% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 34201 % Primary Name: COLLBRAN 3 ENE % Record Type: TAVG % Country: United States % State: CO % Latitude: 39.25000 +/- 0.00005 % Longitude: -107.93330 +/- 0.00005 % Elevation (m): 1969.90 +/- 0.05 % # of Months: 24 % % IDs: coop - 51745 % ghcnd - USC00051745 % ncdc - 20003676 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: a30126d37a59e4ae58417478111daf58 % Raw Data Hash: ba6ddbc3718ba3344d58a2a1a4d3f08f % Adj Data Hash: d3b93cff72b18cb19c7f84585378a70f % % 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 1967 1 NaN NaN NaN NaN NaN NaN -6.187 0.191 1967 2 NaN NaN NaN NaN NaN NaN -1.579 1.176 1967 3 NaN NaN NaN NaN NaN NaN 3.879 2.452 1967 4 NaN NaN NaN NaN NaN NaN 6.133 -0.332 1967 5 NaN NaN NaN NaN NaN NaN 10.889 -1.208 1967 6 NaN NaN NaN NaN NaN NaN 15.174 -2.209 1967 7 NaN NaN NaN NaN NaN NaN 21.062 -0.008 1967 8 NaN NaN NaN NaN NaN NaN 19.565 0.086 1967 9 NaN NaN NaN NaN NaN NaN 15.309 0.544 1967 10 NaN NaN NaN NaN NaN NaN 9.386 1.113 1967 11 NaN NaN NaN NaN NaN NaN 1.900 1.378 1967 12 NaN NaN NaN NaN NaN NaN -8.362 -3.116 1968 1 -3.167 2.418 0 0 -3.167 2.418 -9.170 -2.793 1968 2 0.000 1.963 0 0 0.000 1.963 -1.014 1.742 1968 3 2.944 0.724 0 0 2.944 0.724 1.823 0.395 1968 4 4.333 -2.924 0 0 4.333 -2.924 3.626 -2.838 1968 5 10.722 -2.167 0 0 10.722 -2.167 10.693 -1.404 1968 6 16.889 -1.287 0 0 16.889 -1.287 17.362 -0.020 1968 7 19.667 -2.196 0 0 19.667 -2.196 20.622 -0.448 1968 8 16.722 -3.550 0 0 16.722 -3.550 16.819 -2.660 1968 9 13.500 -2.057 0 0 13.500 -2.057 13.360 -1.405 1968 10 8.611 -0.454 0 0 8.611 -0.454 8.817 0.545 1968 11 1.778 0.463 0 0 1.778 0.463 -0.138 -0.660 1968 12 -4.167 0.286 0 0 -4.167 0.286 -6.783 -1.538 1969 1 -2.556 3.029 0 0 -2.556 3.029 -3.683 2.695 1969 2 -2.889 -0.926 0 0 -2.889 -0.926 -2.827 -0.072 1969 3 0.167 -2.053 0 0 0.167 -2.053 -1.337 -2.765 1969 4 9.111 1.854 0 0 9.111 1.854 7.704 1.239 1969 5 14.778 1.888 0 0 14.778 1.888 14.317 2.220 1969 6 15.444 -2.731 0 0 15.444 -2.731 15.198 -2.185 1969 7 20.722 -1.141 0 0 20.722 -1.141 21.383 0.313 1969 8 21.111 0.839 0 0 21.111 0.839 20.985 1.506 1969 9 16.222 0.665 0 0 16.222 0.665 15.750 0.985 1969 10 5.500 -3.565 0 0 5.500 -3.565 5.015 -3.258 1969 11 NaN NaN NaN NaN NaN NaN 0.003 -0.519 1969 12 -1.722 2.731 0 0 -1.722 2.731 -3.106 2.140 1970 1 -3.889 1.696 0 0 -3.889 1.696 -4.607 1.771 1970 2 NaN NaN NaN NaN NaN NaN 0.886 3.641 1970 3 NaN NaN NaN NaN NaN NaN -0.207 -1.634 1970 4 NaN NaN NaN NaN NaN NaN 3.155 -3.310 1970 5 NaN NaN NaN NaN NaN NaN 12.615 0.518 1970 6 NaN NaN NaN NaN NaN NaN 16.535 -0.847 1970 7 NaN NaN NaN NaN NaN NaN 21.081 0.011 1970 8 NaN NaN NaN NaN NaN NaN 20.693 1.213 1970 9 NaN NaN NaN NaN NaN NaN 13.305 -1.460 1970 10 NaN NaN NaN NaN NaN NaN 5.612 -2.660 1970 11 NaN NaN NaN NaN NaN NaN 1.450 0.928 1970 12 NaN NaN NaN NaN NaN NaN -3.625 1.621 1971 1 NaN NaN NaN NaN NaN NaN -4.825 1.553