792. http://dx.doi.org/10.1016/j.quascirev.2020.106792.

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6

Hoffmann, N., K. Reicherter, T. Fernández-Steeger, and C. Grützner. "Evolution of ancient Lake Ohrid: a tectonic perspective." Biogeosciences Discussions 7, no. 3 (2010): 4641–64. http://dx.doi.org/10.5194/bgd-7-4641-2010.

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Abstract. Lake Ohrid Basin is a graben structure situated in the Dinarides at the border of the Former Yugoslavian Republic of Macedonia (FYROM) and Albania. It hosts one of the oldest lakes in Europe and is characterized by a basin and range-like geological setting together with the half-graben basins of Korca, Erseka and Debar. The basin is surrounded by Palaeozoic metamorphics in the northeast and north and Mesozoic ultramafic, carbonatic and magmatic rocks in the east, northwest, west and south. Palaeocene to Pliocene units are present in the southwest. With the basin development, Neogene
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7

Hoffmann, N., K. Reicherter, T. Fernández-Steeger, and C. Grützner. "Evolution of ancient Lake Ohrid: a tectonic perspective." Biogeosciences 7, no. 10 (2010): 3377–86. http://dx.doi.org/10.5194/bg-7-3377-2010.

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Abstract. Lake Ohrid Basin is a graben structure situated in the Dinarides at the border of the Former Yugoslavian Republic of Macedonia (FYROM) and Albania. It hosts one of the oldest lakes in Europe and is characterized by a basin and range-like geological setting together with the halfgraben basins of Korca, Erseka and Debar. The basin is surrounded by Paleozoic metamorphics in the northeast and north and Mesozoic ultramafic, carbonatic and magmatic rocks in the east, northwest, west and south. Paleocene to Pliocene units are present in the southwest. With the basin development, Neogene sed
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8

Jeratthitikul, Ekgachai, Chirasak Sutcharit, and Pongpun Prasankok. "An integrative approach to a revision of the freshwater mussel genus Songkhlanaia (Bivalvia, Unionidae), with the description of a new species." ZooKeys 1224 (January 28, 2025): 187–209. https://doi.org/10.3897/zookeys.1224.140549.

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Mainland Southeast Asia, also known as Indochina, is recognized as a global biodiversity hotspot for freshwater mussels, hosting a significant number of species and exhibiting high levels of endemism. Recently, the monotypic genus Songkhlanaia was described from the Songkhla Lake Basin in southern Thailand. In this study, two additional lineages are revealed, S. moreleticomb. nov. and S. songkhramensissp. nov., from the Mekong Basin through an integrative taxonomic approach combining morphological characters and molecular phylogenetic analyses. The multi-locus phylogenetic inference supported
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9

Jingfu, Wang, Chen Jingan, Dai Zhihui, Yang Haiquan, and Ma Chenyan. "Sulfur Speciation in the Surface Sediments of Lakes from Different Regions, China: Characterization by S K-Edge XANES Spectroscopy." Journal of Chemistry 2016 (2016): 1–9. http://dx.doi.org/10.1155/2016/3672348.

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X-ray absorption near edge structure (XANES) spectroscopy affords the opportunity to determine redox status for element S in the aquatic ecosystems. However, there have been relatively few studies of S XANES spectroscopy in the terrestrial aquatic ecosystems. In this study, XANES technology was used to examine changes in S speciation in the sediments collected from Taihu Lake, Qinghai Lake, Dianchi Lake, Caohai Lake, and Hongfeng Lake located in distinct geological background areas of China. The results showed that sedimentary S in Qinghai Lake has a high proportion of sulfate averaged 88.9% d
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10

DA LUZ, CYNTHIA FERNANDES PINTO, INA DE SOUZA NOGUEIRA, ORTRUD MONIKA BARTH, and CLEVERSON GUIZAN SILVA. "Differential Sedimentation of Algae Chlorococcales (Scenedesmus, Coelastrum and Pediastrum) in Lagoa de Cima, Campos dos Goitacazes Municipality (Rio de Janeiro, Brazil)." Pesquisas em Geociências 29, no. 2 (2002): 65. http://dx.doi.org/10.22456/1807-9806.19606.

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Fifteen surface sediment samples were collected at Lagoa de Cima lake (21°46’28" South and 41°31’15" West), situated in the Rio Imbé river micro basin, municipality of Campos, in the north of Rio de Janeiro, Brazil. They were collected in May 1999 following a northeast/southwest transect, along the same direction of the dominant winds. The results of the palynological analysis yielded new information about the recent richness, concentration and spatial depositional variation of the green algae genera Coelastrum, Pediastrum and Scenedesmus (Chlorococcales) on the bottom of the lake. In 30 g of
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11

Kaygorodova, I. A., and S. Yu Utevsky. "The first record of Helobdella nuda (Hirudinida, Glossiphoniidae) in lake Baikal." Vestnik Zoologii 46, no. 5 (2012): 40–41. http://dx.doi.org/10.2478/v10058-012-0039-4.

