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Relevant bibliographies by topics / Lake

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Academic literature on the topic 'Lake'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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Journal articles on the topic "Lake"

1

Sellers, Todd J., Brian R. Parker, David W. Schindler, and William M. Tonn. "Pelagic distribution of lake trout (Salvelinus namaycush) in small Canadian Shield lakes with respect to temperature, dissolved oxygen, and light." Canadian Journal of Fisheries and Aquatic Sciences 55, no. 1 (1998): 170–79. http://dx.doi.org/10.1139/f97-232.

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The distribution of lake trout (Salvelinus namaycush) with respect to water temperature, dissolved oxygen, and light intensity was surveyed in three small Canadian Shield lakes at the Experimental Lakes Area, northwestern Ontario. Based on hydroacoustic and gillnet surveys, there was considerable variation among lakes in temperatures occupied by lake trout during the summer. During the day, lake trout were concentrated at 4-8°C in Lake 375, broadly distributed from 6 to 15°C in Lake 442, and concentrated in the epilimnion at 19°C in Lake 468. At night, lake trout in all lakes occupied epilimne

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Rodriguez, Yarice, David A. R. Kristovich, and Mark R. Hjelmfelt. "Lake-to-Lake Cloud Bands: Frequencies and Locations." Monthly Weather Review 135, no. 12 (2007): 4202–13. http://dx.doi.org/10.1175/2007mwr1960.1.

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Abstract Premodification of the atmosphere by upwind lakes is known to influence lake-effect snowstorm intensity and locations over downwind lakes. This study highlights perhaps the most visible manifestation of the link between convection over two or more of the Great Lakes lake-to-lake (L2L) cloud bands. Emphasis is placed on L2L cloud bands observed in high-resolution satellite imagery on 2 December 2003. These L2L cloud bands developed over Lake Superior and were modified as they passed over Lakes Michigan and Erie and intervening land areas. This event is put into a longer-term context th

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Yan, Norman D., Warren I. Dunlop, Trevor W. Pawson, and Lori E. MacKay. "Bythotrephes cederstroemi (Schoedler) in Muskoka Lakes: First Records of the European Invader in Inland Lakes in Canada." Canadian Journal of Fisheries and Aquatic Sciences 49, no. 2 (1992): 422–26. http://dx.doi.org/10.1139/f92-048.

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The large predaceous European zooplankter Bythotrephes cederstroemi is now present in eight large recreational lakes in south-central Ontario, Canada: Lake Muskoka, Lake Joseph, Lake Rosseau, Fairy Lake, Mary Lake, Peninsula Lake, Lake Vernon, and Go Home Lake. These observations represent the first evidence that B. cederstroemi has invaded inland lakes in Canada, and we suggest that close monitoring is now needed to establish whether or not pelagic food webs of the lakes will respond.

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Cengiz, Taner. "Periodic structures of Great Lakes levels using wavelet analysis." Journal of Hydrology and Hydromechanics 59, no. 1 (2011): 24–35. http://dx.doi.org/10.2478/v10098-011-0002-z.

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Periodic structures of Great Lakes levels using wavelet analysisThe recently advanced approach of wavelet transforms is applied to the analysis of lake levels. The aim of this study is to investigate the variability of lake levels in four lakes in the Great Lakes region where the method of continuous wavelet transform and global spectra are used. The analysis of lake-level variations in the time-scale domain incorporates the method of continuous wavelet transform and the global spectrum. Four lake levels, Lake Erie, Lake Michigan, Lake Ontario, and Lake Superior in the Great Lakes region were

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Laird, Neil, Ryan Sobash, and Natasha Hodas. "The Frequency and Characteristics of Lake-Effect Precipitation Events Associated with the New York State Finger Lakes." Journal of Applied Meteorology and Climatology 48, no. 4 (2009): 873–86. http://dx.doi.org/10.1175/2008jamc2054.1.

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Abstract This study presents a climatological analysis of the frequency and characteristics of lake-effect precipitation events that were initiated or enhanced by lakes within the New York State (NYS) Finger Lakes region for the 11 winters (October–March) from 1995/96 through 2005/06. Weather Surveillance Radar-1988 Doppler (WSR-88D) data from Binghamton, New York, were used to identify 125 lake-effect events. Events occurred as 1) a well-defined, isolated precipitation band over and downwind of a lake, 2) an enhancement of mesoscale lake-effect precipitation originating from Lake Ontario and

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Sikder, Md Safat, Jida Wang, George H. Allen, et al. "Lake-TopoCat: a global lake drainage topology and catchment database." Earth System Science Data 15, no. 8 (2023): 3483–511. http://dx.doi.org/10.5194/essd-15-3483-2023.

