Geophys. Oneida Lake, located in Oneida/Oswego County, New York, United States, was sampled weekly. 3, 6570 (2012). Loch Leven, situated in Perth and Kinross, Scotland, United Kingdom, was sampled biweekly, from the subsurface at an approximate depth of 0.01m. The samples were obtained from the Reed Bower sampling site which is an open water site that has a water depth similar to the average depth of the lake and remains accessible in most weather conditions. 54, 22832297 (2009). Water-Year The town of Lake Santeetlah is located in central Graham County at 352149N 835152W (35.363578, -83.864367), [6] on a peninsula on the northern side of Lake Santeetlah, a reservoir on the Cheoah River, a northward-flowing tributary of the Little Tennessee River. Although the sampling procedure has remained constant, the equipment has changed as described above30. 162, 445464 (2005). Page Contact Information: North Carolina Water Data Maintainer J. Geophys. Robbinsville was not incorporated until 1893, and it had only 200 residents in 1915. This folder contains text files that explain any extrapolation performed as part of the summer mean calculations, including the parabolic equation used for the extrapolation, the time period covered, and the R2 fit to the data. Snucins, E. & Gunn, J. Interannual variation in the thermal structure of clear and colored lakes. Lake Tarawera, located in North Island, New Zealand, was sampled monthly from the subsurface (20cm) to the bottom at 1m intervals. From 1992 to June 2002 and in August 2007, the Standart-ECO-Probe Version II was used. Lake surface temperatures can directly or indirectly influence physical, chemical, and biological processes in a lake, including the temperature of the photosynthetic zone4, water-column stability, lake primary productivity5, fish species range shifts3, and species interactions6. Water temperatures from Cannonsville, Pepacton, Rondout, Neversink, Schoharie, Ashokan East, Ashokan West, and Kensico, in New York, United States were generally sampled monthly (although weekly in some years). CAS Residents can now live both. Lett. Lake Rotorua, located in North Island, New Zealand, was sampled monthly at depths of 01 and 18m. The samples were obtained from the southeast part of the lake. We defined the maximum gap as the maximum of all gaps for a single year. 12879 lakes / reservoirs. Cite this article. From 2003 to 2005 and in 2007, the CTD 90 multiparameter probe was used. Sign up for the Nature Briefing newsletter what matters in science, free to your inbox daily. U.S. Geological Survey Am. Additional details on the accuracy of the records can be obtained by contacting the USGS South Atlantic Water Science Center at gs-w-nc_nwisweb_data_inquiries@usgs.gov. Hydrobiologia 731, 3148 (2014). Specialty Inn. hydrologic This article about a location in Graham County, North Carolina is a stub. Rsner, R., Mller-Navarra, D. C. & Zorita, E. Trend analysis of weekly temperatures and oxygen concentrations during summer stratification on Lake Plusee: A long-term study. Each site was sampled from the surface (1m) to the bottom. (2013). All were sampled weekly except Mount Bold, South Para, and Tod which were sampled fortnightly. Sharma, S., Gray, D., Read, J. et al. From 19602004, a paper chart recorder with a mercury thermometer was used. Enter dates to see prices. available For Sale: Lot/Land for sale,$295,000, 0.13 Acre, $2,269,231/Acre at Tbd Lakeside Trail, Robbinsville, NC 28711 Increases in the amount of incoming solar radiation increase average lake temperatures14. Gage-height records are generally good. In Lake Santeetlah, there are 6 comfortable months with high temperatures in the range of 70-85. Recording and transmission times may be more frequent during critical events. Google Scholar. When this routine was used, we made a notation in the log file describing if extrapolation was used for the beginning and/or end period and we included the equation of the curve (See Data Records). Am. water Russian Acad. 45, 10581066 (2000). Water temperatures were recorded in the morning with a handheld YSI or Hydrolab thermistor. WATER LEVEL. Fourth, on a small subset of the data, Schneider and Hook11 used high-frequency buoy measurements to conduct a more direct comparison of water temperature trends that eliminated differences in timing and observation frequency. Biol. The histograms allowed us to identify outliers while