% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 28312 % Primary Name: HAGERMAN 10 ESE % Record Type: TAVG % Country: United States % State: NM % Latitude: 33.08752 +/- 0.00005 % Longitude: -104.16170 +/- 0.00005 % Elevation (m): 1082.65 +/- 0.15 % # of Months: 39 % % IDs: coop - 293793 % ghcnd - USW00053015 % gsod - 999999-53015 % icao - 025E % ncdc - 30015638 % nws - HRMN5 % wban - 53015 % % Sources: Global Historical Climatology Network - Daily % Global Summary of the Day % Multi-network Metadata System % % Site Hash: 210c0f517011b2f54153a23ee59f1e41 % Raw Data Hash: fda54b40ec23f1b736a4a3e8d4a38dcf % Adj Data Hash: fe304130eb6abb1bb893504460919d39 % % 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 2009 9 NaN NaN NaN NaN NaN NaN 20.447 -0.754 2009 10 NaN NaN NaN NaN NaN NaN 14.766 -0.444 2009 11 NaN NaN NaN NaN NaN NaN 9.787 1.272 2009 12 NaN NaN NaN NaN NaN NaN 2.533 -2.169 2010 1 NaN NaN NaN NaN NaN NaN 3.345 -0.761 2010 2 NaN NaN NaN NaN NaN NaN 4.665 -1.774 2010 3 NaN NaN NaN NaN NaN NaN 9.286 -0.874 2010 4 NaN NaN NaN NaN NaN NaN 15.334 0.323 2010 5 NaN NaN NaN NaN NaN NaN 19.238 -0.573 2010 6 NaN NaN NaN NaN NaN NaN 26.843 2.186 2010 7 NaN NaN NaN NaN NaN NaN 24.591 -1.343 2010 8 NaN NaN NaN NaN NaN NaN 25.805 0.946 2010 9 24.167 2.267 1 0 NaN NaN 22.963 1.763 2010 10 17.211 1.301 0 0 17.211 1.301 16.607 1.396 2010 11 8.807 -0.408 0 0 8.807 -0.408 8.752 0.237 2010 12 6.726 1.324 0 0 6.726 1.324 6.981 2.279 2011 1 3.974 -0.831 0 0 3.974 -0.831 3.970 -0.136 2011 2 4.855 -2.283 0 0 4.855 -2.283 4.529 -1.910 2011 3 14.884 4.023 0 0 14.884 4.023 13.523 3.362 2011 4 18.913 3.203 0 0 18.913 3.203 18.094 3.084 2011 5 20.353 -0.157 0 0 20.353 -0.157 19.700 -0.111 2011 6 28.550 3.193 0 0 28.550 3.193 27.867 3.210 2011 7 29.763 3.130 0 0 29.763 3.130 28.204 2.271 2011 8 29.969 4.411 0 0 29.969 4.411 28.662 3.803 2011 9 22.568 0.668 0 0 22.568 0.668 22.208 1.007 2011 10 17.069 1.159 0 0 17.069 1.159 16.423 1.213 2011 11 9.850 0.635 0 0 9.850 0.635 9.447 0.932 2011 12 1.660 -3.742 0 0 1.660 -3.742 1.793 -2.909 2012 1 6.276 1.471 0 0 6.276 1.471 6.401 2.295 2012 2 6.469 -0.670 1 0 NaN NaN 6.008 -0.431 2012 3 13.508 2.648 0 0 13.508 2.648 12.596 2.435 2012 4 18.808 3.098 0 0 18.808 3.098 18.066 3.055 2012 5 21.665 1.154 0 0 21.665 1.154 20.622 0.811 2012 6 28.317 2.960 0 0 28.317 2.960 27.217 2.560 2012 7 27.674 1.041 0 0 27.674 1.041 26.236 0.303 2012 8 27.473 1.914 0 0 27.473 1.914 26.607 1.748 2012 9 22.630 0.730 0 0 22.630 0.730 21.948 0.748 2012 10 16.574 0.664 0 0 16.574 0.664 16.004 0.794 2012 11 11.427 2.212 0 0 11.427 2.212 11.062 2.547 2012 12 5.284 -0.118 0 0 5.284 -0.118 5.677 0.975 2013 1 4.392 -0.413 0 0 4.392 -0.413 3.885 -0.220 2013 2 6.827 -0.312 0 0 6.827 -0.312 6.101 -0.338 2013 3 11.955 1.095 0 0 11.955 1.095 11.310 1.149 2013 4 15.980 0.270 0 0 15.980 0.270 15.179 0.169 2013 5 21.392 0.881 0 0 21.392 0.881 20.245 0.434 2013 6 28.080 2.723 0 0 28.080 2.723 27.331 2.673 2013 7 26.590 -0.043 0 0 26.590 -0.043 25.073 -0.861 2013 8 27.624 2.066 0 0 27.624 2.066 26.122 1.262 2013 9 23.165 1.265 0 0 23.165 1.265 22.017 0.817 2013 10 15.821 -0.089 0 0 15.821 -0.089 14.972 -0.238 2013 11 13.460 4.245 1 0 NaN NaN NaN NaN