% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 38760 % Primary Name: UTICA 7 SSW % Record Type: TAVG % Country: United States % State: NY % Latitude: 43.00000 +/- 0.00005 % Longitude: -75.26670 +/- 0.00005 % Elevation (m): 318.80 +/- 0.05 % # of Months: 28 % % IDs: coop - 308742 % ghcnd - USC00308742 % ncdc - 20020230 % nws - UTCN6 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: c71b5ee6f150c1758ee6f399a925be53 % Raw Data Hash: df052c2dbbdf768a0a657606e93a53c9 % Adj Data Hash: 4ab1e371cded5ce34f5d57ed0f1b5280 % % 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 2 NaN NaN NaN NaN NaN NaN -1.991 3.207 1991 3 NaN NaN NaN NaN NaN NaN 2.559 2.345 1991 4 NaN NaN NaN NaN NaN NaN 9.844 2.670 1991 5 NaN NaN NaN NaN NaN NaN 16.309 2.849 1991 6 NaN NaN NaN NaN NaN NaN 19.683 1.166 1991 7 NaN NaN NaN NaN NaN NaN 21.251 0.163 1991 8 NaN NaN NaN NaN NaN NaN 21.110 1.143 1991 9 NaN NaN NaN NaN NaN NaN 14.960 -0.688 1991 10 NaN NaN NaN NaN NaN NaN 10.654 1.213 1991 11 NaN NaN NaN NaN NaN NaN 4.605 1.056 1991 12 NaN NaN NaN NaN NaN NaN -2.216 1.220 1992 1 NaN NaN NaN NaN NaN NaN -4.899 1.400 1992 2 -4.111 1.552 0 0 -4.111 1.552 -3.818 1.380 1992 3 -2.278 -2.025 0 0 -2.278 -2.025 -1.269 -1.483 1992 4 5.889 -0.820 0 0 5.889 -0.820 6.327 -0.848 1992 5 13.222 0.228 0 0 13.222 0.228 13.307 -0.154 1992 6 16.778 -1.274 0 0 16.778 -1.274 17.287 -1.231 1992 7 18.278 -2.345 0 0 18.278 -2.345 19.451 -1.637 1992 8 18.222 -1.279 0 0 18.222 -1.279 18.745 -1.222 1992 9 15.389 0.206 0 0 15.389 0.206 15.621 -0.027 1992 10 6.833 -2.142 0 0 6.833 -2.142 7.334 -2.106 1992 11 2.889 -0.195 0 0 2.889 -0.195 3.575 0.026 1992 12 -1.889 2.013 0 0 -1.889 2.013 -2.935 0.501 1993 1 -4.111 2.654 0 0 -4.111 2.654 -3.887 2.413 1993 2 -8.944 -3.281 0 0 -8.944 -3.281 -8.810 -3.612 1993 3 -1.667 -1.414 0 0 -1.667 -1.414 -1.285 -1.498 1993 4 7.556 0.846 0 0 7.556 0.846 8.014 0.840 1993 5 13.222 0.228 0 0 13.222 0.228 14.135 0.675 1993 6 17.389 -0.663 0 0 17.389 -0.663 17.822 -0.696 1993 7 20.444 -0.178 0 0 20.444 -0.178 21.931 0.843 1993 8 20.222 0.721 0 0 20.222 0.721 20.960 0.993 1993 9 14.556 -0.627 0 0 14.556 -0.627 15.266 -0.382 1993 10 8.333 -0.642 0 0 8.333 -0.642 8.377 -1.063 1993 11 2.778 -0.306 0 0 2.778 -0.306 3.864 0.315 1993 12 -4.167 -0.265 0 0 -4.167 -0.265 -3.842 -0.406 1994 1 -11.333 -4.568 0 0 -11.333 -4.568 -11.328 -5.029 1994 2 -7.944 -2.281 0 0 -7.944 -2.281 -8.210 -3.012 1994 3 -1.389 -1.137 0 0 -1.389 -1.137 -0.484 -0.698 1994 4 8.278 1.569 0 0 8.278 1.569 8.386 1.212 1994 5 11.667 -1.328 0 0 11.667 -1.328 12.612 -0.848 1994 6 NaN NaN NaN NaN NaN NaN 19.712 1.195 1994 7 NaN NaN NaN NaN NaN NaN 22.578 1.490 1994 8 NaN NaN NaN NaN NaN NaN 19.079 -0.888 1994 9 NaN NaN NaN NaN NaN NaN 15.406 -0.242 1994 10 NaN NaN NaN NaN NaN NaN 9.314 -0.126 1994 11 NaN NaN NaN NaN NaN NaN 6.480 2.930 1994 12 NaN NaN NaN NaN NaN NaN -0.958 2.478 1995 1 NaN NaN NaN NaN NaN NaN -1.894 4.405 1995 2 NaN NaN NaN NaN NaN NaN -6.809 -1.611 1995 3 NaN NaN NaN NaN NaN NaN 3.035 2.822 1995 4 NaN NaN NaN NaN NaN NaN 5.708 -1.467 1995 5 NaN NaN NaN NaN NaN NaN 12.728 -0.732