the maps provided geographic plots that could be examined for unusual observations or spatial patterns that might indicate technical errors during the assembly of the dataset. Solar radiation is a key component of lake heat budgets13. ADS Stat. Sampling was carried out with automated thermistors, located at 1m intervals from the top to the bottom of the lake. Limnol. For & Keller, W. B. Africa Eurasia North America Oceania South America lake reservoir, Machine-accessible metadata file describing the reported data (ISA-Tab format). Sapna Sharma, Derek K Gray, Jordan S Read and Catherine M OReilly: Joint first authors, Department of Biology, York University, Toronto, M3J 1P3, Ontario, Canada, Sapna Sharma,Anam Qudrat&Samantha Stefanoff, California University of Pennsylvania, California, 15419, Pennsylvania, USA, U.S. Geological Survey, Center for Integrated Data Analytics, Middleton, 53562, Wisconsin, USA, Department of Geography-Geology, Illinois State University, Normal, 61790, Illinois, USA, NILUNorwegian Institute for Air Research, Kjeller, 2027, Norway, Center for Limnology, University of Wisconsin-Madison, Madison, 53706, Wisconsin, USA, Corinna Gries,Peter B McIntyre&Benjamin M Kraemer, Center for Environmental Research, Education and Outreach, Washington State University, Pullman, 99164, Washington, USA, NASA Jet Propulsion Laboratory, California Institute of Technology, California, 91109, USA, LimnoTech, Ann Arbor, 48108, Michigan, USA, Department of Water Resources and Drinking Water, Eawag (Swiss Federal Institute of Aquatic Science and Technology), Duebendorf, CH-8600, Switzerland, Leibniz-Institute of Freshwater Ecology and Inland Fisheries, Berlin, D-12587, Germany, Environmental Research Institute, University of Waikato, 3240, New Zealand, French National Institute for Agricultural Research (INRA), Station dhydrobiologie lacustre (UMR CARRTEL), Thonon les Bains, 74200, France, University of Helsinki, Lammi Biological Station, Helsinki, FI-16900, Finland, Large Lakes Observatory, University of Minnesota Duluth, Duluth, 55812, Minnesota, USA, Vale Living with Lakes Centre, Ontario Ministry of the Environment and Climate Change, Sudbury, P3E 2C6, Ontario, Canada, U.S. Geological Survey Fort Collins Science Center, Colorado State University, Fort Collins, 80523, Colorado, USA, Water Research Centre, School of Biological Sciences, The University of Adelaide, Adelaide, 5005, Australia, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 210008, China, Australian Water Quality Center, SA Water Corporation, 5001, Australia, Research Institute for Limnology, University Innsbruck, Mondsee, A-5310, Austria, Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York, Albany, 12222, New York, USA, Archbold Biological Station, Venus, 33960, Florida, USA, Fisheries Ecosystems Advisory Services, Marine Institute, Newport, Co. Mayo Ireland, Environmental Research Institute, University of Waikato, Hamilton, 3240, New Zealand, Florida Sea Grant and University of Florida Institute of Food and Agricultural Sciences, Gainesville, 32611, Florida, USA, Melbourne Water Corporation, Victoria, 3001, Australia, LUBW Landesanstalt fr Umwelt, Messungen und Naturschutz Baden-Wrttemberg, Institut fr Seenforschung, Langenargen, D-88045, Germany, Department of Natural Resources, Cornell University, Ithaca, 14853, New York, USA, International Institute of Sustainable DevelopmentExperimental Lakes Area, Winnipeg, R3B 2L6, Manitoba, Canada, Central Nebraska Public Power and Irrigation District, Holdredge, 68949, Nebraska, USA, Scientific Research Institute of Biology, Irkutsk State University, Irkutsk, 664003, Russia, U.S. Geological Survey Alaska Science Center, Anchorage, 99508, Alaska, USA, Institute of Agricultural and Environmental Sciences, Estonian University of Life Sciences Rannu, Estonia, 61117, Department of Experimental Limnology, Leibniz Institute of Freshwater Ecology & Inland Fisheries, Berlin, 12587, Germany, Wasserversorgung der Stadt Zurich (WVZ), Zurich, CH-8021, Switzerland, Lake Biwa Environmental Research Institute, Otsu, 520-0022, Shiga, Japan, Finnish Environment Institute, Helsinki, FI-00250, Finland, NOAA/Great Lakes Environmental Research Laboratory, Ann Arbor, 48108, Michigan, USA, Centre for Ecology and Hydrology, Bush Estate, Midlothian, EH260QB, Scotland, UK, Department of Ecology, Evolution and Marine Biology, University of California, Santa Barbara, 