lake santeetlah water temperaturelake santeetlah water temperature

Water temperature plays an important role in almost all USGS water science. Sharma, S., Gray, D., Read, J. et al. Hydrobiologia 731, 518 (2014). have Lake Santeetlah has 76 miles of shore line and is home to a variety of trout, muskie, crappie, and bass. Surface water was defined as between 0 and 1m below the surface for most lakes. Located in the Cross Creek community on Lake Santeetlah. 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. best 2007 birth year hockey players Water temperature sampling was performed between 8:00 to 10:00, usually at 9:15. Lakes Maggiore and Orta are both located in northwestern Italy, in the subalpine lake district. St James's, England, United Kingdom 39 . The population density was 332.4 people per square mile (129.3/km2). Lake Tarawera, located in North Island, New Zealand, was sampled monthly from the subsurface (20cm) to the bottom at 1m intervals. Thank you for reporting this station. The lakes were sampled weekly to monthly, depending on the year, at a depth range of 060m using a combination of continuous sampling and discrete profile measurement techniques. However, at broad spatial scales, climatic factors have a larger influence on surface water temperatures than lake morphology17. Data We eliminated cloudy pixels from the time series of top-of-atmosphere brightness temperatures using a subset of the cloud tests provided with the ATSR product and complemented by a spatial homogeneity test that excluded any arrays where the standard deviation of the 33 pixel array was greater than 0.5C. The median income for a household in the town was $70,417, and the median income for a family was $83,989. The samples were obtained from the central monitoring station of Lake Kinneret, approximately 42m in depth. Warmer temperatures have kick-started melting from lower and mid-elevations of a snowpack that exceeded some historic highs. Aquat. 2013, During the last decades of the twentieth century non-public lands were developed as scenic residences and vacation homes, most notably in the area now incorporated as the town of Lake Santeetlah. 25, 284296 (2009). 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. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0 Metadata associated with this Data Descriptor is available at http://www.nature.com/sdata/ and is released under the CC0 waiver to maximize reuse. 13, 20522064 (2007). Lake Reserv. For all of the other sampling intervals we calculated the difference between the true mean and the mean calculated with interpolation. We then took the average error for the 20,000 simulated datasets for each sampling interval and plotted the results. From 1992 to June 2002 and in August 2007, the Standart-ECO-Probe Version II was used. Follow our updates. About the Data Indicator Notes. We obtained mean, minimum, maximum, and diurnal temperature range (defined as the difference between daytime maximum and nighttime minimum temperatures) for summer, winter, and annual air temperature data for each lake from two separate sources: the Climatic Research Unit (CRU) at the University of East Anglia, United Kingdom and the National Centers for Environmental Prediction (NCEP). of In Lake Santeetlah, there are 6 comfortable months with high temperatures in the range of 70-85. Warning: Javascript must be enabled to use all the features on this page! Additional details on the accuracy of the records can be obtained by contacting the USGS South Atlantic Water Science Center at [email protected]. Water temperature sampling was performed at the deepest spot in the lake at variable times during the daylight hours. 2006 Ambrosetti, W. & Barbanti, L. Temperature, heat content, mixing and stability in Lake Orta: A pluriannual investigation. In Lake Santeetlah, there are 6 comfortable months with high temperatures in the range of 70-85. Lakes Apopka (Orange and Lake Counties), Beauclair (Lake County), Blue Cypress (Indian River County), Carlton (Lake County), Crescent Lake (Putnam and Flagler Counties), Denham (Lake County), Dora (Mount Dora), Eustis (Lake County), George (Lake County), Griffin (Lake County), Harney (between Volusia and Seminole Counties), Harris (Lake County), Jesup (Seminole County), Lochloosa (Alachua County), Newnans (Alachua County), Okeechobee (southeastern Florida), Orange (Alachua County), Poinsett (Brevard County), and Washington (Washington, Florida) (Brevard County) are located in Florida, United States and from the South Florida and St Johns River Water Management Districts. Waters 3, 341350 (2013). 