% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 42862 % Primary Name: WARLAND 12 N % Record Type: TAVG % Country: United States % State: MT % Latitude: 48.66670 +/- 0.00005 % Longitude: -115.31670 +/- 0.00005 % Elevation (m): 680.00 +/- 0.05 % # of Months: 35 % % Alternate Names: Missing Station ID - 248683 % % IDs: coop - 248683 % ghcnd - USC00248683 % ncdc - 20012813 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: e19d90930ae680a1099f08f31fb3ea38 % Raw Data Hash: 61f1974f2c9d20ba8399c8c83223cdaf % Adj Data Hash: 63cf33e2aaf2b0f4499b00bd9e510b8e % % 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 1962 8 NaN NaN NaN NaN NaN NaN 13.189 -0.747 1962 9 NaN NaN NaN NaN NaN NaN 9.248 0.065 1962 10 NaN NaN NaN NaN NaN NaN 4.519 1.238 1962 11 NaN NaN NaN NaN NaN NaN -0.767 2.708 1962 12 NaN NaN NaN NaN NaN NaN -3.293 4.136 1963 1 NaN NaN NaN NaN NaN NaN -14.958 -5.066 1963 2 NaN NaN NaN NaN NaN NaN -0.576 4.949 1963 3 NaN NaN NaN NaN NaN NaN -0.729 1.871 1963 4 NaN NaN NaN NaN NaN NaN 2.695 0.122 1963 5 NaN NaN NaN NaN NaN NaN 7.445 -0.214 1963 6 NaN NaN NaN NaN NaN NaN 11.268 -0.158 1963 7 NaN NaN NaN NaN NaN NaN 13.847 -0.968 1963 8 17.395 -1.049 1 0 NaN NaN 14.851 0.915 1963 9 16.722 3.031 0 0 16.722 3.031 12.292 3.109 1963 10 9.278 1.490 0 0 9.278 1.490 6.052 2.772 1963 11 2.278 1.245 0 0 2.278 1.245 -2.262 1.213 1963 12 -4.889 -1.968 0 0 -4.889 -1.968 -8.180 -0.751 1964 1 -1.444 3.940 0 0 -1.444 3.940 -6.696 3.196 1964 2 0.111 1.129 0 0 0.111 1.129 -3.521 2.005 1964 3 1.167 -0.742 0 0 1.167 -0.742 -4.831 -2.231 1964 4 6.389 -0.693 0 0 6.389 -0.693 1.446 -1.127 1964 5 11.056 -1.112 0 0 11.056 -1.112 6.920 -0.740 1964 6 15.222 -0.712 0 0 15.222 -0.712 10.666 -0.760 1964 7 19.000 -0.324 0 0 19.000 -0.324 15.035 0.219 1964 8 15.333 -3.111 0 0 15.333 -3.111 11.475 -2.460 1964 9 NaN NaN NaN NaN NaN NaN 7.273 -1.910 1964 10 NaN NaN NaN NaN NaN NaN 4.399 1.118 1964 11 NaN NaN NaN NaN NaN NaN -3.383 0.092 1964 12 -12.535 -9.614 1 0 NaN NaN -11.274 -3.845 1965 1 -1.778 3.606 0 0 -1.778 3.606 -7.024 2.868 1965 2 -1.167 -0.149 0 0 -1.167 -0.149 -4.414 1.111 1965 3 -0.722 -2.631 0 0 -0.722 -2.631 -6.766 -4.166 1965 4 7.444 0.363 0 0 7.444 0.363 3.227 0.653 1965 5 10.278 -1.889 0 0 10.278 -1.889 6.554 -1.105 1965 6 15.667 -0.267 0 0 15.667 -0.267 10.439 -0.987 1965 7 18.944 -0.379 0 0 18.944 -0.379 15.213 0.397 1965 8 19.389 0.945 0 0 19.389 0.945 14.636 0.700 1965 9 9.778 -3.913 0 0 9.778 -3.913 4.750 -4.433 1965 10 9.000 1.212 0 0 9.000 1.212 6.046 2.766 1965 11 2.056 1.023 0 0 2.056 1.023 -3.052 0.423 1965 12 -1.278 1.643 0 0 -1.278 1.643 -6.353 1.076 1966 1 -4.000 1.384 0 0 -4.000 1.384 -9.578 0.314 1966 2 -0.778 0.240 0 0 -0.778 0.240 -4.310 1.216 1966 3 2.056 0.147 0 0 2.056 0.147 -2.423 0.177 1966 4 6.722 -0.359 0 0 6.722 -0.359 1.582 -0.992 1966 5 14.000 1.833 0 0 14.000 1.833 8.752 1.093 1966 6 14.278 -1.656 0 0 14.278 -1.656 9.467 -1.959 1966 7 19.056 -0.268 0 0 19.056 -0.268 14.661 -0.154 1966 8 18.278 -0.166 0 0 18.278 -0.166 13.385 -0.550 1966 9 16.703 3.012 1 0 NaN NaN 12.145 2.962 1966 10 NaN NaN NaN NaN NaN NaN 3.927 0.647 1966 11 NaN NaN NaN NaN NaN NaN -3.652 -0.177 1966 12 NaN NaN NaN NaN NaN NaN -4.601 2.828 1967 1 NaN NaN NaN NaN NaN NaN -5.967 3.925 1967 2 NaN NaN NaN NaN NaN NaN -2.346 3.179 1967 3 NaN NaN NaN NaN NaN NaN -4.848 -2.248 1967 4 NaN NaN NaN NaN NaN NaN 0.165 -2.409 1967 5 NaN NaN NaN NaN NaN NaN 6.941 -0.718 1967 6 NaN NaN NaN NaN NaN NaN 11.307 -0.118 1967 7 NaN NaN NaN NaN NaN NaN 15.882 1.067 1967 8 NaN NaN NaN NaN NaN NaN 16.703 2.767 1967 9 NaN NaN NaN NaN NaN NaN 13.561 4.378