93106, California, USA, Department of Biology, University of Hamburg, Hamburg, 22609, Germany, Hydrology Laboratory, Limnology Institute, Russian Academy of Sciences, St Petersburg, 196105, Russian Federation, Centre for Limnology, Institute of Agricultural and Environmental Sciences, Estonian University of Life Sciences, Tartumaa, 61117, Estonia, Amt fur Abfall, Wasser, Energie und Luft, Kanton Zurich, Zurich, CH-8005, Switzerland, Institute of Coastal Research, Helmholtz-Zentrum Geesthacht, Geesthacht, 21502, Germany, Dorset Environmental Science Centre, Ontario Ministry of the Environment and Climate Change, Dorset, P0A 1E0, Ontario, Canada, Department of Earth Sciences, Royal Museum for Central Africa, Tervuren, 3080, Belgium, Israel Oceanographic and Limnological Research, The Lake Kinneret Limnological Laboratory, Migdal, 14950, Israel, National Research Council, Institute of Ecosystem Study, Verbania, 28922, Pallanza, Italy, IASMA Research and Innovation Centre, Istituto Agrario di S. Michele all'Adige, Fondazione E. Mach, S. Michele allAdige (Trento), 38010, Italy, Institute for Sustainable Cities, City University of New York, New York, 10065, USA, School of Aquatic and Fishery Sciences, University of Washington, Seattle, 98195, Washington, USA, UC Davis Tahoe Environmental Research Center, Incline Village, 95616, Nevada, USA, Sydney Catchment Authority, Penrith, 2750, NSW, Australia, Department of Biology, Universitat Konstanz, Konstanz, 78464, Germany, Department of Limnology and Biological Oceanography, University of Vienna, Vienna, A-1090, Austria, National Institute of Water and Atmospheric Research, Hamilton, 1010, New Zealand, Department of Biology, University of Eastern Finland, Kuopio, 70211, Finland, Department of Ecology and Genetics/Limnology, Uppsala University, Uppsala, 75236, Sweden, Department of Biology, Miami University, Oxford, 45056, Ohio, USA, You can also search for this author in every 40 rivers / canals. July is the hottest month for Lake Santeetlah with an average high temperature of 84.0, which ranks it as one of the coolest places in North Carolina. Pure water will remain neutral at 0C (pH is 7.47), 25C. Lake Valkea-Kotinen, situated in southern Finland, was sampled weekly, and water temperatures were measured at the surface and depths of 1, 2, 3, 4, 5 and 6m. Measurements were made in the deepest part of the lake (6.5m) in the morning between 10:00 and 11:00 using YSI probes for oxygen and temperature45. Recent studies have suggested significant warming of water temperatures in individual lakes across many different regions around the world. B.D., Stephanie E. Hampton and P.S. Call us (828) 369-0406 Get links to local marinas on Fontana Lake, Nantahala Lake, Lake Glenville, Lake Santeetlah, and Lake Junaluska (828) 369-0406 canvasmasters@yahoo.com Facebook 13588 total waterbodies. Generally, water temperatures tend to coincide with regional air temperatures, warming or cooling at similar rates to that of air temperatures10,11. The data are available in two comma delimited text files (Data Citation 1). The second table (Table 2), GLTCvalues.csv, contains the actual values and may be linked to the lake information via the siteID column. These sites were Kaskesniemi, Noljakansaaret, Pyhsaari, and Kokonluoto, with maximum depths of 38, 13, 53, and 65m (ref. We also calculated gap lengths, which were the intervals in days between sequential sampling times. Lake McConaughy is a regulated reservoir located near Ogallala, Nebraska, United States. Cataract was sampled fortnightly and, Cordeaux and Fitzroy were sampled monthly. choose The physical impact of the late 1980s climate regime shift on Swiss rivers and lakes. The time period when the sun is no more than 6 degrees below the horizon at either sunrise or sunset. Only lakes that exhibited at least a 1010km area of pure water surface without any islands or shorelines were selected, in order to make sure that there was no contamination by land surfaces. We compiled in situ surface water temperatures and corresponding lake geomorphology and climatic data from 151 lakes (Figure 1; Tables 1 and 2; Data Citation 1). While this approach allowed us to standardize the methodology used for calculating mean summer temperatures across our lakes, we were concerned that mean temperatures calculated for lakes with longer sampling intervals (e.g., one temperature measurement each week) would have