13588 total waterbodies. Aquat. Am. Air temperatures for the NCEP reanalysis data are projected onto a global T62 Gaussian grid of 192 equally spaced points in longitude and 94 unequally spaced points in latitude65. Magnuson, J. J., Bowser, C. J. 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 samples were obtained from the region with greatest water depth within each lake. "[12] In 1971, Smoky Mountain Resorts sold its interest to W. Bennett Collette, "a dabbler in buying financially distressed properties. Santeetlah Reservoir is located on the Cheoah River in North Carolina, USA, in the state of South . From 2003 to 2005 and in 2007, the CTD 90 multiparameter probe was used. & Prata, F. E. An extraordinary upwelling event in a deep thermally stratified lake. Edmondson, W. T. & Lehman, J. T. The effect of changes in the nutrient income on the condition of Lake Washington. From 19912010, a temperature sensor of an oxygen probe was used (WTW Oxi 197S, Weilheim, Germany)43. J. Geophys. led development and information acquisition for manuscript. We also calculated gap lengths, which were the intervals in days between sequential sampling times. Page Contact Information: North Carolina Water Data Maintainer Queens Printer for Ontario, 2007). Lakes are sentinels of climate change2 and are an effective indicator of a limnological response to global climate change, as they integrate climatic and landscape factors3. 48, 14321438 (2003). Plisnier, P. D. et al. Limnol. Cleveland, W. S. Robust locally weighted regression and smoothing scatterplots. Summer and winter surface solar (i.e., shortwave) and longwave radiation data are a satellite product taken from the NASA/Global Energy and Water Cycle Experiment (GEWEX) Surface Radiation Budget (SRB) radiation dataset, version 3.0 (obtained from the NASA Langley Research Center Atmospheric Science Data Center). All remaining authors provided water temperature and geomorphometric data, summarized how data were acquired and sampled, verified data, and revised the manuscript. Page Last Modified: 2023-04-18 09:31:40 EDT In the epilimnion, profiles were taken at 2.5m intervals (1.0m intervals after 1991), and the depth intervals in the meta- and hypolimnion varied from 5 to 20m. Surface temperature was measured at approximately 10 cm depth using a self-made sonde which functioned based on the Wheatstone-Bridge technique from 19851990. 12879 lakes / reservoirs. Monit. Language links are at the top of the page across from the title. Water temperatures were recorded between 10:00 and 18:00 with a Kahl thermistor, although a Yellow Springs Instrument Co. (YSI) sonde 600XLM V2 was used starting in 1999 in Lake Aleknagik and YSI 660V24 in Lake Washington18,19. Lake Tanganyika is located at the border of four countries (Republic of Burundi, Democratic Republic of Congo, United Republic of Tanzania, Republic of Zambia). Therefore, variation among the simulated datasets for each sampling interval was driven by random variation in the choice of the initial sampling date. Water temperature sampling was usually performed in the mornings with a temperature probe (OXI191 from WTW)39. The time period when the sun is between 6 and 12 degrees below the horizon at either sunrise or sunset. 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. Satellite-derived multivariate world-wide lake physical variable timeseries for climate studies, A long-term dataset of lake surface water temperature over the Tibetan Plateau derived from AVHRR 19812015, Global data set of long-term summertime vertical temperature profiles in 153 lakes, Seasonal overturn and stratification changes drive deep-water warming in one of Earths largest lakes, Global lake thermal regions shift under climate change, Deeper waters are changing less consistently than surface waters in a global analysis of 102 lakes, The global lake area, climate, and population dataset, High resolution temperature data for ecological research and management on the Southern Ocean Islands, Machine-accessible metadata file describing the reported data, http://ecosystems.mbl.edu/ARC/dataprotocol/ArcticLTERIM.html, https://lter.limnology.wisc.edu/about/lakes, https://knb.ecoinformatics.org/#view/kgordon.35.49, http://www.pref.shiga.lg.jp/d/biwako-kankyo/lberi/, http://www.waikatoregion.govt.nz/PageFiles/19451/TR2011-12.pdf, https://doi.org/10.6073/pasta/379a6cebee50119df2575c469aba19c5, http://creativecommons.org/licenses/by/4.0, Analysis of surface temperature variation of lakes in China using MODIS land surface temperature data, Maximum lake surface water temperatures changing characteristics under climate change, Warming of surface water in the large and shallow lakes across the Yangtze River Basin, China, and its driver analysis, Reply to: Concerns about phytoplankton bloom trends in global lakes, Southern coastal subtropical shallow lakes skin temperature driven by climatic and non-climatic factors. Lake Pyhselk (Pyhaselka), located in North Karelia, Finland, was sampled 0 to 3 times per month. Hydrol. We validated the satellite data with the in situ data by conducting four analyses. archived the database. Water from Santeetlah Lake, 7.5 mi upstream, is diverted to hydro powerplant on the Little Tennessee River, which bypasses gage. Markovic, M., Jones, C. G., Winger, K. & Paquin, D. The surface radiation budget over North America: gridded data assessment and evaluation of regional climate models. 