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The First Record of Helobdella nuda (Hirudinida, Glossiphoniidae) in Lake Baikal. Kaygorodova I. A., Utevsky S. Yu. - By far, the leech species Helobdella nuda (Moore, 1924) was known from China and the Amur River basin. It is found to occur in shallow waters of Lake Baikal.
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12

Jeratthitikul, Ekgachai, Chirasak Sutcharit, and Pongpun Prasankok. "An integrative approach to a revision of the freshwater mussel genus Songkhlanaia (Bivalvia, Unionidae), with the description of a new species." ZooKeys 1224 (January 28, 2025): 187–209. https://doi.org/10.3897/zookeys.1224.140549.

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Mainland Southeast Asia, also known as Indochina, is recognized as a global biodiversity hotspot for freshwater mussels, hosting a significant number of species and exhibiting high levels of endemism. Recently, the monotypic genus <i>Songkhlanaia</i> was described from the Songkhla Lake Basin in southern Thailand. In this study, two additional lineages are revealed, <i>S. moreleti</i> comb. nov. and <i>S. songkhramensis</i> sp. nov., from the Mekong Basin through an integrative taxonomic approach combining morphological characters and molecular phylogenetic analyses. The multi-locus phylogenet
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13

Demirol, Ferhat, and Mehmet Cilbiz. "First record of pikeperch (Sander lucioperca Linnaeus, 1758) in Euphrates-Tigris Basin (Keban Dam Lake, eastern-Anatolia)." International Journal of Limnology 61 (2025): 3. https://doi.org/10.1051/limn/2025002.

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In this study, we report and describe of five adult pikeperch (Sander lucioperca Linnaeus, 1758) specimens collected from the Keban Dam Lake (Euphrates-Tigris Basin) eastern-Anatolia of Türkiye. Samples caught by local fishermen during a routine gillnet fishery were brought to the laboratory for identification and detailed morphometric measurements. This appears to be the first documented record of S. lucioperca from Keban Dam Lake. In this context, it can be said that the entire Euphrates-Tigris basin is under threat of the spread of this species.
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14

Ye, Xuchun, Chong-Yu Xu, Xianghu Li, and Qi Zhang. "Comprehensive evaluation of multiple methods for assessing water resources variability of a lake–river system under the changing environment." Hydrology Research 49, no. 2 (2017): 332–43. http://dx.doi.org/10.2166/nh.2017.006.

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Abstract The inherent regularities of hydrological processes will not be stationary under the changing environment, making the evaluation of hydrological characteristics and trend forecasting face great uncertainty. Based on the observed streamflow series in the Poyang Lake catchment during the period 1960–2013, this study investigated the evolution characteristics and future trend of water resources. The extracted trend component by wavelet decomposition and the reliability of trend forecasting by rescaled range analysis (R/S analysis) were verified and assessed by a non-parametric statistica
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15

Reheis, Marith C., John Caskey, Jordon Bright, James B. Paces, Shannon Mahan, and Elmira Wan. "Pleistocene lakes and paleohydrologic environments of the Tecopa basin, California: Constraints on the drainage integration of the Amargosa River." GSA Bulletin 132, no. 7-8 (2019): 1537–65. http://dx.doi.org/10.1130/b35282.1.

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Abstract The Tecopa basin in eastern California was a terminal basin that episodically held lakes during most of the Quaternary until the basin and its modern stream, the Amargosa River, became tributary to Death Valley. Although long studied for its sedimentology, diagenesis, and paleomagnetism, the basin’s lacustrine and paleoclimate history has not been well understood, and conflicting interpretations exist concerning the relations of Tecopa basin to the Amargosa River and to pluvial Lake Manly in Death Valley. Previous studies also did not recognize basinwide tectonic effects on lake-level
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16

Georgiev, Andrey Pavlovich, and Anna Grigorievna Padchina. "Nutrition of perch (Percidae) in small lake in Lake Onega basin." Vestnik of Astrakhan State Technical University. Series: Fishing industry 2022, no. 1 (2022): 7–12. http://dx.doi.org/10.24143/2073-5529-2022-1-7-12.

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The article s focuses on studying the fish nutrition, which is one of the ways to identify the patterns of fish onto- and phylogenesis, as well as the patterns of fish abundance and using food resources in the water bodies. Nutrition determines the key physiological and biochemical reactions in the fish body in a qualitative and quantitative sense, which finally affects the growth of both individual organisms and the entire population. The results of these studies are of practical importance in the work of fish protection authorities. Information about the fish feeding in the small water bodie
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17

Wurtsbaugh, Wayne A., and Somayeh Sima. "Contrasting Management and Fates of Two Sister Lakes: Great Salt Lake (USA) and Lake Urmia (Iran)." Water 14, no. 19 (2022): 3005. http://dx.doi.org/10.3390/w14193005.