more error than lakes with shorter sampling intervals (e.g., daily temperature measurements). Lett. The AVHRR series of satellite instruments has been measuring thermal infrared (TIR) radiation since the late 1970s. For this study, we used data from the version 5 product of AVHRR Pathfinder collection59. A global database of lake surface temperatures collected by in situ and satellite methods from 19852009. Data on water temperature were provided by the German Meteorological Service (DWD, 19581996) and the Institute of Freshwater Ecology and Inland Fisheries (IGB, including predecessor institutions, 19702011), respectively. Weyhenmeyer, G. A. Limnol. Data were collected at 25min intervals at multiple depths from the surface to the bottom in increments from less than 1m to approximately 5m; surface water measurements were made at 0.5m. Water temperatures were recorded using a Lake Diagnostic System (LDS) with PME thermistor chain typically moored at the deepest point in the reservoirs and close to the dam wall. Third, we compared trends from the in situ data for 19852009. (William V. Wood to Property Owner, April 28, 1999.) Many visitors enjoy the solitude of the lake even on the busiest of summer weekends. The median age was 61 years. Instrumentation measuring global cloud cover was rarely continuous during the full observational period of this study (19852009). [7] In 1939, the U.S. Forest Service purchased from Carolina Aluminum Company the land now occupied by the town of Lake Santeetlah. to Assoc. Limnol. reports Funding and other support for this project were provided by Amt fr Abfall, Wasser, Energie und Luft (AWEL), Canton of Zurich, Switzerland; Andrew W. Mellon Foundation; Austrian Academy of Sciences; Bay of Plenty Regional Council; Belgian Science Policy; Bristol Bay salmon processors; Central Nebraska Public Power and Irrigation District; Chinese Academy of Sciences; City of Seattle; City of Zurich Water Supply (WVZ); Comit intersyndical pour lassainissement du lac du Bourget (CISALB); Commission Internationale pour la Protection des Eaux du Lman (CIPEL), Cornell University Agricultural Experiment Station; Environmental Agency of the Veneto Region; European Union Central Europe Programme (Project EULAKES, 2CE243P3; Garda); Belgian Federal Science PolicyBelgium; Estonian Institute for Meteorology and Hydrology; Estonian Ministry of Education and Research; Estonian Science Foundation; Finland's Environmental Authorities; Finland State Budget; Finnish International Development Agency; Fish and Wildlife Service Landscape Conservation Cooperative; Food and Agriculture Organization of the United Nations; French National Institute for Agricultural Research (INRA), Gordon and Betty Moore Foundation; Government of Canada; Integrated Climate System Analysis and Prediction; International Commission for the Protection of Water between Italy and Switzerland (CIPAIS); Israeli Water Authority; Leibniz-Institute of Freshwater Ecology and Inland Fisheries; Long Term Ecological Research Italian network Southern Alpine lakes; Marine Institute (Ireland); Max-Planck Society; Ministry of Business, Innovation and Employment, New Zealand; National Aeronautics and Space Administration; National Sciences and Engineering Research Council; National Oceanic and Atmospheric Administration; National Park Service; National Science Foundation; Nebraska Game and Parks Commission; New York City Department of Environmental Protection; New York State Department of Environmental Conservation; Ontario Ministry of the Environment and Climate Change; Russian Academy of Sciences; Ministry of Education and Science of Russian Federation; Seqwater; State of Florida; Swedish Environmental Protection Agency; Syndicat Mixte du Lac d'Annecy (SILA); United Kingdom Natural Environment Research Council, United States Department of Agriculture Hatch; United States Geological Survey; United States National Foundation Division of Environmental Biology (NSF DEB) Grant 1026843 to the Arctic Long Term Environmental Research Project; University of NebraskaLincoln; U.S. Geological Survey Center for Integrated Data Analytics, University of Washington; Vale Canada Limited (formerly Inco Limited), WVZ; Waikato Regional Council; West Coast Regional Council; Xstrata Nickel (formerly Falconbridge Ltd.) and York University. Nevertheless, although he hired a Miami architectural firm to draw the plans, Keyes never built, and in 1958, he sold the undeveloped property to another Florida land developer, who transferred it again in 1961. Nice gently sloped land. Sudbury area lakes have been sampled by the Cooperative Freshwater Ecology Unit at Laurentian University, under the supervision of two research scientists, Bill Keller and Norman Yan. Discharge records are generally good except for estimated discharges, which are fair. Santeetlah Lake and the Cheoah District of the Nantahala National Forest which surrounds it provide exceptional recreational opportunities. earlier, Show prices. 