% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 37610 % Primary Name: NORTH SOMERS % Record Type: TAVG % Country: United States % State: CT % Latitude: 42.03330 +/- 0.00005 % Longitude: -72.43330 +/- 0.00005 % Elevation (m): 85.30 +/- 0.05 % # of Months: 16 % % IDs: coop - 65757 % ghcnd - USC00065757 % ncdc - 20004152 % nws - SOMC3 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: da243fc6ed43d56f58c4d6c4512643ec % Raw Data Hash: c33e63d74d49d4b6eb494466b103caa0 % Adj Data Hash: a18cb46a09d4bd3bb462c25da0b15d32 % % 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 1991 5 NaN NaN NaN NaN NaN NaN 15.998 2.765 1991 6 NaN NaN NaN NaN NaN NaN 18.851 0.556 1991 7 NaN NaN NaN NaN NaN NaN 20.864 -0.123 1991 8 NaN NaN NaN NaN NaN NaN 20.821 0.992 1991 9 NaN NaN NaN NaN NaN NaN 14.605 -0.827 1991 10 NaN NaN NaN NaN NaN NaN 10.466 1.069 1991 11 NaN NaN NaN NaN NaN NaN 4.822 1.153 1991 12 NaN NaN NaN NaN NaN NaN -2.464 0.875 1992 1 NaN NaN NaN NaN NaN NaN -4.480 1.265 1992 2 NaN NaN NaN NaN NaN NaN -3.539 1.128 1992 3 NaN NaN NaN NaN NaN NaN -0.581 -1.164 1992 4 NaN NaN NaN NaN NaN NaN 6.003 -1.003 1992 5 13.944 0.174 0 0 13.944 0.174 12.859 -0.374 1992 6 18.056 -0.776 0 0 18.056 -0.776 17.508 -0.787 1992 7 19.444 -2.080 0 0 19.444 -2.080 19.096 -1.892 1992 8 19.333 -1.033 0 0 19.333 -1.033 18.902 -0.927 1992 9 15.167 -0.802 0 0 15.167 -0.802 15.224 -0.208 1992 10 7.167 -2.768 0 0 7.167 -2.768 7.453 -1.944 1992 11 3.444 -0.761 0 0 3.444 -0.761 3.183 -0.486 1992 12 -2.222 0.580 0 0 -2.222 0.580 -2.938 0.401 1993 1 -2.556 2.652 0 0 -2.556 2.652 -3.731 2.014 1993 2 -6.778 -2.648 0 0 -6.778 -2.648 -8.040 -3.373 1993 3 -0.611 -1.731 0 0 -0.611 -1.731 -0.750 -1.333 1993 4 NaN NaN NaN NaN NaN NaN 7.581 0.576 1993 5 15.722 1.952 0 0 15.722 1.952 14.205 0.972 1993 6 NaN NaN NaN NaN NaN NaN 18.014 -0.281 1993 7 22.111 0.587 0 0 22.111 0.587 21.431 0.444 1993 8 NaN NaN NaN NaN NaN NaN 20.809 0.980 1993 9 16.056 0.087 0 0 16.056 0.087 15.240 -0.192 1993 10 NaN NaN NaN NaN NaN NaN 7.973 -1.425 1993 11 NaN NaN NaN NaN NaN NaN 4.170 0.501 1993 12 NaN NaN NaN NaN NaN NaN -3.037 0.302 1994 1 -10.167 -4.959 0 0 -10.167 -4.959 -10.163 -4.418 1994 2 NaN NaN NaN NaN NaN NaN -7.270 -2.603 1994 3 0.389 -0.731 0 0 0.389 -0.731 0.428 -0.155 1994 4 NaN NaN NaN NaN NaN NaN 8.181 1.175 1994 5 NaN NaN NaN NaN NaN NaN 12.445 -0.788 1994 6 NaN NaN NaN NaN NaN NaN 19.750 1.455 1994 7 NaN NaN NaN NaN NaN NaN 22.961 1.973 1994 8 NaN NaN NaN NaN NaN NaN 19.225 -0.604 1994 9 NaN NaN NaN NaN NaN NaN 14.772 -0.659 1994 10 NaN NaN NaN NaN NaN NaN 9.391 -0.007 1994 11 NaN NaN NaN NaN NaN NaN 6.428 2.759 1994 12 NaN NaN NaN NaN NaN NaN -0.896 2.443 1995 1 NaN NaN NaN NaN NaN NaN -1.836 3.908 1995 2 NaN NaN NaN NaN NaN NaN -5.749 -1.082 1995 3 NaN NaN NaN NaN NaN NaN 2.510 1.927