% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39602 % Primary Name: MARLBOROUGH % Record Type: TAVG % Country: United States % State: MI % Latitude: 43.86470 +/- 0.00005 % Longitude: -85.84170 +/- 0.00005 % Elevation (m): 252.98 +/- 0.15 % # of Months: 11 % % Alternate Names: Missing Station ID - 205165 % % IDs: coop - 205165 % ghcnd - USC00205165 % ncdc - 30015145 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: ff6e3a4684304e75da4a25888a536a9d % Raw Data Hash: da876f8fcc0ee2e25512828da16085f5 % Adj Data Hash: da7afbe5225b54615c1c8f0199b1322b % % 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 1905 6 NaN NaN NaN NaN NaN NaN 17.232 -0.654 1905 7 NaN NaN NaN NaN NaN NaN 19.353 -0.771 1905 8 NaN NaN NaN NaN NaN NaN 18.857 -0.174 1905 9 NaN NaN NaN NaN NaN NaN 15.731 1.001 1905 10 NaN NaN NaN NaN NaN NaN 8.840 0.014 1905 11 NaN NaN NaN NaN NaN NaN 1.034 -1.005 1905 12 NaN NaN NaN NaN NaN NaN -3.209 1.415 1906 1 NaN NaN NaN NaN NaN NaN -3.255 4.452 1906 2 NaN NaN NaN NaN NaN NaN -7.789 -0.787 1906 3 NaN NaN NaN NaN NaN NaN -5.113 -3.344 1906 4 NaN NaN NaN NaN NaN NaN 7.576 1.581 1906 5 NaN NaN NaN NaN NaN NaN 12.037 -0.630 1906 6 21.114 2.383 1 0 NaN NaN 17.945 0.059 1906 7 20.370 -0.600 0 0 20.370 -0.600 19.424 -0.700 1906 8 21.682 1.805 0 0 21.682 1.805 20.600 1.569 1906 9 NaN NaN NaN NaN NaN NaN 17.600 2.870 1906 10 8.387 -1.284 0 0 8.387 -1.284 8.460 -0.365 1906 11 2.862 -0.023 0 0 2.862 -0.023 2.015 -0.024 1906 12 -4.121 -0.343 1 0 NaN NaN -5.705 -1.081 1907 1 -6.417 0.444 1 0 NaN NaN -7.856 -0.150 1907 2 -11.388 -5.230 1 0 NaN NaN -9.078 -2.076 1907 3 0.742 1.665 0 0 0.742 1.665 0.106 1.875 1907 4 2.267 -4.574 0 0 2.267 -4.574 1.503 -4.491 1907 5 NaN NaN NaN NaN NaN NaN 8.117 -4.550 1907 6 NaN NaN NaN NaN NaN NaN 17.353 -0.532 1907 7 21.069 0.100 0 0 21.069 0.100 19.352 -0.772 1907 8 NaN NaN NaN NaN NaN NaN 17.445 -1.586 1907 9 NaN NaN NaN NaN NaN NaN 14.179 -0.551 1907 10 NaN NaN NaN NaN NaN NaN 6.622 -2.204 1907 11 NaN NaN NaN NaN NaN NaN 1.117 -0.921 1907 12 NaN NaN NaN NaN NaN NaN -4.440 0.183 1908 1 NaN NaN NaN NaN NaN NaN -6.814 0.892 1908 2 NaN NaN NaN NaN NaN NaN -8.868 -1.866 1908 3 NaN NaN NaN NaN NaN NaN -1.784 -0.015 1908 4 NaN NaN NaN NaN NaN NaN 6.053 0.058 1908 5 NaN NaN NaN NaN NaN NaN 12.885 0.218 1908 6 NaN NaN NaN NaN NaN NaN 18.136 0.250 1908 7 NaN NaN NaN NaN NaN NaN 20.403 0.279