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Abstract. Lakes and reservoirs are ubiquitous across global landscapes, functioning as the largest repository of liquid surface freshwater, hotspots of carbon cycling, and sentinels of climate change. Although typically considered lentic (hydrologically stationary) environments, lakes are an integral part of global drainage networks. Through perennial and intermittent hydrological connections, lakes often interact with each other, and these connections actively affect water mass, quality, and energy balances in both lacustrine and fluvial systems. Deciphering how global lakes are hydrologicall

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Lara, Mark Jason, and Melissa Lynn Chipman. "Periglacial Lake Origin Influences the Likelihood of Lake Drainage in Northern Alaska." Remote Sensing 13, no. 5 (2021): 852. http://dx.doi.org/10.3390/rs13050852.

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Nearly 25% of all lakes on earth are located at high latitudes. These lakes are formed by a combination of thermokarst, glacial, and geological processes. Evidence suggests that the origin of periglacial lake formation may be an important factor controlling the likelihood of lakes to drain. However, geospatial data regarding the spatial distribution of these dominant Arctic and subarctic lakes are limited or do not exist. Here, we use lake-specific morphological properties using the Arctic Digital Elevation Model (DEM) and Landsat imagery to develop a Thermokarst lake Settlement Index (TSI), w

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Zhang, Ao, Xinwen Zhao, Jun He, Xuan Huang, Xingyuezi Zhao, and Yongbo Zhao. "Characteristics of Hydrogen and Oxygen Isotope Composition in Precipitation, Rivers, and Lakes in Wuhan and the Ecological Environmental Effects of Lakes." Water 15, no. 16 (2023): 2996. http://dx.doi.org/10.3390/w15162996.

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Wuhan has a dense network of rivers and lakes. Due to the city’s development, the water system has been fragmented, the degradation of lakes is becoming increasingly severe, and the eco-environment has been significantly damaged. By collecting samples of the central surface water bodies in Wuhan, including Yangtze River water, Han River water, lake water, and precipitation, and by utilizing hydrogen and oxygen isotopes and multivariate statistical methods, the hydraulic connectivity and ecological environmental effects between the Yangtze River, the Han River, and the lakes were revealed. The

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Jia, Junmei, Qiuwen Chen, Haidong Ren, Renjie Lu, Hui He, and Peiwen Gu. "Phytoplankton Composition and Their Related Factors in Five Different Lakes in China: Implications for Lake Management." International Journal of Environmental Research and Public Health 19, no. 5 (2022): 3135. http://dx.doi.org/10.3390/ijerph19053135.

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In this paper, two trophic lakes: Lake Taihu and Lake Yanghe, and three alpine lakes: Lake Qinghai, Lake Keluke, and Lake Tuosu, were investigated to discover the connections between environmental factors and the phytoplankton community in lakes with differences in trophic levels and climatic conditions. Three seasonal data, including water quality and phytoplankton, were collected from the five lakes. The results demonstrated clear differences in water parameters and phytoplankton compositions in different lakes. The phytoplankton was dominated by Bacillariophyta, followed by Cyanobacteria an

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Donald, David B., and David J. Alger. "Geographic distribution, species displacement, and niche overlap for lake trout and bull trout in mountain lakes." Canadian Journal of Zoology 71, no. 2 (1993): 238–47. http://dx.doi.org/10.1139/z93-034.

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Indigenous lacustrine populations of bull trout (Salvelinus confluentus) and lake trout (S. namaycush) are spatially separated within the southern part of the zone of distributional overlap (northern Montana, southwestern Alberta, and east-central British Columbia). In this area, lake trout occurred primarily in mountain lakes of 1032–1500 m elevation, while bull trout were found primarily in lakes between 1500 and 2200 m. Introductions of lake trout in the twentieth century and data obtained from beyond the study area indicated that both fishes can establish significant allopatric populations

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Dissertations / Theses on the topic "Lake"

1

Schnellmann, Michael P. Schnellmann Michael P. "Late quaternary mass movements in a perialpine lake (Lake Lucerne, Switzerland) /." [S.l.] : [s.n.], 2004. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=15533.

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O'Connor, Jim E. "Hydrology, hydraulics, and sediment transport of pleistocene Lake Bonneville flooding on the Snake River, Idaho." Diss., The University of Arizona, 1990. http://hdl.handle.net/10150/191159.