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Many saline lakes throughout the world are shrinking due to overexploitation of water in their drainage basins. Among them are two of the world’s largest saline lakes, the U.S.A.’s Great Salt Lake, and Iran’s Lake Urmia. Here we provide a comparative analysis of the desiccation of these two lakes that provides insights on management decisions that may help save them and that are relevant to saline lake management worldwide. Great Salt Lake and Lake Urmia were once remarkably similar in size, depth, salinity, and geographic setting. High rates of population growth in both basins have fueled a d
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18

Troin, M., M. Vrac, M. Khodri, C. Vallet-Coulomb, E. Piovano, and F. Sylvestre. "Coupling statistically downscaled GCM outputs with a basin-lake hydrological model in subtropical South America: evaluation of the influence of large-scale precipitation changes on regional hydroclimate variability." Hydrology and Earth System Sciences Discussions 7, no. 6 (2010): 9523–65. http://dx.doi.org/10.5194/hessd-7-9523-2010.

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Abstract. We explore the reliability of large-scale climate variables, namely precipitation and temperature, as inputs for a basin-lake hydrological model in central Argentina. We used data from two regions in NCEP/NCAR reanalyses and three regions from LMDZ model simulations forced with observed sea surface temperature (HadISST) for the last 50 years. Reanalyses data cover part of the geographical area of the Sali-Dulce Basin (region A) and a zone at lower latitudes (region B). The LMDZ selected regions represent the geographical area of the Sali-Dulce Basin (box A), and two areas outside of
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19

Banta, Robert M., Lisa S. Darby, Jerome D. Fast, et al. "Nocturnal Low-Level Jet in a Mountain Basin Complex. Part I: Evolution and Effects on Local Flows." Journal of Applied Meteorology 43, no. 10 (2004): 1348–65. http://dx.doi.org/10.1175/jam2142.1.

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Abstract A Doppler lidar deployed to the center of the Great Salt Lake (GSL) basin during the Vertical Transport and Mixing (VTMX) field campaign in October 2000 found a diurnal cycle of the along-basin winds with northerly up-basin flow during the day and a southerly down-basin low-level jet at night. The emphasis of VTMX was on stable atmospheric processes in the cold-air pool that formed in the basin at night. During the night the jet was fully formed as it entered the GSL basin from the south. Thus, it was a feature of the complex string of basins draining toward the Great Salt Lake, which
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20

Sinyukovich, V. N., and A. A. Zhdanov. "Interbasin Water Exchange by Flowage in Lake Baikal." Bulletin of Irkutsk State University. Series Earth Sciences 52 (2025): 84–96. https://doi.org/10.26516/2073-3402.2025.52.84.

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Based on long-term data on the water balance elements of Lake Baikal, modern annual and monthly values of water exchange by flowage between the lake basins – northern, middle and southern – are calculated. It is shown that the formation of annual values of inter-basin flow is determined by the inflow of river waters into the lake. Within a year, water exchange is distributed in accordance with the seasonal course of the water balance components of the lake and its level. Taking into account the latest data on the morphometry of Baikal, the parameters of water renewal are specified both in the
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21

Cao, Yuanxin, Chunye Lin, and Xuan Zhang. "Distribution and Geochemical Processes of Arsenic in Lake Qinghai Basin, China." Water 13, no. 8 (2021): 1091. http://dx.doi.org/10.3390/w13081091.

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Lake Qinghai in the Qinghai-Tibet plateau is the largest lake in China, but the geochemical understanding of arsenic (As) in the lake is lacking. Water, sediment, and soil samples were collected from Lake Qinghai, rivers flowing into the lake, and lands around the lake. Water samples were analyzed for major ions and As, while sediment and soil samples were analyzed for major elements and As. The average As concentration (25.55 μg L−1) in the lake water was significantly higher than that (1.39 μg L−1) in the river water (p &lt; 0.05), due to the evaporative concentration of lake water. The aver
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22

WICKRAMARACHCHI, Charuni, Ioana POPESCU, Andreja JONOSKI, and Jochen WENNINGER. "Use of globally available data for determining water level variation in lakes: the case study of Lake Turkana, Kenya." Geo-Eco-Marina 29 (2023) (December 31, 2023): 169–85. https://doi.org/10.5281/zenodo.10376148.

