% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 29020 % Primary Name: AUBURN % Record Type: TAVG % Country: United States % State: GA % Latitude: 34.01670 +/- 0.00005 % Longitude: -83.83330 +/- 0.00005 % Elevation (m): 358.14 +/- 0.15 % # of Months: 11 % % Alternate Names: Missing Station ID - 90485 % % IDs: coop - 90485 % ghcnd - USC00090485 % ncdc - 12001412 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: d8f4e9f8d31894120e12d16d39f40a04 % Raw Data Hash: 986a92d1ebcfc4a20f509ccbe47c14e9 % Adj Data Hash: 4db3df106b10cee7977d4a2eda753db4 % % 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 1899 11 NaN NaN NaN NaN NaN NaN 10.527 0.919 1899 12 NaN NaN NaN NaN NaN NaN 3.715 -1.682 1900 1 NaN NaN NaN NaN NaN NaN 3.226 -0.895 1900 2 NaN NaN NaN NaN NaN NaN 2.679 -2.951 1900 3 NaN NaN NaN NaN NaN NaN 8.213 -1.547 1900 4 NaN NaN NaN NaN NaN NaN 14.953 0.132 1900 5 NaN NaN NaN NaN NaN NaN 18.440 -0.588 1900 6 NaN NaN NaN NaN NaN NaN 21.803 -0.786 1900 7 NaN NaN NaN NaN NaN NaN 24.480 0.099 1900 8 NaN NaN NaN NaN NaN NaN 25.703 1.619 1900 9 NaN NaN NaN NaN NaN NaN 22.827 1.814 1900 10 NaN NaN NaN NaN NaN NaN 17.211 2.390 1900 11 11.893 0.482 0 0 11.893 0.482 10.330 0.722 1900 12 7.226 0.027 0 0 7.226 0.027 4.865 -0.531 1901 1 6.679 0.756 0 0 6.679 0.756 3.969 -0.152 1901 2 4.970 -2.464 1 0 NaN NaN 2.520 -3.110 1901 3 11.488 -0.075 1 0 NaN NaN 8.699 -1.061 1901 4 12.162 -4.462 0 0 12.162 -4.462 11.112 -3.709 1901 5 20.403 -0.428 0 0 20.403 -0.428 18.760 -0.269 1901 6 24.408 0.017 0 0 24.408 0.017 22.919 0.331 1901 7 NaN NaN NaN NaN NaN NaN 25.406 1.026 1901 8 24.903 -0.983 1 0 NaN NaN 23.218 -0.866 1901 9 21.454 -1.362 1 0 NaN NaN 20.017 -0.996 1901 10 NaN NaN NaN NaN NaN NaN 14.114 -0.706 1901 11 NaN NaN NaN NaN NaN NaN 6.982 -2.626 1901 12 NaN NaN NaN NaN NaN NaN 3.088 -2.308 1902 1 NaN NaN NaN NaN NaN NaN 2.836 -1.284 1902 2 NaN NaN NaN NaN NaN NaN 1.372 -4.259 1902 3 11.420 -0.143 1 0 NaN NaN 9.052 -0.708 1902 4 NaN NaN NaN NaN NaN NaN 13.347 -1.474 1902 5 NaN NaN NaN NaN NaN NaN 21.039 2.010 1902 6 NaN NaN NaN NaN NaN NaN 23.602 1.014 1902 7 NaN NaN NaN NaN NaN NaN 25.293 0.913 1902 8 NaN NaN NaN NaN NaN NaN 24.381 0.298 1902 9 NaN NaN NaN NaN NaN NaN 19.802 -1.211 1902 10 NaN NaN NaN NaN NaN NaN 14.847 0.027 1902 11 NaN NaN NaN NaN NaN NaN 12.456 2.848 1902 12 NaN NaN NaN NaN NaN NaN 4.687 -0.709 1903 1 NaN NaN NaN NaN NaN NaN 3.028 -1.093 1903 2 NaN NaN NaN NaN NaN NaN 5.507 -0.124 1903 3 NaN NaN NaN NaN NaN NaN 12.506 2.745