% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 9324 % Primary Name: CAPE SCOTT LH % Record Type: TAVG % Country: Canada % State: BC % Latitude: 50.78300 +/- 0.00050 % Longitude: -128.43300 +/- 0.00050 % Elevation (m): 72.00 +/- 0.05 % # of Months: 36 % % IDs: gsod - 710328-99999 % icao - CWES % usaf - 710328 % % Sources: Global Summary of the Day % % Site Hash: 50bb9a6545e941cd58313b09ab65cf19 % Raw Data Hash: effb43705d650f852057a74c6dca8b25 % Adj Data Hash: 889ea58b3722266e58c828984b706b5e % % 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 1998 1 NaN NaN NaN NaN NaN NaN 3.762 0.845 1998 2 NaN NaN NaN NaN NaN NaN 6.986 2.639 1998 3 NaN NaN NaN NaN NaN NaN 6.127 1.658 1998 4 NaN NaN NaN NaN NaN NaN 6.939 0.800 1998 5 NaN NaN NaN NaN NaN NaN 10.107 1.377 1998 6 NaN NaN NaN NaN NaN NaN 11.808 0.879 1998 7 NaN NaN NaN NaN NaN NaN 13.903 1.044 1998 8 NaN NaN NaN NaN NaN NaN 14.508 1.124 1998 9 NaN NaN NaN NaN NaN NaN 13.173 1.118 1998 10 NaN NaN NaN NaN NaN NaN 10.058 1.011 1998 11 NaN NaN NaN NaN NaN NaN 6.926 0.981 1998 12 NaN NaN NaN NaN NaN NaN 4.365 0.254 1999 1 4.554 1.004 1 0 NaN NaN 4.310 1.394 1999 2 5.640 0.661 1 0 NaN NaN 4.825 0.479 1999 3 4.971 -0.132 1 0 NaN NaN 4.077 -0.393 1999 4 7.033 0.261 0 0 7.033 0.261 5.902 -0.238 1999 5 7.935 -1.427 0 0 7.935 -1.427 7.395 -1.334 1999 6 10.231 -1.331 0 0 10.231 -1.331 10.045 -0.885 1999 7 11.889 -1.603 1 0 NaN NaN 12.289 -0.570 1999 8 13.504 -0.513 0 0 13.504 -0.513 13.725 0.341 1999 9 11.822 -0.866 0 0 11.822 -0.866 11.976 -0.079 1999 10 9.360 -0.319 0 0 9.360 -0.319 8.714 -0.332 1999 11 7.552 0.974 0 0 7.552 0.974 6.500 0.555 1999 12 6.593 1.849 0 0 6.593 1.849 5.343 1.233 2000 1 4.265 0.715 0 0 4.265 0.715 3.034 0.117 2000 2 5.684 0.705 0 0 5.684 0.705 5.646 1.300 2000 3 6.228 1.125 0 0 6.228 1.125 5.382 0.913 2000 4 7.293 0.520 0 0 7.293 0.520 6.472 0.332 2000 5 8.849 -0.513 0 0 8.849 -0.513 8.224 -0.505 2000 6 11.494 -0.068 0 0 11.494 -0.068 11.106 0.176 2000 7 13.584 0.093 0 0 13.584 0.093 13.241 0.383 2000 8 13.713 -0.304 0 0 13.713 -0.304 13.587 0.203 2000 9 12.354 -0.335 0 0 12.354 -0.335 12.312 0.257 2000 10 10.382 0.702 0 0 10.382 0.702 9.611 0.564 2000 11 7.935 1.357 0 0 7.935 1.357 6.578 0.633 2000 12 5.544 0.801 0 0 5.544 0.801 4.485 0.375 2001 1 6.726 3.176 0 0 6.726 3.176 5.284 2.368 2001 2 5.240 0.261 0 0 5.240 0.261 4.926 0.580 2001 3 6.000 0.898 0 0 6.000 0.898 5.064 0.595 2001 4 7.196 0.424 0 0 7.196 0.424 6.161 0.021 2001 5 8.248 -1.115 0 0 8.248 -1.115 7.718 -1.011 2001 6 10.845 -0.718 0 0 10.845 -0.718 10.107 -0.823 2001 7 12.537 -0.955 0 0 12.537 -0.955 12.419 -0.439 2001 8 13.590 -0.427 0 0 13.590 -0.427 13.327 -0.057 2001 9 12.504 -0.185 0 0 12.504 -0.185 12.267 0.211 2001 10 9.781 0.102 0 0 9.781 0.102 8.909 -0.137 2001 11 7.757 1.180 0 0 7.757 1.180 6.692 0.748 2001 12 5.217 0.473 1 0 NaN NaN 4.836 0.725 2002 1 NaN NaN NaN NaN NaN NaN 4.462 1.546 2002 2 NaN NaN NaN NaN NaN NaN 5.140 0.794 2002 3 NaN NaN NaN NaN NaN NaN 3.059 -1.411 2002 4 NaN NaN NaN NaN NaN NaN 6.159 0.019 2002 5 NaN NaN NaN NaN NaN NaN 8.202 -0.528 2002 6 NaN NaN NaN NaN NaN NaN 11.125 0.196 2002 7 NaN NaN NaN NaN NaN NaN 13.154 0.296 2002 8 NaN NaN NaN NaN NaN NaN 14.250 0.866 2002 9 NaN NaN NaN NaN NaN NaN 12.854 0.799 2002 10 NaN NaN NaN NaN NaN NaN 9.453 0.406 2002 11 NaN NaN NaN NaN NaN NaN 8.300 2.355 2002 12 NaN NaN NaN NaN NaN NaN 6.179 2.069