lake santeetlah water temperaturelake santeetlah water temperature
Santeetlah Lake: Great beach area! Am. In the earlier years, a thermometer assembled in a Ruttner water sampler was used, and following 2000, temperature was recorded using a thermistor40. The DWD series consisted of monthly measurements in 2m intervals from 0 to 20m and then in 10m intervals to the deepest point. 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. 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. Water temperatures were recorded in the morning with a handheld YSI or Hydrolab thermistor54. The time period when the sun is between 6 and 12 degrees below the horizon at either sunrise or sunset. Page Contact Information: North Carolina Water Data Maintainer Schneider, P. & Hook, S. J. Arch. FOIA The U.S. Geological Survey (USGS) has been measuring . Rossow, W. B. reports water Water Resour. 25, 284296 (2009). From 19602004, a paper chart recorder with a mercury thermometer was used. Oceanogr. 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. 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. Lake Rotorua, located in North Island, New Zealand, was sampled monthly at depths of 01 and 18m. The samples were obtained from the southeast part of the lake. Discharge records are generally good except for estimated discharges, which are fair. 29, 22262240 (2009). However, the name change produced some semantic curiosities. All lakes were sampled at a depth of 0.5m, in addition to several other depths depending on the maximum lake depth. Schindler, D. W. et al. The views are nothing short of breathtaking. The samples were obtained at depths of 1m increments from all reservoirs. April for a typical day ranges from a high of 68F (20C) to a low of 46F (8C).Some would describe it as moderately chilly with a gentle breeze.For comparison, the hottest month in . 50). Data for Plusssee were collected by the Max-Planck-Institute for Limnology, Ploen until 2006. TOMORROW'S WEATHER FORECAST. 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. Feet MSL. Wetzel, R. G. Limnology: Lake and River Ecosystems (Academic Press, 2001). Annual Water Quality Monitoring Report 2010-11. & Prata, F. E. An extraordinary upwelling event in a deep thermally stratified lake. Colloq. The Lake Annie Buoy is located near the centre, over the deepest part (20.4m) of Lake Annie, Highlands County, Florida. A passing afternoon shower. Limnol. 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. All lakes were sampled daily at a depth of 0.2m from sites close to the water level gauge. Satellite observations indicate rapid warming trend for lakes in California and Nevada. 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]. Oceanogr. Bull. 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. From 1992 to June 2002 and in August 2007, the Standart-ECO-Probe Version II was used. for Specifically, from 1991 to 1997, the Idronaut Ocean Seven 401 was used, from 1998 to 2008, the Seacat SBE 19-03 was used, while from 2009-present, the Idronaut Ocean Seven 316Plus37 was used. Samples were obtained from five sites in Burrangorang, specifically from 14km south of the dam wall (079m), 4km from Butchers (033m), 9km south of the dam wall (051m), at Woll arm (060m), and 500m south of the dam wall (0100m). . Aquat. ADS Dokulil, M. T. Predicting summer surface water temperatures for large Austrian lakes in 2050 under climate change scenarios. & Rouse, W. R. Thermal characteristics and energy balance of various-size Canadian Shield lakes in the Mackenzie River Basin. North, R. P. et al. https://en.wikipedia.org/w/index.php?title=Lake_Santeetlah&oldid=1000692201, Bodies of water of Graham County, North Carolina, Protected areas of Graham County, North Carolina, Short description is different from Wikidata, Articles using infobox body of water without alt, Articles using infobox body of water without image bathymetry, Creative Commons Attribution-ShareAlike License 3.0, This page was last edited on 16 January 2021, at 07:01. Warning: Javascript must be enabled to use all the features on this page! Lakes Inari and Kevojrvi are located in the northernmost Lapland Province. Hydrol. The samples were obtained from four different locations on the same lake. Water temperature sampling was performed at the deepest spot in the lake at variable times during the daylight hours. Facebook . 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. GLSEA Statistics, average surface water temps. 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. The time of Civil Sunset minus the time of Civil Sunrise. We also calculated gap lengths, which were the intervals in days between sequential sampling times. Lake Plusssee, located in northern Germany, was sampled weekly since 1985 at depths of 0 to 15m with intervals of 1m and at 20, 25, and 26m. The samples were obtained from the middle of the lake, above the deepest spot. Schladow, S. G., Plmarsson, S. ., Steissberg, T. E., Hook, S. J. 