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. instructions 00010 Temperature, water(Max.,Min.,Mean) 00045 Precipitation(Sum) 00060 Discharge(Max.,Min.,Mean) . Oceanogr. [citation needed], Lake Santeetlah adjoins a portion of U.S. 129 called the Tail of the Dragon, a road frequently used for recreational purposes by motorcycle and sports car enthusiasts because of its purported 318 curves in 11 miles (18km).[25]. [18], In 1979, the State of North Carolina had prohibited any new connections to the antiquated water system. Lake Tarawera, located in North Island, New Zealand, was sampled monthly from the subsurface (20cm) to the bottom at 1m intervals. no moonlight, or other lights). The physical impact of the late 1980s climate regime shift on Swiss rivers and lakes. S.Sh. Gage-height records are generally good. Sci. Report Water Temp. & Scholes, P. Managing the lakes of the Rotorua District, New Zealand. Lakes Inari and Kevojrvi are located in the northernmost Lapland Province. choose The Best Time To Camp In Lake Santeetlah. 42). Water temperature sampling was performed between 8:00 to 10:00, usually at 9:15. This avoided any possible bias due to contamination from mixed pixels containing both land and water. A Fisher Scientific thermometer was used until 2003, a YSI temperature probe was used from 2003 to 2009, and an Orion Conductivity Meter 105A+ was used from 2009 to present23. year We computed a separate LOWESS fit for the temperature curve of each calendar year and at each inland water body. Lough Feeagh, located in County Mayo, Ireland was sampled daily from the surface at less than 1m depth. Oneida Lake, located in Oneida/Oswego County, New York, United States, was sampled weekly. Ymp 566, 1115 (2002). Water temperature plays an important role in almost all USGS water science. Ambrosetti, W. & Barbanti, L. Temperature, heat content, mixing and stability in Lake Orta: A pluriannual investigation. Kaskesniemi was sampled at an interval of 2 to 4m, Noljakansaaret at an interval of 2m, and both Pyhsaari and Kokonluoto at an interval of 5m depth. An independent assessment of pathfinder AVHRR sea surface temperature accuracy using the marine atmosphere emitted radiance interferometer (MAERI). Enter dates to see prices. Water temperature sampling was performed from 7:30 to 11:00, usually at 10:00 with a thermometer assembled in a Ruttner water sampler in the early years, and a YSI profiler later on51. Verhandlungen Int. An interesting fact about Lake Santeetlah's population is that the median age is relatively high at 70.3 years old, which is almost double the state average. Recording and transmission times may be more frequent during critical events. Water temperatures were recorded in the morning with a handheld YSI or Hydrolab thermistor54. 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 . Warmer temperatures have kick-started melting from lower and mid-elevations of a snowpack that exceeded some historic highs. Winds are out of the W at 3mph, with wind gusts of 10mph. Santeetlah Lake's current water temperature is 57F Todays forecast is, Clear With a high around 74F and the low around 37F. 29, 22262240 (2009). Water-Year Water temperature samples were collected at 10cm depth in the late morning to early afternoon. Freshw. Fourth Inter Celt. Profiles at each metre were taken frequently between 9:0011:00, but due to weather related challenges were sometimes taken later20. Water temperatures were recorded from 9:00 to 14:00 with multiprobes such as Hydrolab used in the early years and YSI used in more recent years28. Girard, R. E. et al. The change in length of daylight between today and tomorrow is also listed when available. Limnol. We calculated summer mean temperatures for a 3-month period. Since May 2009, an automatic station (VAISALA, MAWS110 and water temperature sensor QMT110) was used every hour for water temperature measurements. Temperatures were obtained from a consistent sampling location at or near the deepest portion of the lake. The difference was calculated by year for each simulated dataset. 5, 129144 (2004). Geophys. 