% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 35771 % Primary Name: MOON TOWNSHIP % Record Type: TAVG % Country: United States % State: PA % Latitude: 40.53190 +/- 0.00005 % Longitude: -80.21720 +/- 0.00005 % Elevation (m): 357.23 +/- 0.15 % # of Months: 37 % % Alternate Names: Missing Station ID - 365918 % % IDs: coop - 365918 % ghcnd - USC00365918 % ncdc - 30015516 % nws - PBZP1 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 852b126918c87fd146f20f5760032f78 % Raw Data Hash: 3a4468833c29f31ef083b1660c8d0f82 % Adj Data Hash: 45d9da7105aef160822a7ed675bdf688 % % 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 2009 10 NaN NaN NaN NaN NaN NaN 10.103 -1.118 2009 11 NaN NaN NaN NaN NaN NaN 8.601 3.460 2009 12 NaN NaN NaN NaN NaN NaN -1.411 -0.532 2010 1 NaN NaN NaN NaN NaN NaN -4.210 -0.606 2010 2 NaN NaN NaN NaN NaN NaN -4.040 -1.671 2010 3 NaN NaN NaN NaN NaN NaN 5.469 2.517 2010 4 NaN NaN NaN NaN NaN NaN 12.551 3.242 2010 5 NaN NaN NaN NaN NaN NaN 16.839 1.743 2010 6 NaN NaN NaN NaN NaN NaN 21.830 1.808 2010 7 NaN NaN NaN NaN NaN NaN 23.953 1.793 2010 8 NaN NaN NaN NaN NaN NaN 23.381 1.950 2010 9 NaN NaN NaN NaN NaN NaN 18.884 1.104 2010 10 11.667 0.429 0 0 11.667 0.429 11.918 0.697 2010 11 5.056 -0.102 0 0 5.056 -0.102 6.044 0.903 2010 12 -3.889 -3.027 0 0 -3.889 -3.027 -4.052 -3.172 2011 1 -4.500 -0.914 0 0 -4.500 -0.914 -5.478 -1.874 2011 2 -0.833 1.518 0 0 -0.833 1.518 -1.959 0.410 2011 3 2.889 -0.080 0 0 2.889 -0.080 3.046 0.095 2011 4 11.389 2.063 0 0 11.389 2.063 10.618 1.309 2011 5 16.778 1.664 0 0 16.778 1.664 16.409 1.313 2011 6 20.778 0.739 0 0 20.778 0.739 21.081 1.060 2011 7 24.667 2.489 0 0 24.667 2.489 24.737 2.577 2011 8 22.111 0.663 0 0 22.111 0.663 22.155 0.724 2011 9 18.389 0.592 0 0 18.389 0.592 18.931 1.152 2011 10 11.000 -0.238 0 0 11.000 -0.238 11.448 0.228 2011 11 8.111 2.953 0 0 8.111 2.953 8.894 3.754 2011 12 2.523 3.385 0 0 2.523 3.385 2.254 3.133 2012 1 -0.542 3.044 0 0 -0.542 3.044 -0.843 2.761 2012 2 1.502 3.853 0 0 1.502 3.853 0.942 3.311 2012 3 10.355 7.386 0 0 10.355 7.386 10.277 7.326 2012 4 9.450 0.124 0 0 9.450 0.124 9.504 0.195 2012 5 19.221 4.108 0 0 19.221 4.108 18.652 3.556 2012 6 21.116 1.077 0 0 21.116 1.077 21.140 1.119 2012 7 24.795 2.618 0 0 24.795 2.618 24.757 2.598 2012 8 21.776 0.328 0 0 21.776 0.328 21.846 0.416 2012 9 17.352 -0.445 0 0 17.352 -0.445 17.736 -0.044 2012 10 11.350 0.112 0 0 11.350 0.112 11.686 0.465 2012 11 4.080 -1.078 0 0 4.080 -1.078 4.731 -0.410 2012 12 3.429 4.291 0 0 3.429 4.291 2.824 3.704 2013 1 -0.905 2.682 0 0 -0.905 2.682 -1.479 2.125 2013 2 -2.498 -0.147 0 0 -2.498 -0.147 -2.809 -0.441 2013 3 1.150 -1.819 0 0 1.150 -1.819 1.428 -1.524 2013 4 10.377 1.050 0 0 10.377 1.050 10.015 0.707 2013 5 16.329 1.216 0 0 16.329 1.216 16.567 1.471 2013 6 20.620 0.581 0 0 20.620 0.581 20.441 0.419 2013 7 NaN NaN NaN NaN NaN NaN 22.670 0.510 2013 8 20.510 -0.938 1 0 NaN NaN 21.021 -0.410 2013 9 17.402 -0.395 0 0 17.402 -0.395 17.954 0.175 2013 10 12.145 0.907 0 0 12.145 0.907 12.610 1.389 2013 11 9.050 3.892 1 0 NaN NaN NaN NaN