% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 10701 % Primary Name: CREE LAKE (AWS) % Record Type: TAVG % Country: Canada % State: SK % Latitude: 57.35000 +/- 0.00050 % Longitude: -107.13300 +/- 0.00050 % Elevation (m): 495.00 +/- 0.05 % # of Months: 22 % % IDs: gsod - 719201-99999 % icao - CWFN % usaf - 719201 % % Sources: Global Summary of the Day % % Site Hash: 08c7313e124bdbc34d900cdd9c65f1b9 % Raw Data Hash: 6b7131eeed1b8e91e62d73f060416771 % Adj Data Hash: e7fa753a0a8c0f577ad780af957f2288 % % The data for this station is presented below in several columns and in % several forms. The temperature values are reported as "raw", % "adjusted", and "regional expectation". % % The "raw" values reflect the observations as originally ingested by % the Berkeley Earth system from one or more originating archive(s). % These "raw" values may reflect the merger of more than one temperature % time series if multiple archives reported values for this location. % Alongside the raw data we have also provided a flag indicating which % values failed initial quality control checks. A further column % dates at which the raw data may be subject to continuity "breaks" % due to documented station moves (denoted "1"), prolonged measurement % gaps (denoted "2"), documented time of observation changes (denoted "3") % and other empirically determined inhomogeneities (denoted "4"). % % In many cases, raw temperature data contains a number of artifacts, % caused by issues such as typographical errors, instrumentation changes, % station moves, and urban or agricultural development near the station. % The Berkeley Earth analysis process attempts to identify and estimate % the impact of various kinds of data quality problems by comparing each % time series to neighboring series. At the end of the analysis process, % the "adjusted" data is created as an estimate of what the weather at % this location might have looked like after removing apparent biases. % This "adjusted" data will generally to be free from quality control % issues and be regionally homogeneous. Some users may find this % "adjusted" data that attempts to remove apparent biases more % suitable for their needs, while other users may prefer to work % with raw values. % % Lastly, we have provided a "regional expectation" time series, based % on the Berkeley Earth expected temperatures in the neighborhood of the % station. This incorporates information from as many weather stations as % are available for the local region surrounding this location. Note % that the regional expectation may be a systematically a bit warmer or % colder than the weather stations by a few degrees due to differences % in mean elevation and other local characteristics. % % For each temperature time series, we have also included an "anomaly" % time series that removes both the seasonality and the long-term mean. % These anomalies may provide an easier way of seeing changes through % time. % % Reported temperatures are in Celsius and reflect monthly averages. As % these files are intended to be summaries for convenience, additional % information, including more detailed flagging and metadata, may be % available in our whole data set files. % % The Berkeley Earth analysis was run on 15-Nov-2013 19:55:48 % % Raw Data QC Continuity Adjusted Data Regional Expectation % Year, Month, Temperature, Anomaly, Failed, Breaks, Temperature, Anomaly, Temperature, Anomaly 1956 1 NaN NaN NaN NaN NaN NaN -25.701 -0.930 1956 2 NaN NaN NaN NaN NaN NaN -19.923 -0.805 1956 3 NaN NaN NaN NaN NaN NaN -13.972 -1.222 1956 4 NaN NaN NaN NaN NaN NaN -3.221 -2.018 1956 5 NaN NaN NaN NaN NaN NaN 7.666 0.125 1956 6 NaN NaN NaN NaN NaN NaN 14.301 0.805 1956 7 NaN NaN NaN NaN NaN NaN 16.814 0.385 1956 8 NaN NaN NaN NaN NaN NaN 14.798 0.157 1956 9 NaN NaN NaN NaN NaN NaN 5.863 -2.272 1956 10 NaN NaN NaN NaN NaN NaN 2.070 0.596 1956 11 NaN NaN NaN NaN NaN NaN -7.241 3.070 1956 12 NaN NaN NaN NaN NaN NaN -20.710 -0.860 1957 1 -23.913 0.282 1 0 NaN NaN -25.352 -0.581 1957 2 NaN NaN NaN NaN NaN NaN -20.955 -1.837 1957 3 NaN NaN NaN NaN NaN NaN -11.992 0.759 1957 4 NaN NaN NaN NaN NaN NaN -1.603 -0.400 1957 5 NaN NaN NaN NaN NaN NaN 6.667 -0.874 1957 6 NaN NaN NaN NaN NaN NaN 11.428 -2.068 1957 7 17.613 0.608 0 0 17.613 0.608 16.746 0.317 1957 8 14.446 -0.771 0 0 14.446 -0.771 14.351 -0.290 1957 9 9.739 1.028 0 0 9.739 1.028 8.681 0.547 1957 10 4.134 2.084 0 0 4.134 2.084 2.320 0.846 1957 11 -8.481 1.253 0 0 -8.481 1.253 -9.379 0.932 1957 12 -19.661 -0.388 0 0 -19.661 -0.388 -20.038 -0.188 1958 1 -18.674 5.521 0 0 -18.674 5.521 -18.502 6.269 1958 2 -20.964 -2.422 0 0 -20.964 -2.422 -20.336 -1.217 1958 3 -6.998 5.176 0 0 -6.998 5.176 -9.356 3.394 1958 4 1.641 2.267 0 0 1.641 2.267 1.606 2.809 1958 5 8.367 0.250 0 0 8.367 0.250 8.709 1.168 1958 6 10.963 -3.109 0 0 10.963 -3.109 10.903 -2.593 1958 7 15.864 -1.141 0 0 15.864 -1.141 15.900 -0.529 1958 8 15.044 -0.172 0 0 15.044 -0.172 15.339 0.698 1958 9 8.894 0.183 0 0 8.894 0.183 7.329 -0.805 1958 10 3.348 1.297 0 0 3.348 1.297 3.932 2.457 1958 11 -7.393 2.342 0 0 -7.393 2.342 -9.514 0.798 1958 12 -21.409 -2.135 0 0 -21.409 -2.135 -21.029 -1.179 1959 1 -26.048 -1.854 0 0 -26.048 -1.854 -29.142 -4.371 1959 2 -19.145 -0.603 0 0 -19.145 -0.603 -17.716 1.402 1959 3 -7.932 4.242 0 0 -7.932 4.242 -9.560 3.190 1959 4 NaN NaN NaN NaN NaN NaN -0.096 1.107 1959 5 NaN NaN NaN NaN NaN NaN 4.215 -3.326 1959 6 NaN NaN NaN NaN NaN NaN 11.624 -1.872 1959 7 NaN NaN NaN NaN NaN NaN 17.208 0.779 1959 8 NaN NaN NaN NaN NaN NaN 12.467 -2.173 1959 9 NaN NaN NaN NaN NaN NaN 7.028 -1.107 1959 10 NaN NaN NaN NaN NaN NaN -0.777 -2.252 1959 11 NaN NaN NaN NaN NaN NaN -12.602 -2.291 1959 12 NaN NaN NaN NaN NaN NaN -11.583 8.267 1960 1 NaN NaN NaN NaN NaN NaN -24.865 -0.094 1960 2 NaN NaN NaN NaN NaN NaN -16.900 2.218 1960 3 NaN NaN NaN NaN NaN NaN -15.922 -3.172