Sci. 47). 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). Rabone, F. A. ISSN 2052-4463 (online). Sky Pond, located in Loch Vale watershed northwest of Denver, Colorado, United States, was sampled at Sky Pond outlet where Sky Pond drains to Icy Brook. Data for Plusssee were collected by the Max-Planck-Institute for Limnology, Ploen until 2006. Robbinsville was not incorporated until 1893, and it had only 200 residents in 1915. 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). instructions This final step was probably the most important as it allowed us to get feedback from the individuals that are most familiar with the lakes in our dataset. 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. 80, 22612287 (1999). . The samples were obtained from the region with greatest water depth within each lake. The time period when the sun is no more than 6 degrees below the horizon at either sunrise or sunset. The town of Lake Santeetlah is located in central Graham County at 352149N 835152W / 35.36361N 83.86444W / 35.36361; -83.86444 (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. Summary Water temperature sampling was performed in the daytime with a CTD profiler and a thermistor. Res. In these cases, we conducted searches in the primary literature, online web sources (ILEC (http://www.ilec.or.jp/en/), IAGLR (http://www.iaglr.org/), LakeNet (http://www.worldlakes.org/), Wikipedia (http://en.wikipedia.org/wiki/Main_Page)), Google Earth, or contacted colleagues in the relevant countries to obtain information. Ymp 566, 1115 (2002). Waikato Regional Council Technical Report 2011/12. Water temperatures were recorded between 10:00 and 12:00 depending on the sampling day using reversing thermometers connected to the bottle for water sampling36. 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. Offering 2 buildable Lots for the price of 1. Glob. Houston, TX 76 Sunny. This was done in order to avoid the cloudy wet season in the tropics and instead collect data during the dry season, which allows for an increased number of cloud-free satellite observations11. Hampton, S. E. et al. We treated the mean annual summer temperature calculated with a sampling interval of 1 (daily measurements) as the true mean temperature. J. Climatol. Title: USGS: Water-Year Summary for North Carolina 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. Before 2003, a YSI 6000 probe was used58. 48). Lett. Limnol. years the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in . water This novel dataset can be used to address additional research questions including those pertaining to understanding the mechanistic drivers of surface water temperature warming and ecological consequences of changes in lake temperatures. Lake Santeetlah Water Level. Lake Annecy and Lake Bourget (located in France) and Lake Geneva located in France and Switzerland were sampled one or two times per month from the middle of the lake at the deepest point. When we compared interannual anomalies (average deviations from the 19852009 mean), the RMSE declined to 0.72C. organized, processed, verified, and collated data. Heidinger, A. K., Evan, A. T., Foster, M. J. Current data typically are recorded at 15- to 60-minute intervals, stored onsite, and then transmitted to USGS offices every 1 to 4 hours, depending on the data relay technique used. Limnol. Schneider and Hook11 also applied two additional methods to summer means from these nine sites to confirm that these biases did not negatively affect the computed trends: Firstly a direct validation of satellite-derived trends against corresponding trends obtained for in situ observations at buoys was carried out and the results indicated a good correspondence with an RMSE of 0.013C per year. Station Name Station Identifier; Smoky Hill River at Ellsworth, KS: 06864500: Big Blue River at Marysville, KS: 06882510: Little Blue River near Barnes, KS . Twelve (from 0 to 360m) and nine (from 0 to 140m) depths were considered for Lake Maggiore and Orta, respectively. Lake Reserv. Effects of climatic warming on lakes of the central Boreal Forest. Water temperatures were recorded at various depths at 1m intervals from surface to bottom. We assembled a database of summer lake surface temperatures for 291 lakes collected in situ and/or by satellites for the period 19852009. Only lakes that exhibited at least a 1010km area of pure water surface without any islands or shorelines were selected, in order to make sure that there was no contamination by land surfaces. All lakes were sampled at a depth of 0.5m, in addition to several other depths depending on the maximum lake depth. Summary Water temperature plays an important role in almost all USGS water science. Space observations of inland water bodies show rapid surface warming since 1985. Manhattan, NY 48 F Mostly Cloudy. Google Scholar. Gage-height records are generally good. 51, 11291144 (2012). Use the Previous and Next buttons to navigate the slides or the slide controller buttons at the end to navigate through each slide. Oceanogr. Bull. In order to estimate the amount of error attributable to differences in sampling interval, we designed bootstrap simulations in the R programming language. Blue Chalk, Chub, Crosson, Dickie, Harp, Heney, Red Chalk East, Red Chalk Main, and Plastic Lakes are located near the Dorset Environmental Science Centre in Ontario, Canada. When this routine was used, we made a notation in the log file describing if extrapolation was used for the beginning and/or end period and we included the equation of the curve (See Data Records). "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. 