% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 36933 % Primary Name: MOLINE BRG % Record Type: TAVG % Country: United States % State: IL % Latitude: 41.47030 +/- 0.00005 % Longitude: -90.51140 +/- 0.00005 % Elevation (m): 167.64 +/- 0.15 % # of Months: 13 % % Alternate Names: Missing Station ID - 115748 % % IDs: coop - 115748 % ghcnd - USC00115748 % ncdc - 20005882 % nws - MLII2 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 7b58b02f989e6d6800e940342cca4ea3 % Raw Data Hash: e80b348b285cca873995aecea22c0b1a % Adj Data Hash: 83f7076ca945e60d0c88af0a8f1f66f0 % % 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 1954 6 NaN NaN NaN NaN NaN NaN 23.975 2.237 1954 7 NaN NaN NaN NaN NaN NaN 24.874 1.131 1954 8 NaN NaN NaN NaN NaN NaN 22.513 -0.124 1954 9 NaN NaN NaN NaN NaN NaN 20.505 1.840 1954 10 NaN NaN NaN NaN NaN NaN 12.847 0.690 1954 11 NaN NaN NaN NaN NaN NaN 5.469 1.040 1954 12 NaN NaN NaN NaN NaN NaN -0.937 1.409 1955 1 NaN NaN NaN NaN NaN NaN -5.114 0.712 1955 2 NaN NaN NaN NaN NaN NaN -2.856 0.046 1955 3 NaN NaN NaN NaN NaN NaN 2.694 -0.161 1955 4 NaN NaN NaN NaN NaN NaN 14.469 3.994 1955 5 NaN NaN NaN NaN NaN NaN 17.532 0.974 1955 6 19.747 -1.311 0 0 19.747 -1.311 19.862 -1.876 1955 7 27.037 3.973 0 0 27.037 3.973 26.534 2.791 1955 8 24.750 2.793 0 0 24.750 2.793 24.709 2.073 1955 9 18.885 0.900 0 0 18.885 0.900 19.603 0.939 1955 10 11.652 0.174 0 0 11.652 0.174 12.905 0.748 1955 11 1.143 -2.607 0 0 1.143 -2.607 2.169 -2.260 1955 12 -4.357 -1.331 0 0 -4.357 -1.331 -3.698 -1.351 1956 1 -5.368 1.138 0 0 -5.368 1.138 -4.542 1.284 1956 2 -3.121 0.461 0 0 -3.121 0.461 -2.076 0.826 1956 3 1.836 -0.338 0 0 1.836 -0.338 2.965 0.111 1956 4 8.058 -1.737 0 0 8.058 -1.737 9.601 -0.874 1956 5 16.900 1.022 0 0 16.900 1.022 17.285 0.727 1956 6 16.758 -4.300 1 0 NaN NaN 23.097 1.359 1956 7 NaN NaN NaN NaN NaN NaN 22.734 -1.009 1956 8 NaN NaN NaN NaN NaN NaN 22.862 0.225 1956 9 NaN NaN NaN NaN NaN NaN 18.525 -0.140 1956 10 NaN NaN NaN NaN NaN NaN 16.038 3.881 1956 11 NaN NaN NaN NaN NaN NaN 4.646 0.216 1956 12 NaN NaN NaN NaN NaN NaN -0.211 2.135 1957 1 NaN NaN NaN NaN NaN NaN -8.376 -2.550 1957 2 NaN NaN NaN NaN NaN NaN 0.509 3.411 1957 3 NaN NaN NaN NaN NaN NaN 2.956 0.101 1957 4 NaN NaN NaN NaN NaN NaN 10.706 0.231 1957 5 NaN NaN NaN NaN NaN NaN 15.933 -0.625 1957 6 NaN NaN NaN NaN NaN NaN 21.797 0.060