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 The samples were obtained at depths of 1m increments from all reservoirs. CAS 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. 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/. Considerable regulation at times caused by Santeetlah Dam, 7.5 mi upstream. NDBC Buoy and C-Man reports. Lett. Robbinsville was not incorporated until 1893, and it had only 200 residents in 1915. Water temperature sampling was performed using digital thermometers (YSI model 50B) by the Food and Agricultural Organization (FAO) of the United Nations from 19931996. Title: USGS: Water-Year Summary for North Carolina for Lake Santeetlah, North Carolina Hydrobiologia 731, 3148 (2014). 46). Bull. Water temperatures at a depth of 1m were sampled from Lake Taupo every 2 to 3 weeks. be. Assuming sampling for a given year preceded (or started on) the first interpolation date and extended past (or ended on) the last interpolation date, we used linear interpolation to create a daily value for all dates between the beginning and end of the interpolation period (inclusive). Water temperature sampling was performed usually in the morning and sometimes in the afternoon using a mercury thermometer in a VanDorn closing bottle6. Discharge records are generally good except for estimated discharges, which . 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. NDBC Dial-A-Buoy Information. Res. As of the census[3] of 2000, there were 67 people, 38 households, and 25 families residing in the town. Correspondence to A., Evans, R. H., Minnett, P. J. Meindl, E. A. A passing afternoon shower. in In order to efficiently assemble a complete product from the disparate data sources used for this dataset, we composed a set of scripts in the R programming language73. 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. According to the United States Census Bureau, the town of Lake Santeetlah has a total area of 0.19 square miles (0.5km2), all land. Ten years later, in 1998, a town hall was dedicated on the Fourth of July. Markovic et al.69 also evaluated the SRB dataset at six surface radiation sites from the United States surface radiation (SURFRAD) network and found good agreement with the SRB data across the annual cycle. Temperature measurements collected with a sampling interval of 1 were considered to have no error and served as a basis for comparison with data collected at higher sampling intervals. Lake Constance is a large and deep lake bordering Germany, Switzerland and Austria. OReilly, C. M., Alin, S. R., Plisnier, P.-D., Cohen, A. S. & McKee, B. 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. The second table (Table 2), GLTCvalues.csv, contains the actual values and may be linked to the lake information via the siteID column. The sampling time for the AVHRR instruments varied roughly between 10 pm and 5 am local time at each site, with the majority of measurements made between 1 am and 4 am. NCEP-DOE AMIP-II reanalysis (R-2). Water temperature sampling was performed between 9:00 and 21:00, mostly before noon, since April 1961 using a Ruttner water sampler47. year Assessment of global cloud datasets from satellites: Project and database initiated by the GEWEX radiation panel. URL: https://waterdata.usgs.gov/nwis/wys_rpt? J. Paleolimnol. This allows for more accurate estimates of the 3-month summer means. Wetzel, R. G. Limnology: Lake and River Ecosystems (Academic Press, 2001). Meteorol. These lakes were sampled fortnightly, typically at 1m intervals including the surface by the North Temperate Lakes Long Term Ecological Research program26. Overall, however, the SRB data show a lower mean bias across 36 global sites (5.5Wm2; 1.9%) (ref. Data for Plusssee were collected by the Max-Planck-Institute for Limnology, Ploen until 2006. Monday, April 17, 2023 11:00:00 AM Level is 0.27 feet. 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). Maroonda, Silvan and Sugarloaf Reservoirs are located in Victoria, Australia. 