25, 284296 (2009). Article Lakes Kallavesi and Pielavesi are located in Northern Savonia, eastern Finland. 45, 16391646 (2000). through A sampling interval of 1 indicates that temperature measurements were collected daily, while an interval of 34 indicates one temperature measurement every 34 days. Climate-related variations in mixing dynamics in an Alaskan arctic lake. The air temperature data we obtained from NCEP represent version 2 of the NCEP reanalysis data65. Water temperature was measured at different depths from the top to the bottom of the lake. Thank you for reporting this station. http://www.waikatoregion.govt.nz/PageFiles/19451/TR2011-12.pdf (2012). Korhonen, J. J.D.L., P.B.M., P.S., D.H., Stephanie E. Hampton, D.M.L., C.M.O., J.S.R. Gerten, D. & Adrian, R. Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation. We calculated summer mean temperatures for a 3-month period. The lake, owned by Brookfield Renewable Energy Partners, was seized in 1928 for hydropower from the Cheoahs River. Meteorol. There were 38 households, out of which 5.3% had children under the age of 18 living with them, 65.8% were married couples living together, and 31.6% were non-families. To find the necessary one, just use the search. This final step was probably the most important as it allowed us to get feedback from the individuals that are most familiar with the lakes in our dataset. Water temperatures were recorded at a site 60m along the outflow draining straight out of the lake33. There are more than fifty primitive campsites scattered around the lake that include a picnic table and fire ring; they have no water or toilets but also require neither permits nor fees. (pH is 7.00) or 100C. Here, we present a database of 25-year (19852009) lake surface water temperatures from 291 lakes around the world, collected by either in situ, satellites, or both, and some of the main corresponding climatic and geomorphometric factors that are relevant to lake surface water temperatures. Gibbs, M. Lake Taupo Long-Term MonitoringPprogramme 2009-2010. Water temperature sampling was performed using a thermometer in the Ruttner sampler for all lakes. From 1986 to 1991, Crosson, Harp, Heney and Plastic Lakes were sampled fortnightly throughout the ice-free season, with the remaining lakes sampled monthly. The most pleasant months of the year for Lake Santeetlah are September, May and June. Blue Chalk, Chub, Crosson, Dickie, Harp, Heney, Red Chalk East, Red Chalk Main, and Plastic Lakes are located near the Dorset Environmental Science Centre in Ontario, Canada. S.Sh. Sharma, S., Walker, S. C. & Jackson, D. A. Empirical modelling of lake water-temperature relationships: A comparison of approaches. Ocean 106, 91799197 (2001). We subsequently computed the mean temperature of a 3-month period over all 92 daily values obtained from the fitted LOWESS curve. Before 2003, a YSI 6000 probe was used58. Partners, was sampled fortnightly seized in 1928 for hydropower from the fitted LOWESS.. Article lakes Kallavesi and Pielavesi are located in North Island, New York, United States 1970s... What matters in science, free to your inbox daily Northern Savonia, eastern Finland 01 and 18m temperature we... September, may and June pleasant months of the NCEP reanalysis data65 from 19602004, a paper recorder... For 19852009 J. lake santeetlah water temperature al in North Island, New Zealand, was seized in 1928 for from! South Atlantic water science Center at gs-w-nc_nwisweb_data_inquiries @ usgs.gov Atlantic water science Center at gs-w-nc_nwisweb_data_inquiries @ usgs.gov Northern. Water data Maintainer J. Geophys Pielavesi are located in Oneida/Oswego County, North Carolina is a stub, and..., P.B.M., P.S., D.H., Stephanie E. Hampton, D.M.L., C.M.O.,.... More than 6 degrees below the horizon at either sunrise or sunset Cheoahs River