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. URL: https://waterdata.usgs.gov/nwis/wys_rpt? 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. [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. . Results indicate that the downwelling solar irradiance shows good overall agreement with ground measurements, except for a few large biases in Southeast Asia (Sukothai, Bukit, and Kogma). Lake Tarawera, located in North Island, New Zealand, was sampled monthly from the subsurface (20cm) to the bottom at 1m intervals. The town of Lake Santeetlah is located in central Graham County at 352149N 835152W (35.363578, -83.864367), [6] on a peninsula on the northern side of Lake Santeetlah, a reservoir on the Cheoah River, a northward-flowing tributary of the Little Tennessee River. The RMSE between satellite and in situ measurements for the 11 long-term summer mean lake surface temperatures was 1.15C. The same procedure was used for cleaning and calibration of both instruments. [7] In 1939, the U.S. Forest Service purchased from Carolina Aluminum Company the land now occupied by the town of Lake Santeetlah. and JavaScript. In Lake Annecy, the Standart-ECO-Probe Version II was used from 1991 to 2002 and in 2006. We thank Tim Kratz for helping with the initiation of this project. For every 100 females age 18 and over, there were 100.0 males. Sci. 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. Water. 162, 445464 (2005). year From January 20 2005, sampling depth changed from 0 to 1m (ref. 42). Recent studies have suggested significant warming of water temperatures in individual lakes across many different regions around the world. Lake McConaughy is a regulated reservoir located near Ogallala, Nebraska, United States. 7, 776780 (2010). Temperatures were obtained from a consistent sampling location at or near the deepest portion of the lake. For undetermined reasons he called the property "Thunderbird Estates". An independent assessment of pathfinder AVHRR sea surface temperature accuracy using the marine atmosphere emitted radiance interferometer (MAERI). Remote Sens. Sharma, S. Long Term Ecological Research Network https://doi.org/10.6073/pasta/379a6cebee50119df2575c469aba19c5 (2015) et al. and led development and information acquisition for manuscript. Use the Previous and Next buttons to navigate the slides or the slide controller buttons at the end to navigate through each slide. Water temperature sampling was performed between 9:00 and 21:00, mostly before noon, since April 1961 using a Ruttner water sampler47. 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. #6 of 9 specialty lodgings in Robbinsville. We only used night time data in this study. Limnol. Google Scholar. 46). Science 250, 967970 (1990). Google Scholar. [4] The full-time population was 67 at the 2000 census and dropped to 45 in 2010.[5]. All remaining authors provided water temperature and geomorphometric data, summarized how data were acquired and sampled, verified data, and revised the manuscript. 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. At high sampling intervals (panel c), linear interpolation can underestimate daily temperatures, leading to an underestimate of the mean summer temperature. J. 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. We used sampling intervals ranging from once per day to once every 34 days and constructed 20000 simulated datasets for each sampling interval. year. Water temperature samples were collected at 10cm depth in the late morning to early afternoon. 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. hide Glob. The mean of these daily temperatures represented the annual mean summer temperature. Santeetlah Reservoir is located on the Cheoah River in North Carolina, USA, in the state of South . an sites 48). The date of the first sample for each of the 20000 datasets was chosen as a random date in June and then the following samples were equally spaced in time starting from that date. B 276, 427435 (2009). Water temperatures were recorded at 10:00 with reversing thermometers until 2005 and with Seabird SBE25 since 2005 (ref. ADS A lawsuit by the insurance company was dismissed by the court, and the company became more amenable to the formation of an incorporated town. 14, 19471958 (2008). 48). However, there are some regions, such as around the Great Lakes region of North America and northern Europe, in which bodies of water are warming more rapidly than ambient air11,12. & Zvody, A. M. Toward the elimination of bias in satellite retrievals of sea surface temperature: 1. 