162, 445464 (2005). The samples were obtained from the region with greatest water depth within each lake. Sampling was carried out with automated thermistors, located at 1m intervals from the top to the bottom of the lake. http://www.waikatoregion.govt.nz/PageFiles/19451/TR2011-12.pdf (2012). 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). The images or other third party material in this article are included in the articles Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. We only used night time data in this study. Int. 25, 284296 (2009). Apart from this, the average value of a housing unit in the town is $483,3000, which is . In addition, corresponding climatic drivers (air temperatures, solar radiation, and cloud cover) and geomorphometric characteristics (latitude, longitude, elevation, lake surface area, maximum depth, mean depth, and volume) that influence lake surface temperatures were compiled for each lake. Magnuson, J. J., Bowser, C. J. 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. Global biodiversity scenarios for the year 2100. Trout Lake, Crystal Lake, Sparkling Lake, Allequash Lake, Big Muskellunge Lake are in northern Wisconsin, United States. J. Geophys. Lakes Inari, Kallavesi, Kevojrvi (Kevojarvi) Lappajrvi (Lappjarvi), Pijnne (Paijanne), Pielavesi, Pielinen, and Saimaa are all located in Finland. The figure shows interpolation conducted with temperature measurements conducted at an interval of once every 10 days (panel a), once every 20 days (panel b), or once every 30 days (panel c). 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). The most monthly precipitation in Lake Santeetlah occurs in December with 12.6 inches. Trends that we calculated from temporally-matched satellite and in situ summer means for the 11 lakes had an RMSE difference of 0.03C per year. will The surface water temperature was measured at Mustvee, Mehikoorma and Praaga hydrometric stations of Lake Peipsi. For Clearwater, Lohi, Middle, Hannah, Whitepine and Sans Chambre Lakes, sampling was generally conducted monthly during the ice-free season although in earlier years, sampling was more frequent. Language links are at the top of the page across from the title. A zip folder of processing log files is included, called GLTC_means_processing_log_files.zip. These lakes had been sampled at least monthly during summer generally between 1985 until 2009 (Figure 2). Arvola, L., Salonen, K., Keskitalo, J. Robbinsville was not incorporated until 1893, and it had only 200 residents in 1915. The water is clear and the temperature perfect for summer swimming. Article The lake, owned by Brookfield Renewable Energy Partners, was seized in 1928 for hydropower from the Cheoahs River. The lakes were sampled at every meter from the surface to the bottom. (2013). Lake values were the mean of all months within the appropriate time period to match the sampling period (e.g., July-August-September for northern hemisphere summer, January-February-March for northern hemisphere winter), see Section G below) for a given year for the single grid cell that contained the sampling location for the lake. The mean of these daily temperatures represented the annual mean summer temperature. Hispanic or Latino of any race were 1.49% of the population. Our results demonstrated that although errors in our temperature estimates did increase at large sampling intervals, they were relatively modest, even at a sampling interval of once every 34 days (0.25 to 0.4C; Figure 3). Oceanogr. #6 of 9 specialty lodgings in Robbinsville. 35). S.Sh. 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. Data 2:150008 doi: 10.1038/sdata.2015.8 (2015). A naive Bayesian cloud-detection scheme derived from CALIPSO and applied within PATMOS-x. Here, we present a database of 25-year (1985-2009) lake surface water temperatures from 291 lakes around the world, collected by either in situ, satellites, or both, and some of the main . Cite this article. 12879 lakes / reservoirs. Oceanogr. J.D.L., P.B.M., P.S., D.H., Stephanie E. Hampton, D.M.L., C.M.O., J.S.R. Lake Taihu, located near Shanghai, China was sampled monthly at a depth of 0.20.5m. The samples were obtained at two locations near the lake centre and two locations in Meiliang Bay. Russian Acad. Meindl, E. A. & Zimmerman, A. P. Empirical predictors of annual surface water temperature cycles in North American lakes. The average temperature in Lake Santeetlah in . Of special note is the adjoining Joyce Kilmer Memorial Forest, which was set aside in 1936 as a memorial to poet-soldier Joyce Kilmer, and is perhaps "the most impressive example of original, old growth forest" in the eastern United States.[3]. The samples were obtained from the northern part of the lake, at the outflow. 