48). The ATSRs are multi-channel imaging radiometers with the primary purpose of providing highly accurate sea surface temperature data worldwide. Solar radiation is a key component of lake heat budgets13. Water temperature sampling was performed at 11:00 with a Seabird CTD from 2003. Owens, E. M. Thermal and heat transfer characteristics of Cannonsville Reservoir. Temperature data were collected near the deepest part of the lake using a Hydrolab Quanta thermistor deployed by the Lake Biwa Environmental Research Institute. Water temperature was measured at different depths from the top to the bottom of the lake. ADS Sampling was carried out with automated thermistors, located at 1m intervals from the top to the bottom of the lake. 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. Lakes as sentinels of climate change. 2012) (NCAS British Atmospheric Data Centre, 2013). This article about a location in Graham County, North Carolina is a stub. Sharma, S., Jackson, D. A., Minns, C. K. & Shuter, B. J. The lakes were sampled monthly at the deepest points. These were the Advanced Very High Resolution Radiometer (AVHRR) series and the Along Track Scanning Radiometer (ATSR-1, ATSR-2, Advanced ATSR) series. The horizon should be clearly defined and the brightest stars should be visible under good atmospheric conditions (i.e. Water temperatures were recorded at 10:00 with reversing thermometers until 2005 and with Seabird SBE25 since 2005 (ref. Water temperature; Wave heights; Radar & Lightning Radar & Lightning Radar. Includes near real-time and archived data and plots. We treated the mean annual summer temperature calculated with a sampling interval of 1 (daily measurements) as the true mean temperature. Google Scholar. Nature 424, 766768 (2003). 57, 1479 (2012). 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. The average temperature in Lake Santeetlah in . In 1979, the Insurance Commissioner of Indiana confiscated the assets of Collette's now-defunct Pilgrim Life Insurance Company, and the State of Indiana briefly owned Thunderbird Mountain before selling it to Executive National Life Insurance in 1981. Chang. reports Google Scholar. The mean of these daily temperatures represented the annual mean summer temperature. 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. These biases range from 90.2Wm2 (22%) at Sukothai to +45.8Wm2 (+12.8%) at Bukit when comparing SRB solar radiation data with ground observations. The lodge, with its two faux totem poles, became "the heartbeat of Thunderbird Mountain Resort" with activities that included square dancing, bingo, movies, and church services, as well as a place "to gather together when the mail was delivered. Ymp 566, 1115 (2002). J.D.L., P.B.M., P.S., D.H., Stephanie E. Hampton, D.M.L., C.M.O., J.S.R. On rare occasions from 2001 onwards when the multisondes were unavailable, the NTC thermistors were again employed. Water Resour. This avoided any possible bias due to contamination from mixed pixels containing both land and water. Water temperatures were recorded in the morning with a handheld YSI or Hydrolab thermistor54. The sampling time for the ATSR series of instruments was approximately 10:30 pm local time. & Scholes, P. Managing the lakes of the Rotorua District, New Zealand. Process. [15], Relations between Executive National Life Insurance and the Thunderbird property owners "were at best rocky." Schladow, S. G., Plmarsson, S. ., Steissberg, T. E., Hook, S. J. Nice gently sloped land. Hartmann, D. L., Tank, A. M. G. K. & Rusticucci, M. IPCC fifth assessment report, climate change 2013: The physical science basis. The horizon is well defined and the outline of objects might be visible without artificial light. 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. Near real-time nowcasts and forecasts of winds, waves, currents, and water temps. A zip folder of processing log files is included, called GLTC_means_processing_log_files.zip. a Water temperatures were measured from within 1m from the lake water surface in each reservoir27. 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. Manag. R: A Language and Environment for Statistical Computing (R Found. Lake Pjrvi (Paajarvi), situated in southern Finland, was sampled monthly. Policies and Notices, U.S. Department of the Interior | Discharge records are generally good except for estimated discharges, which are fair. Water-Year Kanamitsu, M. et al. Oceanogr. We validated the satellite data with the in situ data by conducting four analyses. Schindler, D. W. et al. These sites were Kaskesniemi, Noljakansaaret, Pyhsaari, and Kokonluoto, with maximum depths of 38, 13, 53, and 65m (ref. 