Houston, TX 76 Sunny. [2], Although the area below the highwater mark continues to be managed by Alcoa, approximately 80% of the surrounding land is under the jurisdiction of the U.S. Forest Service, which provides swimming, camping, picnicking, fishing and boating facilities. Clearwater, Hannah, Lohi, Middle, Sans Chambre, Swan and Whitepine Lakes are all located near Sudbury, Ontario, Canada. We used sampling intervals ranging from once per day to once every 34 days and constructed 20000 simulated datasets for each sampling interval. Hispanic or Latino of any race were 1.49% of the population. Comput: Vienna, Austria, 2013). and Sky Pond, located in Loch Vale watershed northwest of Denver, Colorado, United States, was sampled at Sky Pond outlet where Sky Pond drains to Icy Brook. 72, 467483 (2010). Hartmann, D. L., Tank, A. M. G. K. & Rusticucci, M. IPCC fifth assessment report, climate change 2013: The physical science basis. [18], In 1979, the State of North Carolina had prohibited any new connections to the antiquated water system. "Santeetlah Lake," undated pamphlet, Alcoa. The Challenge of Implementing Water Harvesting and Reuse in South Australian Towns (The University of Adelaide, 2006). Lakes as sentinels of climate change. Please select the information that is incorrect. provided. Temperatures were obtained from a consistent sampling location at or near the deepest portion of the lake. which is a beach area that has gradual slopes in the depth of the water as well as markers to keep kids and others in a confined area. B. 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). [10], In the early 1960s, a new corporation, Smoky Mountain Resorts, built a lodge and some cabins, and the first landowners began to build on the north shore of the peninsula. 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). information, Suggested citation: U.S. Geological Survey, 2023, National Water Information System data available on the World Wide Web, USGS Water and years The change in length of daylight between today and tomorrow is also listed when available. hydrologic (2013). Generally, the lakes were sampled from the surface to the maximum depth at 1m intervals at the deepest sampling location between 10:00 to 14:00, using analog and digital versions of the YSI temperature/DO probe (YSI models 58 and 95) (ref. For Manag. Colloq. S.Sh., D.K.G., J.S.R., C.M.O., J.D.L., A.Q., S.St. Data from current sites are relayed to USGS offices via satellite, telephone, and/or . 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. J.D.L., P.B.M., P.S., D.H., Stephanie E. Hampton, D.M.L., C.M.O., J.S.R. Water temperature; Wave heights; Radar & Lightning Radar & Lightning Radar. We compiled satellite-derived surface water temperatures from 154 lakes (Figure 1). Data for Plusssee were collected by the Max-Planck-Institute for Limnology, Ploen until 2006. Water. This technique provides a continuous temperature estimate and is robust against outliers in the observations helping to avoid sampling bias in the calculation of the 3-month mean. 94, 10311049 (2013). U.S. Route 129 passes just north of the town, leading southeast 6 miles (10km) to Robbinsville, the county seat, and northwest 9 miles (14km) to Tapoco at the Little Tennessee River. Slider with three articles shown per slide. We then merged the cloud-free observations from both series of instruments into a single dataset to maximize the sampling frequency. Data Sci. Global environmental change has influenced lake surface temperatures, a key driver of ecosystem structure and function. Plisnier, P. D. et al. Lake Samsonvale (North Pine Dam) is located in Queensland, Australia. We used the satellite data to calculate bulk water temperatures from skin temperatures using sensor-specific correction factors derived from the Laurentian Great Lakes11. Assess. 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. The population density was 332.4 people per square mile (129.3/km2). The samples were obtained from the region with greatest water depth within each lake. Water temperatures were recorded in the morning usually between 9:00 and 10:00 using a thermometer from an open water site in the middle of Upper Lake Constance (water column depth at sampling site: 252m) (ref. 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 . C.G. Samal, N. R. et al. Resources of the South Atlantic Water Science Center. For Sale: Lot/Land for sale,$425,000, 0.11 Acre, $3,863,636/Acre at Tbd Lakeside Trail, Robbinsville, NC 28711 1144 (2011). Taylor, M. W. & Hams, K. M. The physical and chemical limnology of Lake McConaughy with reference to fisheries management (Nebraska Technical Series No.9, Nebraska Game and Parks Commission, 1981). Lake Garda, located in northern Italy was sampled monthly from the surface at a depth of 0.5m. The samples were obtained from the centre of the lake, in the zone of maximum depth. & Bouten, W. RNCEP: Global weather and climate data at your fingertips. Water temperatures were recorded between 10:00 and 12:00 depending on the sampling day using reversing thermometers connected to the bottle for water sampling36. 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. The NOAA 5-channel Advanced Very High Resolution Radiometer (AVHRR) cloud imagery record began in 1981, and cloud statistics derived using Pathfinder Atmospheres Extended (PATMOS-x) processing system are available with global coverage70. hide format. Boston, MA warning41 Partly Cloudy. Santeetlah Lake: Great beach area! 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 every 100 females, there were 97.1 males. Discharge records are generally good except for estimated discharges, which . & Scholes, P. Managing the lakes of the Rotorua District, New Zealand. "Graham County: A Quiet Place in the Smokies," undated pamphlet, Graham County Travel and Tourism, Robbinsville, NC. & Anneville, O. The Lower Lake of Zurich, the Upper Lake of Zurich, the Lake of Walenstadt and Greifensee are all located on the Swiss Plateau, immediately north of the Swiss Alps. All lakes were sampled at a depth of 0.5m, in addition to several other depths depending on the maximum lake depth. J. Appl. Apparently Keyes hoped to build a large hotel complex in the area of the community now known as Chalet Village, and that area was graded in preparation for building. Sydney Catchment Authority. B.D., Stephanie E. Hampton and P.S. 