% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 159326 % Primary Name: PALGRUNDEN % Record Type: TAVG % Country: Sweden % Latitude: 58.75000 +/- 0.00500 % Longitude: 13.15000 +/- 0.00500 % Elevation (m): 50.00 +/- 0.05 % # of Months: 16 % % IDs: gsod - 024170-99999 % usaf - 24170 % wmo - 2417 % % Sources: Global Summary of the Day % World Meteorological Organization Metadata % % Site Hash: bc0fee953ca4521e42469c83b1cb6d1d % Raw Data Hash: 312b974aff4506d8dc941738f10e1c43 % Adj Data Hash: 65c14ac40d7c71e4a1ff96184f6e961a % % 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 1995 5 NaN NaN NaN NaN NaN NaN 10.027 -0.373 1995 6 NaN NaN NaN NaN NaN NaN 15.269 0.136 1995 7 NaN NaN NaN NaN NaN NaN 16.510 0.127 1995 8 NaN NaN NaN NaN NaN NaN 17.421 1.984 1995 9 NaN NaN NaN NaN NaN NaN 11.464 -0.021 1995 10 NaN NaN NaN NaN NaN NaN 9.523 2.867 1995 11 NaN NaN NaN NaN NaN NaN 0.344 -1.197 1995 12 NaN NaN NaN NaN NaN NaN -4.803 -2.903 1996 1 NaN NaN NaN NaN NaN NaN -4.588 -0.714 1996 2 NaN NaN NaN NaN NaN NaN -7.080 -3.063 1996 3 NaN NaN NaN NaN NaN NaN -0.689 -0.220 1996 4 NaN NaN NaN NaN NaN NaN 5.362 1.051 1996 5 6.419 -4.009 0 0 6.419 -4.009 8.992 -1.408 1996 6 12.581 -2.580 0 0 12.581 -2.580 14.713 -0.421 1996 7 14.606 -1.805 0 0 14.606 -1.805 15.116 -1.267 1996 8 17.643 2.179 0 0 17.643 2.179 17.734 2.297 1996 9 11.958 0.445 1 0 NaN NaN 9.761 -1.724 1996 10 9.125 2.441 0 0 9.125 2.441 8.124 1.467 1996 11 4.511 2.943 0 0 4.511 2.943 2.359 0.818 1996 12 -0.590 1.283 0 0 -0.590 1.283 -3.937 -2.037 1997 1 -1.113 2.734 0 0 -1.113 2.734 -3.555 0.318 1997 2 0.439 4.429 1 0 NaN NaN -0.653 3.364 1997 3 1.928 2.370 0 0 1.928 2.370 2.379 2.848 1997 4 3.657 -0.680 0 0 3.657 -0.680 4.288 -0.022 1997 5 7.797 -2.630 0 0 7.797 -2.630 9.655 -0.745 1997 6 15.159 -0.002 0 0 15.159 -0.002 16.345 1.211 1997 7 18.801 2.390 0 0 18.801 2.390 17.957 1.573 1997 8 18.592 3.128 1 0 NaN NaN 19.709 4.272 1997 9 NaN NaN NaN NaN NaN NaN 12.416 0.930 1997 10 NaN NaN NaN NaN NaN NaN 5.200 -1.457 1997 11 NaN NaN NaN NaN NaN NaN 1.615 0.074 1997 12 NaN NaN NaN NaN NaN NaN -0.732 1.168 1998 1 NaN NaN NaN NaN NaN NaN -0.691 3.183 1998 2 NaN NaN NaN NaN NaN NaN 1.516 5.533 1998 3 NaN NaN NaN NaN NaN NaN 1.080 1.549 1998 4 NaN NaN NaN NaN NaN NaN 4.582 0.272 1998 5 NaN NaN NaN NaN NaN NaN 11.411 1.011 1998 6 NaN NaN NaN NaN NaN NaN 14.084 -1.050 1998 7 NaN NaN NaN NaN NaN NaN 15.223 -1.160 1998 8 NaN NaN NaN NaN NaN NaN 14.248 -1.189