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Journal articles on the topic 'Lake Champlain Basin Program'

Author: Grafiati

Published: 4 June 2021

Last updated: 29 July 2025

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1

Stickney, Michaela, Colleen Hickey, and Roland Hoerr. "Lake Champlain Basin Program: Working together today for tomorrow." Lakes and Reservoirs: Research and Management 6, no. 3 (2001): 217–23. http://dx.doi.org/10.1046/j.1440-1770.2001.00150.x.

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2

Young, Bradley, BJ Allaire, and Stephen Smith. "Achieving Sea Lamprey Control in Lake Champlain." Fishes 6, no. 1 (2021): 2. http://dx.doi.org/10.3390/fishes6010002.

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The control of parasitic sea lamprey in Lake Champlain has been a necessary component of its fishery restoration and recovery goals for 30 years. While adopting the approach of the larger and established sea lamprey control program of the Laurentian Great Lakes, local differences emerged that shifted management focus and effort as the program evolved. Increased investment in lamprey assessment and monitoring revealed under-estimations of population density and distribution in the basin, where insufficient control efforts went unnoticed. As control efforts improved in response to a better under

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3

Meals, D. W. "Water quality response to riparian restoration in an agricultural watershed in Vermont, USA." Water Science and Technology 43, no. 5 (2001): 175–82. http://dx.doi.org/10.2166/wst.2001.0280.

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Achievement of management goals for Lake Champlain (Vermont/New York, USA and Quebec, Canada) will require reduction of agricultural phosphorus loads, the dominant nonpoint source in the Basin. Cost-effective phosphorus reduction strategies need reliable treatment techniques beyond basic cropland and waste management practices. The Lake Champlain Basin Agricultural Watersheds National Monitoring Program (NMP) Project evaluates the effectiveness of livestock exclusion, streambank protection, and riparian restoration practices in reducing concentrations and loads of nutrients, sediment, and bact

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Meals, D. W., and R. B. Hopkins. "Phosphorus reductions following riparian restoration in two agricultural watersheds in Vermont, USA." Water Science and Technology 45, no. 9 (2002): 51–60. http://dx.doi.org/10.2166/wst.2002.0203.

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Achievement of management goals for Lake Champlain (Vermont/New York, USA and Quebec, Canada) will require significant reductions of phosphorus (P) loads from agriculture, the dominant diffuse source in the basin. Cost-effective P reduction strategies must be based on reliable treatment techniques beyond basic erosion control and animal waste storage practices. The Lake Champlain Basin Agricultural Watersheds National Monitoring Program (NMP) Project evaluates the effectiveness of low-cost livestock exclusion, streambank protection, and riparian restoration practices in reducing concentrations

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5

Meals, Donald W., and Lenore F. Budd. "LAKE CHAMPLAIN BASIN NONPOINT SOURCE PHOSPHORUS ASSESSMENT." Journal of the American Water Resources Association 34, no. 2 (1998): 251–65. http://dx.doi.org/10.1111/j.1752-1688.1998.tb04132.x.

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6

Parent, Michel, and Serge Occhietti. "Late Wisconsinan Deglaciation and Champlain Sea Invasion in the St. Lawrence Valley, Québec." Géographie physique et Quaternaire 42, no. 3 (2007): 215–46. http://dx.doi.org/10.7202/032734ar.

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ABSTRACT Champlain Sea history is directly linked to Late Wisconsinan deglacial episodes. Champlain Sea Phase I (Charlesbourg Phase) began in the Québec area at about 12.4 ka. It represented a western extension of the Goldthwait Sea between remnant Appalachian ice masses and the Laurentide Ice Sheet. Further south, at about the same time, in the Appalachian uplands and piedmont, high-level glacial lakes were impounded by the ice-front during glacial retreat toward NNW: lakes Vermont, Memphrémagog and Mégantic. Lowlands of the Upper St. Lawrence and Lake Champlain valleys were progressively deg

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7

Howe, Eric A., J. Ellen Marsden, and Wayne Bouffard. "Movement of Sea Lamprey in the Lake Champlain Basin." Journal of Great Lakes Research 32, no. 4 (2006): 776. http://dx.doi.org/10.3394/0380-1330(2006)32[776:moslit]2.0.co;2.