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Approximately 14,500 years ago, Pleistocene Lake Bonneville discharged 4750 km 3 of water over the divide between the closed Bonneville Basin and the watershed of the Snake River. The resulting flood, emanating from the divide at Red Rock Pass, Idaho, followed the present courses of Marsh Creek, the Portneuf River, and the Snake and Columbia Rivers before reaching the Pacific Ocean. For the 1100 kilometers between Red Rock Pass and Lewiston, Idaho, the Bonneville Flood left a spectacular array of flood features that have allowed for geologic reconstruction and quantitative evaluation of many a

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Metcalfe, Elisabet Joan. "Late-glacial through Holocene Stratigraphy and Lake-level Record of Rangely Lake, Western Maine." Fogler Library, University of Maine, 2007. http://www.library.umaine.edu/theses/pdf/MetcalfeEJ2007.pdf.

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Maki, Angela Pelkie. "Effects of Air Temperature and Lake Ice on Snowfall on the South Shore of Lake Superior." ScholarWorks@UNO, 2009. http://scholarworks.uno.edu/td/941.

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Lake Superior is a forcing factor for local weather systems, causing substantial amounts of lake effect snow in the winter (particularly on the south shore). This study assesses decreasing ice cover of Lake Superior and its effects upon synoptic weather factors. Data were collected from eleven National Weather Service (NWS) stations located on the south shore of the lake. Rainfall and snowfall amounts from December to May were regressed on percent ice coverage and average monthly temperatures from 1972-2002. Ice coverage and average monthly temperature had a negative relationship with sn

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Sapota, Tomasz. "Late Cenozoic Geoarchives from Lake Baikal, Siberia." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-4552.

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<p>Three long sediment cores (BDP-98 – 600 m, BDP-96 – 200 m and BDP-93 – 100 m) drilled in Lake Baikal (Siberia) have been studied with the aims of establishing an absolute chronology and reconstructing paleoclimatic and paleoenvironmental changes in the region. The location of the lake at relatively high latitude and continental interior and a thick continuous sedimentary archive that developed in a rift system tectonic setting provide unique material for this investigation. The cosmogenic isotope <sup>10</sup>Be was used for dating and the results indicate time spans of 8 (+0.8\-0.6) Myr fo

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Lacey, Jack H. "Late Quaternary palaeoenvironmental reconstruction from Lake Ohrid." Thesis, University of Nottingham, 2016. http://eprints.nottingham.ac.uk/31993/.

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Lake Ohrid is a large, deep, ancient lake located on the Balkan Peninsula and has an extraordinary degree of endemic biodiversity. A deep drilling campaign was carried out in 2013 as part of the Scientific Collaboration on Past Speciation Conditions in Lake Ohrid (SCOPSCO) project to better understand the influence of climate and environmental change on evolutionary patterns and endemism. Initial results from a 569 m sediment succession drilled in the centre of the basin indicate continuous lacustrine conditions over the past ca. 1.2 Ma. This thesis presents new stable isotope data from carbon

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Lally, Corinne M. "Late Pleistocene to Holocene climate variability recorded in lake sediment of Silver Lake, Summit County, Ohio." University of Akron / OhioLINK, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=akron1479127321585964.

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Olago, Daniel Ochieng. "Late Quaternary lake sediments of Mount Kenya, Kenya." Thesis, University of Oxford, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.296036.

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Griffiths, S. J. "Late Quaternary palaeoclimatology of Lake Kopais, central Greece." Thesis, Swansea University, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.507951.

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Ferian, Michael R. "The Effect of Global Temperature Increase on Lake-Effect Snowfall Downwind of Lake Erie." Ohio University / OhioLINK, 2008. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1229968622.

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Books on the topic "Lake"

1

N, Smirnov N., ed. Lake Glubokoe. W. Junk, 1987.

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Seelye, Elizabeth Eggleston. Lake George in history. 5th ed. E. Seelye, 1986.

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Armbruster, Ann. Lake Superior. Children's Press, 1996.

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UNEP International Environmental Technology Centre., ed. Technology needs for lake management in Indonesia: Case studies : Lakes Rawa Danau and Rawa Pening, Java. UNEP International Environmental Technology Centre, 1999.

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1942-, Goldstein Robert A., ed. Integrated lake-watershed acidification. D. Reidel Pub. Co., 1985.

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Association of Summer Villages of Alberta., ed. Lake stewardship reference guide. 2nd ed. Association of Summer Villages of Alberta, 2006.

