% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 40926 % Primary Name: BIRNEY 7 E % Record Type: TAVG % Country: United States % State: MT % Latitude: 45.28330 +/- 0.00005 % Longitude: -106.35000 +/- 0.00005 % Elevation (m): 915.00 +/- 0.05 % # of Months: 13 % % Alternate Names: Missing Station ID - 240821 % % IDs: coop - 240821 % ghcnd - USC00240821 % ncdc - 20012207 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 9ab4db5a73ee2ff2fd7bb24de96f922a % Raw Data Hash: be0a7b9560f3e4a1188a1c2d285abfbe % Adj Data Hash: 25acc4b273b0e7fa7bb88a4d8a12f435 % % 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 1948 11 NaN NaN NaN NaN NaN NaN 0.137 0.034 1948 12 NaN NaN NaN NaN NaN NaN -8.336 -3.468 1949 1 NaN NaN NaN NaN NaN NaN -15.889 -7.802 1949 2 NaN NaN NaN NaN NaN NaN -8.740 -4.950 1949 3 NaN NaN NaN NaN NaN NaN -2.065 -2.041 1949 4 NaN NaN NaN NaN NaN NaN 9.811 3.535 1949 5 NaN NaN NaN NaN NaN NaN 14.154 1.882 1949 6 NaN NaN NaN NaN NaN NaN 16.689 -0.464 1949 7 NaN NaN NaN NaN NaN NaN 21.253 -0.101 1949 8 NaN NaN NaN NaN NaN NaN 21.849 1.613 1949 9 NaN NaN NaN NaN NaN NaN 13.350 -0.875 1949 10 NaN NaN NaN NaN NaN NaN 6.451 -1.700 1949 11 5.889 5.568 0 0 5.889 5.568 5.899 5.796 1949 12 -8.056 -3.405 0 0 -8.056 -3.405 -7.685 -2.817 1950 1 -15.611 -7.742 0 0 -15.611 -7.742 -17.957 -9.870 1950 2 -8.271 -4.698 1 0 NaN NaN -1.928 1.863 1950 3 -1.068 -1.263 1 0 NaN NaN -2.732 -2.709 1950 4 NaN NaN NaN NaN NaN NaN 4.883 -1.393 1950 5 NaN NaN NaN NaN NaN NaN 9.728 -2.545 1950 6 NaN NaN NaN NaN NaN NaN 14.903 -2.249 1950 7 NaN NaN NaN NaN NaN NaN 19.120 -2.233 1950 8 NaN NaN NaN NaN NaN NaN 18.790 -1.446 1950 9 13.222 -1.220 0 0 13.222 -1.220 12.965 -1.260 1950 10 9.500 1.131 0 0 9.500 1.131 10.753 2.602 1950 11 -1.056 -1.376 0 0 -1.056 -1.376 -1.713 -1.816 1950 12 -3.000 1.650 0 0 -3.000 1.650 -2.318 2.550 1951 1 -10.278 -2.409 0 0 -10.278 -2.409 -9.465 -1.378 1951 2 -2.444 1.128 0 0 -2.444 1.128 -2.381 1.410 1951 3 -4.000 -4.194 0 0 -4.000 -4.194 -6.111 -6.087 1951 4 5.322 -1.172 1 0 NaN NaN 4.227 -2.049 1951 5 NaN NaN NaN NaN NaN NaN 13.162 0.889 1951 6 NaN NaN NaN NaN NaN NaN 12.949 -4.203 1951 7 NaN NaN NaN NaN NaN NaN 21.173 -0.181 1951 8 NaN NaN NaN NaN NaN NaN 19.362 -0.874 1951 9 NaN NaN NaN NaN NaN NaN 11.307 -2.918 1951 10 NaN NaN NaN NaN NaN NaN 7.133 -1.018 1951 11 NaN NaN NaN NaN NaN NaN -0.451 -0.554 1951 12 NaN NaN NaN NaN NaN NaN -9.695 -4.827 1952 1 NaN NaN NaN NaN NaN NaN -11.008 -2.922 1952 2 NaN NaN NaN NaN NaN NaN -2.868 0.922 1952 3 NaN NaN NaN NaN NaN NaN -3.092 -3.069 1952 4 NaN NaN NaN NaN NaN NaN 9.232 2.956