% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 42695 % Primary Name: CONRAD 29 ENE PAR % Record Type: TAVG % Country: United States % State: MT % Latitude: 48.28330 +/- 0.00005 % Longitude: -111.33330 +/- 0.00005 % Elevation (m): 1196.00 +/- 0.05 % # of Months: 21 % % Alternate Names: Missing Station ID - 241976 % % IDs: coop - 241976 % ghcnd - USC00241976 % ncdc - 20012728 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 85861da14e6ebd288a1f86f713d8ea2d % Raw Data Hash: dd60baf169476f89c0dbd7b223f42b84 % Adj Data Hash: 08a68018b2c63c864f8e0a97715c4a57 % % 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 1969 11 NaN NaN NaN NaN NaN NaN 0.228 3.301 1969 12 NaN NaN NaN NaN NaN NaN -6.119 3.211 1970 1 NaN NaN NaN NaN NaN NaN -16.317 -2.727 1970 2 NaN NaN NaN NaN NaN NaN -6.358 2.519 1970 3 NaN NaN NaN NaN NaN NaN -6.574 -2.477 1970 4 NaN NaN NaN NaN NaN NaN 2.335 -1.858 1970 5 NaN NaN NaN NaN NaN NaN 11.435 0.467 1970 6 NaN NaN NaN NaN NaN NaN 17.830 2.408 1970 7 NaN NaN NaN NaN NaN NaN 20.047 1.059 1970 8 NaN NaN NaN NaN NaN NaN 19.719 1.675 1970 9 NaN NaN NaN NaN NaN NaN 10.658 -1.415 1970 10 NaN NaN NaN NaN NaN NaN 5.298 -0.545 1970 11 -2.167 -1.619 0 0 -2.167 -1.619 -6.016 -2.942 1970 12 -8.056 -1.251 0 0 -8.056 -1.251 -13.670 -4.341 1971 1 -11.389 -0.324 0 0 -11.389 -0.324 -17.116 -3.526 1971 2 -2.944 3.407 0 0 -2.944 3.407 -6.548 2.329 1971 3 -0.056 1.516 0 0 -0.056 1.516 -5.458 -1.361 1971 4 6.944 0.225 0 0 6.944 0.225 4.868 0.674 1971 5 12.944 -0.549 0 0 12.944 -0.549 12.003 1.035 1971 6 15.500 -2.447 0 0 15.500 -2.447 14.801 -0.621 1971 7 19.389 -2.125 0 0 19.389 -2.125 18.220 -0.769 1971 8 23.889 3.319 0 0 23.889 3.319 22.640 4.596 1971 9 11.944 -2.654 0 0 11.944 -2.654 10.435 -1.638 1971 10 7.222 -1.146 0 0 7.222 -1.146 5.781 -0.062 1971 11 0.333 0.881 0 0 0.333 0.881 -1.888 1.185 1971 12 -11.556 -4.751 0 0 -11.556 -4.751 -14.944 -5.614 1972 1 -15.333 -4.269 0 0 -15.333 -4.269 -18.653 -5.063 1972 2 -8.833 -2.482 0 0 -8.833 -2.482 -11.688 -2.811 1972 3 0.833 2.405 0 0 0.833 2.405 -2.352 1.745 1972 4 6.222 -0.497 0 0 6.222 -0.497 4.366 0.172 1972 5 11.111 -2.382 0 0 11.111 -2.382 11.713 0.745 1972 6 NaN NaN NaN NaN NaN NaN 16.973 1.551 1972 7 18.695 -2.819 1 0 NaN NaN 16.799 -2.189 1972 8 21.500 0.930 0 0 21.500 0.930 20.496 2.452 1972 9 NaN NaN NaN NaN NaN NaN 8.602 -3.470 1972 10 NaN NaN NaN NaN NaN NaN 4.540 -1.303 1972 11 NaN NaN NaN NaN NaN NaN -1.765 1.308 1972 12 NaN NaN NaN NaN NaN NaN -13.406 -4.076 1973 1 NaN NaN NaN NaN NaN NaN -9.173 4.417 1973 2 NaN NaN NaN NaN NaN NaN -6.336 2.541 1973 3 NaN NaN NaN NaN NaN NaN 0.947 5.044 1973 4 NaN NaN NaN NaN NaN NaN 3.163 -1.031 1973 5 NaN NaN NaN NaN NaN NaN 12.014 1.046 1973 6 NaN NaN NaN NaN NaN NaN 15.528 0.106 1973 7 NaN NaN NaN NaN NaN NaN 19.616 0.628 1973 8 NaN NaN NaN NaN NaN NaN 19.806 1.762