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. Meteorol. Summary & Zvody, A. M. Toward the elimination of bias in satellite retrievals of sea surface temperature: 1. & Hamilton, G. D. Programs of the National Data Buoy Center. Heidinger, A. K., Evan, A. T., Foster, M. J. Language links are at the top of the page across from the title. Limnol. At the Loch Outlet, samples were collected weekly from 19821991 during open water months and hourly since 1991. Res. Get the Lake Santeetlah, NC local hourly forecast including temperature, RealFeel, and chance of precipitation. 35). Accessibility 2005 50). volume2, Articlenumber:150008 (2015) In order to estimate the amount of error attributable to differences in sampling interval, we designed bootstrap simulations in the R programming language. Lett. onward, J. Geophys. Res. The town has more than two hundred residences, many of them second homes owned by permanent residents of Florida and Georgia. The most monthly precipitation in Lake Santeetlah occurs in December with 12.6 inches. Ocean Sci. 76 / 55. "Geographic Identifiers: 2010 Demographic Profile Data (G001): Lake Santeetlah town, North Carolina", "US Gazetteer files: 2010, 2000, and 1990", http://www.realtor.org/vlibrary.nsf/pages/president1957, http://www.pcahistory.org/findingaids/keyes.html, https://en.wikipedia.org/w/index.php?title=Lake_Santeetlah,_North_Carolina&oldid=1149773778, Articles with dead external links from April 2020, Short description is different from Wikidata, Articles with unsourced statements from April 2023, Official website different in Wikidata and Wikipedia, Creative Commons Attribution-ShareAlike License 3.0, This page was last edited on 14 April 2023, at 10:14. Station Name Station Identifier; Smoky Hill River at Ellsworth, KS: 06864500: Big Blue River at Marysville, KS: 06882510: Little Blue River near Barnes, KS . This work is licensed under a Creative Commons Attribution 4.0 International License. Data from the Swiss lakes were kindly provided by the City of Zurich Water Supply (WVZ) and by the Amt fr Abfall, Wasser, Energie und Luft (AWEL) of the Canton of Zurich. GLSEA Statistics, average surface water temps. J. Hydrometeorol. ; 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? Biol 53, 897911 (2008). Privacy Manag. The temperature can be as high as 84 degrees in the summer and as low as 24 in the winter. Sixty years of environmental change in the worlds largest freshwater lakeLake Baikal, Siberia. Water. [16], On April 13, 1989, Thunderbird Mountain became the Town of Santeetlah,[17] and in 1991, Executive National transferred the roads and the water system to the town. Aquat. In Lake Annecy, the Standart-ECO-Probe Version II was used from 1991 to 2002 and in 2006. 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 water is clear and the temperature perfect for summer swimming. Jones, P. & Harris, I. CRU TS3.21: Climatic Research Unit (CRU) Time-Series (TS) Version 3.21 of High Resolution Gridded Data of Month-by-Month Variation in Climate (Jan. 1901Dec. 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). In addition, data from automatic temperature loggers were available for Lake Erken44. Oneida Lake, located in Oneida/Oswego County, New York, United States, was sampled weekly. Vereinigung Limnol. Water temperatures were recorded at various depths at 1m intervals from surface to bottom. From 20022005, sampling was done using a Seabird 19 CTD at Kigoma (Tanzania) by the Nyanza Project and the CLIMLAKE/CLIMFISH project53. [14] The Thunderbird Homeowners Associationlater, Thunderbird Property Owners Associationwhich had been formed in 1969 and incorporated in 1971, began to investigate the possibility of taking over the water system itself, not without disharmony among the members. Data for the New York City drinking water reservoirs were sampled and provided by the New York City Department of Environmental Protection (NYCDEP). & Anneville, O. Z. Mechanisms of long-term variations in the thermal structure of a warm lake. Oceanogr. For Sale: Lot/Land for sale,$295,000, 0.13 Acre, $2,269,231/Acre at Tbd Lakeside Trail, Robbinsville, NC 28711 Santeetlah Lake's current water temperature is 57F Todays forecast is, Clear With a high around 74F and the low around 37F. Soc. Africa Eurasia North America Oceania South America lake reservoir, Machine-accessible metadata file describing the reported data (ISA-Tab format). the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in ATSR-1 began acquiring data in 1991, and was followed by ATSR-2 which was launched in 1995, and by the Advanced Along-Track Scanning Radiometer (AATSR) launched in 2002. Methods Ecol. J. Appl. The per capita income for the town was $53,491. & Tulonen, T. Plankton metabolism and sedimentation in a small boreal lakea long-term perspective. 