% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 175272 % Primary Name: BJORKFORS % Record Type: TAVG % Country: Sweden % Latitude: 65.92000 +/- 0.00500 % Longitude: 23.47000 +/- 0.00500 % Elevation (m): 20.00 +/- 0.50 % # of Months: 18 % % IDs: ghcnd - SWE00140644 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 8a51d03d2f8dc0f1cec857929f2547c3 % Raw Data Hash: 83ca45c56fac64f6033da3ec75050c0d % Adj Data Hash: 7af71aa5d1da805b6a1c5cf23889d2a8 % % 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 1961 1 NaN NaN NaN NaN NaN NaN -12.081 2.258 1961 2 NaN NaN NaN NaN NaN NaN -9.457 4.416 1961 3 NaN NaN NaN NaN NaN NaN -5.358 2.972 1961 4 NaN NaN NaN NaN NaN NaN -3.137 -1.183 1961 5 NaN NaN NaN NaN NaN NaN 4.727 -0.595 1961 6 NaN NaN NaN NaN NaN NaN 14.692 2.502 1961 7 NaN NaN NaN NaN NaN NaN 16.312 1.761 1961 8 NaN NaN NaN NaN NaN NaN 12.184 -0.142 1961 9 NaN NaN NaN NaN NaN NaN 7.188 0.646 1961 10 NaN NaN NaN NaN NaN NaN 5.697 6.093 1961 11 NaN NaN NaN NaN NaN NaN -2.830 4.205 1961 12 NaN NaN NaN NaN NaN NaN -13.936 -1.978 1962 1 -13.582 0.620 0 0 -13.582 0.620 -14.191 0.148 1962 2 -12.080 1.655 0 0 -12.080 1.655 -12.424 1.449 1962 3 -16.300 -8.107 0 0 -16.300 -8.107 -15.194 -6.864 1962 4 1.328 3.146 0 0 1.328 3.146 0.593 2.548 1962 5 5.677 0.219 0 0 5.677 0.219 5.345 0.024 1962 6 10.057 -2.271 0 0 10.057 -2.271 10.736 -1.454 1962 7 12.773 -1.915 0 0 12.773 -1.915 12.419 -2.132 1962 8 10.673 -1.790 0 0 10.673 -1.790 10.187 -2.139 1962 9 6.877 0.197 0 0 6.877 0.197 6.136 -0.407 1962 10 3.134 3.392 0 0 3.134 3.392 1.697 2.093 1962 11 -3.642 3.256 0 0 -3.642 3.256 -4.086 2.948 1962 12 -14.798 -2.977 0 0 -14.798 -2.977 -15.274 -3.315 1963 1 -17.068 -2.866 0 0 -17.068 -2.866 -15.579 -1.241 1963 2 -15.118 -1.382 0 0 -15.118 -1.382 -16.738 -2.865 1963 3 -12.481 -4.287 0 0 -12.481 -4.287 -12.060 -3.729 1963 4 0.378 2.196 0 0 0.378 2.196 -0.327 1.628 1963 5 8.511 3.053 0 0 8.511 3.053 9.787 4.466 1963 6 10.105 -2.222 0 0 10.105 -2.222 10.952 -1.238 1963 7 NaN NaN NaN NaN NaN NaN 13.190 -1.361 1963 8 NaN NaN NaN NaN NaN NaN 13.048 0.721 1963 9 NaN NaN NaN NaN NaN NaN 9.298 2.755 1963 10 NaN NaN NaN NaN NaN NaN 1.427 1.823 1963 11 NaN NaN NaN NaN NaN NaN -7.329 -0.294 1963 12 NaN NaN NaN NaN NaN NaN -10.925 1.033 1964 1 NaN NaN NaN NaN NaN NaN -7.437 6.901 1964 2 NaN NaN NaN NaN NaN NaN -16.379 -2.507 1964 3 NaN NaN NaN NaN NaN NaN -8.261 0.069 1964 4 NaN NaN NaN NaN NaN NaN -1.742 0.212 1964 5 NaN NaN NaN NaN NaN NaN 6.066 0.745 1964 6 NaN NaN NaN NaN NaN NaN 10.908 -1.283