% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 42846 % Primary Name: SEVILLE % Record Type: TAVG % Country: United States % State: MT % Latitude: 48.63330 +/- 0.00005 % Longitude: -112.53330 +/- 0.00005 % Elevation (m): 1203.96 +/- 0.15 % # of Months: 20 % % Alternate Names: Missing Station ID - 247462 % % IDs: coop - 247462 % ghcnd - USC00247462 % ncdc - 12003180 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 369164c32103c6c5380d6526d1ac8a54 % Raw Data Hash: dbae9ca1cdc8a908e16218b6f3e44523 % Adj Data Hash: 03bcba45b8c836b6183538d6de7096f7 % % 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 1909 11 NaN NaN NaN NaN NaN NaN -3.196 -1.799 1909 12 NaN NaN NaN NaN NaN NaN -9.563 -3.710 1910 1 NaN NaN NaN NaN NaN NaN -6.606 2.893 1910 2 NaN NaN NaN NaN NaN NaN -9.751 -4.394 1910 3 NaN NaN NaN NaN NaN NaN 3.639 6.340 1910 4 NaN NaN NaN NaN NaN NaN 8.271 4.774 1910 5 NaN NaN NaN NaN NaN NaN 10.318 0.845 1910 6 NaN NaN NaN NaN NaN NaN 13.993 0.413 1910 7 NaN NaN NaN NaN NaN NaN 18.097 1.045 1910 8 NaN NaN NaN NaN NaN NaN 13.974 -2.322 1910 9 NaN NaN NaN NaN NaN NaN 9.798 -1.599 1910 10 NaN NaN NaN NaN NaN NaN 8.533 2.428 1910 11 -4.219 -3.031 1 0 NaN NaN -1.552 -0.156 1910 12 -3.682 1.962 0 0 -3.682 1.962 -3.421 2.432 1911 1 -13.783 -4.492 1 0 NaN NaN -13.954 -4.455 1911 2 -11.161 -6.012 0 0 -11.161 -6.012 -8.009 -2.652 1911 3 1.041 3.533 0 0 1.041 3.533 0.604 3.304 1911 4 2.768 -0.938 0 0 2.768 -0.938 1.991 -1.506 1911 5 8.008 -1.674 0 0 8.008 -1.674 8.069 -1.404 1911 6 15.867 2.078 0 0 15.867 2.078 14.313 0.733 1911 7 15.303 -1.957 0 0 15.303 -1.957 14.854 -2.197 1911 8 14.674 -1.831 0 0 14.674 -1.831 13.600 -2.696 1911 9 8.155 -3.450 0 0 8.155 -3.450 8.429 -2.967 1911 10 5.497 -0.817 0 0 5.497 -0.817 5.864 -0.241 1911 11 -7.167 -5.979 0 0 -7.167 -5.979 -6.463 -5.066 1911 12 -5.925 -0.281 0 0 -5.925 -0.281 -5.824 0.029 1912 1 -8.915 0.376 0 0 -8.915 0.376 -10.831 -1.331 1912 2 -2.605 2.543 0 0 -2.605 2.543 -2.243 3.114 1912 3 -7.550 -5.059 0 0 -7.550 -5.059 -8.322 -5.622 1912 4 5.477 1.771 0 0 5.477 1.771 4.947 1.450 1912 5 10.153 0.472 0 0 10.153 0.472 9.584 0.111 1912 6 15.750 1.961 0 0 15.750 1.961 14.787 1.207 1912 7 NaN NaN NaN NaN NaN NaN 14.419 -2.632 1912 8 NaN NaN NaN NaN NaN NaN 14.526 -1.770 1912 9 NaN NaN NaN NaN NaN NaN 7.610 -3.787 1912 10 NaN NaN NaN NaN NaN NaN 5.654 -0.450 1912 11 NaN NaN NaN NaN NaN NaN 1.103 2.500 1912 12 NaN NaN NaN NaN NaN NaN -2.757 3.096 1913 1 NaN NaN NaN NaN NaN NaN -13.683 -4.184 1913 2 NaN NaN NaN NaN NaN NaN -8.751 -3.394 1913 3 NaN NaN NaN NaN NaN NaN -7.514 -4.814 1913 4 NaN NaN NaN NaN NaN NaN 4.842 1.345 1913 5 NaN NaN NaN NaN NaN NaN 8.402 -1.071 1913 6 NaN NaN NaN NaN NaN NaN 14.397 0.817