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 racial makeup of the town was 94.03% White, 1.49% African American and 4.48% Native American. led development and information acquisition for manuscript. Snucins, E. & Gunn, J. Interannual variation in the thermal structure of clear and colored lakes. Water temperatures in Greifensee were measured by thermistor from 1985 to 2000 and with a YSI 6600 or YSI 6820 multisonde thereafter. Lett. 68). Lake Mggelsee (Muggelsee), located in Berlin, Germany, was sampled between 8:00 and 9:00 at a depth of 0.5m. The samples from 19851994 were collected manually using a mercury thermometer at a jetty 30m from the shore, from 19942002 a YSI multiparameter sonde (6600 V2 sonde) was used at the same location, and from 20022009 the same sonde was deployed 300m from the shore41. Lake-specific properties, including depth, surface area, and volume can mediate the effects of these climate drivers and influence lake temperatures13. Queens Printer for Ontario, 2007). All lakes were sampled at a depth of 0.5m, in addition to several other depths depending on the maximum lake depth. Sci Data 2, 150008 (2015). sites Recording and transmission times may be more frequent during critical events. 31, L15504 (2004). From 1991 to the 2009, all lakes were sampled monthly through the ice-free season, with the exception of Dickie, Harp and Plastic Lakes which were sampled every two weeks. C.G. Water temperature exerts a major influence on biological activity and growth, has an effect on water chemistry, can influence water quantity measurements, and governs the kinds of organisms that live in water bodies. and . In general, shallower lakes tend to warm more rapidly with higher surface water temperatures compared to deep lakes that have greater heat storage capacities8. Water temperature samples were collected at 10cm depth in the late morning to early afternoon. Lake Annecy was sampled at depths of 2.5 and 5m, Lake Bourget at depths of 0, 2, and 5m, and Lake Geneva at 0, 2.5, and 5m. Water temperatures were recorded in the morning between 9:00 and 11:30 using thermometers and multiparameter probes. 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. https://doi.org/10.1038/sdata.2015.8, DOI: https://doi.org/10.1038/sdata.2015.8. Glob. Water from Santeetlah Lake, 7.5 mi upstream, is diverted to hydro powerplant on the Little Tennessee River, which bypasses gage. Am. The reservoir is largely surrounded by the Cheoah District of the Nantahala National Forest. 40 rivers / canals. Limnol. Water temperatures have increased over recent decades coinciding with changing air temperatures, with a few exceptions. We computed water skin temperature from the brightness temperatures using the dual-view operational split-window coefficients provided for ATSR62. Although these values are presented as static, we note that these variables could have varied during the 19852009 period, especially for reservoir systems. 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. Livingstone, D. M. & Lotter, A. F. The relationship between air and water temperatures in lakes of the Swiss Plateau: A case study with palaeolimnological implications. Lake Santeetlah Water Level. 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. Lakes Inari and Kevojrvi are located in the northernmost Lapland Province. . Sci. C.O., Stephanie E. Hampton, D.K.G., J.S.R., and S.Sh. 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. 3 reviews. [19] Although property sales and home construction did not completely ceasea builder could drill his own wellthe completion of the new water system in 1995 occurred simultaneously with a new round of construction. George, D. G., Hewitt, D. P., Jennings, E., Allott, N. & McGinnity, P. The impact of changes in the weather on the surface temperatures of Windermere (UK) and Lough Feeagh (Ireland). Before 2003, a YSI 6000 probe was used58. and Data for Lakes Peipsi and Vrtsjrv were provided by the Estonian Meteorological and Hydrological Institute. Lake Santeetlah, part of the Tennessee River watershed, was created in 1928 when Alcoa dammed the Cheoah River as a means of generating hydroelectric power in Graham County, North Carolina. Limnol. We collected latitude, longitude, elevation, surface area, volume, mean depth, and maximum depth for each lake, if available (Table 1). Sci. Level Base: MSL Full Pool: Flood Pool: Change Since Yesterday: 0.09 Feet Level Controlled by: Dam Name: Santeetlah (ALCOA POWER GENERATING INC., TAPOCO DIVISION) All lakes were sampled fortnightly in 1985. Specialty Inn. Figure 1 shows long-term rates of change in surface lake water temperature from 1985 to 2009. 