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. Lake Santeetlah, July, has days with highs of 87F (31C) and lows of 66F (19C).The coldest month, January has days with highs of 45F (7C) and lows . The DWD series consisted of monthly measurements in 2m intervals from 0 to 20m and then in 10m intervals to the deepest point. 40 rivers / canals. We assembled a database of summer lake surface temperatures for 291 lakes collected in situ and/or by satellites for the period 19852009. 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. 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. 27, 30613074 (2013). Generally, water temperatures tend to coincide with regional air temperatures, warming or cooling at similar rates to that of air temperatures10,11. 2005 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. From 1999 to 2002 the CTD SBE 19 SeaCAT Profiler was used and thereafter the CTD SBE 19plus V2 SeaCAT profiler. Keyes, an evangelical Christian, was also finance chairman of the National Association of Evangelicals and a founder of the Presbyterian Church in America. The data are available in two comma delimited text files (Data Citation 1). [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]. Burragorang and Wingecarribee were sampled weekly. Water temperatures were measured in situ with either a YSI or Hydrolab data sonde in the morning, and calibration was done on the day or week of sampling against National Bureau of Standards thermometers. Water temperatures were collected at 8:00 with mercury thermometers (with an accuracy of 0.5C) prior to the 1990s and with digital thermometers in the 1990 and 2000s (ref. onward, The samples were obtained from the central monitoring station of Lake Kinneret, approximately 42m in depth. generated. This article about a location in Graham County, North Carolina is a stub. Annual The horizon is well defined and the outline of objects might be visible without artificial light. 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. Language links are at the top of the page across from the title. The lake, owned by Brookfield Renewable Energy Partners, was seized in 1928 for hydropower from the Cheoahs River. The same year a volunteer fire department and community center were constructed. These sites were Kaskesniemi, Noljakansaaret, Pyhsaari, and Kokonluoto, with maximum depths of 38, 13, 53, and 65m (ref. 3 reviews. 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). Lett. Google Scholar. Schindler, D. W. et al. year 162, 445464 (2005). WATER LEVEL. the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in 3, 6570 (2012). Provided by the Springer Nature SharedIt content-sharing initiative, Environmental Science and Pollution Research (2022), Environmental Monitoring and Assessment (2021), Scientific Data (Sci Data) Cloud cover can reduce incident solar radiation, but also result in greater longwave (atmospheric) radiation15. Ten years later, in 1998, a town hall was dedicated on the Fourth of July. The lake was sampled at the following depths: 0, 10, 25, 50, 100, 250m. The samples were obtained from a long-term station in the southern basin approximately 2.7km offshore from Bolshie Koty where the water depth is approximately 800m (ref. Anyone you share the following link with will be able to read this content: Sorry, a shareable link is not currently available for this article. report The motivation to assemble a global database of lake surface water temperatures, climatic forcing variables, and geomorphometric characteristics was to address two key scientific issues by the Global Lake Temperature Collaboration (www.laketemperature.org): i) What are the global and regional patterns of water temperature changes over the past 25 years and are they coherent over spatial and temporal scales? Fee, E. J., Hecky, R. E., Kasian, S. E. M. & Cruikshank, D. R. Effects of lake size, water clarity, and climatic variability on mixing depths in Canadian Shield lakes. Santeetlah Lake's current water temperature is 57F Todays forecast is, Clear With a high around 74F and the low around 37F. S.Sh. For Rabone, F. A. The reservoir is largely surrounded by the Cheoah District of the Nantahala National Forest. Water temperature sampling was performed using digital thermometers (YSI model 50B) by the Food and Agricultural Organization (FAO) of the United Nations from 19931996. Water temperature sampling was conducted continuously (in situ paper or sensor record), but compiled daily at midnight. Snucins, E. & Gunn, J. Interannual variation in the thermal structure of clear and colored lakes. The RMSE between satellite and in situ measurements for the 11 long-term summer mean lake surface temperatures was 1.15C. The highest monthly average temperature in Lake Santeetlah for July is 73.4 degrees. Res. In this manner, we were able to construct a relationship between sampling interval and error in our temperature estimates (Figure 4). We retrieved air temperature data at a height of 2m for each lake using the RNCEP package, a user-friendly package for use in the R programming language66. The per capita income for the town was $53,491. & Zimmerman, A. P. Empirical predictors of annual surface water temperature cycles in North American lakes. (pH is 7.00) or 100C. The most monthly precipitation in Lake Santeetlah occurs in December with 12.6 inches. led development and information acquisition for manuscript. The lakes were sampled monthly at the deepest points. For Sale: Lot/Land for sale,$295,000, 0.13 Acre, $2,269,231/Acre at Tbd Lakeside Trail, Robbinsville, NC 28711 To calculate seasonal means for this study we used temporally interpolated values representing 13:30 local time for cloud amount (fractional cloud cover) from a 1 re-gridded version of this dataset71. This novel dataset can be used to address additional research questions including those pertaining to understanding the mechanistic drivers of surface water temperature warming and ecological consequences of changes in lake temperatures. Lake Tarawera, located in North Island, New Zealand, was sampled monthly from the subsurface (20cm) to the bottom at 1m intervals. Girard, R. E., Yan, N. D., Heneberry, J. 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. 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. Accessibility & Brown, O. Limnol. J. Paleolimnol. 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