% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 9212 % Primary Name: HARRINGTON HRBR % Record Type: TAVG % Country: Canada % Latitude: 50.53300 +/- 0.00050 % Longitude: -59.50000 +/- 0.00050 % Elevation (m): 3.00 +/- 0.05 % # of Months: 16 % % IDs: gsod - 718141-99999 % usaf - 718141 % % Sources: Global Summary of the Day % % Site Hash: eb267216f615adfac695609892c2aca8 % Raw Data Hash: 6ad378d5ca80a317b4bbafd709ee6470 % Adj Data Hash: 08e6b9085007d490a66e9216d62a4942 % % 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 1976 7 NaN NaN NaN NaN NaN NaN 12.710 -0.219 1976 8 NaN NaN NaN NaN NaN NaN 12.113 -0.709 1976 9 NaN NaN NaN NaN NaN NaN 8.912 -0.205 1976 10 NaN NaN NaN NaN NaN NaN 2.300 -1.305 1976 11 NaN NaN NaN NaN NaN NaN -2.654 -0.901 1976 12 NaN NaN NaN NaN NaN NaN -12.618 -3.029 1977 1 NaN NaN NaN NaN NaN NaN -10.469 2.013 1977 2 NaN NaN NaN NaN NaN NaN -10.961 0.615 1977 3 NaN NaN NaN NaN NaN NaN -4.062 2.400 1977 4 NaN NaN NaN NaN NaN NaN -1.591 -0.410 1977 5 NaN NaN NaN NaN NaN NaN 3.637 -0.200 1977 6 NaN NaN NaN NaN NaN NaN 9.250 0.364 1977 7 12.228 -1.377 0 0 12.228 -1.377 12.579 -0.350 1977 8 12.946 -0.552 0 0 12.946 -0.552 12.414 -0.408 1977 9 8.870 -0.923 0 0 8.870 -0.923 7.521 -1.596 1977 10 4.633 0.352 0 0 4.633 0.352 3.450 -0.155 1977 11 1.359 2.436 0 0 1.359 2.436 1.097 2.850 1977 12 -7.417 1.496 0 0 -7.417 1.496 -8.916 0.673 1978 1 -9.915 1.890 1 0 NaN NaN -11.920 0.562 1978 2 -6.318 4.581 1 0 NaN NaN -7.117 4.459 1978 3 -8.456 -2.670 0 0 -8.456 -2.670 -9.140 -2.679 1978 4 -2.389 -1.884 0 0 -2.389 -1.884 -2.119 -0.938 1978 5 3.798 -0.715 1 0 NaN NaN 3.166 -0.671 1978 6 8.245 -1.317 0 0 8.245 -1.317 7.976 -0.910 1978 7 13.066 -0.539 1 0 NaN NaN 12.955 0.026 1978 8 11.875 -1.624 0 0 11.875 -1.624 11.677 -1.145 1978 9 7.920 -1.873 0 0 7.920 -1.873 6.473 -2.644 1978 10 3.400 -0.881 0 0 3.400 -0.881 2.089 -1.516 1978 11 NaN NaN NaN NaN NaN NaN -4.611 -2.858 1978 12 NaN NaN NaN NaN NaN NaN -10.492 -0.903 1979 1 NaN NaN NaN NaN NaN NaN -7.870 4.612 1979 2 NaN NaN NaN NaN NaN NaN -12.149 -0.573 1979 3 NaN NaN NaN NaN NaN NaN -3.049 3.413 1979 4 NaN NaN NaN NaN NaN NaN 0.764 1.945 1979 5 NaN NaN NaN NaN NaN NaN 6.779 2.942 1979 6 NaN NaN NaN NaN NaN NaN 10.562 1.676 1979 7 NaN NaN NaN NaN NaN NaN 12.773 -0.156 1979 8 NaN NaN NaN NaN NaN NaN 12.129 -0.693 1979 9 NaN NaN NaN NaN NaN NaN 8.145 -0.972 1979 10 NaN NaN NaN NaN NaN NaN 3.436 -0.169