% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 29335 % Primary Name: RED HILL 12 NW % Record Type: TAVG % Country: United States % State: NM % Latitude: 34.31670 +/- 0.00005 % Longitude: -109.03330 +/- 0.00005 % Elevation (m): 2084.80 +/- 0.05 % # of Months: 29 % % Alternate Names: Missing Station ID - 297297 % % IDs: coop - 297297 % ghcnd - USC00297297 % ncdc - 20020919 % nws - RDHN5 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 534cb02cf29e7336394f1912260bb37f % Raw Data Hash: 14d3d4b3a1f305a9070d3980080ca479 % Adj Data Hash: 242f959eb886f01f387c3f7fca2b0c4c % % 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 1991 4 NaN NaN NaN NaN NaN NaN 7.298 -0.599 1991 5 NaN NaN NaN NaN NaN NaN 12.057 -0.636 1991 6 NaN NaN NaN NaN NaN NaN 16.325 -1.675 1991 7 NaN NaN NaN NaN NaN NaN 20.535 -0.493 1991 8 NaN NaN NaN NaN NaN NaN 19.393 -0.188 1991 9 NaN NaN NaN NaN NaN NaN 16.438 0.266 1991 10 NaN NaN NaN NaN NaN NaN 11.020 0.929 1991 11 NaN NaN NaN NaN NaN NaN 3.253 -0.200 1991 12 NaN NaN NaN NaN NaN NaN -0.480 0.458 1992 1 NaN NaN NaN NaN NaN NaN -3.535 -2.144 1992 2 NaN NaN NaN NaN NaN NaN 2.016 1.127 1992 3 NaN NaN NaN NaN NaN NaN 4.433 0.568 1992 4 10.444 4.469 0 0 10.444 4.469 10.415 2.518 1992 5 12.722 1.951 0 0 12.722 1.951 12.809 0.116 1992 6 14.914 -1.165 1 0 NaN NaN 16.750 -1.251 1992 7 18.667 -0.440 0 0 18.667 -0.440 19.865 -1.164 1992 8 18.556 0.897 0 0 18.556 0.897 18.733 -0.847 1992 9 15.222 0.972 0 0 15.222 0.972 16.716 0.544 1992 10 9.944 1.775 0 0 9.944 1.775 11.618 1.528 1992 11 -0.944 -2.476 0 0 -0.944 -2.476 0.707 -2.747 1992 12 -5.080 -2.220 0 0 -5.080 -2.220 -2.745 -1.808 1993 1 -3.389 -0.076 0 0 -3.389 -0.076 0.978 2.369 1993 2 -2.439 -1.406 1 0 NaN NaN 1.630 0.741 1993 3 0.797 -1.146 1 0 NaN NaN 4.668 0.803 1993 4 5.025 -0.951 1 0 NaN NaN 8.533 0.636 1993 5 9.667 -1.105 0 0 9.667 -1.105 13.098 0.405 1993 6 13.722 -2.357 0 0 13.722 -2.357 17.528 -0.472 1993 7 17.385 -1.721 1 0 NaN NaN 20.709 -0.319 1993 8 16.111 -1.548 0 0 16.111 -1.548 19.049 -0.531 1993 9 NaN NaN NaN NaN NaN NaN 15.823 -0.349 1993 10 9.020 0.851 1 0 NaN NaN 9.752 -0.339 1993 11 0.722 -0.809 0 0 0.722 -0.809 2.575 -0.878 1993 12 -1.538 1.321 1 0 NaN NaN -0.575 0.362 1994 1 NaN NaN NaN NaN NaN NaN -0.359 1.032 1994 2 -3.124 -2.091 1 0 NaN NaN 0.378 -0.511 1994 3 -0.321 -2.265 1 0 NaN NaN 5.159 1.294 1994 4 4.688 -1.288 1 0 NaN NaN 8.460 0.563 1994 5 NaN NaN NaN NaN NaN NaN 12.632 -0.061 1994 6 15.855 -0.224 1 0 NaN NaN 20.157 2.156 1994 7 17.500 -1.607 1 0 NaN NaN 21.697 0.668 1994 8 16.186 -1.472 1 0 NaN NaN 20.880 1.300 1994 9 15.437 1.186 1 0 NaN NaN 16.700 0.527 1994 10 6.391 -1.778 1 0 NaN NaN 9.193 -0.898 1994 11 2.340 0.808 1 0 NaN NaN 2.631 -0.823 1994 12 NaN NaN NaN NaN NaN NaN 0.960 1.897 1995 1 NaN NaN NaN NaN NaN NaN -0.299 1.091 1995 2 NaN NaN NaN NaN NaN NaN 4.507 3.617 1995 3 NaN NaN NaN NaN NaN NaN 4.982 1.117 1995 4 NaN NaN NaN NaN NaN NaN 6.760 -1.137 1995 5 NaN NaN NaN NaN NaN NaN 10.790 -1.903 1995 6 NaN NaN NaN NaN NaN NaN 16.561 -1.440 1995 7 NaN NaN NaN NaN NaN NaN 20.912 -0.116 1995 8 NaN NaN NaN NaN NaN NaN 21.086 1.506 1995 9 NaN NaN NaN NaN NaN NaN 17.047 0.875 1995 10 NaN NaN NaN NaN NaN NaN 10.838 0.747 1995 11 NaN NaN NaN NaN NaN NaN 6.253 2.800