% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 41973 % Primary Name: GREENLAND 6N % Record Type: TAVG % Country: United States % State: MI % Latitude: 46.87360 +/- 0.00005 % Longitude: -89.10060 +/- 0.00005 % Elevation (m): 241.10 +/- 0.15 % # of Months: 38 % % Alternate Names: Missing Station ID - 203421 % % IDs: coop - 203421 % ghcnd - USC00203421 % ncdc - 30015047 % nws - GNLM4 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 316003de7913d489fcb6b999a770df46 % Raw Data Hash: 269d88880c43202b92c86a766ad87213 % Adj Data Hash: 5fa1fa6df3635d7889ba27ca5fb56b8d % % 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 2009 10 NaN NaN NaN NaN NaN NaN 6.401 -1.598 2009 11 NaN NaN NaN NaN NaN NaN 6.219 4.550 2009 12 NaN NaN NaN NaN NaN NaN -5.564 -0.748 2010 1 NaN NaN NaN NaN NaN NaN -6.202 2.501 2010 2 NaN NaN NaN NaN NaN NaN -5.403 2.395 2010 3 NaN NaN NaN NaN NaN NaN 2.640 5.868 2010 4 NaN NaN NaN NaN NaN NaN 7.353 4.173 2010 5 NaN NaN NaN NaN NaN NaN 11.206 2.835 2010 6 NaN NaN NaN NaN NaN NaN 13.231 0.346 2010 7 NaN NaN NaN NaN NaN NaN 19.148 2.402 2010 8 NaN NaN NaN NaN NaN NaN 19.434 2.725 2010 9 NaN NaN NaN NaN NaN NaN 11.101 -1.325 2010 10 8.056 0.060 0 0 8.056 0.060 10.037 2.038 2010 11 1.556 -0.111 0 0 1.556 -0.111 3.515 1.846 2010 12 -5.389 -0.570 0 0 -5.389 -0.570 -4.759 0.057 2011 1 -8.167 0.540 0 0 -8.167 0.540 -9.245 -0.541 2011 2 -6.111 1.690 0 0 -6.111 1.690 -6.451 1.346 2011 3 -3.056 0.176 0 0 -3.056 0.176 -2.984 0.245 2011 4 3.667 0.491 0 0 3.667 0.491 3.471 0.292 2011 5 9.944 1.576 0 0 9.944 1.576 8.372 0.001 2011 6 14.889 2.007 0 0 14.889 2.007 12.380 -0.505 2011 7 20.111 3.368 0 0 20.111 3.368 18.882 2.135 2011 8 18.056 1.350 0 0 18.056 1.350 18.660 1.952 2011 9 13.167 0.744 0 0 13.167 0.744 13.177 0.751 2011 10 9.444 1.449 0 0 9.444 1.449 10.589 2.590 2011 11 2.111 0.445 0 0 2.111 0.445 3.967 2.298 2011 12 -2.839 1.980 0 0 -2.839 1.980 -2.164 2.652 2012 1 -5.423 3.284 0 0 -5.423 3.284 -4.797 3.907 2012 2 -3.602 4.199 0 0 -3.602 4.199 -2.478 5.319 2012 3 5.658 8.890 0 0 5.658 8.890 4.623 7.851 2012 4 5.062 1.886 0 0 5.062 1.886 4.536 1.357 2012 5 12.762 4.394 0 0 12.762 4.394 11.131 2.759 2012 6 17.193 4.311 0 0 17.193 4.311 15.308 2.423 2012 7 20.129 3.386 0 0 20.129 3.386 19.892 3.146 2012 8 16.902 0.196 0 0 16.902 0.196 18.125 1.416 2012 9 11.660 -0.763 0 0 11.660 -0.763 12.425 -0.000 2012 10 6.400 -1.596 0 0 6.400 -1.596 7.880 -0.119 2012 11 1.225 -0.441 0 0 1.225 -0.441 2.711 1.041 2012 12 -2.884 1.935 0 0 -2.884 1.935 -2.136 2.679 2013 1 -6.215 2.492 0 0 -6.215 2.492 -6.562 2.141 2013 2 -7.289 0.511 0 0 -7.289 0.511 -7.466 0.332 2013 3 -4.310 -1.078 0 0 -4.310 -1.078 -4.180 -0.952 2013 4 1.207 -1.969 0 0 1.207 -1.969 1.111 -2.068 2013 5 9.829 1.461 0 0 9.829 1.461 7.339 -1.033 2013 6 14.692 1.810 0 0 14.692 1.810 12.693 -0.192 2013 7 17.565 0.821 0 0 17.565 0.821 16.648 -0.098 2013 8 17.250 0.545 0 0 17.250 0.545 17.677 0.969 2013 9 13.673 1.251 0 0 13.673 1.251 13.493 1.067 2013 10 7.392 -0.604 0 0 7.392 -0.604 9.010 1.011 2013 11 4.450 2.784 1 0 NaN NaN NaN NaN