% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 29940 % Primary Name: RAMAH 9 SE % Record Type: TAVG % Country: United States % State: NM % Latitude: 35.04610 +/- 0.00005 % Longitude: -108.36360 +/- 0.00005 % Elevation (m): 2183.59 +/- 0.15 % # of Months: 39 % % IDs: coop - 297249 % ghcnd - USW00053009 % gsod - 999999-53009 % icao - E458 % ncdc - 30015633 % nws - RMHN5 % wban - 53009 % % Sources: Global Historical Climatology Network - Daily % Global Summary of the Day % Multi-network Metadata System % % Site Hash: 9a5d075a86288e6a328b685e3a65c18a % Raw Data Hash: 6547f237353c20c99c1f2346285a7a42 % Adj Data Hash: aa9bb807e68eb569513f73420f10c4d8 % % 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 16.353 0.181 2009 10 NaN NaN NaN NaN NaN NaN 9.560 -0.531 2009 11 NaN NaN NaN NaN NaN NaN 4.822 1.368 2009 12 NaN NaN NaN NaN NaN NaN -2.778 -1.841 2010 1 NaN NaN NaN NaN NaN NaN -1.529 -0.139 2010 2 NaN NaN NaN NaN NaN NaN -0.039 -0.928 2010 3 NaN NaN NaN NaN NaN NaN 3.395 -0.470 2010 4 NaN NaN NaN NaN NaN NaN 8.192 0.294 2010 5 NaN NaN NaN NaN NaN NaN 11.992 -0.701 2010 6 NaN NaN NaN NaN NaN NaN 18.870 0.869 2010 7 NaN NaN NaN NaN NaN NaN 21.816 0.788 2010 8 NaN NaN NaN NaN NaN NaN 19.832 0.252 2010 9 15.534 1.783 0 0 15.534 1.783 18.262 2.090 2010 10 9.381 1.711 0 0 9.381 1.711 11.662 1.571 2010 11 -0.573 -1.606 0 0 -0.573 -1.606 2.485 -0.969 2010 12 0.395 3.754 0 0 0.395 3.754 2.681 3.618 2011 1 -4.966 -1.154 0 0 -4.966 -1.154 -2.170 -0.779 2011 2 -3.432 -1.900 0 0 -3.432 -1.900 -0.761 -1.650 2011 3 4.092 2.648 0 0 4.092 2.648 6.085 2.220 2011 4 6.950 1.474 0 0 6.950 1.474 9.442 1.544 2011 5 8.821 -1.451 0 0 8.821 -1.451 11.479 -1.214 2011 6 15.647 0.067 0 0 15.647 0.067 18.959 0.958 2011 7 19.853 1.246 0 0 19.853 1.246 22.014 0.985 2011 8 19.744 2.584 0 0 19.744 2.584 21.431 1.851 2011 9 15.095 1.344 0 0 15.095 1.344 17.246 1.074 2011 10 8.015 0.345 0 0 8.015 0.345 10.567 0.476 2011 11 2.098 1.066 0 0 2.098 1.066 3.962 0.509 2011 12 -5.073 -1.714 0 0 -5.073 -1.714 -2.125 -1.188 2012 1 -0.237 3.575 0 0 -0.237 3.575 1.093 2.484 2012 2 0.086 1.618 1 0 NaN NaN 1.441 0.552 2012 3 2.818 1.374 0 0 2.818 1.374 4.771 0.906 2012 4 8.030 2.554 0 0 8.030 2.554 10.327 2.429 2012 5 12.052 1.780 0 0 12.052 1.780 14.450 1.756 2012 6 17.463 1.884 0 0 17.463 1.884 20.490 2.490 2012 7 19.926 1.318 0 0 19.926 1.318 21.614 0.585 2012 8 19.074 1.915 0 0 19.074 1.915 20.780 1.199 2012 9 14.998 1.247 0 0 14.998 1.247 17.176 1.003 2012 10 8.166 0.496 0 0 8.166 0.496 11.426 1.336 2012 11 2.382 1.349 0 0 2.382 1.349 5.485 2.032 2012 12 -3.187 0.171 0 0 -3.187 0.171 -0.256 0.682 2013 1 -6.616 -2.804 0 0 -6.616 -2.804 -3.405 -2.014 2013 2 -3.130 -1.598 0 0 -3.130 -1.598 -0.703 -1.592 2013 3 3.505 2.061 0 0 3.505 2.061 5.786 1.921 2013 4 5.888 0.412 0 0 5.888 0.412 8.943 1.046 2013 5 10.758 0.486 0 0 10.758 0.486 13.278 0.585 2013 6 17.488 1.909 0 0 17.488 1.909 20.408 2.407 2013 7 20.079 1.472 0 0 20.079 1.472 21.681 0.653 2013 8 18.495 1.336 0 0 18.495 1.336 19.689 0.108 2013 9 14.840 1.089 0 0 14.840 1.089 16.793 0.620 2013 10 6.181 -1.489 0 0 6.181 -1.489 9.091 -1.000 2013 11 3.680 2.648 1 0 NaN NaN NaN NaN