% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 37578 % Primary Name: RAWSONVILLE % Record Type: TAVG % Country: United States % State: MI % Latitude: 42.00000 +/- 0.00833 % Longitude: -83.50000 +/- 0.00833 % Elevation (m): 152.40 +/- 0.15 % # of Months: 20 % % Alternate Names: Missing Station ID - 206851 % % IDs: coop - 206851 % ghcnd - USC00206851 % ncdc - 30015165 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: f41dc2b348c58f0fdac0fdc4c669b8f9 % Raw Data Hash: bba25e6192603840ce6380a47f51bd91 % Adj Data Hash: bba25e6192603840ce6380a47f51bd91 % % 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 1892 1 NaN NaN NaN NaN NaN NaN -7.505 -2.111 1892 2 NaN NaN NaN NaN NaN NaN -2.776 1.414 1892 3 NaN NaN NaN NaN NaN NaN -1.212 -2.187 1892 4 NaN NaN NaN NaN NaN NaN 6.856 -0.949 1892 5 NaN NaN NaN NaN NaN NaN 12.420 -1.679 1892 6 NaN NaN NaN NaN NaN NaN 20.628 0.933 1892 7 NaN NaN NaN NaN NaN NaN 21.783 -0.422 1892 8 NaN NaN NaN NaN NaN NaN 20.981 -0.312 1892 9 NaN NaN NaN NaN NaN NaN 16.917 -0.352 1892 10 NaN NaN NaN NaN NaN NaN 10.149 -0.663 1892 11 NaN NaN NaN NaN NaN NaN 2.017 -2.048 1892 12 NaN NaN NaN NaN NaN NaN -4.063 -1.628 1893 1 -8.103 -3.529 0 0 -8.103 -3.529 -10.494 -5.101 1893 2 -5.682 -2.312 0 0 -5.682 -2.312 -6.794 -2.604 1893 3 0.852 -0.942 0 0 0.852 -0.942 -0.160 -1.134 1893 4 NaN NaN NaN NaN NaN NaN 6.621 -1.184 1893 5 13.352 -1.566 0 0 13.352 -1.566 12.123 -1.976 1893 6 21.241 0.727 0 0 21.241 0.727 20.620 0.925 1893 7 22.706 -0.318 0 0 22.706 -0.318 22.099 -0.106 1893 8 20.627 -1.486 0 0 20.627 -1.486 20.301 -0.993 1893 9 17.050 -1.038 0 0 17.050 -1.038 16.370 -0.898 1893 10 11.427 -0.204 0 0 11.427 -0.204 11.001 0.190 1893 11 NaN NaN NaN NaN NaN NaN 3.334 -0.732 1893 12 NaN NaN NaN NaN NaN NaN -3.334 -0.900 1894 1 -0.789 3.786 0 0 -0.789 3.786 -2.345 3.049 1894 2 -4.521 -1.151 0 0 -4.521 -1.151 -5.618 -1.429 1894 3 5.204 3.410 0 0 5.204 3.410 4.405 3.430 1894 4 9.296 0.672 0 0 9.296 0.672 8.374 0.568 1894 5 14.427 -0.492 0 0 14.427 -0.492 12.949 -1.150 1894 6 NaN NaN NaN NaN NaN NaN 20.984 1.290 1894 7 23.389 0.364 0 0 23.389 0.364 22.647 0.442 1894 8 20.806 -1.307 0 0 20.806 -1.307 20.094 -1.199 1894 9 18.796 0.709 0 0 18.796 0.709 18.540 1.272 1894 10 10.944 -0.686 0 0 10.944 -0.686 10.805 -0.007 1894 11 1.556 -3.330 0 0 1.556 -3.330 1.511 -2.555 1894 12 -0.427 1.188 0 0 -0.427 1.188 -0.666 1.768 1895 1 NaN NaN NaN NaN NaN NaN -7.732 -2.339 1895 2 NaN NaN NaN NaN NaN NaN -9.061 -4.871 1895 3 NaN NaN NaN NaN NaN NaN -2.714 -3.688 1895 4 NaN NaN NaN NaN NaN NaN 8.737 0.932 1895 5 NaN NaN NaN NaN NaN NaN 14.758 0.659 1895 6 NaN NaN NaN NaN NaN NaN 21.374 1.679 1895 7 NaN NaN NaN NaN NaN NaN 20.853 -1.352 1895 8 NaN NaN NaN NaN NaN NaN 21.255 -0.039 1895 9 NaN NaN NaN NaN NaN NaN 18.832 1.563 1895 10 NaN NaN NaN NaN NaN NaN 7.317 -3.495 1895 11 NaN NaN NaN NaN NaN NaN 2.904 -1.162 1895 12 NaN NaN NaN NaN NaN NaN -2.395 0.040