% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 30169 % Primary Name: SOUTH CUMBERLAND SP % Record Type: TAVG % Country: United States % State: TN % Latitude: 35.25690 +/- 0.00005 % Longitude: -85.79080 +/- 0.00005 % Elevation (m): 548.64 +/- 0.15 % # of Months: 17 % % Alternate Names: Missing Station ID - 408158 % % IDs: coop - 408158 % ghcnd - USC00408158 % ncdc - 30001729 % nws - SCPT1 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: b12c77458b9f093816bced668c158eb1 % Raw Data Hash: 9d93bb28da43d5f0b4cd2f1d6a638c5c % Adj Data Hash: 112b28c3eb6158424b237f4e332322b6 % % 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 2003 8 NaN NaN NaN NaN NaN NaN 25.974 0.813 2003 9 NaN NaN NaN NaN NaN NaN 22.179 0.101 2003 10 NaN NaN NaN NaN NaN NaN 15.601 0.180 2003 11 NaN NaN NaN NaN NaN NaN 13.249 3.489 2003 12 NaN NaN NaN NaN NaN NaN 4.839 -0.753 2004 1 NaN NaN NaN NaN NaN NaN 3.793 -0.282 2004 2 NaN NaN NaN NaN NaN NaN 4.879 -1.030 2004 3 NaN NaN NaN NaN NaN NaN 12.947 2.739 2004 4 NaN NaN NaN NaN NaN NaN 15.471 -0.026 2004 5 NaN NaN NaN NaN NaN NaN 21.758 2.002 2004 6 NaN NaN NaN NaN NaN NaN 24.267 0.637 2004 7 NaN NaN NaN NaN NaN NaN 25.205 -0.265 2004 8 19.931 -2.272 1 0 NaN NaN 23.847 -1.314 2004 9 20.313 1.194 1 0 NaN NaN 22.356 0.278 2004 10 14.278 1.815 0 0 14.278 1.815 18.105 2.684 2004 11 10.389 3.587 0 0 10.389 3.587 12.814 3.054 2004 12 4.074 1.440 1 0 NaN NaN 5.432 -0.160 2005 1 3.222 2.106 0 0 3.222 2.106 6.987 2.913 2005 2 6.675 3.723 1 0 NaN NaN 7.678 1.768 2005 3 7.778 0.528 0 0 7.778 0.528 9.642 -0.566 2005 4 12.611 0.072 0 0 12.611 0.072 15.418 -0.079 2005 5 15.278 -1.520 0 0 15.278 -1.520 18.036 -1.719 2005 6 21.000 0.328 0 0 21.000 0.328 24.046 0.416 2005 7 23.556 1.044 0 0 23.556 1.044 26.177 0.706 2005 8 23.333 1.131 0 0 23.333 1.131 26.552 1.391 2005 9 20.722 1.603 0 0 20.722 1.603 24.128 2.051 2005 10 13.722 1.259 0 0 13.722 1.259 16.344 0.923 2005 11 8.444 1.643 0 0 8.444 1.643 11.580 1.820 2005 12 0.850 -1.784 1 0 NaN NaN 3.848 -1.744 2006 1 NaN NaN NaN NaN NaN NaN 7.860 3.785 2006 2 NaN NaN NaN NaN NaN NaN 4.579 -1.331 2006 3 NaN NaN NaN NaN NaN NaN 11.023 0.815 2006 4 NaN NaN NaN NaN NaN NaN 18.666 3.169 2006 5 NaN NaN NaN NaN NaN NaN 19.561 -0.194 2006 6 NaN NaN NaN NaN NaN NaN 24.357 0.727 2006 7 NaN NaN NaN NaN NaN NaN 26.831 1.361 2006 8 NaN NaN NaN NaN NaN NaN 27.616 2.456 2006 9 NaN NaN NaN NaN NaN NaN 21.648 -0.430 2006 10 NaN NaN NaN NaN NaN NaN 14.432 -0.989 2006 11 NaN NaN NaN NaN NaN NaN 10.470 0.710 2006 12 NaN NaN NaN NaN NaN NaN 7.762 2.170