22). Sci. Soc. Annual 31.6% of all households were made up of individuals, and 13.2% had someone living alone who was 65 years of age or older. Manag. The methodology used for obtaining satellite-based lake surface temperatures largely follows the approach described in Schneider and Hook11. Lakes Vnern (Vanern), Mlaren (Malaren), Skrglen (Skargolen), Stensjn (Stensjon), Remmarsjn (Remmarsjon), Allgjuttern, Brunnsjn (Brunnsjon), vre Skrjn (Ovre Skarjon), Stora Envttern (Stora Envattern), Rotehogstjrnen (Rotehogstjarnen), Fiolen, St Skrsjn (St Skarsjon) and Fracksjn (Fracksjon), all located in Sweden were sampled monthly during the ice-free season, while Lakes Vttern (Vattern) and Erken, also in Sweden were sampled daily throughout the year. 54, 2401 (2009). 57). Methods Ecol. Internet Explorer). The only exception to this time period was the in situ data for Toolik Lake, Alaska, for which we used June-August because of the lack of data available for September due to the early onset of winter at this high latitude. The time of Civil Sunset minus the time of Civil Sunrise. B.D., Stephanie E. Hampton and P.S. Sixty years of environmental change in the worlds largest freshwater lakeLake Baikal, Siberia. Lake Santeetlah Water Level. J. Biol. Soc. Near real-time meteorological observations (text and graphics). Sci. Lake Constance is a large and deep lake bordering Germany, Switzerland and Austria. Stat. Thus, a global data set of water temperature is required to understand and synthesize global, long-term trends in surface water temperatures of inland bodies of water. Clayton, J., Edwards, T. & Winton, M. The Condition of Twelve Lakes in the Rotorua Lakes Region Using LakeSPI (National Institute of Water & Atmospheric Research Ltd, 2005). & Schiffer, R. A. Water temperature sampling was performed in the daytime with a CTD profiler and a thermistor. 68). Kirillin, G., Shatwell, T. & Kasprzak, P. Consequences of thermal pollution from a nuclear plant on lake temperature and mixing regime. Richer, E. & Baron, J. S. Loch Vale Watershed long-term ecological research and monitoring program: quality assurance report, 20032009 (Open-File Report 2011-1137, US Geological Survey, 2011). Whenever there were inconsistencies in data, we worked directly with the original data provider to resolve the issue and update the data accordingly. WDR NC-04-1: 2002 (annual maximum discharge). Izmesteva, L. R., Moore, M. V. & Hampton, S. E. Seasonal dynamics of common phytoplankton in Lake Baikal. Although there were equipment upgrades over the years, there have been no substantive change to equipment55. 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. For reference, approximately 38% of the in situ lakes in our dataset have sampling intervals of at least once every 10 days, while 58% have sampling intervals of at least once every 20 days (Figure 4). J. Appl. Facebook . Will northern fish populations be in hot water because of climate change? J. Limnol. Global biodiversity scenarios for the year 2100. Scottish Natural Heritage Commissioned Report No. Lake Santeetlah, NC 10-Day Weather Forecast. This populated place also has portions in an adjacent county or counties, In 1999, the current mayor thought that adding the word "Lake" to the name added "spice" and also clarified the town's location. Data Current data typically are recorded at 15- to 60-minute intervals, stored onsite, and then transmitted to USGS offices every 1 to 4 hours, depending on the data relay technique used. 27, 30613074 (2013). We calculated mean cloud cover (01) during the summer and winter periods using the average of these daytime values for 19852009. In the town, the population was spread out, with 4.5% under the age of 18, 10.4% from 25 to 44, 41.8% from 45 to 64, and 43.3% who were 65 years of age or older. Lakes Inari, Kallavesi, Kevojrvi (Kevojarvi) Lappajrvi (Lappjarvi), Pijnne (Paijanne), Pielavesi, Pielinen, and Saimaa are all located in Finland. are there alligators in lake chatuge. Effects of climatic warming on lakes of the central Boreal Forest. The lakes were sampled at every meter from the surface to the bottom. Second, we compared interannual anomalies. & Walther, A. The time period when the sun is no more than 6 degrees below the horizon at either sunrise or sunset. Figure 1 shows long-term rates of change in surface lake water temperature from 1985 to 2009. Although the sampling procedure has remained constant, the equipment has changed as described above30. Yellowin situ sampled lakes; Redsatellite sampled lakes. The U.S. Geological Survey (USGS) has been measuring . Exceptions were latitudes less than 23.5, for which the JAS metric was used south of the equator and the JFM metric was used north of the equator. 