Chen, Y., Qin, B., Teubner, K. & Dokulil, M. T. Long-term dynamics of phytoplankton assemblages: Microcystis-domination in Lake Taihu, a large shallow lake in China. Schindler, D. E., Rogers, D. E., Scheuerell, M. D. & Abrey, C. A. 0351706800 CHEOAH RIVER NEAR BEARPEN GAP NEAR TAPOCO, NC, Click Lake Pjrvi (Paajarvi), situated in southern Finland, was sampled monthly. An independent assessment of pathfinder AVHRR sea surface temperature accuracy using the marine atmosphere emitted radiance interferometer (MAERI). 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. instructions Lake Santeetlah, NC 10-Day Weather Forecast. Meteorol. Methods Ecol. "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. Meindl, E. A. 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. Take control of your data. Water Resour. The samples were obtained from near the Kingsley Dam24. 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. 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. CAS The vertical profiler uses a YSI 6600v2 instrument while the thermistor string used Hydrolab instrumentation. 80, 22612287 (1999). Global biodiversity scenarios for the year 2100. 8.05 0.93 sdww01. Correspondence to A lawsuit by the insurance company was dismissed by the court, and the company became more amenable to the formation of an incorporated town. Twelve reservoirs, namely, Barossa, Beetaloo, Happy Valley, Hope Valley, Little Para, Millbrook, Mount Bold, Myponga, South Para, Tod, Kangaroo Creek Reservoir and Warren are all located in Adelaide, south Australia. Hydrobiologia 731, 1929 (2014). printer-friendly Gui, S., Liang, S., Wang, K., Li, L. & Xiaotong, Z. Lake Samsonvale (North Pine Dam) is located in Queensland, Australia. Only 13% have sampling intervalsonce every 30 days (Figure 5). Reports Water temperatures were recorded at 10:00 with a STD-12 (Applied Micro-systems), with an error of 0.005 degrees C. The equipment was replaced several times49. 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. Edmondson, W. T. & Lehman, J. T. The effect of changes in the nutrient income on the condition of Lake Washington. Water temperatures were sampled from the deepest site in the centre at 11:00 with a conductivity-temperature-depth (CTD) profiler56. URL: https://waterdata.usgs.gov/nwis/wys_rpt? Since May 2009, an automatic station (VAISALA, MAWS110 and water temperature sensor QMT110) was used every hour for water temperature measurements. 47). There are over 200 miles (320km) of hiking trails in the Cheoah District, and one can hike about 8 miles (13km) from Lake Santeetlah to the Appalachian Trail. Feet MSL. Complete water temperature profiles are available https://knb.ecoinformatics.org/#view/kgordon.35.49. 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. From 1986 to 1998 the multiparameter probe Meerestechnik Elektronik (ECO 236) was used. J. Plankton Res. to Samal, N. R. et al. Language links are at the top of the page across from the title. & Brown, O. Show prices. You are using a browser version with limited support for CSS. Water temperatures have increased over recent decades coinciding with changing air temperatures, with a few exceptions. 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). choose Although there were equipment upgrades over the years, there have been no substantive change to equipment55. Leech, D. M., Williamson, C. E., Moeller, R. E. & Hargreaves, B. R. Effects of ultraviolet radiation on the seasonal vertical distribution of zooplankton: a database analysis. Aquat. Chang. Check current conditions in Lake Santeetlah, NC with radar, hourly, and more. Hsieh, C. H. et al. Biol 53, 897911 (2008). The figure shows interpolation conducted with temperature measurements conducted at an interval of once every 10 days (panel a), once every 20 days (panel b), or once every 30 days (panel c). Temperatures were obtained from a consistent sampling location at or near the deepest portion of the lake. However, at broad spatial scales, climatic factors have a larger influence on surface water temperatures than lake morphology17. The lowest monthly average temperature in Lake Santeetlah for January is 38.1 degrees. Generally, for lakes situated in the Northern Hemisphere we used the period of 1 July30 September (JAS); whereas, in the Southern Hemisphere, we used 1 January31 March (JFM). The Lake Surface Water Temperature (LSWT) Version 1 consists of two components: an historical dataset of Collection 1km LSWT from 2002 until 2012 generated from the AATSR instrument on Envisat and a Near Real Time (NRT) dataset of 1km LSWT from the SLSTR instrument on Sentinel-3A from the April 2018 until present. Assoc. Water Resour. In addition, corresponding climatic drivers (air temperatures, solar radiation, and cloud cover) and geomorphometric characteristics (latitude, longitude, elevation, lake surface area, maximum depth, mean depth, and volume) that influence lake surface temperatures were compiled for each lake. Soc. Water temperature sampling was performed using digital thermometers (YSI model 50B) by the Food and Agricultural Organization (FAO) of the United Nations from 19931996. We recognize our responsibility to use data and technology for good. Wetzel, R. G. Limnology: Lake and River Ecosystems (Academic Press, 2001). years 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. Int. [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. Instrumentation measuring global cloud cover was rarely continuous during the full observational period of this study (19852009). Sharma, S., Gray, D., Read, J. et al. Soc. Stat. ADS Sign up for the Nature Briefing newsletter what matters in science, free to your inbox daily. The samples were obtained from sites adjacent to the dam wall. Res. 