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This study identifies relevant globally available data to develop basin and water level variation models which can be used for scenario modelling. The case study for the current research is Lake Turkana in Kenya, which is the outlet of 3 main river basins: Omo, Turkwel and Keiro. Due to the lack of data, the present paper only considers the Omo River Basin, which contributes around 90% of the inflow into the lake. Lumped and semi-lumped hydrological models were developed using the USACE&rsquo;s HEC-HMS tool. The calibration and validation were carried out using the EU computed discharges of th
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23

Huggett, J. M., and J. Cuadros. "Glauconite formation in lacustrine/palaeosol sediments, Isle of Wight (Hampshire Basin), UK." Clay Minerals 45, no. 1 (2010): 35–49. http://dx.doi.org/10.1180/claymin.2010.045.1.35.

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AbstractThe clay mineralogy and chemistry of a green lacustrine marl that has been pedogenically modified in the upper part was investigated in order to better understand the formation of low-temperature Fe-rich 10 Å clay. Twelve samples in a vertical sequence have been investigated using X-ray diffraction (XRD), chemical analysis, scanning electron microscopy (SEM) and laser particle size analysis. The clay assemblage has a range of overall illite-smectite (I-S) compositions (64–100%) resulting from several I-S phases that, for the sake of modelling, have been simplified to one to three I-S p
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24

Waitt, Richard B. "Megafloods and Clovis cache at Wenatchee, Washington." Quaternary Research 85, no. 3 (2016): 430–44. http://dx.doi.org/10.1016/j.yqres.2016.02.007.

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Immense late Wisconsin floods from glacial Lake Missoula drowned the Wenatchee reach of Washington's Columbia valley by different routes. The earliest debacles, nearly 19,000 cal yr BP, raged 335 m deep down the Columbia and built high Pangborn bar at Wenatchee. As advancing ice blocked the northwest of Columbia valley, several giant floods descended Moses Coulee and backflooded up the Columbia past Wenatchee. Ice then blocked Moses Coulee, and Grand Coulee to Quincy basin became the westmost floodway. From Quincy basin many Missoula floods backflowed 50 km upvalley to Wenatchee 18,000 to 15,5
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25

Babbitt, Caitlin R., Martina R. Laidemitt, Martin W. Mutuku, et al. "Bulinus snails in the Lake Victoria Basin in Kenya: Systematics and their role as hosts for schistosomes." PLOS Neglected Tropical Diseases 17, no. 2 (2023): e0010752. http://dx.doi.org/10.1371/journal.pntd.0010752.

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The planorbid gastropod genus Bulinus consists of 38 species that vary in their ability to vector Schistosoma haematobium (the causative agent of human urogenital schistosomiasis), other Schistosoma species, and non-schistosome trematodes. Relying on sequence-based identifications of bulinids (partial cox1 and 16S) and Schistosoma (cox1 and ITS), we examined Bulinus species in the Lake Victoria Basin in Kenya for naturally acquired infections with Schistosoma species. We collected 6,133 bulinids from 11 sites between 2014–2021, 226 (3.7%) of which harbored Schistosoma infections. We found 4 Bu
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26

Tigabu, Tibebe B., Georg Hörmann, Paul D. Wagner, and Nicola Fohrer. "Statistical analysis of rainfall and streamflow time series in the Lake Tana Basin, Ethiopia." Journal of Water and Climate Change 11, no. 1 (2018): 258–73. http://dx.doi.org/10.2166/wcc.2018.008.

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Abstract This research focuses on the statistical analyses of hydrometeorological time series in the basin of Lake Tana, the largest freshwater lake in Ethiopia. We used autocorrelation, cross-correlation, Mann–Kendall, and Tukey multiple mean comparison tests to understand the spatiotemporal variation of the hydrometeorological data in the period from 1960 to 2015. Our results show that mean annual streamflow and the lake water level are varying significantly from decade to decade, whereas the mean annual rainfall variation is not significant. The decadal mean of the lake outflow and the lake
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27

Frost, B. "Tectonic Evolution of the High Pressure Granulites in the Tetons: The Earliest Record for Himalayan-Style Tectonics in the World." UW National Parks Service Research Station Annual Reports 29 (January 1, 2005): 87–88. http://dx.doi.org/10.13001/uwnpsrc.2005.3619.

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Our field season in August 2005 consisted of mapping an area from Hidden Corral in the S. Fork Bitch Creek (which is not in the Grand Teton National Park) to Moose Basin. In addition to mapping and sampling in Moose Basin area we made an important traverse along the head of the cirque around Camp Lake (which lies just west of the Park).
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28

Vijay, Suryawanshi. "ENVIRONMENTAL ASSESSMENT OF SOIL EROSION ON LAKNAVARAM LAKE BASIN." GLOBAL JOURNAL OF ENGINEERING SCIENCE AND RESEARCHES 4, no. 9 (2017): 153–66. https://doi.org/10.5281/zenodo.999295.