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8

Trescott, Adam, Elizabeth Isenstein, and Mi-Hyun Park. "Remote sensing of cyanobacterial blooms in Lake Champlain, USA." Water Supply 13, no. 5 (2013): 1402–9. http://dx.doi.org/10.2166/ws.2013.114.

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The objective of this study was to develop cyanobacteria remote sensing models using Landsat 7 Enhanced Thematic Mapper Plus (ETM+) as an alternative to shipboard monitoring efforts in Lake Champlain. The approach allowed for estimation of cyanobacteria directly from satellite images, calibrated and validated with 4 years of in situ monitoring data from Lake Champlain's Long-Term Water Quality and Biological Monitoring Program (LTMP). The resulting stepwise regression model was applied to entire satellite images to provide distribution of cyanobacteria throughout the surface waters of Lake Cha

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9

Cutter, Zachary A., Timothy B. Mihuc, and Luke W. Myers. "Invasion of Bythotrephes longimanus and Cercopagis pengoi in Lake Champlain: Impacts on the Native Zooplankton Community." Diversity 15, no. 11 (2023): 1112. http://dx.doi.org/10.3390/d15111112.

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The zooplankton community of Lake Champlain has been altered over the past decade due to the introduction of two predatory zooplankton species. Bythotrephes longimanus Leydig, 1860 was first detected in Lake Champlain in August 2014, and Cercopagis pengoi (Ostroumov, 1891) was detected in August 2018. Monitoring for both invasive species at 15 lake sites using whole water tow sampling has been ongoing since 2010 with no detection of either species until 2014. Utilizing data from the Lake Champlain long-term monitoring program, we assessed pre- and post-invasion population dynamics of both inva

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10

Bitterman, Patrick, and Christopher Koliba. "Engagement in water governance action situations in the Lake Champlain Basin." PLOS ONE 18, no. 3 (2023): e0282797. http://dx.doi.org/10.1371/journal.pone.0282797.

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Water quality governance encompasses multiple “wicked” interacting problems that manifest within social-ecological systems. Concerned governments, institutions, and actors concerned with addressing these issues must wrestle with complex systems that span time, space, and scale. This complexity of connected systems requires the participation of multiple actors across political boundaries, problem areas, and hydrologic domains. In Lake Champlain (US), frequent cyanobacteria blooms negatively affect property values, recreational activities, and public infrastructure, in addition to their impacts

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11

Rayburn, John A., Thomas M. Cronin, David A. Franzi, Peter L. K. Knuepfer, and Debra A. Willard. "Timing and duration of North American glacial lake discharges and the Younger Dryas climate reversal." Quaternary Research 75, no. 3 (2011): 541–51. http://dx.doi.org/10.1016/j.yqres.2011.02.004.

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AbstractRadiocarbon-dated sediment cores from the Champlain Valley (northeastern USA) contain stratigraphic and micropaleontologic evidence for multiple, high-magnitude, freshwater discharges from North American proglacial lakes to the North Atlantic. Of particular interest are two large, closely spaced outflows that entered the North Atlantic Ocean via the St. Lawrence estuary about 13,200–12,900 cal yr BP, near the beginning of the Younger Dryas cold event. We estimate from varve chronology, sedimentation rates and proglacial lake volumes that the duration of the first outflow was less than

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12

Guilbert, Justin, Brian Beckage, Jonathan M. Winter, Radley M. Horton, Timothy Perkins, and Arne Bomblies. "Impacts of Projected Climate Change over the Lake Champlain Basin in Vermont." Journal of Applied Meteorology and Climatology 53, no. 8 (2014): 1861–75. http://dx.doi.org/10.1175/jamc-d-13-0338.1.