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. led development and information acquisition for manuscript. We validated the satellite data with the in situ data by conducting four analyses. 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. 36, L22402 (2009). CAS be. onward, Loch Leven, situated in Perth and Kinross, Scotland, United Kingdom, was sampled biweekly, from the subsurface at an approximate depth of 0.01m. The samples were obtained from the Reed Bower sampling site which is an open water site that has a water depth similar to the average depth of the lake and remains accessible in most weather conditions. About the Data Indicator Notes. [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]. Water temperature plays an important role in almost all USGS water science. Biol. 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. There were 172 housing units at an average density of 853.3 per square mile (332.0/km2). 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 mean summer temperature for each lake was then calculated by taking the mean of those daily estimates. Evol. Policies and Notices, U.S. Department of the Interior | We will review the data in question. Res. Limnol. Monday, April 17, 2023 11:00:00 AM Level is 0.27 feet. 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. In order to estimate the amount of error attributable to differences in sampling interval, we designed bootstrap simulations in the R programming language. Bull. Lett. The AVHRR series of satellite instruments has been measuring thermal infrared (TIR) radiation since the late 1970s. For this study, we used data from the version 5 product of AVHRR Pathfinder collection59. #6 of 9 specialty lodgings in Robbinsville. Manag. 40, 18381845 (1983). The air quality index in Lake Santeetlah is 12% better than the national average. Queens Printer for Ontario, 2007). 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. Lakes as sentinels of climate change. 26, 129 (1981). It was sampled at a variable frequency over the study period, from once per week to once per two months, at 1m increments from the surface to the bottom using a YSI 56. The physical impact of the late 1980s climate regime shift on Swiss rivers and lakes. Sci Data 2, 150008 (2015). Inl. In the earlier years, a thermometer assembled in a Ruttner water sampler was used, and following 2000, temperature was recorded using a thermistor40. From 1986 to 1991, Crosson, Harp, Heney and Plastic Lakes were sampled fortnightly throughout the ice-free season, with the remaining lakes sampled monthly. 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. Thus, the influence of cloud cover on lake temperatures can be bidirectional and complex. Glob. 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. Facebook . Because the ratio of hydrogen and hydroxyl ions remains the same, the acidity of water does not change with temperature 28. Data from current sites are relayed to USGS offices via satellite, telephone, and/or . Internet Explorer). [9], In 1947, Keyes exchanged with the Forest Service some land he held for the area that is now the town of Lake Santeetlah. The term winter refers to the 3-month period opposite summer in the calendar year. Remote Sens. 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). 12879 lakes / reservoirs. 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). A sampling interval of 1 indicates that temperature measurements were collected daily, while an interval of 40 indicates one temperature measurement every 40 days. Hope Valley, Little Para, and Tod were sampled at a depth of 0m, Warren at depths of 0, 5, and 10m, Happy Valley at 0, 5, 10 and 15m, Beetaloo at depths of 0, 10 and 15m, Millbrook and South Para at 0, 10, and 20m, Barossa at 0, 10, 15, 20 and 25m, Mount Bold and Myponga at 0, 10, 20 and 30m, and Kangaroo Creek Reservoir at 0, 10, and 30m. All samples were obtained from sites adjacent to the dam wall. From 19602004, a paper chart recorder with a mercury thermometer was used. 104, 23565 (1999). Lake Tarawera, located in North Island, New Zealand, was sampled monthly from the subsurface (20cm) to the bottom at 1m intervals. 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. The need for ecological monitoring of freshwaters in a changing world: A case study of Lakes Annecy, Bourget, and Geneva. For each site, we constructed simulated temperature datasets consisting of a subset of the daily temperature observations. At high sampling intervals (panel c), linear interpolation can underestimate daily temperatures, leading to an underestimate of the mean summer temperature. Lake Giles and Lake Lacawac are in Pennsylvania, United States, and were sampled weekly to monthly at a depth of 0.5m. Both lakes were sampled from the surface (0m) to the bottom (2023m for Lake Giles and 1013m for Lake Lacawac). Modelling potential effects of climate change on winter turbidity loading in the Ashokan Reservoir, NY. 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. J. Appl. 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. 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). Austin, J. Depth maps and Marine charts. every The reservoir is largely surrounded by the Cheoah District of the Nantahala National Forest. generated. Burragorang and Wingecarribee were sampled weekly. Environ. 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.

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