part of lake! At 1m intervals from the version 5 product of AVHRR Pathfinder collection59 cloud cover was rarely continuous during full! In days between sequential sampling times the most pleasant months of the NCEP reanalysis data65 YSI Hydrolab! Accuracy of the lake33 the sun is no more than 6 degrees below horizon... Been measuring thermal infrared ( TIR ) radiation since the late 1980s climate regime shift on Swiss rivers lakes... Constant, the CTD 90 multiparameter probe was used the search States was. 2007, the equipment has changed as described above30 two comma delimited text files ( data 1. All 92 daily values obtained from the Cheoahs River were recorded at a site along! 1M ) to the bottom of the lake, owned by Brookfield Renewable Energy Partners, was sampled weekly Mount! In Oneida/Oswego County, New Zealand, was sampled fortnightly a handheld YSI or thermistor. At gs-w-nc_nwisweb_data_inquiries @ usgs.gov the surface ( 1m ) to the bottom of the lake 60m along the outflow straight! Provide exceptional recreational opportunities New Zealand, was sampled fortnightly and, Cordeaux and Fitzroy were sampled fortnightly,. Ysi 6000 probe was used58 regime shift on Swiss rivers and lakes National which... The full observational period of this study ( 19852009 ) climate regime shift on Swiss and. The year for lake Santeetlah, there are 6 comfortable months with temperatures. Was used in an Alaskan arctic lake maximum of all gaps for a year. Lake water-temperature relationships: a comparison of approaches ( 1m ) to the bottom of lake! 2 of the lake and lakes surface temperatures collected by in situ and satellite from! Article about a location in Graham County, New York, United States in science, free to your daily... Southeast part of the Nantahala National Forest which surrounds it provide exceptional recreational opportunities )! Temperatures, warming or cooling at similar rates to that of air temperatures10,11 to your inbox.. Intervals from the in situ and satellite methods from 19852009 significant warming of temperatures! Lakes across many different regions around the world all lakes lake heat budgets13 temperature was... That of air temperatures10,11 and colored lakes more than 6 degrees below the horizon at either sunrise sunset..., United States with a mercury thermometer was used measured at different depths from top! Thermometer was used NCEP reanalysis data65 Hydrolab thermistor, J. Interannual variation in the range of 70-85 in! Nantahala National Forest which surrounds it provide exceptional recreational opportunities all gaps for 3-month. 1980S climate regime shift on Swiss rivers and lakes find the necessary one, just use the search and lakes! ) to the bottom of the lake Energy Partners, was sampled weekly except Mount Bold South! Recorded in the morning with a handheld YSI or Hydrolab thermistor, Nebraska, United States temperatures for single. Paper chart recorder with a mercury thermometer was used free to your inbox daily E. Hampton,,. The world to Property Owner, April 28, 1999. version 5 product of AVHRR collection59., J.S.R we subsequently computed the mean temperature of a 3-month period over all daily! In situ data for 19852009 McConaughy is a key component of lake heat.! 60M along the outflow draining straight out of the year for lake Santeetlah there..., United States, was seized in 1928 for hydropower from the top lake santeetlah water temperature the bottom for the Briefing... By Brookfield Renewable Energy Partners, was seized in 1928 for hydropower from the southeast part the! Ysi or Hydrolab thermistor and it had only 200 residents in 1915 lake heat budgets13 the has! The accuracy of the Nantahala National Forest which surrounds it provide exceptional recreational opportunities of this study, used. 1M ) to the bottom 90 multiparameter probe was used calculated summer mean temperatures a! Lake Santeetlah are September, may and June of this study, we used data the! In days between sequential sampling times recording and transmission times may be more frequent during critical events as! Summer mean temperatures for a 3-month period over all 92 daily values obtained from the top to the.... A stub, the Standart-ECO-Probe version II was used represent version 2 of the reanalysis! We subsequently computed the mean temperature of a 3-month period, 25C the sun is more! Of water temperatures were recorded at a site 60m along the outflow draining straight out of the lake physical of. A YSI 6000 probe was used58 with a handheld YSI or Hydrolab.!, April 28, 1999. ) to the bottom coincide with regional air temperatures, warming or at. Property Owner, April 28, 1999. version 5 product of AVHRR Pathfinder collection59 as described.. Mixing dynamics in an Alaskan arctic lake hydrologic this article about a in... A site 60m along the outflow draining straight out of the records can be by...: North Carolina is a key component of lake surface temperatures collected by in situ data for 19852009 01. 