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AbstractThe Lake Champlain basin is a critical ecological and socioeconomic resource of the northeastern United States and southern Quebec, Canada. While general circulation models (GCMs) provide an overview of climate change in the region, they lack the spatial and temporal resolution necessary to fully anticipate the effects of rising global temperatures associated with increasing greenhouse gas concentrations. Observed trends in precipitation and temperature were assessed across the Lake Champlain basin to bridge the gap between global climate change and local impacts. Future shifts in prec

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13

L. T. Ghebremichael, T. L. Veith, and M. C. Watzin. "Determination of Critical Source Areas for Phosphorus Loss: Lake Champlain Basin, Vermont." Transactions of the ASABE 53, no. 5 (2010): 1595–604. http://dx.doi.org/10.13031/2013.34898.

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14

D’Aloia, Cassidy C., Christina B. Azodi, Sallie P. Sheldon, Stephen C. Trombulak, and William R. Ardren. "Genetic models reveal historical patterns of sea lamprey population fluctuations within Lake Champlain." PeerJ 3 (October 29, 2015): e1369. http://dx.doi.org/10.7717/peerj.1369.

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The origin of sea lamprey (Petromyzon marinus) in Lake Champlain has been heavily debated over the past decade. Given the lack of historical documentation, two competing hypotheses have emerged in the literature. First, it has been argued that the relatively recent population size increase and concomitant rise in wounding rates on prey populations are indicative of an invasive population that entered the lake through the Champlain Canal. Second, recent genetic evidence suggests a post-glacial colonization at the end of the Pleistocene, approximately 11,000 years ago. One limitation to resolvin

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15

Richard, Pierre J. H., and Serge Occhietti. "14C chronology for ice retreat and inception of Champlain Sea in the St. Lawrence Lowlands, Canada." Quaternary Research 63, no. 3 (2005): 353–58. http://dx.doi.org/10.1016/j.yqres.2005.02.003.

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AMS radiocarbon cross-dating of plant debris and marine shells trapped in a lake basin on Mount St. Hilaire (Québec, Canada) provides a direct assessment of a reservoir effect totaling ca. 1800 14C years during the early stage of Champlain Sea. Pollen-based extrapolation of bottommost ages on terrestrial plant macrofossils in sediments of this lake, and of another lake nearby support an estimate of 11,100 ± 100 14C yr B.P. for marine invasion in the Central St. Lawrence River Lowlands. Results indicate a 400–1000 years younger regional chronology of ice retreat, now congruent with the one infe

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16

Ishee, Eulaila R., Donald S. Ross, Kerrie M. Garvey, Rebecca R. Bourgault, and Charlotte R. Ford. "Phosphorus Characterization and Contribution from Eroding Streambank Soils of Vermont's Lake Champlain Basin." Journal of Environmental Quality 44, no. 6 (2015): 1745–53. http://dx.doi.org/10.2134/jeq2015.02.0108.

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17

Eisenhower, Marc D., and Donna L. Parrish. "Double-Crested Cormorant and Fish Interactions in a Shallow Basin of Lake Champlain." Waterbirds 32, no. 3 (2009): 388–99. http://dx.doi.org/10.1675/063.032.0303.

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18

Gao, Ning, Amy E. Gildemeister, Kira Krumhansl, et al. "Sources of Fine Particulate Species in Ambient Air over Lake Champlain Basin, VT." Journal of the Air & Waste Management Association 56, no. 11 (2006): 1607–20. http://dx.doi.org/10.1080/10473289.2006.10464557.

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19

Soto-Adames, Felipe. "New species of springtails in the Proisotoma genus complex from Vermont and New York, USA with descriptive notes on Ballistura alpa Christiansen & Bellinger 1980 (Hexapoda, Collembola, Isotomidae)." ZooKeys 147 (November 16, 2011): 19–37. https://doi.org/10.3897/zookeys.147.2093.

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Three new species of isotomid springtails are described from the Lake Champlain Basin (Vermont and New York, USA), Lake Willoughby and Greater Averril Pond in Vermont. <i>Subisotoma</i> <i>joycei</i> <strong>sp. n.</strong> and <i>Scutisotoma champi</i> <strong>sp. n.</strong> were collected in sandy beaches whereas <i>Ballistura rossi</i> <strong>sp. n.</strong> was found only in a constructed wetland built and managed by the University of Vermont. <i>Scutisotoma champi</i> <strong>sp. n.</strong> was found in Lakes Champlain and Willoughby, and Greater Averril Pond and is probably present in

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20

Spett, Emma J. "Building Resilience in Trans-boundary Social-Ecological Systems: Adaptive Governance in the Lake Champlain Richelieu River Basin." Complexity, Governance & Networks 5, no. 1 (2019): 65. http://dx.doi.org/10.20377/cgn-81.

