% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 17145 % Primary Name: HWACHON KOREA/TEAM 830 % Record Type: TAVG % Country: Korea, South % Latitude: 38.13300 +/- 0.00050 % Longitude: 127.68300 +/- 0.00050 % Elevation (m): 145.00 +/- 0.05 % # of Months: 24 % % IDs: gsod - 749373-99999 % usaf - 749373 % % Sources: Global Summary of the Day % % Site Hash: 73250eb75fd09ea899103a644c7aa7c8 % Raw Data Hash: 3e94656d3cbf4d3c2fd654eb1746f984 % Adj Data Hash: 8b6c519c6feffc98af712fc4598c6869 % % 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 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 NaN NaN NaN NaN 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 2.399 -7.835 1 0 NaN NaN 9.949 -0.269 1953 5 16.197 -0.133 0 0 16.197 -0.133 16.665 0.351 1953 6 19.500 -0.627 0 0 19.500 -0.627 19.124 -0.987 1953 7 24.679 0.909 0 0 24.679 0.909 23.960 0.205 1953 8 23.320 -0.727 1 0 NaN NaN 24.497 0.466 1953 9 17.937 -0.607 0 0 17.937 -0.607 18.381 -0.148 1953 10 12.220 0.260 0 0 12.220 0.260 13.740 1.795 1953 11 3.135 -2.088 0 0 3.135 -2.088 4.298 -0.909 1953 12 -0.819 0.817 0 0 -0.819 0.817 -0.239 1.413 1954 1 -3.170 1.565 0 0 -3.170 1.565 -2.574 2.178 1954 2 -1.387 0.855 0 0 -1.387 0.855 -0.410 1.848 1954 3 3.220 -0.091 0 0 3.220 -0.091 3.142 -0.153 1954 4 11.609 1.375 0 0 11.609 1.375 11.160 0.942 1954 5 16.482 0.152 0 0 16.482 0.152 16.875 0.561 1954 6 18.952 -1.175 0 0 18.952 -1.175 17.752 -2.359 1954 7 20.706 -3.064 0 0 20.706 -3.064 20.407 -3.347 1954 8 26.188 2.141 0 0 26.188 2.141 25.139 1.108 1954 9 20.443 1.898 0 0 20.443 1.898 18.837 0.309 1954 10 12.455 0.495 0 0 12.455 0.495 11.092 -0.852 1954 11 8.744 3.521 0 0 8.744 3.521 8.581 3.373 1954 12 -3.441 -1.804 0 0 -3.441 -1.804 -3.068 -1.416 1955 1 -6.919 -2.184 0 0 -6.919 -2.184 -6.294 -1.542 1955 2 -0.427 1.816 0 0 -0.427 1.816 -0.596 1.662 1955 3 5.111 1.800 1 0 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 1955 12 NaN NaN NaN NaN NaN NaN 0.249 1.902 1956 1 NaN NaN NaN NaN NaN NaN -4.843 -0.091 1956 2 NaN NaN NaN NaN NaN NaN -3.583 -1.325 1956 3 NaN NaN NaN NaN NaN NaN 2.275 -1.020