% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 17166 % Primary Name: SOKCHORI KOREA % Record Type: TAVG % Country: Korea, South % Latitude: 38.43300 +/- 0.00050 % Longitude: 127.30000 +/- 0.00050 % Elevation (m): 335.00 +/- 0.05 % # of Months: 15 % % IDs: gsod - 749355-99999 % usaf - 749355 % % Sources: Global Summary of the Day % % Site Hash: 16a375ed265da02de3c63ead34ac80a6 % Raw Data Hash: 546a00f275455a3811a4571d35611fc5 % Adj Data Hash: c4615b762eac2383c0a74dc0dc1e37b1 % % 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 1950 7 NaN NaN NaN NaN NaN NaN 24.674 0.920 1950 8 NaN NaN NaN NaN NaN NaN 25.142 1.111 1950 9 NaN NaN NaN NaN NaN NaN 17.794 -0.734 1950 10 NaN NaN NaN NaN NaN NaN 11.996 0.052 1950 11 NaN NaN NaN NaN NaN NaN 4.931 -0.277 1950 12 NaN NaN NaN NaN NaN NaN -2.842 -1.190 1951 1 NaN NaN NaN NaN NaN NaN -4.924 -0.172 1951 2 NaN NaN NaN NaN NaN NaN -0.906 1.353 1951 3 NaN NaN NaN NaN NaN NaN 2.006 -1.290 1951 4 NaN NaN NaN NaN NaN NaN 9.293 -0.925 1951 5 NaN NaN NaN NaN NaN NaN 16.678 0.364 1951 6 NaN NaN NaN NaN NaN NaN 19.890 -0.221 1951 7 26.098 0.800 1 0 NaN NaN 23.909 0.155 1951 8 25.928 0.354 0 0 25.928 0.354 25.709 1.678 1951 9 20.000 -0.072 0 0 20.000 -0.072 17.058 -1.470 1951 10 14.595 1.107 0 0 14.595 1.107 12.863 0.919 1951 11 7.283 0.532 0 0 7.283 0.532 5.243 0.035 1951 12 4.927 5.035 0 0 4.927 5.035 0.001 1.654 1952 1 0.430 3.638 0 0 0.430 3.638 -4.329 0.423 1952 2 -1.747 -1.033 1 0 NaN NaN -4.028 -1.770 1952 3 5.518 0.679 0 0 5.518 0.679 2.530 -0.765 1952 4 11.322 -0.439 0 0 11.322 -0.439 10.562 0.344 1952 5 17.235 -0.622 0 0 17.235 -0.622 18.343 2.030 1952 6 21.156 -0.499 0 0 21.156 -0.499 20.583 0.472 1952 7 22.799 -2.499 0 0 22.799 -2.499 24.022 0.268 1952 8 23.930 -1.644 0 0 23.930 -1.644 24.014 -0.017 1952 9 20.726 0.654 1 0 NaN NaN 17.993 -0.535 1952 10 NaN NaN NaN NaN NaN NaN 10.925 -1.019 1952 11 NaN NaN NaN NaN NaN NaN 6.378 1.171 1952 12 NaN NaN NaN NaN NaN NaN -3.428 -1.776 1953 1 NaN NaN NaN NaN 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 NaN NaN NaN NaN NaN NaN 16.665 0.351 1953 6 NaN NaN NaN NaN NaN NaN 19.124 -0.987 1953 7 NaN NaN NaN NaN NaN NaN 23.960 0.205 1953 8 NaN NaN NaN NaN NaN NaN 24.497 0.466 1953 9 NaN NaN NaN NaN NaN NaN 18.381 -0.148