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Addressing the management of water bodies that cross political, cultural, and ecological boundaries entails working with a level of complexity that requires creative, adaptive management strategies that build resilience throughout the system and allow for increased capacity in the face of disturbance. To characterize the extent to which such complexity can be managed, this paper explores the application of the social-ecological systems framework, proposed by Brian Walker and David Salt, for assessing and managing resilience. Elements of this framework will be utilized with respect to the Lake

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21

Lewis, C. F. M., and T. W. Anderson. "A younger glacial Lake Iroquois in the Lake Ontario basin, Ontario and New York: re-examination of pollen stratigraphy and radiocarbon dating." Canadian Journal of Earth Sciences 57, no. 4 (2020): 453–63. http://dx.doi.org/10.1139/cjes-2019-0076.

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Revision of palynochronologic and radiocarbon age estimates for the termination of glacial Lake Iroquois, mainly based on a currently accepted younger determination of the key Picea–Pinus pollen transition, shows agreement with recently established constraints for this late glacial event in the Lake Ontario basin at 13 000 cal years BP. The date of emergence or isolation of small lake basins reflects the termination of inundation by glacial lake waters. The increasing upward presence of plant detritus and the onset of organic sedimentation marks the isolation level in the sediments of a small

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22

Parent, Michel, and Serge Occhietti. "Late Wisconsinan deglaciation and glacial lake development in the Appalachians of southeastern Québec." Géographie physique et Quaternaire 53, no. 1 (2002): 117–35. http://dx.doi.org/10.7202/004859ar.

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Abstract Late Wisconsinan deglaciation in southeastern Québec was preceded by a northward ice-flow reversal that was recorded in the northeastern part of the region. The reversal event was generated by flow convergence toward the St. Lawrence Ice Stream, a northeastward-flowing ice stream which formed in the St. Lawrence estuary prior to 13 000 years BP and lasted until at least 12 400 years BP. In the Bois-Francs uplands, the flow reversal event led to the formation of a semi-detached ice mass that underwent widespread stagnation and downwasting. In the southwestern region, northward retreat

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23

Normandeau, Alexandre, Patrick Lajeunesse, Annie-Pier Trottier, Antoine G. Poiré, and Reinhard Pienitz. "Sedimentation in isolated glaciomarine embayments during glacio-isostatically induced relative sea level fall (northern Champlain Sea basin)." Canadian Journal of Earth Sciences 54, no. 10 (2017): 1049–62. http://dx.doi.org/10.1139/cjes-2017-0002.

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The nature of glaciomarine sediments deposited during ice margin retreat can vary according to physiographic setting and relative sea level fluctuations. To understand the effects of these two parameters on sedimentation, we analyzed the sediment records of four lakes located within former isolated glaciomarine embayments of the northern Champlain Sea basin. These lakes were initially inundated by marine water of the Champlain Sea, following deglaciation, and have subsequently experienced basin isolation owing to glacio-isostatic rebound. Three of these lakes reveal a common litho- and acousti

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24

Young, E. O., D. S. Ross, C. Alves, and T. Villars. "Soil and landscape influences on native riparian phosphorus availability in three Lake Champlain Basin stream corridors." Journal of Soil and Water Conservation 67, no. 1 (2012): 1–7. http://dx.doi.org/10.2489/jswc.67.1.1.

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25

Sullivan, S. Mažeika P., Mary C. Watzin, and William S. Keeton. "A riverscape perspective on habitat associations among riverine bird assemblages in the Lake Champlain Basin, USA." Landscape Ecology 22, no. 8 (2007): 1169–86. http://dx.doi.org/10.1007/s10980-007-9097-3.