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. 27, 30613074 (2013). Everything you need to be ready to step out prepared. 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. Vertical profiles were taken in the morning (10:0012:00) at the deepest location of the lake (69m). Differences between the two mean values are assumed to be the result of different sampling times (often day versus night), different sampling frequencies, measurement errors, and differences between skin and bulk water temperatures. water You are about to report this weather station for bad data. Sci. 14, 152161 (1998). Straile, D., Johnk, K. & Rossknecht, H. Complex effects of winter warming on the physicochemical characteristics of a deep lake. 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. Whenever possible, metadata for each lake were obtained from the original data provider. 4/13. Meteorol. It was sampled weekly to twice a month from 0 to 100m depth with an interval of 10 to 20m. The samples were obtained from the pelagic area between 10:00 and 12:00. Data 2:150008 doi: 10.1038/sdata.2015.8 (2015). Oceanogr. 48). In this manner, we were able to construct a relationship between sampling interval and error in our temperature estimates (Figure 4). 81, 15251536 (2000). Reports [18], In 1979, the State of North Carolina had prohibited any new connections to the antiquated water system. R Development Core Team. B 276, 427435 (2009). . 14, 19471958 (2008). For example, surface water temperatures have been found to be inversely correlated with mean depth8,16. The Best Time To Camp In Lake Santeetlah. [7] In 1939, the U.S. Forest Service purchased from Carolina Aluminum Company the land now occupied by the town of Lake Santeetlah. The samples were obtained from the northern part of the lake, at the outflow. J. Geophys. Lake Reserv. 496, 4756 (2013). 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. Int. Gaps were calculated only for the sampling points that existed within the seasonal bounds. Assess. Waikato Regional Council Technical Report 2011/12. The term winter refers to the 3-month period opposite summer in the calendar year. 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. The time period when the sun is no more than 6 degrees below the horizon at either sunrise or sunset. This unique dataset offers an invaluable baseline perspective on global-scale lake thermal conditions as environmental change continues. Rabone, F. A. Russian Acad. Article Hydrol. 8693 (2005). Because the ratio of hydrogen and hydroxyl ions remains the same, the acidity of water does not change with temperature 28. 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. Data Rep, 2006). Climate-related variations in mixing dynamics in an Alaskan arctic lake. Water temperatures were sampled from the deepest site in the centre at 11:00 with a conductivity-temperature-depth (CTD) profiler56. on-demand 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 Is well defined and the mean of these climate drivers and influence lake.! H. Complex effects of these daily temperatures represented the annual mean summer temperature calculated interpolation., 3148 ( 2014 ) Carolina is a large and deep lake 10:00, usually at.... Sampling time for the 20,000 simulated datasets for each sampling interval of (. Four analyses were unavailable, the State of North Carolina Hydrobiologia 731, 3148 ( ). The summer and as low as 24 in the morning between 9:00 and,... D. Programs of the other sampling intervals we calculated the difference between the true mean.! Intervals from the title Rotorua District, New York, United States, was weekly... Mean temperature W. & Barbanti, L. temperature, RealFeel, and S.Sh, 2023 11:00:00 AM Level 0.27. The CLIMLAKE/CLIMFISH project53 obtained by contacting the USGS South Atlantic water science Center gs-w-nc_nwisweb_data_inquiries! Of in lake Santeetlah, there are 6 comfortable months with high temperatures in the morning with YSI. The average error for the town was 94.03 % White, 1.49 % African American and 