% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 27671 % Primary Name: CAMBRAY % Record Type: TAVG % Country: United States % State: NM % Latitude: 32.23330 +/- 0.00005 % Longitude: -107.33330 +/- 0.00005 % Elevation (m): 1289.90 +/- 0.05 % # of Months: 8 % % Alternate Names: Missing Station ID - 291309 % % IDs: coop - 291309 % ghcnd - USC00291309 % ncdc - 20020261 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 183db4e0a51471c74733b3139fd2f763 % Raw Data Hash: 39d2ef87a3df747ae2f6033cb7f5caf6 % Adj Data Hash: 39d2ef87a3df747ae2f6033cb7f5caf6 % % 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 1931 4 NaN NaN NaN NaN NaN NaN 15.467 -0.593 1931 5 NaN NaN NaN NaN NaN NaN 19.969 -0.729 1931 6 NaN NaN NaN NaN NaN NaN 25.831 0.007 1931 7 NaN NaN NaN NaN NaN NaN 26.668 -0.164 1931 8 NaN NaN NaN NaN NaN NaN 24.370 -1.085 1931 9 NaN NaN NaN NaN NaN NaN 24.215 1.590 1931 10 NaN NaN NaN NaN NaN NaN 18.515 1.572 1931 11 NaN NaN NaN NaN NaN NaN 10.214 -0.296 1931 12 NaN NaN NaN NaN NaN NaN 5.499 -0.965 1932 1 NaN NaN NaN NaN NaN NaN 4.754 -1.595 1932 2 NaN NaN NaN NaN NaN NaN 9.840 1.390 1932 3 NaN NaN NaN NaN NaN NaN 10.290 -1.523 1932 4 17.278 0.605 0 0 17.278 0.605 16.315 0.255 1932 5 NaN NaN NaN NaN NaN NaN 19.756 -0.942 1932 6 NaN NaN NaN NaN NaN NaN 25.260 -0.564 1932 7 NaN NaN NaN NaN NaN NaN 26.350 -0.482 1932 8 NaN NaN NaN NaN NaN NaN 25.412 -0.043 1932 9 NaN NaN NaN NaN NaN NaN 21.721 -0.904 1932 10 NaN NaN NaN NaN NaN NaN 16.060 -0.883 1932 11 NaN NaN NaN NaN NaN NaN 10.076 -0.434 1932 12 NaN NaN NaN NaN NaN NaN 5.471 -0.993 1933 1 5.333 -1.630 0 0 5.333 -1.630 5.776 -0.574 1933 2 6.889 -2.174 0 0 6.889 -2.174 6.432 -2.017 1933 3 12.778 0.352 0 0 12.778 0.352 12.725 0.913 1933 4 14.167 -2.507 0 0 14.167 -2.507 14.196 -1.864 1933 5 20.222 -1.089 0 0 20.222 -1.089 18.687 -2.011 1933 6 26.222 -0.215 0 0 26.222 -0.215 25.460 -0.364 1933 7 28.778 1.332 0 0 28.778 1.332 27.168 0.336 1933 8 NaN NaN NaN NaN NaN NaN 25.628 0.173 1933 9 NaN NaN NaN NaN NaN NaN 24.266 1.641 1933 10 NaN NaN NaN NaN NaN NaN 18.088 1.145 1933 11 NaN NaN NaN NaN NaN NaN 11.449 0.939 1933 12 NaN NaN NaN NaN NaN NaN 8.233 1.769 1934 1 NaN NaN NaN NaN NaN NaN 5.788 -0.562 1934 2 NaN NaN NaN NaN NaN NaN 9.986 1.536 1934 3 NaN NaN NaN NaN NaN NaN 12.930 1.117 1934 4 NaN NaN NaN NaN NaN NaN 17.919 1.859 1934 5 NaN NaN NaN NaN NaN NaN 22.359 1.661 1934 6 NaN NaN NaN NaN NaN NaN 26.070 0.246 1934 7 NaN NaN NaN NaN NaN NaN 27.393 0.560