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26

Burke, J., M. Hoyer, G. Keeler, and T. Scherbatskoy. "Wet deposition of mercury and ambient mercury concentrations at a site in the Lake Champlain basin." Water, Air, & Soil Pollution 80, no. 1-4 (1995): 353–62. http://dx.doi.org/10.1007/bf01189685.

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27

Naldrett, Dana L. "The Late Glacial-Early Glaciomarine Transition in the Ottawa Valley: Evidence for a Glacial Lake?" Géographie physique et Quaternaire 42, no. 2 (2007): 171–79. http://dx.doi.org/10.7202/032723ar.

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ABSTRACT Rhythmites overlying either cross-bedded sand or diamicton are found throughout the Ottawa Valley. Previously thought to be restricted glacial lake sediments, they are now known to be widespread, and represent a large proglacial lake which preceded the Champlain Sea. The rhythmites consist of thin silt and clay laminae which fine upwards and contain slump, flame, shear (ice-contact?) and fluid escape structures. Ice-rafted material is common. The ostracode Candona cf. C. subtriangulata occurs in low numbers and indicates a freshwater body with depth of approximately 200 m. The alterna

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28

Huang, Huanping, Jonathan M. Winter, Erich C. Osterberg, et al. "Simulating precipitation and temperature in the Lake Champlain basin using a regional climate model: limitations and uncertainties." Climate Dynamics 54, no. 1-2 (2019): 69–84. http://dx.doi.org/10.1007/s00382-019-04987-8.

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29

Ross, Martin, Michel Parent, Beatriz Benjumea, and James Hunter. "The late Quaternary stratigraphic record northwest of Montréal: regional ice-sheet dynamics, ice-stream activity, and early deglacial events." Canadian Journal of Earth Sciences 43, no. 4 (2006): 461–85. http://dx.doi.org/10.1139/e05-118.

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The Quaternary sediments of previously unstudied buried valleys and sections near Montréal are analyzed and other sites are revisited to further develop the stratigraphic framework of the St. Lawrence Lowland and to establish regional glacial and deglacial models. The southwest-trending buried valleys were investigated by stratigraphic drilling and high-resolution seismic profiling. The Quaternary succession consists, from base to top, of proximal glaciolacustrine sediments, two superposed till sheets (Argenteuil and Oka tills) of inferred Late Wisconsinan age, and Champlain Sea sediments. The

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30

Weller, Christine M., Mary C. Watzin, and Deane Wang. "Role of wetlands in reducing phosphorus loading to surface water in eight watersheds in the Lake Champlain Basin." Environmental Management 20, no. 5 (1996): 731–39. http://dx.doi.org/10.1007/bf01204144.

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31

Mohammed, Ibrahim Nourein, Arne Bomblies, and Beverley C. Wemple. "The use of CMIP5 data to simulate climate change impacts on flow regime within the Lake Champlain Basin." Journal of Hydrology: Regional Studies 3 (March 2015): 160–86. http://dx.doi.org/10.1016/j.ejrh.2015.01.002.

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32

Chen, Meiqiu, Xiaohua Wei, Hongsheng Huang, and Tiangui Lü. "Poyang Lake basin: a successful, large-scale integrated basin management model for developing countries." Water Science and Technology 63, no. 9 (2011): 1899–905. http://dx.doi.org/10.2166/wst.2011.413.

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Protection of water environment while developing socio-economy is a challenging task for lake regions of many developing countries. Poyang Lake is the largest fresh water lake in China, with its total drainage area of 160,000 km2. In spite of rapid development of socio-economy in Poyang Lake region in the past several decades, water in Poyang Lake is of good quality and is known as the “last pot of clear water” of the Yangtze River Basin in China. In this paper, the reasons of “last pot of clear water” of Poyang Lake were analysed to demonstrate how economic development and environmental prote

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33

Аветисян, Горик Д., Вардуи Г. Маргарян, Левон В. Азизян, Оганнес Я. Саядян та Наталья Л. Фролова. "АНАЛИЗ ИЗМЕНЕНИЯ ЛЕСНОГО ПОКРОВА В БАССЕЙНАХ РЕК, ВПАДАЮЩИХ В ОЗЕРО СЕВАН". Proceedings of the YSU C: Geological and Geographical Sciences 57, № 3 (261) (2023): 157–62. http://dx.doi.org/10.46991/pysu:c.2023.57.3.157.

