% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 38524 % Primary Name: GUILFORD CENTER % Record Type: TAVG % Country: United States % State: VT % Latitude: 42.78330 +/- 0.00005 % Longitude: -72.66670 +/- 0.00005 % Elevation (m): 404.12 +/- 218.14 % # of Months: 14 % % Alternate Names: Missing Station ID - 433660 % % IDs: coop - 433660 % ghcnd - USC00433660 % ncdc - 12005690 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: da0bf5588ac9e3ea90acc44d27d24228 % Raw Data Hash: a542b22ca0bf24a79c4476b1003ffba2 % Adj Data Hash: 4c86441c867624940bfda697ab1a5322 % % 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 1886 4 NaN NaN NaN NaN NaN NaN 8.599 1.593 1886 5 NaN NaN NaN NaN NaN NaN 12.725 -0.508 1886 6 NaN NaN NaN NaN NaN NaN 16.431 -1.864 1886 7 NaN NaN NaN NaN NaN NaN 20.188 -0.799 1886 8 NaN NaN NaN NaN NaN NaN 18.696 -1.133 1886 9 NaN NaN NaN NaN NaN NaN 14.946 -0.485 1886 10 NaN NaN NaN NaN NaN NaN 8.804 -0.594 1886 11 NaN NaN NaN NaN NaN NaN 3.665 -0.004 1886 12 NaN NaN NaN NaN NaN NaN -6.371 -3.032 1887 1 NaN NaN NaN NaN NaN NaN -7.848 -2.103 1887 2 NaN NaN NaN NaN NaN NaN -5.191 -0.524 1887 3 NaN NaN NaN NaN NaN NaN -2.906 -3.489 1887 4 5.074 -2.604 0 0 5.074 -2.604 4.677 -2.329 1887 5 17.276 3.371 0 0 17.276 3.371 15.091 1.858 1887 6 19.266 0.299 0 0 19.266 0.299 17.661 -0.634 1887 7 23.405 1.746 0 0 23.405 1.746 22.781 1.794 1887 8 18.111 -2.389 0 0 18.111 -2.389 17.970 -1.859 1887 9 13.770 -2.334 0 0 13.770 -2.334 12.907 -2.524 1887 10 7.613 -2.456 1 0 NaN NaN 7.870 -1.528 1887 11 1.852 -2.489 0 0 1.852 -2.489 2.739 -0.929 1887 12 -3.566 -0.899 0 0 -3.566 -0.899 -4.037 -0.698 1888 1 -10.717 -5.644 0 0 -10.717 -5.644 -10.786 -5.042 1888 2 -5.441 -1.445 1 0 NaN NaN -6.124 -1.457 1888 3 -2.652 -3.907 0 0 -2.652 -3.907 -3.044 -3.627 1888 4 4.058 -3.620 1 0 NaN NaN 3.926 -3.080 1888 5 12.885 -1.020 0 0 12.885 -1.020 11.354 -1.879 1888 6 NaN NaN NaN NaN NaN NaN 18.038 -0.257 1888 7 NaN NaN NaN NaN NaN NaN 18.797 -2.190 1888 8 NaN NaN NaN NaN NaN NaN 19.075 -0.754 1888 9 NaN NaN NaN NaN NaN NaN 13.310 -2.122 1888 10 NaN NaN NaN NaN NaN NaN 5.547 -3.851 1888 11 NaN NaN NaN NaN NaN NaN 3.696 0.027 1888 12 NaN NaN NaN NaN NaN NaN -2.942 0.397 1889 1 NaN NaN NaN NaN NaN NaN -2.272 3.472 1889 2 NaN NaN NaN NaN NaN NaN -7.276 -2.609 1889 3 NaN NaN NaN NaN NaN NaN 1.103 0.520 1889 4 NaN NaN NaN NaN NaN NaN 7.716 0.710 1889 5 NaN NaN NaN NaN NaN NaN 14.543 1.310