% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 11171 % Primary Name: MALLOCH DOME(AUTO8) % Record Type: TAVG % Country: Canada % State: NT % Latitude: 78.21700 +/- 0.00050 % Longitude: -101.05000 +/- 0.00050 % Elevation (m): 12.00 +/- 0.05 % # of Months: 12 % % IDs: gsod - 719248-99999 % icao - CWCN % usaf - 719248 % % Sources: Global Summary of the Day % % Site Hash: f801878ac8e5a014259fa805e1267cb1 % Raw Data Hash: 854de68ed310ccf3cbf723c2396e1337 % Adj Data Hash: b17e945e520d5709e364f9554b47b87f % % 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 1980 11 NaN NaN NaN NaN NaN NaN -26.387 -0.026 1980 12 NaN NaN NaN NaN NaN NaN -30.396 0.625 1981 1 NaN NaN NaN NaN NaN NaN -28.647 4.573 1981 2 NaN NaN NaN NaN NaN NaN -33.070 1.921 1981 3 NaN NaN NaN NaN NaN NaN -31.360 2.155 1981 4 NaN NaN NaN NaN NaN NaN -25.900 -0.572 1981 5 NaN NaN NaN NaN NaN NaN -10.281 1.900 1981 6 NaN NaN NaN NaN NaN NaN 0.170 2.449 1981 7 NaN NaN NaN NaN NaN NaN 1.540 0.060 1981 8 NaN NaN NaN NaN NaN NaN -0.358 -0.446 1981 9 NaN NaN NaN NaN NaN NaN -6.941 0.577 1981 10 NaN NaN NaN NaN NaN NaN -15.098 2.378 1981 11 -26.276 -0.900 1 0 NaN NaN -22.200 4.161 1981 12 -24.755 5.280 1 0 NaN NaN -25.329 5.692 1982 1 -28.079 4.155 1 0 NaN NaN -30.125 3.095 1982 2 -32.971 1.034 1 0 NaN NaN -34.602 0.389 1982 3 -33.004 -0.475 0 0 -33.004 -0.475 -34.102 -0.587 1982 4 -28.211 -3.869 1 0 NaN NaN -27.648 -2.320 1982 5 -9.384 1.811 1 0 NaN NaN -13.077 -0.896 1982 6 -0.086 1.207 1 0 NaN NaN -1.847 0.432 1982 7 2.805 0.338 0 0 2.805 0.338 1.368 -0.112 1982 8 -0.201 -1.275 0 0 -0.201 -1.275 -0.623 -0.712 1982 9 -1.136 5.396 1 0 NaN NaN -8.572 -1.054 1982 10 NaN NaN NaN NaN NaN NaN -18.470 -0.995 1982 11 NaN NaN NaN NaN NaN NaN -29.548 -3.186 1982 12 NaN NaN NaN NaN NaN NaN -33.152 -2.130 1983 1 0.000 32.234 1 0 NaN NaN -34.360 -1.140 1983 2 NaN NaN NaN NaN NaN NaN -35.656 -0.665 1983 3 NaN NaN NaN NaN NaN NaN -33.040 0.475 1983 4 NaN NaN NaN NaN NaN NaN -27.282 -1.954 1983 5 NaN NaN NaN NaN NaN NaN -14.838 -2.656 1983 6 NaN NaN NaN NaN NaN NaN -0.780 1.498 1983 7 NaN NaN NaN NaN NaN NaN 1.632 0.152 1983 8 NaN NaN NaN NaN NaN NaN 1.000 0.912 1983 9 NaN NaN NaN NaN NaN NaN -5.001 2.517 1983 10 NaN NaN NaN NaN NaN NaN -18.791 -1.315 1983 11 NaN NaN NaN NaN NaN NaN -24.665 1.696 1983 12 NaN NaN NaN NaN NaN NaN -28.046 2.975 1984 1 NaN NaN NaN NaN NaN NaN -36.071 -2.851