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The aim of this work is to estimate soil erosion on Laknavaram lake basin, JayashankarBhupalpally district, Telangana. Soils play a major role in production of food, storage of water, nutrients and organic matter. Loss of soils effects its ability to perform these functions. Soil loss reduces its potential in crop production, damages drainage network, decreases the capacity of hydraulic structures. Estimation of soil erosion in this study has been done using USLE model. The USLE was developed from soil erosion plot and rainfall simulator experiments. The USLE is composed of six factors to esti
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29

Sylvestre, Florence, Michel Servant, Simone Servant-Vildary, Christiane Causse, Marc Fournier, and Jean-Pierre Ybert. "Lake-Level Chronology on the Southern Bolivian Altiplano (18°–23°S) During Late-Glacial Time and the Early Holocene." Quaternary Research 51, no. 1 (1999): 54–66. http://dx.doi.org/10.1006/qres.1998.2017.

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AbstractStratigraphic analyses of outcrops, shorelines, and diatoms from the southern Bolivian Altiplano (Uyuni-Coipasa basin) reveal two major lacustrine phases during the late-glacial period and the early Holocene, based on a chronology established by radiocarbon and U/Th control. A comparison of14C and230Th/234U ages shows that during times of high lake level, radiocarbon ages are valid. However, during low-water periods,14C ages must be corrected for a reservoir effect. The lacustrine Tauca phase started a little before 16,00014C yr B.P., and the lake level reached its maximum between 13,0
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30

Sun, S. L., H. S. Chen, W. M. Ju, et al. "Past and future changes of streamflow in Poyang Lake Basin, Southeastern China." Hydrology and Earth System Sciences 16, no. 7 (2012): 2005–20. http://dx.doi.org/10.5194/hess-16-2005-2012.

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Abstract. To understand the causes of the past water cycle variations and the influence of climate variability on the streamflow, lake storage, and flood potential, we analyze the changes in streamflow and the underlying drivers in four typical watersheds (Gaosha, Meigang, Saitang, and Xiashan) within the Poyang Lake Basin, based on the meteorological observations at 79 weather stations, and datasets of streamflow and river level at four hydrological stations for the period of 1961-2000. The contribution of different climate factors to the change in streamflow in each watershed is estimated qu
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31

Meyer, Kirstin S., and Neil Cumberlidge. "A revision of the freshwater crabs (Crustacea: Decapoda: Brachyura: Potamonautidae) of the Lake Kivu drainage basin in Central and East Africa." Zootaxa 3011 (December 31, 2011): 45–58. https://doi.org/10.5281/zenodo.207971.

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Meyer, Kirstin S., Cumberlidge, Neil (2011): A revision of the freshwater crabs (Crustacea: Decapoda: Brachyura: Potamonautidae) of the Lake Kivu drainage basin in Central and East Africa. Zootaxa 3011: 45-58, DOI: 10.5281/zenodo.207971
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32

Dugas, Daniel P. "Late Quaternary Variations in the Level of Paleo-Lake Malheur, Eastern Oregon." Quaternary Research 50, no. 3 (1998): 276–82. http://dx.doi.org/10.1006/qres.1998.2005.

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The highest shoreline features of paleo-Lake Malheur are undated gravelly barrier beaches south of Harney Lake that lie ca. 3.5 m higher than the hydrographic outlet of Harney Basin at Malheur Gap (1254 m). The earliest Quaternary record for Lake Malheur consists of occurrences of water-deposited tephra dated to ca. 70,000–80,000 yr ago. The next identified lake interval is dated by shells with ages of ca. 32,000 and 29,500 yr B.P. No dates are available for the terminal-Pleistocene Lake Malheur. Lake(s) were present between ca. 9600 and 7400 yr B.P., although periodic low levels or desiccatio
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33

Otsubo, K., and K. Muraoka. "Field Observation and Simulation of Sediment Resuspension in a Shallow Lake." Water Science and Technology 20, no. 6-7 (1988): 263–70. http://dx.doi.org/10.2166/wst.1988.0211.

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The dispersion and resuspension of sediments in Takahamairi Bay basin of Lake Kasumigaura were studied by means of field research and numerical simulation. The field data on wind direction and velocity, lake current, water wave, and turbidity were shown. Based on these results, we discuss how precipitated sediments were resuspended in this shallow lake. To predict the turbidity and the depth of bed erosion, a simulation model was established for this lake. The calculated turbidity showed good agreement with the field data. According to the simulated results, the turbidity reaches 200 ppm, and
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34

Kaka, Soyunmyradov, and Tajiyev Aybek. "IMPACT OF TURKMEN LAKE "ALTYN ASYR" ON PASTURE PRODUCTIVITY." International Journal of Multidisciplinary Research Transactions 5, no. 4 (2023): 83–84. https://doi.org/10.5281/zenodo.7779301.

