Surface temperature was measured at eight standard locations throughout Oneida Lake, although the Shackelton Point site approximately 0.7km from the south shore of the lake consisted of the longest time series. Get the most important science stories of the day, free in your inbox. water Meteorol. 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 . 81, 15251536 (2000). J. The most pleasant months of the year for Lake Santeetlah are September, May and June. sites We recognize our responsibility to use data and technology for good. 3, 299310 (2007). By Charles Wellington. for Lake Santeetlah, North Carolina This subdivision is one of the only communities in the area to offer a community pool, tennis courts and a club house. of The lowest monthly average temperature in Lake Santeetlah for January is 38.1 degrees. Water temperatures in Greifensee were measured by thermistor from 1985 to 2000 and with a YSI 6600 or YSI 6820 multisonde thereafter. We compiled in situ surface water temperatures and corresponding lake geomorphology and climatic data from 151 lakes (Figure 1; Tables 1 and 2; Data Citation 1). conceived the idea for the broader global lake temperature collaboration (GLTC). Sala, O. E. et al. Accessibility In this manner, we were able to construct a relationship between sampling interval and error in our temperature estimates (Figure 4). Menu. 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). 48, 14321438 (2003). 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. Burragorang and Wingecarribee were sampled weekly. From 19602004, a paper chart recorder with a mercury thermometer was used. 42). For undetermined reasons he called the property "Thunderbird Estates". 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. Data for Plusssee were collected by the Max-Planck-Institute for Limnology, Ploen until 2006. Water temperatures were measured about 0.3m below the surface, usually at the deepest point of each lake38. Summary 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. Hampton, S. E. et al. Water temperature sampling was conducted continuously (in situ paper or sensor record), but compiled daily at midnight. Page Contact Information: North Carolina Water Data Maintainer Meteorol. Gage-height records are generally good. Lake Santeetlah, NC 10-Day Weather Forecast. 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. Straile, D., Johnk, K. & Rossknecht, H. Complex effects of winter warming on the physicochemical characteristics of a deep lake. Res. 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. 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. Boreal Environ. [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. Sci. Water 5, 129144 (2004). Privacy Biol. Am. All were sampled weekly except Mount Bold, South Para, and Tod which were sampled fortnightly. Oceanogr. Hispanic or Latino of any race were 1.49% of the population. Heidinger, A. K., Evan, A. T., Foster, M. J. We thank Tim Kratz for helping with the initiation of this project. The reservoir is located at an altitude of 1,941 feet and covers 2,881 hectares and holds a total of 2,842,000 cubic meters of water. Oswald, C. J. The air temperature data we obtained from NCEP represent version 2 of the NCEP reanalysis data65. Oceanogr. Considerable regulation at times caused by Santeetlah Dam, 7.5 mi upstream. Salmaso, N. et al. Lake Info Fishing . Reports "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. There were 38 households, out of which 5.3% had children under the age of 18 living with them, 65.8% were married couples living together, and 31.6% were non-families. data FOIA Burragorang, Cataract, Cordeaux, Fitzroy, and Wingecarribee are all reservoirs located in New South Wales, in southeast Australia. 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. Lake Peipsi (Peipus) on the border of Estonia and Russia, was sampled twice daily at 8:00 and 20:00, at a depth of 0.1m (ref. This avoided any possible bias due to contamination from mixed pixels containing both land and water. Climatic factors, including air temperature, cloud cover, and solar radiation, in addition to geomorphometric factors, such as lake surface area and depth, influence surface water temperatures in lakes7,8. Sharma, S. Long Term Ecological Research Network https://doi.org/10.6073/pasta/379a6cebee50119df2575c469aba19c5 (2015) et al. We collected latitude, longitude, elevation, surface area, volume, mean depth, and maximum depth for each lake, if available (Table 1). 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. Google Scholar. Water Discharge records are generally good except for estimated discharges, which . Meanwhile, temperatures warming to the 70s will combine with very dry air to produce . 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. Specialty Inn. Res. [5], Because of its mountainous terrain, Graham County was one of the last sections of the eastern United States to be settled by Europeans. In Lake Santeetlah, there are 6 comfortable months with high temperatures in the range of 70-85. 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. History of Chemical, Physical and Biological Methods, Sample Locations and Lake Morphometry for the Dorset Environmental Science Centre (19732006) (Ontario Ministry of the Environment Data Report. Where necessary, we used a curve-fitting extrapolation technique to extend daily in situ observations to the bounds of the summer mean period. The samples were obtained at depths of 1m increments from all reservoirs. In addition, we performed cloud masking so that any pixels that were acquired at zenith angles of greater than 45 degrees were discarded. The Challenge of Implementing Water Harvesting and Reuse in South Australian Towns (The University of Adelaide, 2006). Oceanogr. 25, 445453 (2003). This allows for more accurate estimates of the 3-month summer means. The ATSRs are multi-channel imaging radiometers with the primary purpose of providing highly accurate sea surface temperature data worldwide. 19, 104114 (2014). A zip folder of processing log files is included, called GLTC_means_processing_log_files.zip. Gibbs, M. Lake Taupo Long-Term MonitoringPprogramme 2009-2010. 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. Water Resour. 53, 27242730 (2008). Sydney Catchment Authority. 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. Sharma, S., Jackson, D. A., Minns, C. K. & Shuter, B. J. Data 2:150008 doi: 10.1038/sdata.2015.8 (2015). NDBC Dial-A-Buoy Information. Modelling potential effects of climate change on winter turbidity loading in the Ashokan Reservoir, NY. OReilly, C. M., Alin, S. R., Plisnier, P.-D., Cohen, A. S. & McKee, B. Girard, R. E., Yan, N. D., Heneberry, J. Weyhenmeyer, G. A. The physical impact of the late 1980s climate regime shift on Swiss rivers and lakes. Call us (828) 369-0406 Get links to local marinas on Fontana Lake, Nantahala Lake, Lake Glenville, Lake Santeetlah, and Lake Junaluska (828) 369-0406 canvasmasters@yahoo.com Facebook In Lake Bourget, water temperature was measured with the ISMA probe DNTC (Ponselle) in 1985. Thank you for visiting nature.com. As of the census[3] of 2000, there were 67 people, 38 households, and 25 families residing in the town. Generally, water temperatures tend to coincide with regional air temperatures, warming or cooling at similar rates to that of air temperatures10,11. 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). hide Report Verhandlungen Int. Overall, however, the SRB data show a lower mean bias across 36 global sites (5.5Wm2; 1.9%) (ref. Sci Data 2, 150008 (2015). Process. Figure 1 shows long-term rates of change in surface lake water temperature from 1985 to 2009. The first, GLTClakeinformation.csv, contains information for each lake, who collected the data, lake location and surroundings. Slider with three articles shown per slide. Article Increases in the amount of incoming solar radiation increase average lake temperatures14. Lett. 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. Although there were equipment upgrades over the years, there have been no substantive change to equipment55. Can. 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). 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. The authors declare no competing financial interest.

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