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The paper presents spatial and temporal changes and the current situation of forests in the Lake Sevan basin. The general physico-geographic characteristics of the Sevan basin, the detailed characteristics of the forests in the Sevan lake basin, the natural and anthropogenic changes are presented, and an analysis of the cause and effect relationships of these changes is carried out. The changes in the forest cover and the negative aquatic biological processes that appeared in the lake’s ecosystem as a result of the program of cutting down the water-covered and subject to water-covering forests

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Galois, Patrick, and Martin Ouellet. "Traumatic Injuries in Eastern Spiny Softshell Turtles (Apalone spinifera) Due to Recreational Activities in the Northern Lake Champlain Basin." Chelonian Conservation and Biology 6, no. 2 (2007): 288. http://dx.doi.org/10.2744/1071-8443(2007)6[288:tiiess]2.0.co;2.

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35

Modley, Margaret D. "Aquatic invasive species rapid response planning partnerships in the Lake Champlain basin: Bridging international, political, social, and economic gaps." Water SA 34, no. 4 (2019): 476. http://dx.doi.org/10.4314/wsa.v34i4.183659.

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36

Bitterman, Patrick, and Christopher J. Koliba. "Modeling Alternative Collaborative Governance Network Designs: An Agent-Based Model of Water Governance in the Lake Champlain Basin, Vermont." Journal of Public Administration Research and Theory 30, no. 4 (2020): 636–55. http://dx.doi.org/10.1093/jopart/muaa013.

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Abstract With the widespread use of collaborative governance mechanisms for mitigating water pollution, an opportunity exists to test alternative institutional designs based on collaborative governance theory using computer simulation models, particularly when there is a clear relationship between governance networks, observable resource allocation decisions, and measurable outcomes. This is especially the case for wicked problems like nonpoint source water pollution where there are compelling questions regarding how best to design policies, allocate funds, and build administrative capacity to

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37

Sparacino, Holden, Kristine F. Stepenuck, and Stephanie E. Hurley. "Understanding reduced salt practices used by commercial snow removal businesses in the Lake Champlain Basin: A mixed methods analysis." Journal of Environmental Management 351 (February 2024): 119957. http://dx.doi.org/10.1016/j.jenvman.2023.119957.

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38

Klaiber, Laura B., Stephen R. Kramer, and Eric O. Young. "Impacts of Tile Drainage on Phosphorus Losses from Edge-of-Field Plots in the Lake Champlain Basin of New York." Water 12, no. 2 (2020): 328. http://dx.doi.org/10.3390/w12020328.

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Quantifying the influence of tile drainage on phosphorus (P) transport risk is important where eutrophication is a concern. The objective of this study was to compare P exports from tile-drained (TD) and undrained (UD) edge-of-field plots in northern New York. Four plots (46 by 23 m) were established with tile drainage and surface runoff collection during 2012–2013. Grass sod was terminated in fall 2013 and corn (Zea mays L.) for silage was grown in 2014 and 2015. Runoff, total phosphorus (TP), soluble reactive phosphorus (SRP), and total suspended solids (TSS) exports were measured from April

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39

Howe, Eric A., J. Ellen Marsden, Therese M. Donovan, and Roland H. Lamberson. "A life cycle approach to modeling sea lamprey population dynamics in the Lake Champlain basin to evaluate alternative control strategies." Journal of Great Lakes Research 38 (January 2012): 101–14. http://dx.doi.org/10.1016/j.jglr.2011.11.002.

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40

Cianfrani, Christina M., S. Mažeika P. Sullivan, W. Cully Hession, and Mary C. Watzin. "A MULTITAXONOMIC APPROACH TO UNDERSTANDING LOCAL- VERSUS WATERSHED-SCALE INFLUENCES ON STREAM BIOTA IN THE LAKE CHAMPLAIN BASIN, VERMONT, USA." River Research and Applications 28, no. 7 (2010): 973–88. http://dx.doi.org/10.1002/rra.1470.