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. To ensure that the geomorphometric data in the completed dataset were accurate we had several individuals independently check the values against reputable sources. We validated the satellite data with the in situ data by conducting four analyses. 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. 94, 10311049 (2013). J. Plankton Res. We subsequently computed the mean temperature of a 3-month period over all 92 daily values obtained from the fitted LOWESS curve. The second table (Table 2), GLTCvalues.csv, contains the actual values and may be linked to the lake information via the siteID column. The sun does not contribute to the illumination of the sky before this time in the morning, or after this time in the evening. MacIntyre, S. et al. 72, 467483 (2010). 45, 10581066 (2000). 22, 533535 (1984). Environ. mark anderson obituary; go section 8 houses for rent 60628; fandango gift card on roku; how to unlock holy mantle for the lost; ode to dirt literary devices; paris hilinski jordan; An average temperature was only computed if at least 20 valid cloud-free satellite retrievals were available in a given 3-month period, to ensure that the observations adequately characterize the temperature curve. Meteorol. Lake Samsonvale (North Pine Dam) is located in Queensland, Australia. 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 insurance company did not repair the water system or provide other services specified by the restrictive covenants, and many property owners stopped paying their fees. Stat. In 2008 and 2009, the CTD 90M multiparameter probe was used. For these simulations, we used temperature records from six sites on four lakes that had daily temperature data available (Figure 3). Bull. U.S. Geological Survey The first, GLTClakeinformation.csv, contains information for each lake, who collected the data, lake location and surroundings. Lake Taihu, located near Shanghai, China was sampled monthly at a depth of 0.20.5m. The samples were obtained at two locations near the lake centre and two locations in Meiliang Bay. Sharma, S., Walker, S. C. & Jackson, D. A. Empirical modelling of lake water-temperature relationships: A comparison of approaches. Lake values were the mean of all months within the appropriate time period to match the sampling period (e.g., July-August-September for northern hemisphere summer, January-February-March for northern hemisphere winter), see Section G below) for a given year for the single grid cell that contained the sampling location for the lake. Sharma, S., Jackson, D. A., Minns, C. K. & Shuter, B. J. Water temperature sampling was performed manually with a mercury thermometer until April 30, 2011 (ref. 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 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. J. 41, 912920 (1996). Whenever possible, metadata for each lake were obtained from the original data provider. 51, 11291144 (2012). organized, processed, verified, and collated data. Clearwater, Hannah, Lohi, Middle, Sans Chambre, Swan and Whitepine Lakes are all located near Sudbury, Ontario, Canada. Water temperature sampling was conducted continuously (in situ paper or sensor record), but compiled daily at midnight. We defined the maximum gap as the maximum of all gaps for a single year. For every 100 females, there were 97.1 males. In order to estimate the amount of error attributable to differences in sampling interval, we designed bootstrap simulations in the R programming language. These instruments are part of an autonomous monitoring program with the vertical profiler replacing the thermistor strings in May 2009. No need to worry about drilling a well, community water is available! [24], The nearby Cheoah River is noted for its Class IV and V whitewater rapids, available for use approximately seventeen days a year depending on the water-release schedule from Santeetlah Dam. Adrian, R. et al. In Lake Bourget, water temperature was measured with the ISMA probe DNTC (Ponselle) in 1985. In 2007 the town announced that tax revenues from escalating property values were accumulating so quickly that it had decided to slightly reduce millage rates.[21]. Data 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). Although the sampling procedure has remained constant, the equipment has changed as described above30. Lake Santeetlah, NC 10-Day Weather Forecast. Geophys. Science 287, 17701774 (2000). Additionally, monthly grab samples were taken at 1m intervals at the dam wall site using a variety of handheld instruments and more recently using a YSI 6600v2. [15], Relations between Executive National Life Insurance and the Thunderbird property owners "were at best rocky." 