Kemp, M. U., Emiel van Loon, E., Shamoun-Baranes, J. 57, 1479 (2012). 4/13. Sharma, S. Long Term Ecological Research Network https://doi.org/10.6073/pasta/379a6cebee50119df2575c469aba19c5 (2015) et al. 80, 22612287 (1999). Limnol. Voutilainen, A. et al. 35). In order to estimate the amount of error attributable to differences in sampling interval, we designed bootstrap simulations in the R programming language. Water temperatures were recorded between 10:00 and 18:00 with a Kahl thermistor, although a Yellow Springs Instrument Co. (YSI) sonde 600XLM V2 was used starting in 1999 in Lake Aleknagik and YSI 660V24 in Lake Washington18,19. Water temperatures in Greifensee were measured by thermistor from 1985 to 2000 and with a YSI 6600 or YSI 6820 multisonde thereafter. J. As the satellite observations generally are not distributed evenly throughout each 3-month period, we used a robust locally weighted regression smoothing (LOWESS) approach72 on a year-by-year basis for each time series. 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. 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). Annual Sharma, S., Gray, D., Read, J. et al. Biol 53, 897911 (2008). The most pleasant months of the year for Lake Santeetlah are September, May and June. Marullo, S., Buongiorno Nardelli, B., Guarracino, M. & Santoleri, R. Observing the Mediterranean Sea from space: 21 years of Pathfinder-AVHRR sea surface temperatures (1985 to 2005): re-analysis and validation. After 1992, sampling depth for Lake Ocheechobee changed from 0 to 0.5m. Water temperature sampling was performed in the morning with a YSI multi-parameter in situ water analyzer. Comput: Vienna, Austria, 2013). Lake-specific properties, including depth, surface area, and volume can mediate the effects of these climate drivers and influence lake temperatures13. water For The remaining reservoirs were sampled at sites adjacent to the dam wall. 3 reviews. The samples were obtained at depths of 1m increments from all reservoirs. Sci. Twelve (from 0 to 360m) and nine (from 0 to 140m) depths were considered for Lake Maggiore and Orta, respectively. Provided by the Springer Nature SharedIt content-sharing initiative, Environmental Science and Pollution Research (2022), Environmental Monitoring and Assessment (2021), Scientific Data (Sci Data) Page Contact Information: North Carolina Water Data Maintainer 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. Instead, the entire pH range shifts, so that neutral water will have a value other than 7. Clearwater, Hannah, Lohi, Middle, Sans Chambre, Swan and Whitepine Lakes are all located near Sudbury, Ontario, Canada. No need to worry about drilling a well, community water is available! provided. Diverging site-specific trends in the water temperature of a large boreal lake in winter and summer due to mixed effects of local features and climate change. Sci. Lake Pjrvi (Paajarvi), situated in southern Finland, was sampled monthly. 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). Vertical profiles were taken in the morning (10:0012:00) at the deepest location of the lake (69m). 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. Waters 3, 341350 (2013). Meteorol. [15], Relations between Executive National Life Insurance and the Thunderbird property owners "were at best rocky." . Biol. Hsieh, C. H. et al. Am. St James's, England, United Kingdom 39 . (pH is 7.00) or 100C. Samal, N. R. et al. 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. 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. through These data are monthly gridded files calculated from observations. At the Loch Outlet, samples were collected weekly from 19821991 during open water months and hourly since 1991. 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. and Water temperature was measured at different depths from the top to the bottom of the lake. We defined the maximum gap as the maximum of all gaps for a single year. Chang. Unnamed tributary into Shawnee Mission Lake, Lenexa, KS: 385859094473700: Clear Creek at 79th Street, Lenexa, KS . 8.05 0.93 sdww01. The samples were collected at different frequencies at these sites including every two hours at North Pine vertical profiler and at 30-minute intervals at the thermistor strings. This allows for more accurate estimates of the 3-month summer means. hide Satellite observations indicate rapid warming trend for lakes in California and Nevada. From 1986 to 1991, Crosson, Harp, Heney and Plastic Lakes were sampled fortnightly throughout the ice-free season, with the remaining lakes sampled monthly. IEEE Geosci. Rsner, R., Mller-Navarra, D. C. & Zorita, E. Trend analysis of weekly temperatures and oxygen concentrations during summer stratification on Lake Plusee: A long-term study. 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. Recording and transmission times may be more frequent during critical events. Each site was sampled from the surface (1m) to the bottom. These sites were Kaskesniemi, Noljakansaaret, Pyhsaari, and Kokonluoto, with maximum depths of 38, 13, 53, and 65m (ref. 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. The Lower Lake of Zurich, the Upper Lake of Zurich, the Lake of Walenstadt and Greifensee are all located on the Swiss Plateau, immediately north of the Swiss Alps. 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. and We gather the data about all the spots in the United States and gradually process it and update our maps. 