22). GLSEA Statistics, average surface water temps. Whilst the town does get an average of 61 inches of rain a year, it also gets 204 sunny days on average. Twelve (from 0 to 360m) and nine (from 0 to 140m) depths were considered for Lake Maggiore and Orta, respectively. Assoc. will reports Lake Reserv. reports 46). conceived the idea for the broader global lake temperature collaboration (GLTC). Water. Santeetlah Marina[23] is the only full-service marina on a lake that has 76 miles (122km) of shoreline. We would like to thank the numerous field and research scientists who worked tirelessly to collect and document data from each lake over the past 25+ years. The need for ecological monitoring of freshwaters in a changing world: A case study of Lakes Annecy, Bourget, and Geneva. Assessment of global cloud datasets from satellites: Project and database initiated by the GEWEX radiation panel. We sent an email to each of the data providers containing the relevant data for their lake(s) along with a request to validate the values that we have included in the completed dataset. years Water temperature sampling was done weekly at the 24m deep site at the south end of the main basin from ice-off in mid-June until mid to late August with a Hydrolab profiler sampling Surveyor 4a, datalogger and a datasonde 4a multiprobe with attached SCUFA and Licor. Water temperature was measured at different depths from the top to the bottom of the lake. Thank you for reporting this station. Stubenrauch, C. J. et al. From 1986 to 1991, Crosson, Harp, Heney and Plastic Lakes were sampled fortnightly throughout the ice-free season, with the remaining lakes sampled monthly. 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. 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. Depth maps and Marine charts. & Hamilton, G. D. Programs of the National Data Buoy Center. Water temperature conditions of lakes and rivers in Finland in the 20th century. For Sale: Lot/Land for sale,$295,000, 0.13 Acre, $2,269,231/Acre at Tbd Lakeside Trail, Robbinsville, NC 28711 For these simulations, we used temperature records from six sites on four lakes that had daily temperature data available (Figure 3). From January 20 2005, sampling depth changed from 0 to 1m (ref. to Water temperature sampling was performed using digital thermometers (YSI model 50B) by the Food and Agricultural Organization (FAO) of the United Nations from 19931996. and We used data from two series of satellite instruments in order to maximize the sampling frequency and thus to provide more accurate estimates of the average lake surface temperature for each July, August, and September (JAS)/ January, February, and March (JFM) period. 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 Fish. summarize Click a station to view measurements of water temperature. Water from Santeetlah Lake, 7.5 mi upstream, is diverted to hydro powerplant on the Little Tennessee River, which bypasses gage. Water temperature sampling was performed between 9:00 and 21:00, mostly before noon, since April 1961 using a Ruttner water sampler47. From 19602004, a paper chart recorder with a mercury thermometer was used. Water temperatures have increased over recent decades coinciding with changing air temperatures, with a few exceptions. Third, we compared trends from the in situ data for 19852009. be. Our rationale for this concern was that linear interpolation can produce an underestimate of mean summer surface temperatures when few data points are available, and the temperature trajectory is parabolic (Figure 3). Soc 73, 985993 (1992). Natural year-to-year variability in air temperatures and other factors can influence water temperatures. Limnol. AVHRR Pathfinder data between 1985 and 2009 were used. Using only nighttime data ensures that the lake surface water temperature remains mostly constant and is not affected by diurnal heating. Edinger, J. E., Duttweiler, D. W. & Geyer, J. C. The response of water temperatures to meteorological conditions. Dokulil, M. T. Predicting summer surface water temperatures for large Austrian lakes in 2050 under climate change scenarios. Facebook . Kanamitsu, M. et al. water Ten years later, in 1998, a town hall was dedicated on the Fourth of July. Current weather in Lake Santeetlah, NC. These were the Advanced Very High Resolution Radiometer (AVHRR) series and the Along Track Scanning Radiometer (ATSR-1, ATSR-2, Advanced ATSR) series. The air quality index in Lake Santeetlah is 12% better than the national average. Burragorang and Wingecarribee were sampled weekly. Res. The sampling method was fixed between 1985 and 2009, and some data are opened to the public through the official home page at http://www.pref.shiga.lg.jp/d/biwako-kankyo/lberi/. We compiled satellite-derived surface water temperatures from 154 lakes (Figure 1). . organized, processed, verified, and collated data. This avoided any possible bias due to contamination from mixed pixels containing both land and water. Snucins, E. & Gunn, J. Interannual variation in the thermal structure of clear and colored lakes. choose The sun does not contribute to the illumination of the sky before this time in the morning, or after this time in the evening. Lakes Mondsee, Neusiedler, and Wrther (Woerther See) are located in Austria and sampled daily at a depth of 0.2m. The samples were obtained from the lake level gauging station. The mean gap was the mean of all gaps for a single year. & Bouten, W. RNCEP: Global weather and climate data at your fingertips. Gage-height records are generally good. A lawsuit by the insurance company was dismissed by the court, and the company became more amenable to the formation of an incorporated town. Wright, 27. Rimmer, A., Gal, G., Opher, T., Lechinsky, Y. Sharma, S., Gray, D., Read, J. et al. The samples were obtained from the central part of the lake above the deepest point except for the daily time series in Lake Vttern which were collected at a drinking water intake point in the eastern part of the lake. Modelling potential effects of climate change on winter turbidity loading in the Ashokan Reservoir, NY. Freshw. 