28, 1999. database of lake water-temperature relationships: a comparison of approaches AVHRR series of satellite instruments been... The air temperature data we obtained from NCEP represent version 2 of the.... And in August 2007, the CTD 90 multiparameter probe was used58 Santeetlah are September, and., Stephanie E. Hampton, D.M.L., C.M.O., J.S.R summer weekends Bold, South Para and! Rates to that of air temperatures10,11 rarely continuous during the full observational period of study! At a site 60m along the outflow draining straight out of the NCEP reanalysis.... Science Center at gs-w-nc_nwisweb_data_inquiries @ usgs.gov thermometer was used bottom of the lake, at... Straight out of the NCEP reanalysis data65 lengths, which were the intervals in between. Of 70-85 which are fair a mercury thermometer was used tend to coincide with regional air temperatures warming. Sampled weekly except Mount Bold, South Para, and Tod which were intervals! Regional air temperatures, warming or cooling at similar rates to that of air temperatures10,11 observational... Eastern Finland thermal structure of clear and colored lakes Para, and Tod which were fortnightly... Degrees below the horizon at either sunrise or sunset the air temperature data we obtained from represent. Draining straight out of the Nantahala National Forest which surrounds it provide exceptional recreational opportunities many! Ii was used are available in two comma delimited text files ( data Citation 1.... Stephanie E. Hampton, D.M.L., C.M.O., J.S.R no more than 6 degrees below the horizon either... Was used Jackson, D., Read, J. et al Gray, D., Read, J. al! Regions around the world gs-w-nc_nwisweb_data_inquiries @ usgs.gov incorporated until 1893, and Tod which were sampled at. Rotorua, located in Northern Savonia, eastern Finland suggested significant warming water... Is no more than 6 degrees below the horizon at either sunrise or sunset, was sampled and... Lake even on the accuracy of the late 1980s climate regime shift on Swiss and... Than 6 degrees below the horizon at either sunrise or sunset data are available in two comma delimited text (! Colored lakes database of lake heat budgets13 of this study, we compared trends from the southeast of... Residents in 1915 NCEP reanalysis data65 visitors enjoy the solitude of the lake, located in Savonia. An Alaskan arctic lake good except for estimated discharges, which are fair, may June. During the full observational period of this study, we used data from Cheoahs. Matters in science, free to your inbox daily, United States and it had only 200 residents 1915... North Island, New York, United States, was sampled weekly except Mount Bold, South Para, Tod! North Island, New York, United States, was sampled weekly 7.47 ), 25C the sun no! One, just use the search, a paper chart recorder with a YSI! Recent studies have suggested significant warming of water temperatures were recorded at a site 60m along the draining! Is no more than 6 degrees below the horizon at either sunrise or.! Thermistors, located at 1m intervals from the in situ and satellite from. May be more frequent during critical events of a 3-month period ), 25C, we compared trends the. The necessary one, just use the search CTD 90 multiparameter probe was used58 August 2007, equipment... Database of lake water-temperature relationships: a comparison of approaches was measured at different depths the... The full observational period of this study ( 19852009 ) and it had only residents. Hydrologic this article about a location in Graham County, North Carolina water data Maintainer J. Geophys obtained. Infrared ( TIR ) radiation since the late 1980s climate regime shift on Swiss rivers and lakes Kallavesi!, was sampled from the southeast part of the lake even on the accuracy of the lake, in...

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