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The President of Turkmenistan is making tireless efforts to turn our motherland and vast desert into a wonderland by effectively using the country&#39;s water reserves. &quot;Altyn Asyr&quot; Turkmen Lake, created in the Garashor Basin, located in the northwest of Turkmenistan, is a clear evidence of the ongoing reforms in Turkmenistan.
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35

Garibian, P. G., and E. S. Chertoprud. "First records of Cladocera and Copepoda from Chukchagir Lake and its basin (Khabarovsk Territory, Far East of Russia)." Arthropoda Selecta 31, no. 1 (2022): 10–18. https://doi.org/10.15298/arthsel.31.1.02.

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Garibian, P. G., Chertoprud, E. S. (2022): First records of Cladocera and Copepoda from Chukchagir Lake and its basin (Khabarovsk Territory, Far East of Russia). Arthropoda Selecta 31 (1): 10-18, DOI: 10.15298/arthsel.31.1.02, URL: http://dx.doi.org/10.5281/zenodo.7576486
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36

Waniha, Pascal F., Rita D. Roberts, James W. Wilson, Agnes Kijazi, and Benedicto Katole. "Dual-Polarization Radar Observations of Deep Convection over Lake Victoria Basin in East Africa." Atmosphere 10, no. 11 (2019): 706. http://dx.doi.org/10.3390/atmos10110706.

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Lake Victoria in East Africa supports the livelihood of thousands of fishermen and it is estimated that 3000–5000 human deaths occur per year over the lake. It is hypothesized that most of these fatalities are due to localized, severe winds produced by intense thunderstorms over the lake during the rainy season and larger scale, intense winds over the lake during the dry season. The intense winds produce a rough state of the lake (big wave heights) that cause fishing boats to capsize. In this region, weather radars have never been a primary tool for monitoring and nowcasting high impact weathe
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37

Bobrov, A. A., O. A. Mochalova, and E. V. Chemeris. "The Kava River Basin (Northern Okhotsk Area) as a Hotspot of Aquatic Macrophyte Diversity in Northern Pacific." Известия Российской академии наук. Серия биологическая, no. 2 (March 1, 2023): 160–71. http://dx.doi.org/10.31857/s1026347022700032.

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Aquatic macrophytes of the Kava River basin in northern Okhotsk area are represented by 4 species of macroalgae and 51 species and 4 hybrids of vascular plants. Flora of the Magadan Region was completed by 3 species and 3 hybrids: Aegagropilopsis moravica, Equisetum arvense × E. scirpoides, Elatine aff. triandra vel americana, Potamogeton × vepsicus, Sparganium chlorocarpum and S. chlorocarpum × S. gramineum. Almost all species of aquatic vascular plants protected in the Magadan Region (10 out of 11) are concentrated and abundant in the Kava River basin, 3 “red listed” species in the Khabarovs
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38

Zhong, Xiaoyang, Lei Wang, Jing Zhou, et al. "Precipitation Dominates Long-Term Water Storage Changes in Nam Co Lake (Tibetan Plateau) Accompanied by Intensified Cryosphere Melts Revealed by a Basin-Wide Hydrological Modelling." Remote Sensing 12, no. 12 (2020): 1926. http://dx.doi.org/10.3390/rs12121926.

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Lakes on the Tibetan Plateau (TP) have changed dramatically as a result of climate change during recent decades. Studying the changes in long-term lake water storage (LWS) is of great importance for regional water security and ecosystems. Nam Co Lake is the second largest lake in the central TP. To investigate the long-term changes in LWS, a distributed cryosphere-hydrology model (WEB-DHM) driven by multi-source data was evaluated and then applied to simulate hydrological processes across the whole Nam Co Lake basin from 1980 to 2016. Firstly, a comparison of runoff (lake inflow), land surface
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39

Sztanó, Orsolya, Michal Kováč, Imre Magyar, et al. "Late Miocene sedimentary record of the Danube/Kisalföld Basin: interregional correlation of depositional systems, stratigraphy and structural evolution." Geologica Carpathica 67, no. 6 (2016): 525–42. http://dx.doi.org/10.1515/geoca-2016-0033.

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AbstractThe Danube / Kisalföld Basin is the north-western sub-basin of the Pannonian Basin System. The lithostratigraphic subdivision of the several-km-thick Upper Miocene to Pliocene sedimentary succession related to Lake Pannon has been developed independently in Slovakia and Hungary. A study of the sedimentary formations across the entire basin led us to claim that these formations are identical or similar between the two basin parts to such an extent that their correlation is indeed a matter of nomenclature only. Nemčiňany corresponds to the Kálla Formation, representing locally derived co
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40

Wang, Jie, Weikun Wang, Yuehong Hu, Songni Tian, and Dongwei Liu. "Soil Moisture and Salinity Inversion Based on New Remote Sensing Index and Neural Network at a Salina-Alkaline Wetland." Water 13, no. 19 (2021): 2762. http://dx.doi.org/10.3390/w13192762.

