% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 37014 % Primary Name: MIDDLETOWN WB % Record Type: TAVG % Country: United States % State: CT % Latitude: 41.55000 +/- 0.00500 % Longitude: -72.55000 +/- 0.00500 % Elevation (m): 41.10 +/- 0.05 % # of Months: 26 % % IDs: coop - 64757 % ghcnd - USC00064757 % ncdc - 20004064 % wban - 4744 % % Sources: US First Order Summary of the Day % US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: a704220f21df159929375ef0f3f807c0 % Raw Data Hash: 770a7cb9933cc507dbf5fa6c224dcf63 % Adj Data Hash: 770a7cb9933cc507dbf5fa6c224dcf63 % % 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 1955 4 NaN NaN NaN NaN NaN NaN 9.281 1.077 1955 5 NaN NaN NaN NaN NaN NaN 14.723 1.247 1955 6 NaN NaN NaN NaN NaN NaN 17.544 -0.985 1955 7 NaN NaN NaN NaN NaN NaN 23.876 2.080 1955 8 NaN NaN NaN NaN NaN NaN 23.159 1.614 1955 9 NaN NaN NaN NaN NaN NaN 17.911 -0.223 1955 10 NaN NaN NaN NaN NaN NaN 13.756 1.061 1955 11 NaN NaN NaN NaN NaN NaN 7.195 -0.475 1955 12 NaN NaN NaN NaN NaN NaN -2.086 -3.835 1956 1 NaN NaN NaN NaN NaN NaN -0.234 0.482 1956 2 NaN NaN NaN NaN NaN NaN 1.168 1.563 1956 3 NaN NaN NaN NaN NaN NaN 1.363 -1.908 1956 4 6.167 -1.186 0 0 6.167 -1.186 6.508 -1.696 1956 5 12.167 -0.458 0 0 12.167 -0.458 11.511 -1.965 1956 6 19.833 2.155 0 0 19.833 2.155 18.778 0.249 1956 7 20.667 -0.279 0 0 20.667 -0.279 20.421 -1.375 1956 8 21.167 0.473 0 0 21.167 0.473 21.206 -0.339 1956 9 15.722 -1.561 0 0 15.722 -1.561 16.683 -1.451 1956 10 11.222 -0.622 0 0 11.222 -0.622 12.878 0.183 1956 11 5.444 -1.374 0 0 5.444 -1.374 8.438 0.769 1956 12 1.500 0.602 0 0 1.500 0.602 3.819 2.071 1957 1 -6.556 -4.989 0 0 -6.556 -4.989 -3.001 -2.285 1957 2 0.222 1.468 0 0 0.222 1.468 1.677 2.072 1957 3 3.278 0.857 0 0 3.278 0.857 4.085 0.813 1957 4 9.500 2.147 0 0 9.500 2.147 9.439 1.236 1957 5 14.611 1.986 0 0 14.611 1.986 13.929 0.454 1957 6 21.611 3.933 0 0 21.611 3.933 20.196 1.667 1957 7 22.167 1.221 0 0 22.167 1.221 21.740 -0.056 1957 8 19.889 -0.805 0 0 19.889 -0.805 20.197 -1.347 1957 9 17.722 0.439 0 0 17.722 0.439 18.749 0.615 1957 10 11.000 -0.844 0 0 11.000 -0.844 12.233 -0.462 1957 11 6.722 -0.096 0 0 6.722 -0.096 9.523 1.853 1957 12 2.111 1.213 0 0 2.111 1.213 4.277 2.528 1958 1 -2.722 -1.156 0 0 -2.722 -1.156 -0.174 0.542 1958 2 -5.167 -3.921 0 0 -5.167 -3.921 -3.252 -2.857 1958 3 2.778 0.357 0 0 2.778 0.357 3.564 0.293 1958 4 8.833 1.480 0 0 8.833 1.480 8.941 0.737 1958 5 12.333 -0.292 0 0 12.333 -0.292 11.976 -1.500 1958 6 NaN NaN NaN NaN NaN NaN 16.165 -2.364 1958 7 NaN NaN NaN NaN NaN NaN 21.788 -0.008 1958 8 NaN NaN NaN NaN NaN NaN 21.258 -0.287 1958 9 NaN NaN NaN NaN NaN NaN 17.739 -0.395 1958 10 NaN NaN NaN NaN NaN NaN 11.870 -0.825 1958 11 NaN NaN NaN NaN NaN NaN 9.016 1.346 1958 12 NaN NaN NaN NaN NaN NaN -2.378 -4.127 1959 1 NaN NaN NaN NaN NaN NaN -0.804 -0.089 1959 2 NaN NaN NaN NaN NaN NaN -1.579 -1.184 1959 3 NaN NaN NaN NaN NaN NaN 2.953 -0.318 1959 4 NaN NaN NaN NaN NaN NaN 9.254 1.051 1959 5 NaN NaN NaN NaN NaN NaN 15.002 1.527