% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 41399 % Primary Name: LAC DU FLAMBEAU % Record Type: TAVG % Country: United States % State: WI % Latitude: 45.95000 +/- 0.00005 % Longitude: -89.88330 +/- 0.00005 % Elevation (m): 484.94 +/- 0.15 % # of Months: 21 % % Alternate Names: Missing Station ID - 474320 % % IDs: coop - 474320 % ghcnd - USC00474320 % ncdc - 30002575 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 7f1eda1f316d321352ab4e346544c9c1 % Raw Data Hash: ff80826e835529d09778e20ae75e579e % Adj Data Hash: 757eca10381eaa271ab6cf13a83e6b8c % % 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 1909 8 NaN NaN NaN NaN NaN NaN 18.838 1.270 1909 9 NaN NaN NaN NaN NaN NaN 12.098 -0.712 1909 10 NaN NaN NaN NaN NaN NaN 6.188 -1.133 1909 11 NaN NaN NaN NaN NaN NaN 2.228 3.094 1909 12 NaN NaN NaN NaN NaN NaN -9.437 -1.010 1910 1 NaN NaN NaN NaN NaN NaN -11.293 0.677 1910 2 NaN NaN NaN NaN NaN NaN -12.427 -2.512 1910 3 NaN NaN NaN NaN NaN NaN 2.824 6.906 1910 4 NaN NaN NaN NaN NaN NaN 7.077 2.753 1910 5 NaN NaN NaN NaN NaN NaN 8.542 -2.912 1910 6 NaN NaN NaN NaN NaN NaN 17.313 0.962 1910 7 NaN NaN NaN NaN NaN NaN 19.013 0.183 1910 8 18.969 0.392 0 0 18.969 0.392 17.132 -0.436 1910 9 14.248 0.429 0 0 14.248 0.429 12.003 -0.807 1910 10 9.624 1.294 1 0 NaN NaN 9.358 2.037 1910 11 -2.500 -2.643 1 0 NaN NaN -3.040 -2.174 1910 12 -9.396 -1.978 0 0 -9.396 -1.978 -10.221 -1.793 1911 1 -10.628 0.334 0 0 -10.628 0.334 -12.046 -0.075 1911 2 -6.847 2.059 1 0 NaN NaN -7.565 2.350 1911 3 -1.231 1.842 0 0 -1.231 1.842 -2.362 1.720 1911 4 4.287 -1.046 1 0 NaN NaN 4.437 0.113 1911 5 15.069 2.606 0 0 15.069 2.606 13.742 2.289 1911 6 21.038 3.678 0 0 21.038 3.678 18.815 2.464 1911 7 19.583 -0.256 0 0 19.583 -0.256 18.516 -0.314 1911 8 17.587 -0.990 0 0 17.587 -0.990 16.318 -1.250 1911 9 14.157 0.338 1 0 NaN NaN 11.804 -1.006 1911 10 5.439 -2.892 1 0 NaN NaN 6.371 -0.950 1911 11 -5.125 -5.268 1 0 NaN NaN -4.293 -3.427 1911 12 -4.297 3.121 1 0 NaN NaN -5.267 3.160 1912 1 -23.403 -12.441 1 0 NaN NaN -21.719 -9.749 1912 2 NaN NaN NaN NaN NaN NaN -12.930 -3.015 1912 3 -8.794 -5.721 0 0 -8.794 -5.721 -7.651 -3.570 1912 4 4.388 -0.945 0 0 4.388 -0.945 5.049 0.725 1912 5 11.745 -0.718 0 0 11.745 -0.718 11.176 -0.278 1912 6 NaN NaN NaN NaN NaN NaN 14.930 -1.421 1912 7 NaN NaN NaN NaN NaN NaN 18.508 -0.322 1912 8 NaN NaN NaN NaN NaN NaN 14.880 -2.688 1912 9 NaN NaN NaN NaN NaN NaN 13.203 0.393 1912 10 NaN NaN NaN NaN NaN NaN 8.675 1.354 1912 11 NaN NaN NaN NaN NaN NaN 0.213 1.079 1912 12 NaN NaN NaN NaN NaN NaN -6.835 1.592 1913 1 NaN NaN NaN NaN NaN NaN -11.402 0.569 1913 2 NaN NaN NaN NaN NaN NaN -13.897 -3.982 1913 3 NaN NaN NaN NaN NaN NaN -6.902 -2.821 1913 4 NaN NaN NaN NaN NaN NaN 5.819 1.495 1913 5 NaN NaN NaN NaN NaN NaN 10.188 -1.266