% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 174888 % Primary Name: ODEBYN % Record Type: TAVG % Country: Sweden % Latitude: 58.78000 +/- 0.00500 % Longitude: 12.18000 +/- 0.00500 % Elevation (m): 150.00 +/- 0.50 % # of Months: 33 % % IDs: ghcnd - SWE00138628 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: a40bf716aa45e4a0b8f22ccf5184e0cc % Raw Data Hash: 2b8828cface95637d941869d9ef7f58c % Adj Data Hash: f7c7a811f627efd4d9534140ff32a8e0 % % 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 -3.896 -0.022 1960 2 NaN NaN NaN NaN NaN NaN -6.179 -2.161 1960 3 NaN NaN NaN NaN NaN NaN 0.336 0.805 1960 4 NaN NaN NaN NaN NaN NaN 4.542 0.231 1960 5 NaN NaN NaN NaN NaN NaN 11.912 1.512 1960 6 NaN NaN NaN NaN NaN NaN 16.115 0.982 1960 7 NaN NaN NaN NaN NaN NaN 15.001 -1.382 1960 8 NaN NaN NaN NaN NaN NaN 15.116 -0.321 1960 9 NaN NaN NaN NaN NaN NaN 11.334 -0.151 1960 10 NaN NaN NaN NaN NaN NaN 5.211 -1.446 1960 11 NaN NaN NaN NaN NaN NaN 1.879 0.338 1960 12 NaN NaN NaN NaN NaN NaN -0.430 1.470 1961 1 -5.048 -0.129 0 0 -5.048 -0.129 -3.635 0.238 1961 2 0.280 5.343 0 0 0.280 5.343 0.123 4.140 1961 3 3.589 5.103 0 0 3.589 5.103 4.090 4.559 1961 4 4.633 1.368 0 0 4.633 1.368 5.789 1.479 1961 5 8.668 -0.687 0 0 8.668 -0.687 10.635 0.235 1961 6 14.108 0.020 0 0 14.108 0.020 16.100 0.966 1961 7 14.265 -1.073 0 0 14.265 -1.073 15.506 -0.877 1961 8 12.732 -1.659 0 0 12.732 -1.659 14.185 -1.252 1961 9 11.075 0.635 0 0 11.075 0.635 12.410 0.924 1961 10 9.653 4.042 0 0 9.653 4.042 10.391 3.735 1961 11 2.045 1.550 0 0 2.045 1.550 2.968 1.427 1961 12 -4.311 -1.366 0 0 -4.311 -1.366 -3.251 -1.351 1962 1 -1.587 3.332 0 0 -1.587 3.332 -1.323 2.551 1962 2 -1.782 3.280 0 0 -1.782 3.280 -1.576 2.442 1962 3 -5.852 -4.337 0 0 -5.852 -4.337 -4.235 -3.766 1962 4 3.973 0.708 0 0 3.973 0.708 4.838 0.528 1962 5 7.156 -2.198 0 0 7.156 -2.198 8.752 -1.649 1962 6 11.578 -2.510 0 0 11.578 -2.510 13.690 -1.444 1962 7 13.176 -2.162 0 0 13.176 -2.162 14.383 -2.000 1962 8 12.353 -2.038 0 0 12.353 -2.038 13.326 -2.111 1962 9 8.820 -1.620 1 0 NaN NaN 10.221 -1.264 1962 10 NaN NaN NaN NaN NaN NaN 8.065 1.409 1962 11 0.287 -0.209 0 0 0.287 -0.209 0.965 -0.576 1962 12 NaN NaN NaN NaN NaN NaN -4.053 -2.153 1963 1 NaN NaN NaN NaN NaN NaN -9.586 -5.712 1963 2 -8.638 -3.575 0 0 -8.638 -3.575 -8.853 -4.836 1963 3 -4.015 -2.500 0 0 -4.015 -2.500 -2.955 -2.486 1963 4 3.132 -0.133 0 0 3.132 -0.133 4.021 -0.289 1963 5 NaN NaN NaN NaN NaN NaN 11.335 0.934 1963 6 13.667 -0.422 0 0 13.667 -0.422 15.946 0.812 1963 7 14.374 -0.964 0 0 14.374 -0.964 15.549 -0.834 1963 8 14.011 -0.380 0 0 14.011 -0.380 15.247 -0.190 1963 9 10.657 0.217 0 0 10.657 0.217 11.644 0.159 1963 10 6.785 1.174 0 0 6.785 1.174 7.691 1.034 1963 11 2.607 2.111 0 0 2.607 2.111 2.816 1.275 1963 12 NaN NaN NaN NaN NaN NaN -2.990 -1.090 1964 1 NaN NaN NaN NaN NaN NaN -1.495 2.379 1964 2 -3.857 1.206 1 0 NaN NaN -3.682 0.335 1964 3 -1.535 -0.021 0 0 -1.535 -0.021 -0.789 -0.320 1964 4 NaN NaN NaN NaN NaN NaN 5.855 1.544 1964 5 NaN NaN NaN NaN NaN NaN 11.590 1.190 1964 6 NaN NaN NaN NaN NaN NaN 14.503 -0.630 1964 7 NaN NaN NaN NaN NaN NaN 14.543 -1.840 1964 8 NaN NaN NaN NaN NaN NaN 14.693 -0.744 1964 9 NaN NaN NaN NaN NaN NaN 10.706 -0.779 1964 10 NaN NaN NaN NaN NaN NaN 6.376 -0.280 1964 11 NaN NaN NaN NaN NaN NaN 2.805 1.264 1964 12 NaN NaN NaN NaN NaN NaN -1.365 0.536 1965 1 NaN NaN NaN NaN NaN NaN -1.980 1.894 1965 2 NaN NaN NaN NaN NaN NaN -3.368 0.649 1965 3 NaN NaN NaN NaN NaN NaN -1.036 -0.567