% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39886 % Primary Name: WEST CONCORD % Record Type: TAVG % Country: United States % State: MN % Latitude: 44.13330 +/- 0.00005 % Longitude: -92.91670 +/- 0.00005 % Elevation (m): 375.51 +/- 0.15 % # of Months: 32 % % Alternate Names: Missing Station ID - 218822 % % IDs: coop - 218822 % ghcnd - USC00218822 % ncdc - 30002946 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: cc1705e1708609269d3ed7c45205ff0e % Raw Data Hash: d78adef877f5d65935eab83ff2d284d5 % Adj Data Hash: 9ceaad83705cf0ee7b4ab56c0158151e % % 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 1907 10 NaN NaN NaN NaN NaN NaN 9.141 -0.525 1907 11 NaN NaN NaN NaN NaN NaN 1.032 0.468 1907 12 NaN NaN NaN NaN NaN NaN -4.603 2.806 1908 1 NaN NaN NaN NaN NaN NaN -8.060 3.628 1908 2 NaN NaN NaN NaN NaN NaN -6.429 1.641 1908 3 NaN NaN NaN NaN NaN NaN -1.521 0.281 1908 4 NaN NaN NaN NaN NaN NaN 8.175 0.796 1908 5 NaN NaN NaN NaN NaN NaN 13.247 -1.385 1908 6 NaN NaN NaN NaN NaN NaN 17.794 -2.157 1908 7 NaN NaN NaN NaN NaN NaN 21.678 -0.667 1908 8 NaN NaN NaN NaN NaN NaN 19.605 -1.460 1908 9 NaN NaN NaN NaN NaN NaN 18.826 2.954 1908 10 5.188 -4.647 1 0 NaN NaN 9.758 0.092 1908 11 2.118 1.385 0 0 2.118 1.385 2.031 1.467 1908 12 -6.055 1.185 1 0 NaN NaN -6.465 0.944 1909 1 -9.055 2.464 0 0 -9.055 2.464 -10.805 0.883 1909 2 -7.532 0.370 0 0 -7.532 0.370 -8.016 0.055 1909 3 -2.900 -1.267 0 0 -2.900 -1.267 -3.082 -1.279 1909 4 3.547 -4.000 0 0 3.547 -4.000 3.554 -3.825 1909 5 12.705 -2.095 0 0 12.705 -2.095 12.777 -1.854 1909 6 18.538 -1.582 1 0 NaN NaN 19.004 -0.946 1909 7 20.929 -1.585 1 0 NaN NaN 21.422 -0.923 1909 8 22.674 1.440 0 0 22.674 1.440 23.071 2.006 1909 9 15.033 -1.008 0 0 15.033 -1.008 15.036 -0.836 1909 10 8.244 -1.591 0 0 8.244 -1.591 8.732 -0.933 1909 11 2.628 1.895 0 0 2.628 1.895 2.524 1.960 1909 12 -11.379 -4.140 0 0 -11.379 -4.140 -11.569 -4.160 1910 1 -10.838 0.680 0 0 -10.838 0.680 -11.815 -0.127 1910 2 -12.052 -4.150 0 0 -12.052 -4.150 -11.858 -3.787 1910 3 6.321 7.954 0 0 6.321 7.954 6.002 7.804 1910 4 10.048 2.500 0 0 10.048 2.500 10.362 2.984 1910 5 11.371 -3.429 0 0 11.371 -3.429 11.897 -2.734 1910 6 20.278 0.159 0 0 20.278 0.159 20.384 0.433 1910 7 NaN NaN NaN NaN NaN NaN 22.520 0.175 1910 8 20.735 -0.499 0 0 20.735 -0.499 20.318 -0.747 1910 9 16.948 0.907 0 0 16.948 0.907 15.660 -0.212 1910 10 11.734 1.899 0 0 11.734 1.899 12.351 2.685 1910 11 -2.613 -3.346 0 0 -2.613 -3.346 -1.959 -2.522 1910 12 -7.674 -0.435 0 0 -7.674 -0.435 -7.652 -0.244 1911 1 -10.235 1.284 1 0 NaN NaN -13.281 -1.594 1911 2 -4.664 3.237 0 0 -4.664 3.237 -5.911 2.160 1911 3 2.800 4.433 0 0 2.800 4.433 1.434 3.236 1911 4 6.760 -0.787 0 0 6.760 -0.787 6.756 -0.623 1911 5 17.052 2.251 0 0 17.052 2.251 17.131 2.499 1911 6 NaN NaN NaN NaN NaN NaN 22.638 2.688 1911 7 NaN NaN NaN NaN NaN NaN 21.884 -0.460 1911 8 NaN NaN NaN NaN NaN NaN 19.209 -1.856 1911 9 NaN NaN NaN NaN NaN NaN 15.350 -0.522 1911 10 7.400 -2.435 0 0 7.400 -2.435 7.771 -1.895 1911 11 NaN NaN NaN NaN NaN NaN -4.649 -5.213 1911 12 NaN NaN NaN NaN NaN NaN -5.084 2.324 1912 1 NaN NaN NaN NaN NaN NaN -20.435 -8.747 1912 2 NaN NaN NaN NaN NaN NaN -9.890 -1.819 1912 3 NaN NaN NaN NaN NaN NaN -5.799 -3.997 1912 4 NaN NaN NaN NaN NaN NaN 8.682 1.304 1912 5 NaN NaN NaN NaN NaN NaN 14.457 -0.174 1912 6 NaN NaN NaN NaN NaN NaN 17.608 -2.343 1912 7 NaN NaN NaN NaN NaN NaN 21.507 -0.838 1912 8 NaN NaN NaN NaN NaN NaN 19.522 -1.543 1912 9 NaN NaN NaN NaN NaN NaN 15.050 -0.822 1912 10 NaN NaN NaN NaN NaN NaN 10.576 0.911