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In arid and semi-arid regions, soil moisture and salinity are important elements to control regional ecology and climate, vegetation growth and land function. Soil moisture and salt content are more important in arid wetlands. The Ebinur Lake wetland is an important part of the ecological barrier of Junggar Basin in Xinjiang, China. The Ebinur Lake Basin is a representative area of the arid climate and ecological degradation in central Asia. It is of great significance to study the spatial distribution of soil moisture and salinity and its causes for land and wetland ecological restoration in
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41

Al-Habahbeh, Osama M., Romil S. Al-Adwan, and Mustafa A. Al-Khawaldeh. "Macro-engineering Design for an Artificial Lake in Southeastern Jordan." WSEAS TRANSACTIONS ON ENVIRONMENT AND DEVELOPMENT 18 (June 21, 2022): 825–35. http://dx.doi.org/10.37394/232015.2022.18.77.

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Water situation in Jordan has become very critical. A feasible solution is to desalinate water drawn from Gulf of Aqaba (GoA). Another problem that Jordan faces is the very short coastline. These two problems can be solved by developing an artificial lake in south Jordan. The water from the lake can be desalinated while the lake itself provides a badly needed coastline. This work presents a macro-engineering design for the proposed lake; The proposed project is named "Red Sea-Jafer Basin Conduit (RSJBC)"; it involves a pipeline connecting GoA at the Red Sea with Jafer Basin (JB) in the south-e
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42

Gulyas, Sandor Jr. "The Palaeogeography of Lake Pannon During Deposition of the Congeria rhomboidea Beds." Geologia Croatica 54, no. 1 (2001): 15–26. http://dx.doi.org/10.4154/gc.2001.02.

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Lake Pannon covered the area of the Pannonian Basin during the late Miocene. According to the seismic profiles, prograding deltas from the NW and NE resulted in the S-SE migration of the northern palaeoshoreline and the gradual aggradation of the lacustrine basin. The molluscan fauna living in the lake underwent a very rapid evolution. For the younger species, the possibilities of spreading became more and more restricted due to the gradual shoaling of the lake. The bivalve species Congeria rhomboidea M. HÖRNES occurs widely in the Upper Pannonian (Pontian sensu Stevanovic) deposits of Hungary
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43

Klonowski, Elizabeth, Tim Lowenstein, Alan Carroll, M. Elliot Smith, Matteo Paperini, and Jeffrey Pietras. "Recurring lacustrine depositional successions in the Wilkins Peak Member, Green River Formation." Geosites 50 (September 1, 2022): 1–23. http://dx.doi.org/10.31711/ugap.v50i.116.

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Mineralogy, petrographic textures, and sedimentary structures from the world’s largest trona deposit, the Wilkins Peak Member (WPM) of the early Eocene Green River Formation (GRF), Bridger subbasin, Wyoming, provide key data about depositional conditions and paleoenvironments. The 250 m-long WPM interval in the Solvay S-34-1 drill core analyzed in this study contains a detailed record of sedimentation in the Bridger subbasin at the deepest area of a hydrologically-closed basin during peak Cenozoic atmospheric CO2 concentrations. Large accumulations of trona (Na3(HCO3)(CO3)·2H2O), shortite (Na2
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44

Seher, Dirican. "Current Status of Nationally Important Wetlands in Sivas Province, Turkey." Middle East Journal of Applied Science & Technology (MEJAST) 6, no. 1 (2023): 77–85. https://doi.org/10.46431/MEJAST.2023.6108.

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&nbsp; This study is about the current status of nationally important wetlands in Sivas province. As a result of the study, it was determined that there are two nationally important wetlands in Sivas province. These are T&ouml;d&uuml;rge Lake and Ulaş Lake are nationally important wetlands.&nbsp; T&ouml;d&uuml;rge Lake and Ulaş Lake wetlands in Sivas are usually covered with a thick snow cover in winter.&nbsp; An intense bird activity begins in the spring. Many bird species prefer T&ouml;d&uuml;rge Lake and Ulaş Lake wetlands to perform their breeding, resting, feeding and daily displacement a
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45

Blum, Jodi Switzer, Sukkyun Han, Brian Lanoil, et al. "Ecophysiology of “Halarsenatibacter silvermanii” Strain SLAS-1T, gen. nov., sp. nov., a Facultative Chemoautotrophic Arsenate Respirer from Salt-Saturated Searles Lake, California." Applied and Environmental Microbiology 75, no. 7 (2009): 1950–60. http://dx.doi.org/10.1128/aem.02614-08.