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Association of Summer Villages of Alberta., ed. Lake stewardship reference guide. 2nd ed. Association of Summer Villages of Alberta, 2006.

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8

James, Mark. Lake level management. Ministry for the Environment, 2002.

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Indiana Lakes Management Work Group. Final report of the Indiana Lakes Management Work Group. Indiana Dept. of Environmental Management, 1999.

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International Workshop on Restoration and Management of Eutrophic Lakes (2001 Kunming Shi, China). Restoration and management of tropical eutrophic lakes. Edited by Reddy M. V. Science Publishers, 2005.

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Book chapters on the topic "Lake"

1

Khera, Dipti. "Lakes within lake-palaces." In Water Histories of South Asia. Routledge India, 2019. http://dx.doi.org/10.4324/9780429242694-4.

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Kumar, Anjani, Abhishek Mishra, and Sanjeev Kumar. "Data Lake, Lake House, and Delta Lake." In Architecting a Modern Data Warehouse for Large Enterprises. Apress, 2023. http://dx.doi.org/10.1007/979-8-8688-0029-0_3.

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Gooch, Jan W. "Lake." In Encyclopedic Dictionary of Polymers. Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-6247-8_6740.

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Gooch, Jan W. "Lake." In Encyclopedic Dictionary of Polymers. Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-6247-8_6741.

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Seip, Knut Lehre, and Fred Wenstop. "Lake." In A Primer on Environmental Decision-Making. Springer Netherlands, 2006. http://dx.doi.org/10.1007/978-1-4020-5067-1_17.

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Filatov, Nikolai, and Leonid Rukhovets. "Ladoga Lake and Onego Lake (Lakes Ladozhskoye and Onezhskoye)." In Encyclopedia of Lakes and Reservoirs. Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-1-4020-4410-6_197.

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Mianping, Zheng. "Saline Lakes and Lake Districts." In An Introduction to Saline Lakes on the Qinghai—Tibet Plateau. Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5458-1_2.

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Renaut, Robin W., and Richard Bernhart Owen. "Lake Nakuru and Lake Elmenteita." In The Kenya Rift Lakes: Modern and Ancient. Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-642-25055-2_10.

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Selley, Richard C. "Lake deposits." In Ancient Sedimentary Environments. Springer US, 1985. http://dx.doi.org/10.1007/978-1-4615-5421-9_4.

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Robitaille, André, and Jean-Marie M. Dubois. "Lake Outbursts." In Encyclopedia of Lakes and Reservoirs. Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-1-4020-4410-6_101.

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Conference papers on the topic "Lake"

1

Gihon, Arik. "Lunar Lake Architecture Session." In 2024 IEEE Hot Chips 36 Symposium (HCS). IEEE, 2024. http://dx.doi.org/10.1109/hcs61935.2024.10664946.

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Choudhary, Vanshika, Kartik, and Neetu Bala. "Cloud-Based Data Lake." In 2024 International Conference on Artificial Intelligence and Quantum Computation-Based Sensor Application (ICAIQSA). IEEE, 2024. https://doi.org/10.1109/icaiqsa64000.2024.10882348.

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Kitazawa, Daisuke, Takero Yoshida, Jinxin Zhou, and Sanggyu Park. "Comparative Study on Vertical Circulation in Deep Lakes: Lake Biwa and Lake Ikeda." In 2018 OCEANS - MTS/IEEE Kobe Techno-Ocean (OTO). IEEE, 2018. http://dx.doi.org/10.1109/oceanskobe.2018.8558877.

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Olson, Kristian, Robert V. Demicco, and Tim Lowenstein. "SEASONAL DYNAMICS OF SALINE-ALKALINE LAKES: MODEL SOLUTIONS FOR SHALLOW (MODERN) OWENS LAKE AND DEEP (LATE PLEISTOCENE) SEARLES LAKE, CALIFORNIA (USA)." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383213.

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Wriston, Teresa A., and Geoffrey M. Smith. "THE LATE PLEISTOCENE TO HOLOCENE ARCHAEOLOGY AND LAKE LEVELS OF PLUVIAL LAKE WARNER, OREGON." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-287174.

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Dickey, Hank, Matthew E. Kirby, Ed Knell, et al. "USING LAKE SEDIMENTS TO INFER LATE-GLACIAL HYDROLOGIC CONDITIONS OF PLUVIAL LAKE MOJAVE, CALIFORNIA." In 116th Annual GSA Cordilleran Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020cd-347676.

