% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 37977 % Primary Name: DEARBORN HEIGHTS FD % Record Type: TAVG % Country: United States % State: MI % Latitude: 42.32500 +/- 0.00005 % Longitude: -83.29360 +/- 0.00005 % Elevation (m): 190.20 +/- 0.15 % # of Months: 8 % % Alternate Names: Missing Station ID - 202017 % % IDs: coop - 202017 % ghcnd - USC00202017 % ncdc - 30001101 % nws - DHTM4 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: e1467d091f37f6c1e472745b49585140 % Raw Data Hash: bcbf956c21557b4bed21e5104236aa27 % Adj Data Hash: 433314c07b6b9eb8b5239667e8348afd % % 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 2000 4 NaN NaN NaN NaN NaN NaN 8.065 0.259 2000 5 NaN NaN NaN NaN NaN NaN 15.749 1.650 2000 6 NaN NaN NaN NaN NaN NaN 20.431 0.736 2000 7 NaN NaN NaN NaN NaN NaN 20.606 -1.599 2000 8 NaN NaN NaN NaN NaN NaN 20.909 -0.385 2000 9 NaN NaN NaN NaN NaN NaN 16.992 -0.276 2000 10 NaN NaN NaN NaN NaN NaN 12.639 1.827 2000 11 NaN NaN NaN NaN NaN NaN 4.707 0.642 2000 12 NaN NaN NaN NaN NaN NaN -7.566 -5.131 2001 1 NaN NaN NaN NaN NaN NaN -4.120 1.273 2001 2 NaN NaN NaN NaN NaN NaN -2.295 1.895 2001 3 NaN NaN NaN NaN NaN NaN 0.841 -0.133 2001 4 8.056 0.692 0 0 8.056 0.692 9.736 1.931 2001 5 15.611 1.954 0 0 15.611 1.954 15.513 1.414 2001 6 19.722 0.470 0 0 19.722 0.470 20.277 0.583 2001 7 NaN NaN NaN NaN NaN NaN 22.376 0.171 2001 8 22.001 1.149 1 0 NaN NaN 22.828 1.534 2001 9 15.667 -1.160 0 0 15.667 -1.160 16.600 -0.668 2001 10 11.500 1.131 0 0 11.500 1.131 11.318 0.506 2001 11 8.000 4.376 0 0 8.000 4.376 8.869 4.803 2001 12 2.333 5.210 0 0 2.333 5.210 1.670 4.104 2002 1 NaN NaN NaN NaN NaN NaN -0.695 4.699 2002 2 NaN NaN NaN NaN NaN NaN -0.610 3.579 2002 3 NaN NaN NaN NaN NaN NaN 1.190 0.215 2002 4 NaN NaN NaN NaN NaN NaN 9.255 1.450 2002 5 NaN NaN NaN NaN NaN NaN 11.847 -2.252 2002 6 NaN NaN NaN NaN NaN NaN 20.947 1.252 2002 7 NaN NaN NaN NaN NaN NaN 24.172 1.967 2002 8 NaN NaN NaN NaN NaN NaN 22.386 1.092 2002 9 NaN NaN NaN NaN NaN NaN 20.239 2.971 2002 10 NaN NaN NaN NaN NaN NaN 10.069 -0.742 2002 11 NaN NaN NaN NaN NaN NaN 4.039 -0.027 2002 12 NaN NaN NaN NaN NaN NaN -2.454 -0.020