% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 174898 % Primary Name: ASKERSUND % Record Type: TAVG % Country: Sweden % Latitude: 58.88000 +/- 0.00500 % Longitude: 14.90000 +/- 0.00500 % Elevation (m): 100.00 +/- 0.50 % # of Months: 22 % % IDs: ghcnd - SWE00138664 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 4b580b00329bf8c5e1ac4854404a1d2f % Raw Data Hash: 211b1dd7a7fb6a08a91faf955996b522 % Adj Data Hash: 211b1dd7a7fb6a08a91faf955996b522 % % 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 1960 1 NaN NaN NaN NaN NaN NaN -4.190 -0.361 1960 2 NaN NaN NaN NaN NaN NaN -5.986 -1.741 1960 3 NaN NaN NaN NaN NaN NaN -0.426 0.338 1960 4 NaN NaN NaN NaN NaN NaN 4.172 0.015 1960 5 NaN NaN NaN NaN NaN NaN 10.865 0.908 1960 6 NaN NaN NaN NaN NaN NaN 16.044 1.175 1960 7 NaN NaN NaN NaN NaN NaN 15.113 -1.125 1960 8 NaN NaN NaN NaN NaN NaN 14.763 -0.613 1960 9 NaN NaN NaN NaN NaN NaN 11.142 -0.187 1960 10 NaN NaN NaN NaN NaN NaN 5.579 -1.060 1960 11 NaN NaN NaN NaN NaN NaN 2.711 0.910 1960 12 NaN NaN NaN NaN NaN NaN 0.447 2.111 1961 1 -4.150 0.122 0 0 -4.150 0.122 -3.318 0.511 1961 2 0.691 5.379 0 0 0.691 5.379 0.390 4.635 1961 3 3.805 5.013 0 0 3.805 5.013 4.157 4.922 1961 4 5.077 1.363 0 0 5.077 1.363 5.553 1.396 1961 5 9.645 0.131 0 0 9.645 0.131 9.694 -0.263 1961 6 16.315 1.889 0 0 16.315 1.889 16.343 1.474 1961 7 NaN NaN NaN NaN NaN NaN 15.255 -0.982 1961 8 NaN NaN NaN NaN NaN NaN 14.448 -0.928 1961 9 11.792 0.906 0 0 11.792 0.906 12.287 0.958 1961 10 10.727 4.531 0 0 10.727 4.531 10.896 4.257 1961 11 2.630 1.273 0 0 2.630 1.273 3.197 1.397 1961 12 -4.181 -2.073 0 0 -4.181 -2.073 -3.398 -1.734 1962 1 -1.647 2.625 0 0 -1.647 2.625 -1.317 2.513 1962 2 -2.584 2.104 0 0 -2.584 2.104 -2.674 1.571 1962 3 -6.161 -4.954 0 0 -6.161 -4.954 -4.930 -4.166 1962 4 4.423 0.710 0 0 4.423 0.710 4.861 0.704 1962 5 8.156 -1.358 0 0 8.156 -1.358 8.290 -1.667 1962 6 13.117 -1.309 0 0 13.117 -1.309 13.649 -1.220 1962 7 13.697 -2.098 0 0 13.697 -2.098 13.779 -2.458 1962 8 NaN NaN NaN NaN NaN NaN 13.282 -2.094 1962 9 9.598 -1.288 0 0 9.598 -1.288 9.877 -1.452 1962 10 7.745 1.549 0 0 7.745 1.549 8.008 1.369 1962 11 0.257 -1.101 0 0 0.257 -1.101 1.323 -0.477 1962 12 -4.742 -2.635 0 0 -4.742 -2.635 -3.938 -2.274 1963 1 -10.661 -6.389 0 0 -10.661 -6.389 -9.434 -5.604 1963 2 NaN NaN NaN NaN NaN NaN -8.559 -4.314 1963 3 NaN NaN NaN NaN NaN NaN -3.348 -2.583 1963 4 NaN NaN NaN NaN NaN NaN 3.985 -0.172 1963 5 NaN NaN NaN NaN NaN NaN 11.579 1.622 1963 6 NaN NaN NaN NaN NaN NaN 15.252 0.383 1963 7 NaN NaN NaN NaN NaN NaN 15.986 -0.251 1963 8 NaN NaN NaN NaN NaN NaN 15.373 -0.003 1963 9 NaN NaN NaN NaN NaN NaN 11.740 0.411 1963 10 NaN NaN NaN NaN NaN NaN 7.577 0.938 1963 11 NaN NaN NaN NaN NaN NaN 2.798 0.998 1963 12 NaN NaN NaN NaN NaN NaN -2.119 -0.454 1964 1 NaN NaN NaN NaN NaN NaN -1.288 2.542