% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 8236 % Primary Name: CHILLIWACK R FOLEY CREEK % Record Type: TAVG % Country: Canada % Latitude: 49.10000 +/- 0.00500 % Longitude: -121.63000 +/- 0.00500 % Elevation (m): 369.00 +/- 0.50 % # of Months: 11 % % IDs: ghcnd - CA001101565 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 15108b2edc527f1cb518f0c074747525 % Raw Data Hash: 429254952b4eb6062203ab76b96d54c4 % Adj Data Hash: 1b436e82d4acb17aba12f603af45aa4b % % 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 1981 11 NaN NaN NaN NaN NaN NaN 4.960 1.728 1981 12 NaN NaN NaN NaN NaN NaN 1.262 0.505 1982 1 NaN NaN NaN NaN NaN NaN -1.676 -1.054 1982 2 NaN NaN NaN NaN NaN NaN 2.210 0.133 1982 3 NaN NaN NaN NaN NaN NaN 3.024 -0.369 1982 4 NaN NaN NaN NaN NaN NaN 4.851 -1.490 1982 5 NaN NaN NaN NaN NaN NaN 9.667 -0.374 1982 6 NaN NaN NaN NaN NaN NaN 14.314 1.537 1982 7 NaN NaN NaN NaN NaN NaN 14.244 -0.827 1982 8 NaN NaN NaN NaN NaN NaN 14.422 -0.377 1982 9 NaN NaN NaN NaN NaN NaN 13.098 0.823 1982 10 NaN NaN NaN NaN NaN NaN 8.207 0.480 1982 11 2.375 -1.485 0 0 2.375 -1.485 1.406 -1.827 1982 12 NaN NaN NaN NaN NaN NaN 1.499 0.742 1983 1 3.000 2.994 1 0 NaN NaN 3.006 3.629 1983 2 5.149 2.444 1 0 NaN NaN 4.955 2.878 1983 3 7.242 3.221 0 0 7.242 3.221 5.626 2.233 1983 4 NaN NaN NaN NaN NaN NaN 6.801 0.461 1983 5 NaN NaN NaN NaN NaN NaN 11.575 1.534 1983 6 NaN NaN NaN NaN NaN NaN 12.355 -0.422 1983 7 NaN NaN NaN NaN NaN NaN 13.978 -1.093 1983 8 NaN NaN NaN NaN NaN NaN 15.380 0.581 1983 9 NaN NaN NaN NaN NaN NaN 11.249 -1.026 1983 10 7.411 -0.943 0 0 7.411 -0.943 7.273 -0.454 1983 11 NaN NaN NaN NaN NaN NaN 4.545 1.313 1983 12 -5.339 -6.723 0 0 -5.339 -6.723 -2.468 -3.224 1984 1 2.250 2.244 0 0 2.250 2.244 1.520 2.142 1984 2 4.155 1.451 1 0 NaN NaN 4.428 2.351 1984 3 6.694 2.673 0 0 6.694 2.673 5.354 1.961 1984 4 8.200 1.232 0 0 8.200 1.232 5.729 -0.612 1984 5 10.250 -0.419 1 0 NaN NaN 8.491 -1.550 1984 6 NaN NaN NaN NaN NaN NaN 11.920 -0.857 1984 7 NaN NaN NaN NaN NaN NaN 15.141 0.070 1984 8 NaN NaN NaN NaN NaN NaN 14.852 0.052 1984 9 NaN NaN NaN NaN NaN NaN 11.595 -0.679 1984 10 NaN NaN NaN NaN NaN NaN 6.285 -1.441 1984 11 NaN NaN NaN NaN NaN NaN 2.668 -0.564 1984 12 NaN NaN NaN NaN NaN NaN -2.163 -2.920 1985 1 NaN NaN NaN NaN NaN NaN -1.281 -0.659 1985 2 NaN NaN NaN NaN NaN NaN 1.400 -0.677 1985 3 NaN NaN NaN NaN NaN NaN 2.716 -0.677 1985 4 NaN NaN NaN NaN NaN NaN 5.948 -0.393 1985 5 NaN NaN NaN NaN NaN NaN 10.221 0.179