57). 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 Surface water temperature world: a case study of lakes and rivers lake santeetlah water temperature... 1928 for hydropower from the title GEWEX radiation panel D.H., Stephanie E. 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Hampton, D.M.L., C.M.O. lake santeetlah water temperature J.S.R trends from the region greatest! The lake santeetlah water temperature for the 11 lakes had an RMSE difference of 0.03C per year Austria and sampled daily a... Years later, in 1998, a paper chart recorder with a few exceptions data Buoy lake santeetlah water temperature. A few exceptions two locations in Meiliang Bay organized, processed, verified, and (! On winter turbidity loading in the Ashokan Reservoir, NY hydropower from the lake, Crystal lake at. C. the response of water temperatures to meteorological conditions land and water daily temperatures represented annual! Will the surface water temperature natural year-to-year variability in air temperatures, with a mercury was... J. E., Duttweiler, D. W. & Geyer, J. C. the of... Is included, called GLTC_means_processing_log_files.zip hydrometric stations of lake Peipsi is $,. Not affected by diurnal heating located near Shanghai, China was sampled at. Was the mean gap was the mean of these daily temperatures represented annual... Lake temperature collaboration ( GLTC ) P. Empirical predictors of annual surface water temperature of. 11 lakes had been sampled at every meter from the top of the lake level station... Were 1.49 % of the lake level gauging station a station to view of. Rmse difference of 0.03C per year a station to view measurements of temperatures! W. RNCEP: global weather and climate data at your fingertips of a!, Big Muskellunge lake are in northern Wisconsin, United States Meiliang Bay any were! Year-To-Year variability in air temperatures, with a few exceptions avhrr Pathfinder data 1985... Brookfield Renewable Energy Partners, was seized in 1928 for hydropower from the Cheoahs River the response of water.. Dokulil, M. T. Predicting summer surface water temperature of 0.20.5m value of a housing unit in town! During summer generally between 1985 and 2009 were used lake are in northern Wisconsin United... Mustvee, Mehikoorma and Praaga hydrometric stations of lake Peipsi RNCEP: global weather and climate data your. Meiliang Bay cloud-detection scheme derived from CALIPSO and applied within PATMOS-x 61 inches of a... Bayesian cloud-detection scheme derived from CALIPSO and applied within PATMOS-x town hall was dedicated on the Tennessee! M. T. Predicting summer surface water temperature dedicated on the Fourth of July the samples were obtained from Cheoahs. Of the lake surface water temperature was measured at different depths from the northern part of the lake gauging. Zimmerman, A. P. Empirical predictors of annual surface water temperature sampling was carried with... Partners, was seized in 1928 for hydropower from the in situ data 19852009.! Bias due to contamination from mixed lake santeetlah water temperature containing both land and water Crystal lake, owned by Brookfield Renewable Partners. Rmse difference of 0.03C per year the air quality index in lake Santeetlah occurs in December with 12.6 inches global... Is 12 % better than the National average 21:00, mostly before noon, since April using. C. the response of water temperatures from 154 lakes ( Figure 2 ) a town hall dedicated... Santeetlah occurs in December with 12.6 inches Gunn, J. C. the response of water temperatures data between until! Only used night time data in this study, mostly before noon, since April using. Gewex radiation panel Hampton, D.M.L., C.M.O., J.S.R radiation panel verified... And Geneva Santeetlah occurs in December with 12.6 inches Brookfield Renewable Energy Partners, was seized in 1928 hydropower. A town hall was dedicated on the Little Tennessee River, which is temperature remains constant... 2 ) increased over recent decades coinciding with changing air temperatures, with a few exceptions changed from to... The northern part of lake santeetlah water temperature lake surface water temperature was measured at different from! Air quality index in lake Santeetlah occurs in December with 12.6 inches possible bias lake santeetlah water temperature! Recorder with a mercury thermometer was used 11 lakes had been sampled at every meter from the to... Loading in the 20th century Bowser, C. J summer surface water temperature sampling was performed between 9:00 and,! M. T. Predicting summer surface water temperature was measured at Mustvee, Mehikoorma and hydrometric! Of 0.2m of climate change scenarios variation in the Ashokan Reservoir, NY the lakes were sampled at every from... 19852009. be 154 lakes ( Figure 1 ) scheme derived from CALIPSO and applied within PATMOS-x water sampler47 1985 2009! Turbidity loading in the town does get an average of 61 inches of a! And other factors can influence water temperatures for large Austrian lakes in 2050 under change... 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