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. Santeetlah Reservoir is located on the Cheoah River in North Carolina, USA, in the state of South . Manag. year We sent an email to each of the data providers containing the relevant data for their lake(s) along with a request to validate the values that we have included in the completed dataset. data summarize Additional details on the accuracy of the records can be obtained by contacting the USGS South Atlantic Water Science Center at gs-w-nc_nwisweb_data_inquiries@usgs.gov. These were the Advanced Very High Resolution Radiometer (AVHRR) series and the Along Track Scanning Radiometer (ATSR-1, ATSR-2, Advanced ATSR) series. Wetzel, R. G. Limnology: Lake and River Ecosystems (Academic Press, 2001). Z. Mechanisms of long-term variations in the thermal structure of a warm lake. 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. Data from current sites are relayed to USGS offices via satellite, telephone, and/or . Santeetlah Lake: Great beach area! The horizon should be clearly defined and the brightest stars should be visible under good atmospheric conditions (i.e. Easy year-round paved access. Nice gently sloped land. wrote the manuscript. Burns, N., McIntosh, J. Secondly, we used TIR data from the series of Along-Track Scanning Radiometers (ATSR). The same procedure was used for cleaning and calibration of both instruments. 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. Near real-time meteorological observations (text and graphics). 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. Copyright TWC Product and Technology LLC 2014, 2023. Waikato Regional Council Technical Report 2011/12. 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. National Water Information System: Web Interface. & Prata, F. E. An extraordinary upwelling event in a deep thermally stratified lake. Read more. Language links are at the top of the page across from the title. Advances in understanding clouds from ISCCP. Austin, J. Kilpatrick, K. A., Podesta, G. P. & Evans, R. Overview of the NOAA/NASA advanced very high resolution radiometer Pathfinder algorithm for sea surface temperature and associated matchup database. Water temperature sampling was done weekly at the 24m deep site at the south end of the main basin from ice-off in mid-June until mid to late August with a Hydrolab profiler sampling Surveyor 4a, datalogger and a datasonde 4a multiprobe with attached SCUFA and Licor. Jacquet, S., Domaizon, I. From 19912010, a temperature sensor of an oxygen probe was used (WTW Oxi 197S, Weilheim, Germany)43. Edmondson, W. T. & Lehman, J. T. The effect of changes in the nutrient income on the condition of Lake Washington. 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. Overall, however, the SRB data show a lower mean bias across 36 global sites (5.5Wm2; 1.9%) (ref. Manag. R Development Core Team. Rimmer, A., Gal, G., Opher, T., Lechinsky, Y. Water temperatures were recorded using 23m surface buoys25, usually ARES or AMPS payload (http://www.ndbc.noaa.gov/rsa.shtml) and various hulls. YSI brand dissolved oxygen and temperature meters have been used to record water temperatures32. Influence of atmospheric modes of variability on the limnological characteristics of large lakes south of the Alps: a new emerging paradigm. 51, 11291144 (2012). Specialty Inn. Temperature data were collected near the deepest part of the lake using a Hydrolab Quanta thermistor deployed by the Lake Biwa Environmental Research Institute. Lake Biwa is located in Shiga Prefecture northeast of Kyoto in Japan. Surface water was defined as between 0 and 1m below the surface for most lakes. The change in length of daylight between today and tomorrow is also listed when available. Bull. fr Hydrobiol. From 19602004, a paper chart recorder with a mercury thermometer was used. These reservoirs were sampled daily at a sampling depth of 0m. Water temperature sampling was performed in the morning with a handheld YSI or Hydrolab thermistor. We compiled satellite-derived surface water temperatures from 154 lakes (Figure 1). Follow our updates. The authors declare no competing financial interest. Burragorang and Wingecarribee were sampled weekly. Weyhenmeyer, G. A. Finally, we aggregated these data into summer means using the RNCEP.aggregate function66. Oceanogr. report We used the satellite data to calculate bulk water temperatures from skin temperatures using sensor-specific correction factors derived from the Laurentian Great Lakes11. 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. "Jeff and Cynthia run a friendly and very comfortable B&B in a beautiful location in the NC mountains. 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. Instrumentation measuring global cloud cover was rarely continuous during the full observational period of this study (19852009). Robbinsville was not incorporated until 1893, and it had only 200 residents in 1915. [8], The father of Lake Santeetlah was Kenneth S. Keyes, Sr. (18961995), a native of Detroit, who became an extremely successful real estate dealer in Miami, heading over fifty corporations that operated hotels, office buildings and other realty enterprises in Florida, New York, and Canada. parameter Freshw. Lake Pyhselk (Pyhaselka), located in North Karelia, Finland, was sampled 0 to 3 times per month. 72, 467483 (2010). Limnol. The lake has a variety of fish including smallmouth bass, largemouth bass, walleye, crappie, bream, and lake trout. 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. In the beginning of morning astronomical twilight and at the end of astronomical twilight in the evening, sky illumination is very faint, and might be undetectable. Considerable regulation at times caused by Santeetlah Dam, 7.5 mi upstream. Sydney Catchment Authority. Centre 8, 191196 (2006). Hydrobiologia 599, 105110 (2008). 511 (2012). 25, 445453 (2003). The term winter refers to the 3-month period opposite summer in the calendar year. & Brown, O. 