% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 6888 % Primary Name: KNOWLTON % Record Type: TAVG % Country: Canada % Latitude: 45.22000 +/- 0.00500 % Longitude: -72.50000 +/- 0.00500 % Elevation (m): 206.00 +/- 0.50 % # of Months: 30 % % IDs: ghcnd - CA007023530 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: b50794a1c67dbae2c3343c943333a707 % Raw Data Hash: 40be75cc3512a0b21952049bcd1ecf8b % Adj Data Hash: 18d0873c11b2bfd7d16b8ca3016f44b0 % % 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 1957 11 NaN NaN NaN NaN NaN NaN 3.410 2.683 1957 12 NaN NaN NaN NaN NaN NaN -5.521 2.734 1958 1 NaN NaN NaN NaN NaN NaN -8.381 3.116 1958 2 NaN NaN NaN NaN NaN NaN -12.497 -2.237 1958 3 NaN NaN NaN NaN NaN NaN -0.181 3.368 1958 4 NaN NaN NaN NaN NaN NaN 5.825 1.433 1958 5 NaN NaN NaN NaN NaN NaN 9.854 -2.049 1958 6 NaN NaN NaN NaN NaN NaN 13.747 -3.453 1958 7 NaN NaN NaN NaN NaN NaN 19.111 -0.583 1958 8 NaN NaN NaN NaN NaN NaN 17.887 -0.384 1958 9 NaN NaN NaN NaN NaN NaN 13.322 -0.206 1958 10 NaN NaN NaN NaN NaN NaN 7.008 -0.405 1958 11 1.900 0.884 0 0 1.900 0.884 2.119 1.392 1958 12 -13.206 -5.240 0 0 -13.206 -5.240 -15.096 -6.841 1959 1 -10.860 0.349 0 0 -10.860 0.349 -11.564 -0.066 1959 2 -12.243 -2.272 0 0 -12.243 -2.272 -13.667 -3.407 1959 3 -4.652 -1.392 0 0 -4.652 -1.392 -5.172 -1.623 1959 4 5.387 0.706 0 0 5.387 0.706 4.874 0.483 1959 5 12.779 0.587 0 0 12.779 0.587 13.714 1.811 1959 6 16.777 -0.713 0 0 16.777 -0.713 16.531 -0.669 1959 7 20.403 0.420 0 0 20.403 0.420 21.288 1.594 1959 8 20.584 2.024 0 0 20.584 2.024 19.985 1.714 1959 9 15.775 1.958 0 0 15.775 1.958 15.327 1.799 1959 10 7.667 -0.036 0 0 7.667 -0.036 6.985 -0.429 1959 11 0.712 -0.304 0 0 0.712 -0.304 0.798 0.072 1959 12 -5.552 2.415 0 0 -5.552 2.415 -7.408 0.847 1960 1 -10.681 0.528 0 0 -10.681 0.528 -11.187 0.311 1960 2 -5.409 4.562 1 0 NaN NaN -6.382 3.878 1960 3 -6.281 -3.021 0 0 -6.281 -3.021 -5.641 -2.093 1960 4 5.075 0.394 0 0 5.075 0.394 4.540 0.149 1960 5 14.887 2.695 0 0 14.887 2.695 15.028 3.125 1960 6 16.593 -0.896 0 0 16.593 -0.896 17.053 -0.147 1960 7 17.734 -2.249 0 0 17.734 -2.249 18.476 -1.218 1960 8 17.571 -0.989 0 0 17.571 -0.989 18.369 0.098 1960 9 13.960 0.143 1 0 NaN NaN 13.946 0.418 1960 10 6.363 -1.340 0 0 6.363 -1.340 6.712 -0.702 1960 11 NaN NaN NaN NaN NaN NaN 3.776 3.049 1960 12 -7.832 0.134 0 0 -7.832 0.134 -9.673 -1.418 1961 1 -13.966 -2.758 0 0 -13.966 -2.758 -15.150 -3.653 1961 2 -8.130 1.840 0 0 -8.130 1.840 -9.109 1.150 1961 3 -3.489 -0.229 0 0 -3.489 -0.229 -4.051 -0.502 1961 4 3.548 -1.132 0 0 3.548 -1.132 4.209 -0.183 1961 5 10.042 -2.150 0 0 10.042 -2.150 10.521 -1.382 1961 6 NaN NaN NaN NaN NaN NaN 16.190 -1.010 1961 7 NaN NaN NaN NaN NaN NaN 19.496 -0.198 1961 8 NaN NaN NaN NaN NaN NaN 18.692 0.421 1961 9 NaN NaN NaN NaN NaN NaN 16.995 3.466 1961 10 NaN NaN NaN NaN NaN NaN 9.173 1.759 1961 11 NaN NaN NaN NaN NaN NaN 2.634 1.907 1961 12 NaN NaN NaN NaN NaN NaN -6.656 1.599 1962 1 NaN NaN NaN NaN NaN NaN -12.138 -0.640 1962 2 NaN NaN NaN NaN NaN NaN -13.058 -2.798 1962 3 NaN NaN NaN NaN NaN NaN -1.786 1.763 1962 4 NaN NaN NaN NaN NaN NaN 3.943 -0.449 1962 5 NaN NaN NaN NaN NaN NaN 12.409 0.506