% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 11626 % Primary Name: CHEN-YUAN % Record Type: TAVG % Country: China % Latitude: 27.05000 +/- 0.00500 % Longitude: 108.40000 +/- 0.00500 % Elevation (m): 463.90 +/- 0.05 % # of Months: 19 % % IDs: gsod - 577380-99999 % usaf - 577380 % % Sources: Global Summary of the Day % % Site Hash: fe02ee965cbb9fe0612f81922c7226f6 % Raw Data Hash: fb05c0743b7273841d32e2579af186e3 % Adj Data Hash: 532feffdcf3fd6dad118025c134a001c % % 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 1955 8 NaN NaN NaN NaN NaN NaN 25.100 -0.816 1955 9 NaN NaN NaN NaN NaN NaN 24.657 1.937 1955 10 NaN NaN NaN NaN NaN NaN 17.431 0.169 1955 11 NaN NaN NaN NaN NaN NaN 11.092 -0.844 1955 12 NaN NaN NaN NaN NaN NaN 9.049 2.048 1956 1 NaN NaN NaN NaN NaN NaN 3.339 -1.429 1956 2 NaN NaN NaN NaN NaN NaN 6.682 0.260 1956 3 NaN NaN NaN NaN NaN NaN 10.176 -0.954 1956 4 NaN NaN NaN NaN NaN NaN 17.659 1.252 1956 5 NaN NaN NaN NaN NaN NaN 19.075 -1.685 1956 6 NaN NaN NaN NaN NaN NaN 25.279 1.088 1956 7 NaN NaN NaN NaN NaN NaN 26.951 0.413 1956 8 26.004 0.028 1 0 NaN NaN 25.575 -0.340 1956 9 22.356 -0.424 0 0 22.356 -0.424 22.714 -0.006 1956 10 17.757 0.436 0 0 17.757 0.436 17.602 0.341 1956 11 11.908 -0.089 1 0 NaN NaN 10.627 -1.309 1956 12 6.424 -0.637 1 0 NaN NaN 5.385 -1.616 1957 1 3.927 -0.900 1 0 NaN NaN 4.710 -0.058 1957 2 3.121 -3.361 1 0 NaN NaN 3.142 -3.280 1957 3 11.235 0.045 0 0 11.235 0.045 11.140 0.009 1957 4 16.783 0.316 0 0 16.783 0.316 16.603 0.196 1957 5 20.374 -0.447 0 0 20.374 -0.447 20.005 -0.755 1957 6 23.638 -0.612 0 0 23.638 -0.612 23.471 -0.719 1957 7 26.763 0.166 0 0 26.763 0.166 26.876 0.339 1957 8 25.224 -0.751 0 0 25.224 -0.751 25.254 -0.661 1957 9 21.254 -1.526 0 0 21.254 -1.526 21.944 -0.776 1957 10 16.921 -0.400 0 0 16.921 -0.400 16.763 -0.498 1957 11 13.874 1.878 0 0 13.874 1.878 13.815 1.879 1957 12 8.237 1.176 0 0 8.237 1.176 7.883 0.882 1958 1 4.642 -0.186 0 0 4.642 -0.186 4.206 -0.562 1958 2 4.215 -2.267 1 0 NaN NaN 6.448 0.026 1958 3 NaN NaN NaN NaN NaN NaN 13.227 2.096 1958 4 NaN NaN NaN NaN NaN NaN 19.142 2.735 1958 5 NaN NaN NaN NaN NaN NaN 18.876 -1.884 1958 6 NaN NaN NaN NaN NaN NaN 24.485 0.295 1958 7 NaN NaN NaN NaN NaN NaN 26.592 0.054 1958 8 NaN NaN NaN NaN NaN NaN 24.658 -1.257 1958 9 NaN NaN NaN NaN NaN NaN 22.000 -0.720 1958 10 NaN NaN NaN NaN NaN NaN 15.340 -1.921 1958 11 NaN NaN NaN NaN NaN NaN 11.802 -0.134 1958 12 NaN NaN NaN NaN NaN NaN 8.587 1.586 1959 1 NaN NaN NaN NaN NaN NaN 4.597 -0.170 1959 2 NaN NaN NaN NaN NaN NaN 5.435 -0.987