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Pellegrino, Jay, Andy Breckenridge, and Matt Wieker. "TOWARDS A COMPREHENSIVE ANALYSIS OF LATE-GLACIAL LAKE LEVELS WITHIN THE LAKE SUPERIOR BASIN." In Joint 60th Annual Meeting of the GSA Northeastern Section and 59th Annual Meeting of the GSA North-Central Section - 2025. Geological Society of America, 2025. https://doi.org/10.1130/abs/2025ne-408499.

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Scholz, Christopher A., and Douglas Wood. "Early-Stage Extension in the Southwest East African Rift: Integration of New Seismic Reflection Data." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2614293-ms.

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ABSTRACT The western branch of the East African Rift is characterized by modest amounts of extension and by deeply-subsided, fault-controlled basins filled with large, deep lakes. Lakes Tanganyika and Nyasa (Malawi) are two of the largest lakes in the world, with maximum water depths of 1450 and 700 m respectively. Newly acquired seismic reflection data, along with newly reprocessed legacy data reveal thick sedimentary sections, in excess of 5 km in some localities. The 1980's vintage legacy data from Project PROBE have been reprocessed through pre-stack depth migration in Lake Tanganyika, and

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Finke, Andrew. "Lake." In CHI '19: CHI Conference on Human Factors in Computing Systems. ACM, 2019. http://dx.doi.org/10.1145/3290607.3308455.

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Steele, Jack Cowan, and William H. Amidon. "LATE PLEISTOCENE CHRONOLOGY OF LAKE TERRETON, SOUTHEASTERN IDAHO." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272806.

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Reports on the topic "Lake"

1

Kerr, D. E. Reconnaissance surficial geology, Nose Lake, Nunavut-Northwest Territories, NTS 76-F. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329666.

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The oldest regional ice flow in the Nose Lake map area is southwestward. Subsequent northwestward flow is inferred from streamlined bedrock in central and eastern regions. The final and youngest flow was southwestward in these same regions, recorded by an abundance of streamlined landforms in till blanket and bedrock. The western edge of this late active ice lobe is defined by recessional moraines, part of the Twin Jugs moraine, also marking the eastern limit of a broad band of hummocky till from downwasting ice. During deglaciation, short-lived proglacial lakes, identified by raised beaches a

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Dyke, A. S., J. E. Campbell, and G. Lauzon. Surficial geology, Abitau Lake, Northwest Territories, NTS 75-B. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330072.

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The Abitau Lake map area lies in the Rae Province of the Canadian Shield. Quaternary deposits are extensive and thick, with bedrock outcrop concentrated in the northwest and southwest. Till is extensively streamlined to the west-southwest by late deglacial ice flow from the Keewatin Ice Divide. The region is incised by west-southwest flowing subglacial meltwater corridors that extend across the map area, spaced 5 to 15 km apart. The ice flow chronology (Figure 1) is recorded both in the landforms and in the striae record. Rare measurements record an old flowset oriented northwest-southeast. We

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Swanson, David, and Celia Hampton-Miller. Drained lakes in Bering Land Bridge National Preserve: Vegetation succession and impacts on loon habitat. National Park Service, 2023. http://dx.doi.org/10.36967/2296593.

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The northern coastal plain of Bering Land Bridge National Preserve (BELA) lost lakes at an alarming rate over the first two decades of this century, including four lakes over 100 ha in size in 2018-2019 alone. To understand the effects of these lake drainages, we sampled vegetation of these lakes in 2019 (a reconnaissance visit) and 2021 (for the installation of permanent vegetation monitoring plots). We used these data to summarize the changes that occurred in the first three years after drainage, and to create vegetation maps from 3-m resolution satellite images coinciding with the visit dat

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Hagedorn, G. W., I. R. Smith, R. C. Paulen, and M. Ross. Surficial geology, Enterprise, Northwest Territories, NTS 85-C/9, 10, 15, and 16. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328292.

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The Enterprise map area is a low-relief terrain bisected by a prominent Devonian carbonate bedrock escarpment. Ice-flow indicators show a clockwise shift in Laurentide Ice Sheet flow from southwest (230°), to west (280°), to northwest (305°). A late-stage southwestward surge from the Great Slave Lake basin is also preserved as drumlinoid ridges below the escarpment. During deglaciation, ice retreat impounded northeastern drainage forming local ice-contact lakes and areas of subaerial glaciofluvial outwash. As ice continued to retreat, the northern portion of the map area became inundated by gl

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Maki, Ryan, Kristen Patterson, Joseph Amundson, et al. Little Shoepack Lake muskellunge (Esox masquinongy) population estimate and genetic evaluation of muskellunge from Shoepack and Little Shoepack lakes. National Park Service, 2024. http://dx.doi.org/10.36967/2305092.

