% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39074 % Primary Name: NORTH BERWICK % Record Type: TAVG % Country: United States % State: ME % Latitude: 43.30360 +/- 0.00005 % Longitude: -70.73330 +/- 0.00005 % Elevation (m): 42.98 +/- 0.15 % # of Months: 9 % % Alternate Names: Missing Station ID - 175835 % % IDs: coop - 175835 % ghcnd - USC00175835 % ncdc - 12002256 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 7b98f7302ad39495044ba5756ef3a0ba % Raw Data Hash: 39fd5e29c451808f94875d26050f42c5 % Adj Data Hash: 5dc8253eb0d22fefc839b7385ea89c13 % % 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 1895 4 NaN NaN NaN NaN NaN NaN 5.780 -0.476 1895 5 NaN NaN NaN NaN NaN NaN 12.046 1.069 1895 6 NaN NaN NaN NaN NaN NaN 16.455 0.742 1895 7 NaN NaN NaN NaN NaN NaN 17.882 -1.382 1895 8 NaN NaN NaN NaN NaN NaN 19.185 -0.229 1895 9 NaN NaN NaN NaN NaN NaN 16.948 0.609 1895 10 NaN NaN NaN NaN NaN NaN 9.184 -2.516 1895 11 NaN NaN NaN NaN NaN NaN 8.274 0.926 1895 12 NaN NaN NaN NaN NaN NaN 2.620 0.892 1896 1 NaN NaN NaN NaN NaN NaN -2.173 -1.628 1896 2 NaN NaN NaN NaN NaN NaN -1.391 -0.603 1896 3 NaN NaN NaN NaN NaN NaN -0.214 -2.432 1896 4 7.200 1.626 0 0 7.200 1.626 6.300 0.044 1896 5 14.803 4.508 0 0 14.803 4.508 12.042 1.065 1896 6 NaN NaN NaN NaN NaN NaN 15.135 -0.578 1896 7 NaN NaN NaN NaN NaN NaN 19.278 0.013 1896 8 NaN NaN NaN NaN NaN NaN 19.337 -0.076 1896 9 NaN NaN NaN NaN NaN NaN 15.499 -0.840 1896 10 8.208 -2.809 0 0 8.208 -2.809 9.952 -1.747 1896 11 4.352 -2.313 1 0 NaN NaN 8.596 1.249 1896 12 -4.206 -5.252 0 0 -4.206 -5.252 -0.483 -2.211 1897 1 -4.731 -3.504 0 0 -4.731 -3.504 -0.488 0.057 1897 2 -4.187 -2.716 0 0 -4.187 -2.716 -0.560 0.228 1897 3 NaN NaN NaN NaN NaN NaN 1.890 -0.327 1897 4 8.372 2.798 0 0 8.372 2.798 6.830 0.574 1897 5 13.823 3.528 0 0 13.823 3.528 11.148 0.171 1897 6 NaN NaN NaN NaN NaN NaN 13.460 -2.253 1897 7 NaN NaN NaN NaN NaN NaN 19.225 -0.040 1897 8 NaN NaN NaN NaN NaN NaN 18.769 -0.645 1897 9 NaN NaN NaN NaN NaN NaN 15.779 -0.560 1897 10 NaN NaN NaN NaN NaN NaN 11.547 -0.153 1897 11 NaN NaN NaN NaN NaN NaN 6.423 -0.925 1897 12 NaN NaN NaN NaN NaN NaN 1.669 -0.058 1898 1 NaN NaN NaN NaN NaN NaN -1.179 -0.635 1898 2 NaN NaN NaN NaN NaN NaN 0.291 1.079 1898 3 NaN NaN NaN NaN NaN NaN 4.526 2.308 1898 4 NaN NaN NaN NaN NaN NaN 4.729 -1.528 1898 5 NaN NaN NaN NaN NaN NaN 10.413 -0.564