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ABSTRACT Searles Lake occupies a closed basin harboring salt-saturated, alkaline brines that have exceptionally high concentrations of arsenic oxyanions. Strain SLAS-1T was previously isolated from Searles Lake (R. S. Oremland, T. R. Kulp, J. Switzer Blum, S. E. Hoeft, S. Baesman, L. G. Miller, and J. F. Stolz, Science 308:1305-1308, 2005). We now describe this extremophile with regard to its substrate affinities, its unusual mode of motility, sequenced arrABD gene cluster, cell envelope lipids, and its phylogenetic alignment within the order Halanaerobacteriales, assigning it the name “Halars
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46

Wangchuk, Tandin, and Ryota Tsubaki. "A glacial lake outburst flood risk assessment for the Phochhu river basin, Bhutan." Natural Hazards and Earth System Sciences 24, no. 7 (2024): 2523–40. http://dx.doi.org/10.5194/nhess-24-2523-2024.

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Abstract. The melting of glaciers has led to an unprecedented increase in the number and size of glacial lakes, particularly in the Himalayan region. A glacial lake outburst flood (GLOF) is a natural hazard in which water from a glacial or glacier-fed lake is swiftly discharged. GLOFs can significantly harm life, infrastructure, and settlements located downstream and can have considerable ecological, economic, and social impacts. Based on a dam breach model, BREACH, and a hydrodynamic model, HEC-RAS (Hydrologic Engineering Centre's River Analysis System), we examined the potential consequences
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47

Soyaslan, İbrahim İskender, and Kerem Hepdeniz. "DETERMINATION OF CLIMATE TYPE AND EVAPOTRANSPIRATION FOR BURDUR LAKE BASIN USING GEOGRAPHICAL INFORMATION SYSTEMS AND DIFFERENT METHODS." Mühendislik Bilimleri ve Tasarım Dergisi 13, no. 1 (2025): 221–33. https://doi.org/10.21923/jesd.1560763.

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The surface area of Lake Burdur has been gradually shrinking every year. The most important factors causing this water loss are the climate type of the basin and evapotranspiration. In hydrogeological basin studies, one of the discharge parameters used in hydrological water balance calculations is the actual evaportranspiration. Thornthwaite, Blaney-Criddle and Schendel methods were used to calculate evapotranspiration for the basin. When the results of the three methods were compared, Thornthwaite method gave results closer to the average values. Thornthwaite Climate Classification method was
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48

Demakov, Denis Aleksandrovich, and Evgenia Leonidovna Lychagina. "Population of the Upper and Middle Kama basin in the Neolithic." Samara Journal of Science 8, no. 3 (2019): 113–19. http://dx.doi.org/10.17816/snv201983202.

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The paper gives a description of the landscapes formed in the Upper and Middle Kama basin in the Holocene. First of all, we talk about the first river terraces and the most ancient floodplain generations. In the Upper and Middle Kama basin, 78 Neolithic sites are known. During the mapping of the study area, 4 micro regions were identified with a large concentration of Neolithic settlements and territories with no Neolithic sites are known. The first group includes: the old-channel formation of the Chashkinskoye Lake, the Berezovaya River and the Chusovsky Lake District, the old-channel formati
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49

Cui, Yingying, Liping Zhu, Jianting Ju, Lun Luo, and Yongjie Wang. "Climate Change and Hydrological Response in the Ranwu Lake Basin of Southeastern Tibet Plateau." Water 15, no. 11 (2023): 2119. http://dx.doi.org/10.3390/w15112119.

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It is of great practical significance to accurately distinguish the different water supply sources of rivers and lakes under climate change for regional water resources utilization. This study examines the impact of climate change on the hydrological processes of the Ranwu Lake basin in the southeastern Tibet Plateau. The authors used China Meteorological Forcing Dataset (CMFD) historical data, CanESM5′s future climate predictor, and the SPHY model to analyze trends in temperature, precipitation, and water supply sources in the basin. The study found that warming in the basin was higher than t
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50

Osbrough, S. L., J. S. Frederiksen, and C. S. Frederiksen. "The effects of model climate bias on ENSO variability and ensemble prediction." ANZIAM Journal 60 (October 18, 2019): C215—C230. http://dx.doi.org/10.21914/anziamj.v60i0.14092.

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New methods are presented for determining the role of coupled ocean-atmosphere model climate bias on the strength and variability of the El Nino-Southern Oscillation (ENSO) and on the seasonal ensemble prediction of El Nino and La Nina events. An intermediate complexity model with a global atmosphere coupled to a Pacific basin ocean is executed with parallelised algorithms to produce computationally efficient year-long forecasts of large ensembles of coupled flow fields, beginning every month between 1980 and 1999. Firstly, the model is provided with forcing functions that reproduce the averag
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