% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 17161 % Primary Name: KANSONG KOREA/TEAM 850 % Record Type: TAVG % Country: Korea, South % Latitude: 38.31600 +/- 0.00050 % Longitude: 128.51600 +/- 0.00050 % Elevation (m): 18.00 +/- 0.05 % # of Months: 24 % % IDs: gsod - 749376-99999 % usaf - 749376 % % Sources: Global Summary of the Day % % Site Hash: 31af74e297fb844476ff16e13d473b76 % Raw Data Hash: 264a67e9d168fbbf506745fb83eb04ca % Adj Data Hash: 553a4b286e4afbfd921f50dd73fddef4 % % 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 1951 9 NaN NaN NaN NaN NaN NaN 17.058 -1.470 1951 10 NaN NaN NaN NaN NaN NaN 12.863 0.919 1951 11 NaN NaN NaN NaN NaN NaN 5.243 0.035 1951 12 NaN NaN NaN NaN NaN NaN 0.001 1.654 1952 1 NaN NaN NaN NaN NaN NaN -4.329 0.423 1952 2 NaN NaN NaN NaN NaN NaN -4.028 -1.770 1952 3 NaN NaN NaN NaN NaN NaN 2.530 -0.765 1952 4 NaN NaN NaN NaN NaN NaN 10.562 0.344 1952 5 NaN NaN NaN NaN NaN NaN 18.343 2.030 1952 6 NaN NaN NaN NaN NaN NaN 20.583 0.472 1952 7 NaN NaN NaN NaN NaN NaN 24.022 0.268 1952 8 NaN NaN NaN NaN NaN NaN 24.014 -0.017 1952 9 15.863 -3.730 1 0 NaN NaN 17.993 -0.535 1952 10 12.841 -0.168 0 0 12.841 -0.168 10.925 -1.019 1952 11 8.183 1.912 0 0 8.183 1.912 6.378 1.171 1952 12 -0.362 0.226 0 0 -0.362 0.226 -3.428 -1.776 1953 1 -3.476 0.212 1 0 NaN NaN -6.157 -1.405 1953 2 NaN NaN NaN NaN NaN NaN -2.602 -0.344 1953 3 NaN NaN NaN NaN NaN NaN 3.944 0.648 1953 4 NaN NaN NaN NaN NaN NaN 9.949 -0.269 1953 5 16.152 -1.226 0 0 16.152 -1.226 16.665 0.351 1953 6 19.400 -1.775 0 0 19.400 -1.775 19.124 -0.987 1953 7 23.430 -1.388 0 0 23.430 -1.388 23.960 0.205 1953 8 23.797 -1.297 0 0 23.797 -1.297 24.497 0.466 1953 9 19.841 0.249 0 0 19.841 0.249 18.381 -0.148 1953 10 16.158 3.150 0 0 16.158 3.150 13.740 1.795 1953 11 6.824 0.553 0 0 6.824 0.553 4.298 -0.909 1953 12 3.473 4.062 0 0 3.473 4.062 -0.239 1.413 1954 1 0.487 4.175 0 0 0.487 4.175 -2.574 2.178 1954 2 1.589 2.783 1 0 NaN NaN -0.410 1.848 1954 3 5.194 0.834 0 0 5.194 0.834 3.142 -0.153 1954 4 11.265 -0.017 0 0 11.265 -0.017 11.160 0.942 1954 5 16.932 -0.446 0 0 16.932 -0.446 16.875 0.561 1954 6 16.574 -4.601 0 0 16.574 -4.601 17.752 -2.359 1954 7 19.222 -5.596 0 0 19.222 -5.596 20.407 -3.347 1954 8 24.480 -0.615 0 0 24.480 -0.615 25.139 1.108 1954 9 21.361 1.769 0 0 21.361 1.769 18.837 0.309 1954 10 14.575 1.567 1 0 NaN NaN 11.092 -0.852 1954 11 14.631 8.359 1 0 NaN NaN 8.581 3.373 1954 12 NaN NaN NaN NaN NaN NaN -3.068 -1.416 1955 1 NaN NaN NaN NaN NaN NaN -6.294 -1.542 1955 2 NaN NaN NaN NaN NaN NaN -0.596 1.662 1955 3 NaN NaN NaN NaN NaN NaN 3.557 0.262 1955 4 NaN NaN NaN NaN NaN NaN 10.555 0.336 1955 5 NaN NaN NaN NaN NaN NaN 16.235 -0.079 1955 6 NaN NaN NaN NaN NaN NaN 20.855 0.744 1955 7 NaN NaN NaN NaN NaN NaN 24.365 0.610 1955 8 NaN NaN NaN NaN NaN NaN 25.191 1.160 1955 9 NaN NaN NaN NaN NaN NaN 18.536 0.007 1955 10 NaN NaN NaN NaN NaN NaN 11.161 -0.784 1955 11 NaN NaN NaN NaN NaN NaN 5.386 0.179