% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 31326 % Primary Name: MOUNT DORA % Record Type: TAVG % Country: United States % State: NM % Latitude: 36.46670 +/- 0.00005 % Longitude: -103.45000 +/- 0.00005 % Elevation (m): 1676.40 +/- 0.15 % # of Months: 13 % % Alternate Names: Missing Station ID - 295950 % % IDs: coop - 295950 % ghcnd - USC00295950 % ncdc - 12003653 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 72f32e514882ecccb4d6d86dc2858ab4 % Raw Data Hash: ed60c2a0bb27338c9f2019c622305f3b % Adj Data Hash: 350caadbd85232da90b101339ad64d6d % % 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 1910 5 NaN NaN NaN NaN NaN NaN 15.328 -0.957 1910 6 NaN NaN NaN NaN NaN NaN 22.298 0.645 1910 7 NaN NaN NaN NaN NaN NaN 24.667 0.721 1910 8 NaN NaN NaN NaN NaN NaN 22.672 -0.189 1910 9 NaN NaN NaN NaN NaN NaN 20.257 1.437 1910 10 NaN NaN NaN NaN NaN NaN 13.649 0.802 1910 11 NaN NaN NaN NaN NaN NaN 7.768 1.971 1910 12 NaN NaN NaN NaN NaN NaN 2.791 0.818 1911 1 NaN NaN NaN NaN NaN NaN 4.554 3.896 1911 2 NaN NaN NaN NaN NaN NaN 0.872 -1.937 1911 3 NaN NaN NaN NaN NaN NaN 7.583 1.662 1911 4 NaN NaN NaN NaN NaN NaN 11.784 0.715 1911 5 19.120 4.178 1 0 NaN NaN 16.767 0.482 1911 6 22.436 2.126 1 0 NaN NaN 22.922 1.269 1911 7 22.114 -0.489 0 0 22.114 -0.489 22.955 -0.991 1911 8 NaN NaN NaN NaN NaN NaN 22.948 0.087 1911 9 19.497 2.021 0 0 19.497 2.021 21.241 2.421 1911 10 NaN NaN NaN NaN NaN NaN 11.724 -1.122 1911 11 2.530 -1.923 1 0 NaN NaN 3.866 -1.931 1911 12 -4.316 -4.946 0 0 -4.316 -4.946 -2.883 -4.857 1912 1 NaN NaN NaN NaN NaN NaN -1.370 -2.028 1912 2 -0.748 -2.213 0 0 -0.748 -2.213 0.121 -2.688 1912 3 1.995 -2.582 1 0 NaN NaN 2.361 -3.560 1912 4 8.357 -1.368 1 0 NaN NaN 9.634 -1.435 1912 5 13.901 -1.040 0 0 13.901 -1.040 15.412 -0.874 1912 6 17.859 -2.451 1 0 NaN NaN 18.991 -2.663 1912 7 NaN NaN NaN NaN NaN NaN 23.483 -0.463 1912 8 20.644 -0.873 1 0 NaN NaN 22.397 -0.464 1912 9 14.372 -3.104 0 0 14.372 -3.104 16.036 -2.784 1912 10 NaN NaN NaN NaN NaN NaN 12.195 -0.652 1912 11 NaN NaN NaN NaN NaN NaN 5.753 -0.044 1912 12 NaN NaN NaN NaN NaN NaN 0.266 -1.708 1913 1 NaN NaN NaN NaN NaN NaN -0.859 -1.517 1913 2 NaN NaN NaN NaN NaN NaN -0.912 -3.720 1913 3 NaN NaN NaN NaN NaN NaN 4.348 -1.573 1913 4 NaN NaN NaN NaN NaN NaN 10.869 -0.200 1913 5 NaN NaN NaN NaN NaN NaN 17.198 0.913 1913 6 NaN NaN NaN NaN NaN NaN 19.946 -1.707 1913 7 NaN NaN NaN NaN NaN NaN 24.243 0.296 1913 8 NaN NaN NaN NaN NaN NaN 23.847 0.986 1913 9 NaN NaN NaN NaN NaN NaN 16.302 -2.518