% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39132 % Primary Name: EAST CANTERBURY % Record Type: TAVG % Country: United States % State: NH % Latitude: 43.35000 +/- 0.00500 % Longitude: -71.50000 +/- 0.00500 % Elevation (m): 243.84 +/- 0.15 % # of Months: 22 % % Alternate Names: Missing Station ID - 272250 % % IDs: coop - 272250 % ghcnd - USC00272250 % ncdc - 12003455 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 7939db4654e40cc1e3bfd49c204b8cc2 % Raw Data Hash: 1e6121bd2e5806e2df4597f9697b9829 % Adj Data Hash: 2b4e0dd8a6d664750350a4667e8da283 % % 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 1891 12 NaN NaN NaN NaN NaN NaN 0.409 3.748 1892 1 NaN NaN NaN NaN NaN NaN -5.608 0.137 1892 2 NaN NaN NaN NaN NaN NaN -4.690 -0.023 1892 3 NaN NaN NaN NaN NaN NaN -1.887 -2.470 1892 4 NaN NaN NaN NaN NaN NaN 6.668 -0.338 1892 5 NaN NaN NaN NaN NaN NaN 11.756 -1.477 1892 6 NaN NaN NaN NaN NaN NaN 19.636 1.341 1892 7 NaN NaN NaN NaN NaN NaN 20.731 -0.256 1892 8 NaN NaN NaN NaN NaN NaN 19.502 -0.327 1892 9 NaN NaN NaN NaN NaN NaN 14.400 -1.032 1892 10 NaN NaN NaN NaN NaN NaN 8.379 -1.018 1892 11 NaN NaN NaN NaN NaN NaN 2.808 -0.861 1892 12 -6.093 -2.249 0 0 -6.093 -2.249 -5.351 -2.012 1893 1 -11.073 -4.823 0 0 -11.073 -4.823 -10.011 -4.266 1893 2 -7.077 -1.905 0 0 -7.077 -1.905 -6.301 -1.634 1893 3 -2.473 -2.551 0 0 -2.473 -2.551 -1.588 -2.171 1893 4 3.426 -3.075 0 0 3.426 -3.075 4.902 -2.104 1893 5 13.244 0.515 0 0 13.244 0.515 12.433 -0.800 1893 6 20.889 3.099 0 0 20.889 3.099 18.205 -0.090 1893 7 21.212 0.730 0 0 21.212 0.730 19.858 -1.129 1893 8 19.516 0.192 0 0 19.516 0.192 19.427 -0.401 1893 9 10.996 -3.931 0 0 10.996 -3.931 12.676 -2.756 1893 10 9.093 0.200 0 0 9.093 0.200 10.091 0.693 1893 11 -0.345 -3.509 0 0 -0.345 -3.509 2.884 -0.785 1893 12 -7.222 -3.378 0 0 -7.222 -3.378 -5.172 -1.833 1894 1 -6.165 0.085 0 0 -6.165 0.085 -4.561 1.183 1894 2 -9.516 -4.344 0 0 -9.516 -4.344 -6.819 -2.152 1894 3 2.151 2.073 0 0 2.151 2.073 3.336 2.753 1894 4 6.630 0.129 0 0 6.630 0.129 7.065 0.059 1894 5 13.065 0.336 0 0 13.065 0.336 13.058 -0.175 1894 6 19.148 1.358 0 0 19.148 1.358 18.770 0.475 1894 7 22.276 1.794 0 0 22.276 1.794 21.586 0.598 1894 8 19.387 0.063 0 0 19.387 0.063 18.331 -1.498 1894 9 16.992 2.065 0 0 16.992 2.065 16.350 0.918 1894 10 NaN NaN NaN NaN NaN NaN 9.441 0.044 1894 11 NaN NaN NaN NaN NaN NaN 0.934 -2.735 1894 12 NaN NaN NaN NaN NaN NaN -4.306 -0.967 1895 1 NaN NaN NaN NaN NaN NaN -6.375 -0.630 1895 2 NaN NaN NaN NaN NaN NaN -8.280 -3.613 1895 3 NaN NaN NaN NaN NaN NaN -1.321 -1.904 1895 4 NaN NaN NaN NaN NaN NaN 6.433 -0.573 1895 5 NaN NaN NaN NaN NaN NaN 14.301 1.068 1895 6 NaN NaN NaN NaN NaN NaN 19.251 0.956 1895 7 NaN NaN NaN NaN NaN NaN 18.958 -2.029 1895 8 NaN NaN NaN NaN NaN NaN 19.355 -0.474 1895 9 NaN NaN NaN NaN NaN NaN 16.159 0.727