% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 40897 % Primary Name: DEAD RIVER 26 N % Record Type: TAVG % Country: United States % State: ME % Latitude: 45.23330 +/- 0.00005 % Longitude: -70.20000 +/- 0.00005 % Elevation (m): 353.90 +/- 0.05 % # of Months: 11 % % IDs: coop - 171870 % ghcnd - USC00171870 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % % Site Hash: faad16f4c77942ccb59ac17e712ce078 % Raw Data Hash: 769fdbb5375f5cef4edfef6be5a8c50b % Adj Data Hash: 95390136d3acac13be7193a0e0456705 % % 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 1950 7 NaN NaN NaN NaN NaN NaN 17.516 -0.324 1950 8 NaN NaN NaN NaN NaN NaN 15.907 -0.611 1950 9 NaN NaN NaN NaN NaN NaN 9.549 -2.380 1950 10 NaN NaN NaN NaN NaN NaN 6.376 0.431 1950 11 NaN NaN NaN NaN NaN NaN 2.802 3.356 1950 12 NaN NaN NaN NaN NaN NaN -7.034 2.003 1951 1 NaN NaN NaN NaN NaN NaN -9.247 2.672 1951 2 NaN NaN NaN NaN NaN NaN -8.661 2.283 1951 3 NaN NaN NaN NaN NaN NaN -3.794 1.019 1951 4 NaN NaN NaN NaN NaN NaN 3.837 1.506 1951 5 NaN NaN NaN NaN NaN NaN 10.142 0.383 1951 6 NaN NaN NaN NaN NaN NaN 14.511 -0.746 1951 7 19.889 0.428 0 0 19.889 0.428 17.581 -0.259 1951 8 18.167 0.028 0 0 18.167 0.028 15.872 -0.646 1951 9 14.500 0.950 0 0 14.500 0.950 11.992 0.062 1951 10 8.611 1.046 0 0 8.611 1.046 6.995 1.050 1951 11 -1.333 -2.400 0 0 -1.333 -2.400 -1.750 -1.196 1951 12 -7.833 -0.417 0 0 -7.833 -0.417 -9.423 -0.386 1952 1 -8.333 1.965 0 0 -8.333 1.965 -10.614 1.305 1952 2 -7.778 1.546 0 0 -7.778 1.546 -8.678 2.266 1952 3 -2.167 1.026 0 0 -2.167 1.026 -3.628 1.186 1952 4 4.389 0.438 0 0 4.389 0.438 3.556 1.226 1952 5 9.673 -1.706 1 0 NaN NaN 8.547 -1.212 1952 6 NaN NaN NaN NaN NaN NaN 15.709 0.452 1952 7 NaN NaN NaN NaN NaN NaN 20.369 2.529 1952 8 NaN NaN NaN NaN NaN NaN 17.442 0.924 1952 9 NaN NaN NaN NaN NaN NaN 12.474 0.545 1952 10 NaN NaN NaN NaN NaN NaN 4.548 -1.396 1952 11 NaN NaN NaN NaN NaN NaN 0.884 1.437 1952 12 NaN NaN NaN NaN NaN NaN -7.162 1.875 1953 1 NaN NaN NaN NaN NaN NaN -8.093 3.826 1953 2 NaN NaN NaN NaN NaN NaN -8.318 2.626 1953 3 NaN NaN NaN NaN NaN NaN -3.295 1.519 1953 4 NaN NaN NaN NaN NaN NaN 3.912 1.582 1953 5 NaN NaN NaN NaN NaN NaN 10.732 0.973