% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 174968 % Primary Name: ASKE % Record Type: TAVG % Country: Sweden % Latitude: 59.62000 +/- 0.00005 % Longitude: 17.66640 +/- 0.00005 % Elevation (m): 15.00 +/- 0.50 % # of Months: 15 % % IDs: ghcnd - SWE00139046 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 572ba13a5fe65d47509f2038d70d418d % Raw Data Hash: b45ef86ef2bdd6494afd40d8250c2091 % Adj Data Hash: 1d52591b513179a37939274e5f15f17e % % 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 -5.630 0.405 1961 2 NaN NaN NaN NaN NaN NaN -1.747 4.250 1961 3 NaN NaN NaN NaN NaN NaN 2.782 4.693 1961 4 NaN NaN NaN NaN NaN NaN 4.350 1.252 1961 5 NaN NaN NaN NaN NaN NaN 9.164 -0.011 1961 6 NaN NaN NaN NaN NaN NaN 15.986 1.518 1961 7 NaN NaN NaN NaN NaN NaN 15.023 -0.837 1961 8 NaN NaN NaN NaN NaN NaN 13.470 -1.132 1961 9 NaN NaN NaN NaN NaN NaN 11.006 0.847 1961 10 NaN NaN NaN NaN NaN NaN 9.357 4.315 1961 11 NaN NaN NaN NaN NaN NaN 1.443 1.783 1961 12 NaN NaN NaN NaN NaN NaN -6.372 -2.328 1962 1 -3.097 2.263 0 0 -3.097 2.263 -4.006 2.030 1962 2 -3.179 2.143 1 0 NaN NaN -4.342 1.656 1962 3 -6.061 -4.826 0 0 -6.061 -4.826 -6.136 -4.225 1962 4 4.317 0.543 0 0 4.317 0.543 3.817 0.719 1962 5 7.810 -2.041 0 0 7.810 -2.041 7.459 -1.716 1962 6 13.552 -1.592 0 0 13.552 -1.592 13.200 -1.268 1962 7 13.716 -2.819 0 0 13.716 -2.819 13.488 -2.371 1962 8 NaN NaN NaN NaN NaN NaN 12.457 -2.146 1962 9 10.068 -0.766 0 0 10.068 -0.766 9.004 -1.155 1962 10 7.115 1.397 0 0 7.115 1.397 6.485 1.443 1962 11 NaN NaN NaN NaN NaN NaN -0.752 -0.412 1962 12 -5.492 -2.123 0 0 -5.492 -2.123 -6.748 -2.704 1963 1 NaN NaN NaN NaN NaN NaN -10.242 -4.206 1963 2 -9.037 -3.716 1 0 NaN NaN -10.995 -4.998 1963 3 NaN NaN NaN NaN NaN NaN -4.529 -2.618 1963 4 3.575 -0.198 0 0 3.575 -0.198 3.117 0.020 1963 5 NaN NaN NaN NaN NaN NaN 11.177 2.001 1963 6 14.663 -0.480 0 0 14.663 -0.480 14.511 0.043 1963 7 16.582 0.047 0 0 16.582 0.047 15.338 -0.522 1963 8 NaN NaN NaN NaN NaN NaN 15.007 0.405 1963 9 12.393 1.559 0 0 12.393 1.559 10.829 0.670 1963 10 NaN NaN NaN NaN NaN NaN 6.005 0.963 1963 11 NaN NaN NaN NaN NaN NaN 0.115 0.454 1963 12 NaN NaN NaN NaN NaN NaN -3.464 0.580 1964 1 NaN NaN NaN NaN NaN NaN -2.924 3.112 1964 2 NaN NaN NaN NaN NaN NaN -5.876 0.121 1964 3 NaN NaN NaN NaN NaN NaN -2.462 -0.551 1964 4 NaN NaN NaN NaN NaN NaN 4.906 1.808 1964 5 NaN NaN NaN NaN NaN NaN 10.729 1.554 1964 6 NaN NaN NaN NaN NaN NaN 13.853 -0.616 1964 7 NaN NaN NaN NaN NaN NaN 14.215 -1.644 1964 8 NaN NaN NaN NaN NaN NaN 13.240 -1.363 1964 9 NaN NaN NaN NaN NaN NaN 9.578 -0.581