% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 17150 % Primary Name: TAEGWANG-NI KOREA/TEAM 813 % Record Type: TAVG % Country: Korea, South % Latitude: 38.16600 +/- 0.00050 % Longitude: 127.10000 +/- 0.00050 % Elevation (m): 87.00 +/- 0.05 % # of Months: 18 % % IDs: gsod - 749370-99999 % usaf - 749370 % % Sources: Global Summary of the Day % % Site Hash: 56205baaed90d7ac637cc8be8d44f8ab % Raw Data Hash: 3242fed111f0184176a2b5e7bb778bb9 % Adj Data Hash: cdeffeced1c92ac5486dafa02a55c948 % % 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 1952 5 NaN NaN NaN NaN NaN NaN 18.155 2.151 1952 6 NaN NaN NaN NaN NaN NaN 20.088 0.226 1952 7 NaN NaN NaN NaN NaN NaN 24.190 0.730 1952 8 NaN NaN NaN NaN NaN NaN 24.450 0.001 1952 9 NaN NaN NaN NaN NaN NaN 19.228 -0.682 1952 10 NaN NaN NaN NaN NaN NaN 12.767 -0.741 1952 11 NaN NaN NaN NaN NaN NaN 7.809 1.381 1952 12 NaN NaN NaN NaN NaN NaN -2.598 -1.862 1953 1 NaN NaN NaN NaN NaN NaN -5.314 -1.505 1953 2 NaN NaN NaN NaN NaN NaN -2.731 -1.075 1953 3 NaN NaN NaN NaN NaN NaN 3.814 0.379 1953 4 NaN NaN NaN NaN NaN NaN 9.459 -0.615 1953 5 17.016 -0.221 0 0 17.016 -0.221 16.456 0.453 1953 6 20.561 -0.535 0 0 20.561 -0.535 18.960 -0.903 1953 7 25.954 1.260 1 0 NaN NaN 23.741 0.281 1953 8 26.534 0.851 0 0 26.534 0.851 24.887 0.438 1953 9 21.670 0.527 0 0 21.670 0.527 19.818 -0.092 1953 10 13.536 -1.206 0 0 13.536 -1.206 15.099 1.591 1953 11 5.289 -2.373 0 0 5.289 -2.373 5.360 -1.068 1953 12 0.159 -0.338 0 0 0.159 -0.338 0.263 0.999 1954 1 -1.767 0.808 0 0 -1.767 0.808 -1.794 2.015 1954 2 -0.197 0.226 1 0 NaN NaN 0.190 1.846 1954 3 5.023 0.355 0 0 5.023 0.355 2.554 -0.881 1954 4 14.122 2.815 0 0 14.122 2.815 11.180 1.106 1954 5 18.930 1.693 0 0 18.930 1.693 16.485 0.482 1954 6 21.461 0.365 0 0 21.461 0.365 18.779 -1.084 1954 7 22.486 -2.208 0 0 22.486 -2.208 21.108 -2.352 1954 8 26.980 1.298 0 0 26.980 1.298 25.641 1.192 1954 9 21.083 -0.060 0 0 21.083 -0.060 19.784 -0.126 1954 10 18.461 3.719 1 0 NaN NaN 12.558 -0.950 1954 11 NaN NaN NaN NaN NaN NaN 9.606 3.178 1954 12 NaN NaN NaN NaN NaN NaN -2.753 -2.017 1955 1 NaN NaN NaN NaN NaN NaN -5.384 -1.575 1955 2 NaN NaN NaN NaN NaN NaN -0.241 1.415 1955 3 NaN NaN NaN NaN NaN NaN 3.253 -0.182 1955 4 NaN NaN NaN NaN NaN NaN 10.257 0.184 1955 5 NaN NaN NaN NaN NaN NaN 15.867 -0.136 1955 6 NaN NaN NaN NaN NaN NaN 20.354 0.491 1955 7 NaN NaN NaN NaN NaN NaN 23.748 0.288 1955 8 NaN NaN NaN NaN NaN NaN 26.188 1.739 1955 9 NaN NaN NaN NaN NaN NaN 20.284 0.374 1955 10 NaN NaN NaN NaN NaN NaN 12.743 -0.765