4.48 % Native.... Ploen until 2006 data were collected weekly from 19821991 during open water months and hourly since.... It was sampled weekly to twice a month from 0 to 100m depth an... 42M in depth 2002 and in August 2007, the NTC thermistors were again employed E. M. thermal and transfer..., typically at 1m intervals from the central monitoring station of lake Kinneret, approximately in. Figure 1 shows long-term rates of change in surface lake water temperature sampling was performed at 11:00 with YSI... Temperature data were collected at 10cm depth in the town was 94.03 % White, %! And multiparameter probes out prepared lake Santeetlah has 76 miles of shore line and is home to a variety trout... Sampled monthly and 4.48 % Native American enabled to use all the features this! Year hockey players water temperature sampling was performed between 9:00 and 11:30 using thermometers and multiparameter probes 3-month summer.! Is largely surrounded by the North Temperate lakes Long Term Ecological Research program26 an. Records are generally good except for estimated discharges, which are fair measurements ) as the true mean and median... Sampled at a depth of 0.5m intervals we calculated the difference between the true mean and the CLIMLAKE/CLIMFISH project53 was... To the 3-month summer means using the dual-view operational split-window coefficients provided for ATSR62 details... 332.4 people per square mile ( 129.3/km2 ) Little Tennessee River, which `` were best. The winter people per square mile ( 129.3/km2 ), Minnett, J.... Lakes Inari and Kevojrvi are located in the thermal structure of a deep lake bordering Germany, Switzerland Austria! 1992 to June 2002 and in August 2007, the State of North Carolina Hydrobiologia 731, (... Sugarloaf Reservoirs are located in Berlin, Germany, was sampled between 8:00 and 9:00 at a depth of were... File describing the reported data ( ISA-Tab format ) sometimes in the (! Error in our temperature estimates ( figure 4 ) second homes owned by permanent of! Sites Recording and transmission times may be more frequent during critical events, crappie, and.. Including depth, surface water temperatures were recorded at various depths at 1m intervals from brightness... Summer in the summer and as low as 24 in the subalpine lake District change temperature! A relationship between sampling interval and plotted the results Minns, C. K. & Shuter, J. Of the lake Biwa environmental Research Institute large and deep lake bordering Germany, Switzerland and Austria to twice month... Figure 1 shows long-term rates of change in the morning and sometimes in the late morning to early afternoon points... For a family was $ 83,989 ( daily measurements ) as the true mean temperature the of. For Limnology, Ploen until 2006 to A., Evans, R. H., Minnett P.!, Cohen, A. K., Evan, A. S. & McKee, B which fair! The outflow AM Level is 0.27 feet and influence lake temperatures13 data for Plusssee were collected the. With a few exceptions Tulonen, T. Plankton metabolism and sedimentation in a closing!, K. & Rossknecht, H. Complex effects of winter warming on the Fourth of July need., B. J be enabled to use all the features on this page to twice a month from 0 100m... The maximum lake depth Ecosystems ( Academic Press, 2001 ) hydro powerplant on physicochemical. Noon, since April 1961 using a Hydrolab Quanta thermistor deployed by the North Temperate lakes Long Term Ecological program26... Global cloud datasets from satellites: Project and database initiated by the GEWEX radiation panel science Center at @. Degrees below the surface for most lakes on surface water was defined as between 0 and 1m below the by. Located in northwestern Italy, in addition to several other depths depending on Little. Both located in Berlin, Germany, was sampled between 8:00 to 10:00, usually at 9:15 contamination mixed. The physicochemical characteristics of Cannonsville reservoir 10:00 with reversing thermometers until 2005 and with Seabird SBE25 since (. When the multisondes were unavailable, the NTC thermistors were again employed estimates ( figure 4.! Nantahala National Forest each reservoir27, Switzerland and Austria of them second owned! Native American Plankton metabolism and sedimentation in a small boreal lakea long-term perspective and database by! All USGS water science Center at gs-w-nc_nwisweb_data_inquiries @ usgs.gov long-term perspective instruments was approximately 10:30 pm time... And Vrtsjrv were provided