% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 34183 % Primary Name: SUNMAN % Record Type: TAVG % Country: United States % State: IN % Latitude: 39.23330 +/- 0.00005 % Longitude: -85.10000 +/- 0.00005 % Elevation (m): 310.29 +/- 0.15 % # of Months: 22 % % Alternate Names: Missing Station ID - 128546 % % IDs: coop - 128546 % ghcnd - USC00128546 % ncdc - 12001796 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 97bf5d2df36493750b6931017a8363bc % Raw Data Hash: 605fc0341816197a5d1921c518b6457a % Adj Data Hash: 1094c4b3fa013071c45c4daf69d03122 % % 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 1894 1 NaN NaN NaN NaN NaN NaN 0.404 2.915 1894 2 NaN NaN NaN NaN NaN NaN -2.029 -1.424 1894 3 NaN NaN NaN NaN NaN NaN 7.690 2.823 1894 4 NaN NaN NaN NaN NaN NaN 11.462 0.027 1894 5 NaN NaN NaN NaN NaN NaN 15.898 -1.071 1894 6 NaN NaN NaN NaN NaN NaN 22.630 0.839 1894 7 NaN NaN NaN NaN NaN NaN 23.482 -0.298 1894 8 NaN NaN NaN NaN NaN NaN 22.848 -0.089 1894 9 NaN NaN NaN NaN NaN NaN 20.543 1.180 1894 10 NaN NaN NaN NaN NaN NaN 12.309 -0.237 1894 11 NaN NaN NaN NaN NaN NaN 3.586 -2.332 1894 12 NaN NaN NaN NaN NaN NaN 1.407 1.138 1895 1 -9.200 -6.449 1 0 NaN NaN -5.444 -2.933 1895 2 NaN NaN NaN NaN NaN NaN -7.331 -6.726 1895 3 NaN NaN NaN NaN NaN NaN 3.432 -1.435 1895 4 NaN NaN NaN NaN NaN NaN 12.152 0.717 1895 5 NaN NaN NaN NaN NaN NaN 16.488 -0.481 1895 6 23.167 1.616 0 0 23.167 1.616 23.280 1.489 1895 7 23.011 -0.528 0 0 23.011 -0.528 22.634 -1.146 1895 8 24.211 1.515 0 0 24.211 1.515 23.686 0.749 1895 9 20.685 1.563 0 0 20.685 1.563 21.308 1.945 1895 10 8.190 -4.115 0 0 8.190 -4.115 8.481 -4.065 1895 11 4.370 -1.307 0 0 4.370 -1.307 5.287 -0.631 1895 12 0.591 0.564 0 0 0.591 0.564 1.196 0.928 1896 1 -1.505 1.246 0 0 -1.505 1.246 -1.924 0.587 1896 2 -0.556 0.290 1 0 NaN NaN -0.666 -0.061 1896 3 1.333 -3.293 0 0 1.333 -3.293 1.399 -3.468 1896 4 14.889 3.694 0 0 14.889 3.694 15.285 3.850 1896 5 20.448 3.720 0 0 20.448 3.720 20.491 3.522 1896 6 20.944 -0.606 0 0 20.944 -0.606 21.669 -0.122 1896 7 22.993 -0.546 0 0 22.993 -0.546 23.348 -0.431 1896 8 22.061 -0.635 0 0 22.061 -0.635 22.558 -0.379 1896 9 17.056 -2.067 0 0 17.056 -2.067 17.659 -1.705 1896 10 9.892 -2.412 0 0 9.892 -2.412 10.251 -2.294 1896 11 6.815 1.138 0 0 6.815 1.138 7.249 1.332 1896 12 1.326 1.298 0 0 1.326 1.298 1.553 1.285 1897 1 -3.852 -1.100 0 0 -3.852 -1.100 -4.210 -1.700 1897 2 0.377 1.222 1 0 NaN NaN 0.017 0.621 1897 3 NaN NaN NaN NaN NaN NaN 6.217 1.351 1897 4 NaN NaN NaN NaN NaN NaN 10.636 -0.800 1897 5 NaN NaN NaN NaN NaN NaN 14.015 -2.954 1897 6 NaN NaN NaN NaN NaN NaN 21.039 -0.752 1897 7 NaN NaN NaN NaN NaN NaN 24.397 0.617 1897 8 NaN NaN NaN NaN NaN NaN 21.408 -1.529 1897 9 NaN NaN NaN NaN NaN NaN 20.611 1.248 1897 10 NaN NaN NaN NaN NaN NaN 15.077 2.532 1897 11 NaN NaN NaN NaN NaN NaN 6.174 0.257 1897 12 NaN NaN NaN NaN NaN NaN 0.277 0.008 1898 1 NaN NaN NaN NaN NaN NaN -0.117 2.394 1898 2 NaN NaN NaN NaN NaN NaN -0.577 0.028