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. You are using a browser version with limited support for CSS. Geophys. We collected latitude, longitude, elevation, surface area, volume, mean depth, and maximum depth for each lake, if available (Table 1). Because the ratio of hydrogen and hydroxyl ions remains the same, the acidity of water does not change with temperature 28. Yellowin situ sampled lakes; Redsatellite sampled lakes. Plisnier, P. D. et al. Santeetlah Lake's current water temperature is 57F Todays forecast is, Clear With a high around 74F and the low around 37F. It was sampled weekly or monthly at 13 depths down to 450m until 2005 and continuously since then. Increases in the amount of incoming solar radiation increase average lake temperatures14. 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]. 36, L22402 (2009). The air temperature data we obtained from NCEP represent version 2 of the NCEP reanalysis data65. be. to 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. 22). Below we describe the sampling methodology for each lake or group of lakes contributed by each data provider, organized by geographic region. January is the snowiest month in Lake Santeetlah with 2.6 inches of snow, and 4 months of the . Theory, modeling and interalgorithm comparison. 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. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 48, 14321438 (2003). Water temperature profiles were obtained during the daylight hours between 9:00 to 14:00 using a Peabody Ryan Model J Thermograph between 198088, a Richard Brancher Temperature Logger XL-800 between 198997, a Hobo onset stow away logger between 19982007, and a Hobo water temperature pro V2 from 2008 to present. Queens Printer for Ontario, 2007). To generate the curve, we pooled all temperature values (for a given depth and given lake) according to day-of-year (DoY), and fit a curve of the type temperature=a*DoY^2+b*DoY+c. Whenever there were inconsistencies in data, we worked directly with the original data provider to resolve the issue and update the data accordingly. 2006 parameter Lake Santeetlah has 76 miles of shore line and is home to a variety of trout, muskie, crappie, and bass. Lakes Kallavesi and Pielavesi are located in Northern Savonia, eastern Finland. The dataset has a spatial resolution of 1 1 and temporal resolution of 3h. In addition to the SRB incoming shortwave radiation (SW) and longwave radiation (LW), we also provide estimates of the total incoming radiation (Rtot=0.93*SW+0.97*LW) that is absorbed by a dark, water surface under ice-free conditions (i.e., an assumed shortwave albedo of 7% and longwave emissivity of 0.97). Sci Data 2, 150008 (2015). Lake Mendota, Lake Monona, Lake Wingra, and Fish Lake are in southern Wisconsin. Lake Washington (King County, Washington) and Lake Aleknagik (Dillingham Census Area, Alaska) are both located in the United States. 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. seaside, ca news shooting; does the entity have zero texas gross receipts? The data are generated on the basis of the International Satellite Cloud Climatology Project (ISCCP) DX radiance and cloud parameters67, using an updated version of the University of Marylands shortwave flux algorithm and an adaptation of the longwave algorithm. Edmondson, W. T. & Lehman, J. T. The effect of changes in the nutrient income on the condition of Lake Washington. 14, 152161 (1998). Sampling was carried out with automated thermistors, located at 1m intervals from the top to the bottom of the lake. Chang. CAS Water temperature sampling was conducted using a Celsius mercury thermometer. 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. The samples were obtained from the central monitoring station of Lake Kinneret, approximately 42m in depth. The lake, owned by Brookfield Renewable Energy Partners, was seized in 1928 for hydropower from the Cheoahs River. Located in the Cross Creek community on Lake Santeetlah. Water from Santeetlah Lake, 7.5 mi upstream, is diverted to hydro powerplant on the Little Tennessee River, which bypasses gage. Lake Valkea-Kotinen, situated in southern Finland, was sampled weekly, and water temperatures were measured at the surface and depths of 1, 2, 3, 4, 5 and 6m. Measurements were made in the deepest part of the lake (6.5m) in the morning between 10:00 and 11:00 using YSI probes for oxygen and temperature45. 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. 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