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41

Yang, Qi Yong, Xin Hua Zhang, and Zhong Wei Wu. "Prevention and Control of Water Pollution Based on Ecosystem Management (EM): A Case Study of Poyang Lake." Applied Mechanics and Materials 295-298 (February 2013): 1575–79. http://dx.doi.org/10.4028/www.scientific.net/amm.295-298.1575.

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The water quality monitoring revealed that the water quality in Poyang Lake is increasely degenerating in the past several years and the deterioration reasons were analyzed. The increasingly serious water pollution indicated that there were inherent drawbacks in current environmental management system of China. Therefore, the typical models of water pollution prevention and control in developed countries and China were researched. The explorations of water pollution prevention and control based on ecosystem management for Poyang Lake were reviewed, especially the practice of Mountain-River-Lak

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42

Jerde, Christopher L., W. Lindsay Chadderton, Andrew R. Mahon, et al. "Detection of Asian carp DNA as part of a Great Lakes basin-wide surveillance program." Canadian Journal of Fisheries and Aquatic Sciences 70, no. 4 (2013): 522–26. http://dx.doi.org/10.1139/cjfas-2012-0478.

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Environmental DNA (eDNA) is a sensitive technique for early detection of rare species, including bighead (Hypophthalmichthys nobilis) and silver (Hypophthalmichthys molitrix) carp, which are incipient invaders of the Great Lakes. Since 2009, 2822 samples have been collected from the Great Lakes basin to delimit the extent of Asian carp incursions. Samples collected in the Chicago Area Waterway System and in the western basin of Lake Erie indicate the presence of Asian carp DNA in the Great Lakes. These positive eDNA detections are within 6 and 4 km from where bighead carps were recovered in La

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43

Wang, Yiming, Zengxin Zhang, and Xi Chen. "The Dominant Driving Force of Forest Change in the Yangtze River Basin, China: Climate Variation or Anthropogenic Activities?" Forests 13, no. 1 (2022): 82. http://dx.doi.org/10.3390/f13010082.

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Under the combined effect of climate variations and anthropogenic activities, the forest ecosystem in the Yangtze River Basin (YRB) has experienced dramatic changes in recent decades. Quantifying their relative contributions can provide a valuable reference for forest management and ecological sustainability. In this study, we selected net primary productivity (NPP) as an indicator to investigate forest variations. Meanwhile, we established eight scenarios based on the slope coefficients of the potential NPP (PNPP) and actual NPP (ANPP), and human-induced NPP (HNPP) to quantify the contributio

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Aga, Alemu, Bayou Chane, and Assefa Melesse. "Soil Erosion Modelling and Risk Assessment in Data Scarce Rift Valley Lake Regions, Ethiopia." Water 10, no. 11 (2018): 1684. http://dx.doi.org/10.3390/w10111684.

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To prolong the useful life of lakes and reservoirs, prioritizing watersheds by severity and risk of soil erosion is an essential index to develop sound sediment management plans. This study aims to predict soil erosion risk and sediment yield using Soil and Water Assessment Tool (SWAT) model in Lake Ziway basin, Ethiopia, and the model result is validated with lake bathymetric changes. The SUFI-2 program was applied for a model calibration and the performance of the model was assessed. The catchment prioritization study indicated that some sub-basins having the same soil type and land use but

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Coakley, John P., and Paul F. Karrow. "Reconstruction of post-Iroquois shoreline evolution in western Lake Ontario." Canadian Journal of Earth Sciences 31, no. 11 (1994): 1618–29. http://dx.doi.org/10.1139/e94-143.

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When Lake Iroquois drained between 11.7 and 11.4 ka BP, lake level in the Ontario basin fell from a high of more than 40 m above present lake level to a minimum close to the then-existing sea level, which was approximately 40 m below present sea level. Since that time, lake level has been rising at an exponentially decreasing rate in the western portion of the basin as a result of postglacial and neotectonic uplift of the outlet near Kingston, at the eastern end. The published lake level history has been combined with other less well-known parameters (the post-Iroquois regional topography, ero

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Boyd, PhD, Ezra, Joao F. Pereira, PhD, Gabriel Retana, PhD, Andy Baker, MS, John Lopez, PhD, and Alex McCorquodale, PhD. "An oil spill surveillance program for Lake Pontchartrain." Journal of Emergency Management 11, no. 6 (2013): 447. http://dx.doi.org/10.5055/jem.2013.0157.

