% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 175217 % Primary Name: ANKARVATTNET % Record Type: TAVG % Country: Sweden % Latitude: 64.87000 +/- 0.00500 % Longitude: 14.25000 +/- 0.00500 % Elevation (m): 470.00 +/- 0.50 % # of Months: 11 % % IDs: ghcnd - SWE00140412 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: eb9fb617d328351b03104731659f86ea % Raw Data Hash: e0e04a24414044f7c00e7c53e77a5b38 % Adj Data Hash: aedbe6994e07954254e732eda8d51e75 % % 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 1964 2 NaN NaN NaN NaN NaN NaN -9.336 0.292 1964 3 NaN NaN NaN NaN NaN NaN -4.422 1.199 1964 4 NaN NaN NaN NaN NaN NaN 0.269 1.588 1964 5 NaN NaN NaN NaN NaN NaN 5.444 1.187 1964 6 NaN NaN NaN NaN NaN NaN 8.084 -1.375 1964 7 NaN NaN NaN NaN NaN NaN 10.266 -1.387 1964 8 NaN NaN NaN NaN NaN NaN 9.270 -1.349 1964 9 NaN NaN NaN NaN NaN NaN 4.474 -1.393 1964 10 NaN NaN NaN NaN NaN NaN 3.202 2.456 1964 11 NaN NaN NaN NaN NaN NaN -3.843 0.842 1964 12 NaN NaN NaN NaN NaN NaN -5.873 2.197 1965 1 NaN NaN NaN NaN NaN NaN -10.688 -0.456 1965 2 -6.498 3.552 1 0 NaN NaN -7.051 2.577 1965 3 -6.226 -0.183 0 0 -6.226 -0.183 -5.268 0.353 1965 4 0.227 1.968 0 0 0.227 1.968 0.518 1.837 1965 5 NaN NaN NaN NaN NaN NaN 2.974 -1.282 1965 6 9.338 0.302 0 0 9.338 0.302 9.604 0.146 1965 7 9.660 -1.572 0 0 9.660 -1.572 9.411 -2.243 1965 8 9.456 -0.740 0 0 9.456 -0.740 9.361 -1.258 1965 9 8.293 2.848 0 0 8.293 2.848 7.749 1.882 1965 10 3.637 3.314 0 0 3.637 3.314 3.075 2.330 1965 11 -8.057 -2.950 0 0 -8.057 -2.950 -7.756 -3.071 1965 12 -15.819 -7.328 0 0 -15.819 -7.328 -13.568 -5.499 1966 1 -16.448 -5.793 0 0 -16.448 -5.793 -14.843 -4.610 1966 2 NaN NaN NaN NaN NaN NaN -18.055 -8.427 1966 3 NaN NaN NaN NaN NaN NaN -6.920 -1.299 1966 4 NaN NaN NaN NaN NaN NaN -3.814 -2.495 1966 5 NaN NaN NaN NaN NaN NaN 3.736 -0.520 1966 6 NaN NaN NaN NaN NaN NaN 12.122 2.663 1966 7 NaN NaN NaN NaN NaN NaN 11.092 -0.562 1966 8 NaN NaN NaN NaN NaN NaN 9.570 -1.049 1966 9 NaN NaN NaN NaN NaN NaN 3.836 -2.032 1966 10 NaN NaN NaN NaN NaN NaN 0.582 -0.164 1966 11 NaN NaN NaN NaN NaN NaN -4.631 0.054 1966 12 NaN NaN NaN NaN NaN NaN -6.932 1.138 1967 1 NaN NaN NaN NaN NaN NaN -13.631 -3.398