25, 445453 (2003). NDBC Buoy and C-Man reports. and Process. WATER LEVEL. The samples were obtained from the northern part of the lake, at the outflow. However, the name change produced some semantic curiosities. The Lake Baikal data are part of a dataset (No. Residents can now live both. From 1986 to 1998 the multiparameter probe Meerestechnik Elektronik (ECO 236) was used. of 19, 181198 (1998). Lake Baikal, located in south of the Russian region of Siberia, was sampled approximately every 1014 days. Russian Acad. [8], The father of Lake Santeetlah was Kenneth S. Keyes, Sr. (18961995), a native of Detroit, who became an extremely successful real estate dealer in Miami, heading over fifty corporations that operated hotels, office buildings and other realty enterprises in Florida, New York, and Canada. Report Limnol. All lakes were sampled at a depth of 0.5m, in addition to several other depths depending on the maximum lake depth. Lake Lappajrvi is located in the municipalities of Lappajrvi, Alajarvi, and Vimpeli, in southern Ostrobothnia, Finland. Approximately a mile north of the town is Cheoah Point Recreation Area, which has developed swimming, camping, and picnicking facilities as well as a boat ramp. Science 287, 17701774 (2000). data The time of Actual Sunset minus the time of Actual Sunrise. Physical and Chemical Data Series from Clearwater, Lohi, Middle and Hannah Lakes Near Sudbury, Ontario: Long-term Responses to Liming and Natural Recovery from Historical Acidification and Metal Contamination (Ontario Ministry of the Environment. In 2008 and 2009, the CTD 90M multiparameter probe was used. be Warning: Javascript must be enabled to use all the features on this page! We defined the maximum gap as the maximum of all gaps for a single year. The reservoir is located at an altitude of 1,941 feet and covers 2,881 hectares and holds a total of 2,842,000 cubic meters of water. How to cite this article: Sharma, S. et al. 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. Get the most important science stories of the day, free in your inbox. ; and ii) Which climatic forcing variables and geomorphometric factors are most important in driving changes in water temperature, i.e., do similar lake types exhibit similar rates of warming or cooling globally? water 94, 10311049 (2013). Water temperatures in the Lower Lake of Zurich, Upper Lake of Zurich and Lake of Walenstadt were measured from January 1985 to January 2001 using three different negative temperature coefficient (NTC) thermistors; from February 2001July 2008 using an FLP-10 multisonde (DMP AG, Switzerland); and from August 2008 onwards using a Hydrolab DS5 multisonde (OTT Hydromet GmbH, Germany). The most monthly precipitation in Lake Santeetlah occurs in December with 12.6 inches. Menu. years Am. Data for Plusssee were collected by the Max-Planck-Institute for Limnology, Ploen until 2006. have We collected latitude, longitude, elevation, surface area, volume, mean depth, and maximum depth for each lake, if available (Table 1). Meteorol. Only 13% have sampling intervalsonce every 30 days (Figure 5). Not Korhonen, J. The lakes were sampled monthly at the deepest points. We recognize our responsibility to use data and technology for good. Ecology 86, 198209 (2005). The term winter refers to the 3-month period opposite summer in the calendar year. Lake Vrtsjrv (Vortsjarv) in southern Estonia, was sampled twice daily at 8:00 and 20:00 until April 30 2011, and hourly since then, at the surface. All were sampled weekly except Mount Bold, South Para, and Tod which were sampled fortnightly. Geophys. In view of this great difference in temperature and the purity of the surface water, the author of the paper suggests that any one living near a deep lake could obtain very pure ice-cold water . The samples were obtained at depths of 1m increments from all reservoirs. [9], In 1947, Keyes exchanged with the Forest Service some land he held for the area that is now the town of Lake Santeetlah. Oswald, C. J. Be prepared with the most accurate 10-day forecast for Santeetlah, NC with highs, lows, chance of precipitation from The Weather Channel and Weather.com Water temperatures were recorded at 10:00 with reversing thermometers until 2005 and with Seabird SBE25 since 2005 (ref. Measurements were made twice a month at 0.5, 5, 10, 15, 20, 30, 40, 60, 80m, and bottom (approximately 9095m) (ref. Limnol. Manag. Chen, Y., Qin, B., Teubner, K. & Dokulil, M. T. Long-term dynamics of phytoplankton assemblages: Microcystis-domination in Lake Taihu, a large shallow lake in China. in This allows for more accurate estimates of the 3-month summer means. Oceanogr. Some of the data for Loch Leven have been published by Dudley et al. The town was organized in 1989 as "Santeetlah"; in 1999, it changed its name to "Lake Santeetlah". We compiled satellite-derived surface water temperatures from 154 lakes (Figure 1). 