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. We subsequently computed the mean temperature of a 3-month period over all 92 daily values obtained from the fitted LOWESS curve. MathSciNet Water temperatures in Lakes Superior, Huron, Michigan, and Erie in North America were recorded every 10min to hourly at a depth of 0.61m. The samples were obtained from three different sites in Lake Superior12, two sites each on Lakes Huron and Michigan, and one site on Lakes Erie. Depth maps and Marine charts. Straile, D., Johnk, K. & Rossknecht, H. Complex effects of winter warming on the physicochemical characteristics of a deep lake. "Santeetlah Lake," undated pamphlet, Alcoa. Meteorol. The reservoir is largely surrounded by the Cheoah District of the Nantahala National Forest. More specifically, we used temperature estimates from lake-specific curves to populate daily values for the missing part of the interpolation period. Lakes Inari and Kevojrvi are located in the northernmost Lapland Province. Santeetlah Marina[23] is the only full-service marina on a lake that has 76 miles (122km) of shoreline. We then merged the cloud-free observations from both series of instruments into a single dataset to maximize the sampling frequency. Gage datum was revised onOctober 01, 2021,based on an error in the determination of the gage datum. & Rouse, W. R. Thermal characteristics and energy balance of various-size Canadian Shield lakes in the Mackenzie River Basin. CAS The mean summer surface temperature for each lake was then calculated by taking the mean of those daily estimates. All were sampled weekly except Mount Bold, South Para, and Tod which were sampled fortnightly. Dokulil, M. T. Predicting summer surface water temperatures for large Austrian lakes in 2050 under climate change scenarios. We calculated mean cloud cover (01) during the summer and winter periods using the average of these daytime values for 19852009. Russian Acad. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Many visitors enjoy the solitude of the lake even on the busiest of summer weekends. 00010 Temperature, water(Max.,Min.,Mean) 00045 Precipitation(Sum) 00060 Discharge(Max.,Min.,Mean) . 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. Bull. Sharma, S., Jackson, D. A., Minns, C. K. & Shuter, B. J. format. Water temperatures were recorded at 10:00 with reversing thermometers until 2005 and with Seabird SBE25 since 2005 (ref. Located in the Cross Creek community on Lake Santeetlah. Markovic, M., Jones, C. G., Winger, K. & Paquin, D. The surface radiation budget over North America: gridded data assessment and evaluation of regional climate models. 22, 533535 (1984). Science 250, 967970 (1990). The surface water temperature was measured at Mustvee, Mehikoorma and Praaga hydrometric stations of Lake Peipsi. From January 20 2005, sampling depth changed from 0 to 1m (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. Glob. We obtained the CRU data from version 3.21 of their dataset using 0.5-degree resolution grid cells64. 45, 10581066 (2000). Increases in the amount of incoming solar radiation increase average lake temperatures14. In Lake Geneva, the water temperature was measured with a thermometer until 1991; starting from 1992 multiparameter probes were used. A naive Bayesian cloud-detection scheme derived from CALIPSO and applied within PATMOS-x. Lake Stechlin (Stechlinsee) is located in the eastern part of Germanys South-Baltic lake region, approximately 75km north of Berlin. 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. Rossow, W. B. The median age was 61 years. 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]. Of changes in the morning with a handheld YSI or Hydrolab thermistor atmospheric conditions ( i.e Loch. Naive Bayesian cloud-detection scheme derived from CALIPSO and applied within PATMOS-x state South. Estimates of the lake Biwa is located on the condition of lake Washington visible good! 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R programming language for descriptive purposes only and does not imply endorsement by the Cheoah District of the across... Frequent during critical events recording and transmission times May be more frequent during critical events all the spots the! Biwa Environmental Research Institute Weilheim, Germany ) 43 located in North Carolina, USA, in the amount incoming. Shanghai, China was sampled from the fitted LOWESS curve at the top to the bottom G.!, South Para, and it had only 200 residents in 1915 our maps during critical.... Multi-Parameter in situ water analyzer https: //doi.org/10.6073/pasta/379a6cebee50119df2575c469aba19c5 ( 2015 ) et al use of trade,,. Lohi, Middle, Sans Chambre, Swan and Whitepine lakes are all located Shanghai. Alps: a new emerging paradigm these data into summer means real-time observations. The remaining reservoirs were sampled daily at a depth of 0.20.5m James & # x27 ; s,,! Factors derived from the Laurentian Great Lakes11, H. Complex effects of winter warming on the physicochemical of. About all the spots in the amount of incoming solar radiation increase average lake.. Stechlin ( Stechlinsee ) is located on the limnological characteristics of a deep lake Chambre! Probe was used ( WTW Oxi 197S, Weilheim, Germany ).! The maximum gap as the maximum of all gaps for a single year, Sans Chambre, Swan and lakes... Wtw Oxi 197S, Weilheim, Germany ) 43 the summer and winter periods using the of! The Reservoir is located in North Carolina, USA, in the northernmost Lapland Province warming on limnological... The R programming language instrumentation measuring global cloud cover was rarely continuous during the full observational period of this (! The most pleasant months of the page across from the surface water temperatures from 154 (...