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Little Shoepack and Shoepack lakes in Voyageurs National Park, Minnesota, are home to native populations of Muskellunge (Esox masquinongy). Due to the small size of these lakes, 20.8 ha and 123 ha, respectively, and the associated, predicted small size of these Muskellunge populations, resource managers are concerned about their persistence. A recent population assessment completed for Shoepack Lake Muskellunge indicated that the population may be below a threshold at which a genetic bottleneck could threaten its persistence. Since Little Shoepack Lake is approximately 20% of the size of Shoep

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Thompson, Anna, Michael Loso, Sydney Mooneyham, Brandon Tober, Christopher Larsen, and John Holt. Surficial geology and proglacial lake change at S?t? Tlein (Malaspina Glacier), Wrangell-St. Elias National Park and Preserve, Alaska. National Park Service, 2024. http://dx.doi.org/10.36967/2301689.

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S?t? Tlein (Tlingit for ?Big Glacier?) is the traditional name for what has recently been called Malaspina Glacier, the largest glacier in Alaska. The piedmont terminal lobe of S?t? Tlein is protected from the adjacent Pacific Ocean by a narrow, vegetated foreland dotted with proglacial lakes. Ice of the piedmont lobe is largely covered with debris and vegetation. These lakes and sedimentary deposits impact rates of melt and calving and therefore impact ongoing evolution of the glacier itself. To document these features, we present 1) a new surficial geology map for the foreland and piedmont l

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Bailard, Jennifer. Mojave Desert Network (MOJN) Streams and Lakes (STLK) Data Quality Report 2024. National Park Service, 2025. https://doi.org/10.36967/2312646.

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This HTML report summarizes data quality evaluations of discrete data collected for the Mojave Desert Network Inventory and Monitoring Program Streams and Lakes protocol. This protocol is designed to monitor the hydrologic and ecosystem health of nine streams and six subalpine lakes in Great Basin National Park. Collected data include lake surface elevations, lake clarity, water quality measurements, stream channel characteristics, water chemistry samples, and benthic macroinvertebrate samples. Lake surface elevations, lake clarity, water quality measurements, and stream channel characteristic

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Bailard, Jennifer. Mojave Desert Network (MOJN) Streams and Lakes (STLK) Data Quality Report 2024. National Park Service, 2025. https://doi.org/10.36967/2313986.

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Abstract:

This HTML report summarizes data quality evaluations of discrete data collected for the Mojave Desert Network Inventory and Monitoring Program Streams and Lakes protocol. This protocol is designed to monitor the hydrologic and ecosystem health of nine streams and six subalpine lakes in Great Basin National Park. Collected data include lake surface elevations, lake clarity, water quality measurements, stream channel characteristics, water chemistry samples, and benthic macroinvertebrate samples. Lake surface elevations, lake clarity, water quality measurements, stream channel characteristics, a

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Ramos-Santiago, Efrain, Norberto Nadal-Caraballo, Fabian Garcia-Moreno, et al. Statistical analysis of storm surge and seiche hazards for Lake Erie. Engineer Research and Development Center (U.S.), 2024. http://dx.doi.org/10.21079/11681/48590.

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Abstract:

Storm surge and seiche events are generally forced by severe storms, initially resulting in a wind-driven super elevation of water level on one or more sides of a lake (surge) followed by a rebound and periodic oscillation of water levels between opposing sides of the lake (seiche). These events have caused flooding along Lake Erie and significant damages to coastal communities and infrastructure. This study builds upon statistical analysis methods initially developed for the 2012 federal interagency Great Lakes Coastal Flood Study. Using the Coastal Hazards System's stochastic Storm Simulatio

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Kerr, D. E. Reconnaissance surficial geology, Keller Lake, Northwest Territories, NTS 95-P. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328293.

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Abstract:

The Keller Lake map area contains three glacial terrains. First, ridged and fluted till cover the northeast region above 300 m elevation. Second, streamlined till, including mega-scale glacial lineations, and till plain with an extensive organic cover, dominate a low-lying basin in the north-central and central regions. Third, till blanket, ridged till, and undifferentiated till cover the highlands at 375 to 575 m elevation in the southeast, south, and west. A dominant regional northwestward ice flow first crossed the map area. Subsequently, an ice stream developed late during deglaciation, cr

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