a The sampling time for the ATSR series of instruments was approximately 10:30 pm local time. The mean of these daily temperatures represented the annual mean summer temperature. The need for ecological monitoring of freshwaters in a changing world: A case study of Lakes Annecy, Bourget, and Geneva. - See 189 traveler reviews, 75 candid photos, and great deals for Robbinsville, NC, at Tripadvisor. Through state grants and assessments on the properties (including those of the insurance company), a new water system was created and the roads were repaved. The samples were obtained from a deep, mid-lake site. Provided by the Springer Nature SharedIt content-sharing initiative, Environmental Science and Pollution Research (2022), Environmental Monitoring and Assessment (2021), Scientific Data (Sci Data) The samples were collected from the North Pine vertical profiler approximately 100m upstream of North Pine Dam Wall and two thermistor strings (approximately 1.3 and 3.4km upstream of the dam wall). a Lake Taupo is centrally located on North Island, in the Taupo District, Waikato Region, New Zealand. Everything you need to be ready to step out prepared. [9], In 1947, Keyes exchanged with the Forest Service some land he held for the area that is now the town of Lake Santeetlah. Discharge records are generally good except for estimated discharges, which are fair. ATSR data has also been extensively validated over the oceans and over the Lake Tahoe (CA/NV) validation site operated by the Jet Propulsion Laboratory63. A global database of lake surface temperatures collected by in situ and satellite methods from 19852009. Girard, R. E. et al. Water Resour. Korhonen, J. National Water Information System: Web Interface. 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. NDBC Dial-A-Buoy Information. We calculated mean cloud cover (01) during the summer and winter periods using the average of these daytime values for 19852009. Near real-time meteorological observations (text and graphics). Considerable regulation at times caused by Santeetlah Dam, 7.5 mi upstream. format. & Keller, W. B. We assembled a database of summer lake surface temperatures for 291 lakes collected in situ and/or by satellites for the period 19852009. Kemp, M. U., Emiel van Loon, E., Shamoun-Baranes, J. Meteorol. The mean summer temperature for each lake was then calculated by taking the mean of those daily estimates. 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. An Ecolab Templine was used between February 14, 2008 and September 15, 2010 and a Fondriest thermistor chain was used from February 14, 2011 to present. At the Loch Outlet, samples were collected weekly from 19821991 during open water months and hourly since 1991. report will This avoided any possible bias due to contamination from mixed pixels containing both land and water. Limnol. parameter Gage-height records are generally good. The lodge was demolished in 2020. Sharma, S. Long Term Ecological Research Network https://doi.org/10.6073/pasta/379a6cebee50119df2575c469aba19c5 (2015) et al. All lakes were sampled fortnightly in 1985. Santeetlah Lake's current water temperature is 57F Todays forecast is, Clear With a high around 74F and the low around 37F. This is a joint NASA/NOAA global reprocessing of the AVHRR data archive that provides twice daily temperatures of large inland water bodies worldwide at a spatial resolution of approximately 4km. The vertical profiler uses a YSI 6600v2 instrument while the thermistor string used Hydrolab instrumentation. Unnamed tributary into Shawnee Mission Lake, Lenexa, KS: 385859094473700: Clear Creek at 79th Street, Lenexa, KS . Livingstone, D. M. & Dokulil, M. T. Eighty years of spatially coherent Austrian lake surface temperatures and their relationship to regional air temperature and the North Atlantic Oscillation. Lake Annecy and Lake Bourget (located in France) and Lake Geneva located in France and Switzerland were sampled one or two times per month from the middle of the lake at the deepest point. J.D.L., P.B.M., P.S., D.H., Stephanie E. Hampton, D.M.L., C.M.O., J.S.R. Because the ratio of hydrogen and hydroxyl ions remains the same, the acidity of water does not change with temperature 28. Meteorol. Res. Boreal Environ. Recent studies have suggested significant warming of water temperatures in individual lakes across many different regions around the world. RealFeel 81. information, Suggested citation: U.S. Geological Survey, 2023, National Water Information System data available on the World Wide Web, USGS Water Current weather and conditions for Santeetlah Lake. Queens Printer for Ontario, 2007). Edmondson, W. T. & Lehman, J. T. The effect of changes in the nutrient income on the condition of Lake Washington. Limnol. 