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This article describes an oil spill surveillance strategy implemented in response to BP’s 2010 MC252 oil well blowout in the Gulf of Mexico. A three-pronged strategy consisted of Geographic Information System (GIS) monitoring of the surface slick, hydrodynamic modeling of the potential movement of the slick within the Basin, and weekly field reconnaissance. Our analysis was completed in near real time during the event and the results and predictions helped local responders minimize oiling impacts in Lake Pontchartrain. No prior planning was undertaken before this crisis response, and this arti

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Russell, James M., Satria Bijaksana, Hendrik Vogel, et al. "The Towuti Drilling Project: paleoenvironments, biological evolution, and geomicrobiology of a tropical Pacific lake." Scientific Drilling 21 (July 27, 2016): 29–40. http://dx.doi.org/10.5194/sd-21-29-2016.

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Abstract. The Towuti Drilling Project (TDP) is an international research program, whose goal is to understand long-term environmental and climatic change in the tropical western Pacific, the impacts of geological and environmental changes on the biological evolution of aquatic taxa, and the geomicrobiology and biogeochemistry of metal-rich, ultramafic-hosted lake sediments through the scientific drilling of Lake Towuti, southern Sulawesi, Indonesia. Lake Towuti is a large tectonic lake at the downstream end of the Malili lake system, a chain of five highly biodiverse lakes that are among the o

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Prepas, E. E., B. Pinel-Alloul, D. Planas, G. Méthot, S. Paquet, and S. Reedyk. "Forest harvest impacts on water quality and aquatic biota on the Boreal Plain: introduction to the TROLS lake program." Canadian Journal of Fisheries and Aquatic Sciences 58, no. 2 (2001): 421–36. http://dx.doi.org/10.1139/f00-259.

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Eleven headwater lakes in Alberta's Boreal Plain were monitored for nutrients and plankton 2 years before and 2 years after variable watershed harvesting (harvesting mean 15%, range 0-35%). After harvesting, variations in annual precipitation resulted in lake water residence times that differed by an order of magnitude from one year to the next. During the first posttreatment year, total phosphorus concentrations increased (overall 40%) in most lakes; however, response was most consistent in lakes that were shallow and the water column mixed or weakly thermally stratified. Chlorophyll a, cyano

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Hovhannisyan, R. L., M. Ya Rukhkyan, L. D. Harutyunova, M. Z. Magomedova, and P. D. Magomedova. "The fish helminth fauna of Lake Sevan during a period of water level change." South of Russia: ecology, development 18, no. 3 (2023): 50–59. http://dx.doi.org/10.18470/1992-1098-2023-3-50-59.

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Aim. The aim of the work is to study the fish helminth fauna of Lake Sevan basin.Material and Methods. Fish helminths and molluscs were collected from the Lake Sevan basin. A total of 214 specimens of fish were studied. The collection, cameral processing and determination of the material was carried out according to generally accepted methods. Statistical processing of the material was carried out using the BioStat 2009 computer program. 124 specimens of molluscs were examined from the littoral of the Lake Sevan. The collection and identification of molluscs was carried out according to genera

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Brown, Erik T., Margarita Caballero, Enrique Cabral Cano, et al. "Scientific drilling of Lake Chalco, Basin of Mexico (MexiDrill)." Scientific Drilling 26 (December 2, 2019): 1–15. http://dx.doi.org/10.5194/sd-26-1-2019.

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Abstract. The primary scientific objective of MexiDrill, the Basin of Mexico Drilling Program, is development of a continuous, high-resolution ∼400 kyr lacustrine record of tropical North American environmental change. The field location, in the densely populated, water-stressed Mexico City region gives this record particular societal relevance. A detailed paleoclimate reconstruction from central Mexico will enhance our understanding of long-term natural climate variability in the North American tropics and its relationship with changes at higher latitudes. The site lies at the northern margin

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