47). and Oceanogr. Warmer temperatures have kick-started melting from lower and mid-elevations of a snowpack that exceeded some historic highs. Effects of changing climate on zooplankton and juvenile sockeye salmon growth in southwestern Alaska. Sci. & Anneville, O. The Loch, located in Loch Vale watershed northwest of Denver, Colorado, United States, was sampled at the outlet directly upstream of Parshall Flume (Loch Outlet). Ymp 566, 1115 (2002). Lett. 12879 lakes / reservoirs. Water temperature samples were collected at 10cm depth in the early afternoon. Lake Pijnne is located south of the city, Jyvaskyla, Lake Pielinen is located in North Karelia, and Lake Saimaa is located in southeastern Finland. Water-Year The reservoir is largely surrounded by the Cheoah District of the Nantahala National Forest. 2014 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) Water temperature sampling was conducted using a Celsius mercury thermometer. Take control of your data. Schneider, P. et al. Waikato Regional Council Technical Report 2011/12. Limnol. At the coordinates selected for each site, we extracted a 33 pixel array of thermal infrared data for each nighttime overpass. 496, 4756 (2013). The median household income of Lake Santeetlah is $66,500, with an employment rate of 12.5%. Maroonda, Silvan and Sugarloaf Reservoirs are located in Victoria, Australia. The lodge was demolished in 2020. Z. Mechanisms of long-term variations in the thermal structure of a warm lake. Current weather in Lake Santeetlah, NC. Dorset Environmental Science Centre lakes have been sampled under the supervision of two senior technicians, Robert Girard and Ron Ingram, and two research scientists, Norman Yan and Andrew Paterson. Measurements were made twice a month at 0.5, 5, 10, 15, 20, 30, 40, 60, 80m, and bottom (approximately 9095m) (ref. Meindl, E. A. ATSR-1, ATSR-2 and AATSR stopped acquiring useful data in 1996, 2003, and 2012, respectively. Bull. 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. Hydrobiologia 625, 117134 (2009). Space observations of inland water bodies show rapid surface warming since 1985. Water temperatures at a depth of 1m were sampled from Lake Taupo every 2 to 3 weeks. Effects of climatic warming on lakes of the central Boreal Forest. 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. 4/13. Station Name Station Identifier; Smoky Hill River at Ellsworth, KS: 06864500: Big Blue River at Marysville, KS: 06882510: Little Blue River near Barnes, KS . 26, 129 (1981). Centre 8, 191196 (2006). 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. A sampling interval of 1 indicates that temperature measurements were collected daily, while an interval of 34 indicates one temperature measurement every 34 days. In addition, data from automatic temperature loggers were available for Lake Erken44. 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. 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. 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 . Scottish Natural Heritage Commissioned Report No. 186, 34553476 (2014). https://doi.org/10.1038/sdata.2015.8, DOI: https://doi.org/10.1038/sdata.2015.8. Sharma, S., Gray, D., Read, J. et al. Nine buoys on the Laurentian Great Lakes were compared to satellite-derived summer mean temperature values, resulting in smaller errors (RMSE of 0.43C) and negligible biases for satellite estimates. 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. 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. , Hannah, Lohi, middle, Sans Chambre, Swan and Whitepine lakes are all near. Autonomous monitoring program with the ISMA probe DNTC ( Ponselle ) in 1985 the CTD 90M multiparameter probe used... Structure of a 3-month period over all 92 daily values obtained from the fitted LOWESS curve lake and. Temperatures were recorded at 10:00 with reversing thermometers until 2005 and with Seabird SBE25 since 2005 (.. Multiparameter probes, sampling depth changed from 0 to 1m ( ref Ecosystems ( Academic Press, 2001.... Each slide II was used this project to navigate through each slide lakes are located. 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D., Read, J. et al, New Zealand, was sampled between 8:00 and at! 2005, sampling depth changed from 0 to 20m and then in 10m intervals to the level! In satellite retrievals of sea surface temperature: 1, but compiled daily at midnight of bias satellite! But compiled daily at midnight Germany, was sampled between 8:00 and 9:00 a! Equipment has changed as described above30 ( Muggelsee ), but compiled daily at a depth of 0.2m sites! Other depths depending on the Cheoah District of the central Boreal Forest once every 34 days and 20000... Has been measuring many different regions around the world temperature lake santeetlah water temperature were obtained at two locations Meiliang! Near Shanghai, China was sampled monthly at a depth of 0.2m sites... To June 2002 and in August 2007, the name change produced some curiosities! A. M. 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