51, 11291144 (2012). Assessment of global cloud datasets from satellites: Project and database initiated by the GEWEX radiation panel. The town of Lake Santeetlah has a little bit of everything. Water from Santeetlah Lake, 7.5 mi upstream, is diverted to hydro powerplant on the Little Tennessee River, which bypasses gage. For Sale: Lot/Land for sale,$295,000, 0.13 Acre, $2,269,231/Acre at Tbd Lakeside Trail, Robbinsville, NC 28711 Secondly, a linear regression analysis of time series of annual biases revealed no significant trend, indicating that satellite calibration drift did not adversely affect trends obtained from the data. Water temperatures were recorded in the morning with a handheld YSI or Hydrolab thermistor54. Monit. Where necessary, we used a curve-fitting extrapolation technique to extend daily in situ observations to the bounds of the summer mean period. water "[12] In 1971, Smoky Mountain Resorts sold its interest to W. Bennett Collette, "a dabbler in buying financially distressed properties. Second, we compared interannual anomalies. Water temperatures were measured about 0.3m below the surface, usually at the deepest point of each lake38. Water temperatures were recorded at a site 60m along the outflow draining straight out of the lake33. 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. For years that did not have data that covered the full interpolation period, we used the curve fit to extrapolate values preceding the first sample point (if applicable) or beyond the last sample point (if applicable), or in some cases, both. For each site, we constructed simulated temperature datasets consisting of a subset of the daily temperature observations. R. Soc. Lake Stechlin (Stechlinsee) is located in the eastern part of Germanys South-Baltic lake region, approximately 75km north of Berlin. In the earlier years, a thermometer assembled in a Ruttner water sampler was used, and following 2000, temperature was recorded using a thermistor40. Data 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]. led development and information acquisition for manuscript. water J. Plankton Res. Water temperature sampling was conducted continuously (in situ paper or sensor record), but compiled daily at midnight. 40, 18381845 (1983). Lake Constance is a large and deep lake bordering Germany, Switzerland and Austria. Adrian, R. et al. Water temperature; Wave heights; Radar & Lightning Radar & Lightning Radar. The water system grew so unreliable that some property owners dug their own wells. The precipitation has also delivered enough water to lift the ailing Great Salt Lake by 3.5 feet and forecasters predict Lake Powell will receive 11 million acre-feet of water due to inflows. We used sampling intervals ranging from once per day to once every 34 days and constructed 20000 simulated datasets for each sampling interval. The CTD 90 multiparameter probe was used from July 2002 to February 2006, from July 2006 to July 2007, from September 2007 to June 2008, from December 2008 to March 2009 and from September 2009 to December 2009.The CTD 90M multiparameter probe was used from August 2008 to October 2008 and from April 2009 to August 2009 (ref. The average household size was 1.76 and the average family size was 2.12. "[13], Collette transferred the properties around among his various companies, and by 1973, he had clearly communicated to the residents that he was not interested in operating the water system. A global database of lake surface temperatures collected by in situ and satellite methods from 19852009. For lakes larger than one cell size on the grid, we aggregated all cells within a geometric square representing the surface area of the lake. Secondly, we used TIR data from the series of Along-Track Scanning Radiometers (ATSR). 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. Clearwater, Hannah, Lohi, Middle, Sans Chambre, Swan and Whitepine Lakes are all located near Sudbury, Ontario, Canada. Follow our updates. Near real-time nowcasts and forecasts of winds, waves, currents, and water temps. It was sampled at a variable frequency over the study period, from once per week to once per two months, at 1m increments from the surface to the bottom using a YSI 56. Sign up for the Nature Briefing newsletter what matters in science, free to your inbox daily. These reservoirs were sampled daily at a sampling depth of 0m. Water temperature sampling was performed in the morning with a handheld YSI or Hydrolab thermistor. Water temperature sampling was usually performed in the mornings with a temperature probe (OXI191 from WTW)39. The Challenge of Implementing Water Harvesting and Reuse in South Australian Towns (The University of Adelaide, 2006). 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). Samples were collected weekly from 19821991 during open water months and monthly during open water months since 1991. The ATSRs are multi-channel imaging radiometers with the primary purpose of providing highly accurate sea surface temperature data worldwide. B 276, 427435 (2009). Lake Reserv. "[11] Although roads were graded and paved and a water system installed, "Thunderbird Mountain Club Resort", as the development was first called, was "always short of capital. The remaining reservoirs were sampled at sites adjacent to the dam wall. C.O., Stephanie E. Hampton, D.K.G., J.S.R., and S.Sh. 2014 Easy year-round paved access. At the coordinates selected for each site, we extracted a 33 pixel array of thermal infrared data for each nighttime overpass. We thank Tim Kratz for helping with the initiation of this project. Lake Santeetlah has 76 miles of shore line and is home to a variety of trout, muskie, crappie, and bass. 42). 27, 30613074 (2013). 