% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 31308 % Primary Name: CIMARRON 8 SE % Record Type: TAVG % Country: United States % State: NM % Latitude: 36.45000 +/- 0.00500 % Longitude: -104.80000 +/- 0.00500 % Elevation (m): 1891.00 +/- 0.05 % # of Months: 8 % % Alternate Names: CIMARRON 7 SE % % IDs: coop - 291819 % ghcnd - USC00291819 % ncdc - 20020807 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 920de5819612e2e687b09531f7681c44 % Raw Data Hash: 1bab95dd6d527326fa1a83864935ab5d % Adj Data Hash: 1bab95dd6d527326fa1a83864935ab5d % % 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 1903 5 NaN NaN NaN NaN NaN NaN 9.843 -1.567 1903 6 NaN NaN NaN NaN NaN NaN 13.567 -2.816 1903 7 NaN NaN NaN NaN NaN NaN 18.324 -0.397 1903 8 NaN NaN NaN NaN NaN NaN 17.736 0.197 1903 9 NaN NaN NaN NaN NaN NaN 13.223 -0.949 1903 10 NaN NaN NaN NaN NaN NaN 8.505 -0.293 1903 11 NaN NaN NaN NaN NaN NaN 3.873 1.398 1903 12 NaN NaN NaN NaN NaN NaN -1.603 -0.262 1904 1 NaN NaN NaN NaN NaN NaN -4.067 -1.734 1904 2 NaN NaN NaN NaN NaN NaN 2.035 2.583 1904 3 NaN NaN NaN NaN NaN NaN 4.031 1.787 1904 4 NaN NaN NaN NaN NaN NaN 7.016 0.545 1904 5 13.880 0.256 0 0 13.880 0.256 11.195 -0.215 1904 6 16.167 -2.431 0 0 16.167 -2.431 14.683 -1.700 1904 7 19.830 -1.105 0 0 19.830 -1.105 17.800 -0.920 1904 8 19.194 -0.559 0 0 19.194 -0.559 16.966 -0.573 1904 9 16.241 -0.145 0 0 16.241 -0.145 14.258 0.086 1904 10 10.251 -0.760 0 0 10.251 -0.760 8.210 -0.588 1904 11 5.954 1.265 0 0 5.954 1.265 3.346 0.871 1904 12 0.941 0.068 0 0 0.941 0.068 -1.713 -0.372 1905 1 NaN NaN NaN NaN NaN NaN -2.817 -0.483 1905 2 NaN NaN NaN NaN NaN NaN -2.739 -2.191 1905 3 NaN NaN NaN NaN NaN NaN 3.778 1.534 1905 4 NaN NaN NaN NaN NaN NaN 5.239 -1.232 1905 5 NaN NaN NaN NaN NaN NaN 10.574 -0.836 1905 6 NaN NaN NaN NaN NaN NaN 16.527 0.144 1905 7 NaN NaN NaN NaN NaN NaN 16.999 -1.721 1905 8 NaN NaN NaN NaN NaN NaN 17.668 0.129 1905 9 NaN NaN NaN NaN NaN NaN 14.292 0.121 1905 10 NaN NaN NaN NaN NaN NaN 7.934 -0.863 1905 11 NaN NaN NaN NaN NaN NaN 3.047 0.572 1905 12 NaN NaN NaN NaN NaN NaN -3.825 -2.485