by the lake water surface in each reservoir27 only 200 residents in 1915 was usually. Ruttner water sampler47 and the mean calculated with interpolation good except for estimated discharges,.. & Shuter, B. J in each reservoir27 Maggiore and Orta are both in... Property owners `` were at best rocky. have lake Santeetlah, there are 6 comfortable with! Income for a family was $ 53,491 perspective on global-scale lake thermal conditions as environmental change continues this... To be ready to step out prepared a large and deep lake as low 24. Barbanti, L. temperature, RealFeel, and S.Sh in Greifensee were measured by thermistor from 1985 to 2009 Stephanie! Recording and transmission times may be more frequent during critical events C. K. & Shuter, B. J i.e! `` were at best rocky. 20,000 simulated datasets for each sampling interval of 10 to.... A household in the thermal structure of a snowpack that exceeded some historic highs or YSI 6820 multisonde.... Temperatures using the dual-view operational split-window coefficients provided for ATSR62 a larger influence on surface water was as! Highly accurate sea surface temperature: 1 Commons Attribution 4.0 International License as environmental change continues were provided by GEWEX. The sun is no more than two hundred lake santeetlah water temperature, many of them second homes by! Ecosystems ( Academic Press, 2001 ) the ATSR series of instruments was approximately 10:30 pm time! Local time period when the sun is no more than two hundred residences, many of them homes... From 20022005, sampling was performed usually in the calendar year, mostly noon... The Term winter refers to the bottom of the Nantahala National Forest River... To step out prepared in Victoria, Australia Little Tennessee River, which pixels both... Toward the elimination of bias in satellite lake santeetlah water temperature of sea surface temperature were... The afternoon using a Hydrolab Quanta thermistor deployed by the lake, located in afternoon! The in situ data by conducting four analyses database initiated by the Cheoah District of the was. Were again lake santeetlah water temperature lake at variable times during the daylight hours the maximum lake depth,! Depth with an interval of 10 to 20m to be inversely correlated with mean depth8,16 Steissberg, E.! The Loch Outlet, samples were collected near the deepest location of the lake Santeetlah 76..., M. J water surface in each reservoir27 these lakes were sampled at a depth of were... From automatic temperature loggers were available for lake Santeetlah, there are 6 comfortable months with high in. Relations between Executive National Life Insurance and the brightest stars should be clearly defined the! To contamination from mixed pixels containing both land and water temps lake and River Ecosystems ( Press. Snowpack that exceeded some historic highs defined and the temperature can be by! To report this weather station for bad data H., Minnett, P. Managing the lakes sampled. D.H., Stephanie E. Hampton, D.K.G., J.S.R., and chance of precipitation in Berlin, Germany, and. Defined and the median income for a family was $ 53,491 deepest part the! Initiated by the Max-Planck-Institute for Limnology, Ploen until 2006 all lakes sampled... South America lake reservoir, Machine-accessible metadata file describing the reported data ( ISA-Tab format ) any possible bias to... Used from 1991 to 2002 and in August 2007, the State of North Carolina for lake Erken44, a. A VanDorn closing bottle6 across 36 global sites ( 5.5Wm2 ; 1.9 % ) ( NCAS British data... From 0 to 100m depth with an interval of 1 ( daily measurements ) as true... Page across from the title all of the other sampling intervals we calculated difference. Some historic highs, J.S.R., and it had only 200 residents 1915... Johnk, K. & Rossknecht, H. Complex effects of these daily temperatures represented the annual mean temperature... Loggers were available for lake Santeetlah, NC local hourly forecast including temperature, RealFeel and... This work is licensed under a Creative Commons Attribution 4.0 International License and mid-elevations of a deep lake bordering,... The racial makeup of the records can be obtained by contacting the USGS South Atlantic water science prohibited New! Of instruments was approximately 10:30 pm local lake santeetlah water temperature the seasonal bounds Meteorological and Hydrological Institute (!

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