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). Title: USGS: Water-Year Summary for North Carolina The median income for a household in the town was $70,417, and the median income for a family was $83,989. Burragorang and Wingecarribee were sampled weekly. Includes near real-time and archived data and plots. At high sampling intervals (panel c), linear interpolation can underestimate daily temperatures, leading to an underestimate of the mean summer temperature. Temperature data were collected near the deepest part of the lake using a Hydrolab Quanta thermistor deployed by the Lake Biwa Environmental Research Institute. 22, 533535 (1984). year Data for the New York City drinking water reservoirs were sampled and provided by the New York City Department of Environmental Protection (NYCDEP). Data Rep, 2006). Freshwater ecosystems are vulnerable to the effects of global environmental change1. Fish. "Santeetlah Lake," undated pamphlet, Alcoa. Each site was sampled from the surface (1m) to the bottom. This was done in order to avoid the cloudy wet season in the tropics and instead collect data during the dry season, which allows for an increased number of cloud-free satellite observations11. Hydrobiologia 731, 1929 (2014). Schindler, D. W. et al. J. Plankton Res. We obtained the CRU data from version 3.21 of their dataset using 0.5-degree resolution grid cells64. Lakes Maggiore and Orta are both located in northwestern Italy, in the subalpine lake district. Santeetlah Marina[23] is the only full-service marina on a lake that has 76 miles (122km) of shoreline. The AVHRR Pathfinder product has been rigorously validated in the past against in situ radiometer data over open oceans60,61 and against buoy observations over inland water bodies11. Water temperatures were recorded using 23m surface buoys25, usually ARES or AMPS payload (http://www.ndbc.noaa.gov/rsa.shtml) and various hulls. 9). Both data entities are documented in the Ecological Metadata Language (EML) and are archived in the Long Term Ecological Research Network Information System and in the R package laketemps. In the meantime, to ensure continued support, we are displaying the site without styles We compiled time series from both series of satellite instruments independently at all 141 sites, with AVHRR data available for the period 19852009 and ATSR data available for the period 19912009. For each site, we constructed simulated temperature datasets consisting of a subset of the daily temperature observations. 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 data are generated on the basis of the International Satellite Cloud Climatology Project (ISCCP) DX radiance and cloud parameters67, using an updated version of the University of Marylands shortwave flux algorithm and an adaptation of the longwave algorithm. Overall, however, the SRB data show a lower mean bias across 36 global sites (5.5Wm2; 1.9%) (ref. In Lake Santeetlah, there are 6 comfortable months with high temperatures in the range of 70-85. Kemp, M. U., Emiel van Loon, E., Shamoun-Baranes, J. Limnol. hide Lakes as sentinels of climate change. Lake Peipsi (Peipus) on the border of Estonia and Russia, was sampled twice daily at 8:00 and 20:00, at a depth of 0.1m (ref. FOIA Africa Eurasia North America Oceania South America lake reservoir, Machine-accessible metadata file describing the reported data (ISA-Tab format). The satellite data with the in situ data by conducting four analyses the state of South ECO. Be Warning: Javascript must be enabled to use data and technology for good use all the on..., Machine-accessible metadata file describing the reported data ( ISA-Tab format ) ) the... Machine-Accessible metadata file describing the reported lake santeetlah water temperature ( ISA-Tab format ) Loon,,! This article: Sharma, S. et al SRB data show a lower mean bias 36... 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T. the effect of changes in the calendar and... Time of Actual sunset minus the time of Civil sunset minus the time Civil! Data by conducting four analyses the physical impact of the page across from the at... Deployed by the lake for 19852009 sixty years of environmental change in length of daylight between and! Has 76 miles ( 122km ) of shoreline an extraordinary upwelling event in a deep thermally stratified.. Transmission times may be more frequent during critical events lakes Inari and are! ], in the calendar year Carolina water data Maintainer Queens Printer for Ontario 2007. Frequent during critical events Santeetlah reservoir is located on the Little Tennessee River, which bypasses gage L. temperature heat. Has been measuring, usually ARES or AMPS payload ( http: //www.ndbc.noaa.gov/rsa.shtml and..., J. J., Bowser, C. J sampled weekly Lappajrvi is located on the Cheoah River in Carolina...
lake santeetlah water temperature