% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 29992 % Primary Name: NETHERWOOD PARK % Record Type: TAVG % Country: United States % State: NM % Latitude: 35.10000 +/- 0.00005 % Longitude: -106.61670 +/- 0.00005 % Elevation (m): 1565.10 +/- 0.05 % # of Months: 40 % % IDs: coop - 296079 % ghcnd - USC00296079 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % % Site Hash: 700967cc2269729a7e46bb5a9b7c085b % Raw Data Hash: fac5cc7749733c22011388581aae0488 % Adj Data Hash: fac5cc7749733c22011388581aae0488 % % 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 1953 1 NaN NaN NaN NaN NaN NaN 3.576 3.692 1953 2 NaN NaN NaN NaN NaN NaN 0.933 -1.457 1953 3 NaN NaN NaN NaN NaN NaN 6.774 0.786 1953 4 NaN NaN NaN NaN NaN NaN 10.075 -0.363 1953 5 NaN NaN NaN NaN NaN NaN 12.849 -2.571 1953 6 NaN NaN NaN NaN NaN NaN 21.875 1.159 1953 7 NaN NaN NaN NaN NaN NaN 23.703 0.558 1953 8 NaN NaN NaN NaN NaN NaN 21.480 -0.190 1953 9 NaN NaN NaN NaN NaN NaN 18.568 0.700 1953 10 NaN NaN NaN NaN NaN NaN 11.549 0.019 1953 11 NaN NaN NaN NaN NaN NaN 5.158 0.577 1953 12 NaN NaN NaN NaN NaN NaN -1.784 -1.935 1954 1 3.000 0.981 0 0 3.000 0.981 1.457 1.574 1954 2 7.278 2.753 0 0 7.278 2.753 5.163 2.774 1954 3 7.389 -0.735 0 0 7.389 -0.735 5.342 -0.646 1954 4 16.222 3.649 0 0 16.222 3.649 13.422 2.984 1954 5 19.000 1.444 0 0 19.000 1.444 16.022 0.601 1954 6 23.778 0.926 0 0 23.778 0.926 21.088 0.372 1954 7 27.111 1.831 0 0 27.111 1.831 24.220 1.075 1954 8 24.111 0.305 0 0 24.111 0.305 21.356 -0.315 1954 9 21.778 1.774 0 0 21.778 1.774 19.443 1.575 1954 10 15.222 1.557 0 0 15.222 1.557 13.479 1.949 1954 11 8.222 1.507 0 0 8.222 1.507 6.330 1.750 1954 12 1.444 -0.843 0 0 1.444 -0.843 0.395 0.243 1955 1 0.167 -1.853 0 0 0.167 -1.853 -1.131 -1.014 1955 2 0.944 -3.581 0 0 0.944 -3.581 -0.644 -3.034 1955 3 8.000 -0.123 0 0 8.000 -0.123 5.805 -0.183 1955 4 12.056 -0.518 0 0 12.056 -0.518 9.807 -0.631 1955 5 17.167 -0.390 0 0 17.167 -0.390 14.478 -0.943 1955 6 22.444 -0.407 0 0 22.444 -0.407 19.997 -0.718 1955 7 24.889 -0.391 0 0 24.889 -0.391 22.206 -0.938 1955 8 24.222 0.416 0 0 24.222 0.416 21.930 0.260 1955 9 21.389 1.386 0 0 21.389 1.386 19.144 1.276 1955 10 14.944 1.279 0 0 14.944 1.279 13.121 1.592 1955 11 6.500 -0.216 0 0 6.500 -0.216 5.196 0.616 1955 12 3.667 1.379 0 0 3.667 1.379 2.474 2.322 1956 1 4.333 2.314 0 0 4.333 2.314 3.157 3.273 1956 2 2.056 -2.470 0 0 2.056 -2.470 -0.395 -2.785 1956 3 8.889 0.765 0 0 8.889 0.765 6.494 0.506 1956 4 12.278 -0.296 0 0 12.278 -0.296 9.724 -0.714 1956 5 19.667 2.110 0 0 19.667 2.110 16.580 1.159 1956 6 25.167 2.315 0 0 25.167 2.315 22.728 2.013 1956 7 25.167 -0.113 0 0 25.167 -0.113 22.788 -0.356 1956 8 23.889 0.083 0 0 23.889 0.083 21.101 -0.570 1956 9 21.889 1.886 0 0 21.889 1.886 19.545 1.678 1956 10 14.333 0.668 0 0 14.333 0.668 12.504 0.974 1956 11 3.833 -2.882 0 0 3.833 -2.882 2.111 -2.469 1956 12 1.222 -1.065 0 0 1.222 -1.065 -0.110 -0.262 1957 1 3.889 1.870 0 0 3.889 1.870 2.477 2.593 1957 2 8.389 3.864 0 0 8.389 3.864 6.652 4.262 1957 3 8.611 0.488 0 0 8.611 0.488 6.181 0.193 1957 4 12.333 -0.240 0 0 12.333 -0.240 9.831 -0.607 1957 5 NaN NaN NaN NaN NaN NaN 13.553 -1.868 1957 6 NaN NaN NaN NaN NaN NaN 20.907 0.191 1957 7 NaN NaN NaN NaN NaN NaN 23.619 0.475 1957 8 NaN NaN NaN NaN NaN NaN 21.154 -0.517 1957 9 NaN NaN NaN NaN NaN NaN 17.546 -0.322 1957 10 NaN NaN NaN NaN NaN NaN 11.008 -0.522 1957 11 NaN NaN NaN NaN NaN NaN 2.542 -2.038 1957 12 NaN NaN NaN NaN NaN NaN 1.824 1.672 1958 1 NaN NaN NaN NaN NaN NaN -0.386 -0.269 1958 2 NaN NaN NaN NaN NaN NaN 4.036 1.646 1958 3 NaN NaN NaN NaN NaN NaN 3.345 -2.643 1958 4 NaN NaN NaN NaN NaN NaN 9.333 -1.105