% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 41177 % Primary Name: BOZEMAN (2) % Record Type: TAVG % Country: United States % State: MT % Latitude: 45.65000 +/- 0.00500 % Longitude: -111.05000 +/- 0.00500 % Elevation (m): 1493.52 +/- 0.15 % # of Months: 23 % % Alternate Names: Missing Station ID - 241046 % % IDs: coop - 241046 % ghcnd - USC00241046 % ncdc - 12003053 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 23ad97b573ccfe93ce81d8af76b978d9 % Raw Data Hash: 0b251b9469bd88f93d5622ab10307840 % Adj Data Hash: a3756c7fa2c61550031757d0a7bab189 % % 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 1895 2 NaN NaN NaN NaN NaN NaN -6.304 -1.667 1895 3 NaN NaN NaN NaN NaN NaN -3.905 -1.477 1895 4 NaN NaN NaN NaN NaN NaN 4.902 1.920 1895 5 NaN NaN NaN NaN NaN NaN 8.279 -0.118 1895 6 NaN NaN NaN NaN NaN NaN 9.996 -2.777 1895 7 NaN NaN NaN NaN NaN NaN 15.727 -1.349 1895 8 NaN NaN NaN NaN NaN NaN 15.600 -0.474 1895 9 NaN NaN NaN NaN NaN NaN 8.723 -2.114 1895 10 NaN NaN NaN NaN NaN NaN 6.249 0.962 1895 11 NaN NaN NaN NaN NaN NaN -3.193 -1.192 1895 12 NaN NaN NaN NaN NaN NaN -7.121 -1.114 1896 1 NaN NaN NaN NaN NaN NaN -6.003 2.284 1896 2 0.421 2.930 1 0 NaN NaN -1.253 3.385 1896 3 -1.865 -1.565 0 0 -1.865 -1.565 -5.351 -2.922 1896 4 3.908 -1.202 0 0 3.908 -1.202 1.092 -1.890 1896 5 7.365 -3.161 0 0 7.365 -3.161 5.648 -2.749 1896 6 16.173 1.272 0 0 16.173 1.272 13.670 0.897 1896 7 18.011 -1.193 0 0 18.011 -1.193 17.440 0.364 1896 8 17.187 -1.016 0 0 17.187 -1.016 15.366 -0.708 1896 9 10.727 -2.239 0 0 10.727 -2.239 8.437 -2.400 1896 10 7.319 -0.096 0 0 7.319 -0.096 6.334 1.048 1896 11 -4.993 -5.121 0 0 -4.993 -5.121 -7.676 -5.675 1896 12 1.508 5.387 0 0 1.508 5.387 -1.153 4.855 1897 1 -7.240 -1.083 0 0 -7.240 -1.083 -9.466 -1.180 1897 2 -3.999 -1.490 1 0 NaN NaN -5.526 -0.888 1897 3 -4.815 -4.515 0 0 -4.815 -4.515 -8.163 -5.735 1897 4 6.222 1.112 0 0 6.222 1.112 3.681 0.699 1897 5 14.767 4.241 0 0 14.767 4.241 12.703 4.306 1897 6 14.857 -0.045 0 0 14.857 -0.045 11.893 -0.879 1897 7 16.690 -2.514 0 0 16.690 -2.514 15.323 -1.752 1897 8 18.335 0.133 0 0 18.335 0.133 17.405 1.331 1897 9 13.337 0.370 0 0 13.337 0.370 11.719 0.881 1897 10 6.732 -0.684 0 0 6.732 -0.684 5.801 0.514 1897 11 -1.056 -1.184 0 0 -1.056 -1.184 -3.746 -1.745 1897 12 -4.481 -0.602 0 0 -4.481 -0.602 -6.974 -0.966 1898 1 NaN NaN NaN NaN NaN NaN -9.146 -0.860 1898 2 NaN NaN NaN NaN NaN NaN -1.410 3.228 1898 3 NaN NaN NaN NaN NaN NaN -7.167 -4.739 1898 4 NaN NaN NaN NaN NaN NaN 4.114 1.133 1898 5 NaN NaN NaN NaN NaN NaN 7.337 -1.060 1898 6 NaN NaN NaN NaN NaN NaN 11.746 -1.027 1898 7 NaN NaN NaN NaN NaN NaN 16.181 -0.895 1898 8 NaN NaN NaN NaN NaN NaN 17.672 1.598 1898 9 NaN NaN NaN NaN NaN NaN 9.977 -0.860 1898 10 NaN NaN NaN NaN NaN NaN 3.142 -2.144 1898 11 NaN NaN NaN NaN NaN NaN -4.035 -2.034 1898 12 NaN NaN NaN NaN NaN NaN -8.101 -2.094