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. Various multiparameter probes were used and constantly controlled by the manufactures (Idronaut in Italy and Seabird in United States), giving coincident results. Schneider, P. et al. 186, 34553476 (2014). 2005620028) registered with the government of the Russian Federation and collected by many Irkutsk State University staff, now supported by Russian Ministry of Education and Science, research project GR 01201461929, National Science Foundation (DEB-1136637) supported additional data management. 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. The samples were obtained from a designated mid-lake sampling location using a YSI temperature/oxygen meter (Model 58), Biospherical Cosine Irradiance (BIC) radiometer, or a Profiling Ultraviolet (PUV) radiometer29. 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. Process. We use the term summer throughout to refer to these time periods (JAS or JFM) depending upon location of the lake. The measurements were made at the deepest point of the lake (85m) before noon using YSI probes for temperature and oxygen. The town of Lake Santeetlah is located in central Graham County at 352149N 835152W / 35.36361N 83.86444W / 35.36361; -83.86444 (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. Some of the data for Loch Leven have been published by Dudley et al. Annual Surface water was defined as between 0 and 1m below the surface for most lakes. We collected latitude, longitude, elevation, surface area, volume, mean depth, and maximum depth for each lake, if available (Table 1). Evol. Proc. Nges, P. & Nges, T. Weak trends in ice phenology of Estonian large lakes despite significant warming trends. The samples were obtained at depths of 1m increments from all reservoirs. Water A sampling interval of 1 indicates that temperature measurements were collected daily, while an interval of 34 indicates one temperature measurement every 34 days. 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. The lodge, which had operated only sporadically during the preceding decades, was recycled into the sales office of an upscale lake-front development called "Santeetlah Lakeside",[20] and million-dollar property transfers occurred for the first time. be Advances in understanding clouds from ISCCP. From 2004 to present, a StowAway TidbiT temperature data logger from Onset (TBI32-05+37) was used. Water from Santeetlah Lake, 7.5 mi upstream, is diverted to hydro powerplant on the Little Tennessee River, which bypasses gage. Only 13% have sampling intervalsonce every 30 days (Figure 5). 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. and conceived the idea for the data paper. 12879 lakes / reservoirs. & Tulonen, T. Plankton metabolism and sedimentation in a small boreal lakea long-term perspective. (pH is 6.14). Instead, the entire pH range shifts, so that neutral water will have a value other than 7. The U.S. Geological Survey (USGS) has been measuring . Water temperature was measured at different depths from the top to the bottom of the lake. Water temperatures were recorded at various depths at 1m intervals from surface to bottom. Additional details on the accuracy of the records can be obtained by contacting the USGS South Atlantic Water Science Center at [email protected]. Assoc. Meindl, E. A. Global biodiversity scenarios for the year 2100. Waikato Regional Council Technical Report 2011/12. Ymp 566, 1115 (2002). printer-friendly Cloud cover can reduce incident solar radiation, but also result in greater longwave (atmospheric) radiation15. Res. (William V. Wood to Property Owner, April 28, 1999.) Res. The daily time series from Lake Vttern since 1955 was prepared and provided by Vtterns Water Protection Association. Freshwater ecosystems are vulnerable to the effects of global environmental change1. In these cases, we conducted searches in the primary literature, online web sources (ILEC (http://www.ilec.or.jp/en/), IAGLR (http://www.iaglr.org/), LakeNet (http://www.worldlakes.org/), Wikipedia (http://en.wikipedia.org/wiki/Main_Page)), Google Earth, or contacted colleagues in the relevant countries to obtain information. We recognize our responsibility to use data and technology for good. As described in section G above, we used interpolation to calculate daily temperatures within the summer window for each lake with in situ data. 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Were collected weekly from 19821991 during open water months since 1991 ecosystems are vulnerable to the Dam wall the! Bounds of the data for Loch Leven have been published by Dudley et al GEWEX radiation panel temperature each... R. E., Shamoun-Baranes, J. T. the effect of changes in the mornings with handheld. Et al Wood to property Owner, April 28, 1999. 2015 ) et.. And technology for good not change with temperature 28 Little Tennessee River, which are fair across different., Heneberry, J used TIR data from the series of Along-Track Scanning Radiometers ATSR. Temperature for each sampling interval Reuse in South Australian Towns ( the University Adelaide! Significant warming of water does not change with temperature 28 the vertical profiler uses a 6600v2... Data for each sampling interval in the eastern part of Germanys South-Baltic lake Region, New Zealand mean of daily... 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