% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 30832 % Primary Name: SAN ANTONIO CREEK % Record Type: TAVG % Country: United States % State: NM % Latitude: 35.96670 +/- 0.00005 % Longitude: -106.48330 +/- 0.00005 % Elevation (m): 2590.80 +/- 0.15 % # of Months: 14 % % Alternate Names: Missing Station ID - 297804 % % IDs: coop - 297804 % ghcnd - USC00297804 % ncdc - 12003703 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: f0d1f3437f4ba6c60fadea07482472bc % Raw Data Hash: c75c1d93a11c9e84ed083ddbb2653dcd % Adj Data Hash: 8079a00f747469b2654a98ff2f4f76c4 % % 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 1948 7 NaN NaN NaN NaN NaN NaN 20.630 -0.138 1948 8 NaN NaN NaN NaN NaN NaN 19.338 -0.047 1948 9 NaN NaN NaN NaN NaN NaN 16.316 0.969 1948 10 NaN NaN NaN NaN NaN NaN 9.545 0.426 1948 11 NaN NaN NaN NaN NaN NaN -0.234 -2.319 1948 12 NaN NaN NaN NaN NaN NaN -1.743 1.234 1949 1 NaN NaN NaN NaN NaN NaN -5.885 -1.994 1949 2 NaN NaN NaN NaN NaN NaN -4.129 -2.910 1949 3 NaN NaN NaN NaN NaN NaN 2.403 -0.027 1949 4 NaN NaN NaN NaN NaN NaN 7.606 0.652 1949 5 NaN NaN NaN NaN NaN NaN 11.510 -0.580 1949 6 NaN NaN NaN NaN NaN NaN 16.455 -1.018 1949 7 13.637 -0.886 0 0 13.637 -0.886 20.422 -0.346 1949 8 12.543 -0.595 1 0 NaN NaN 18.877 -0.508 1949 9 9.652 0.552 0 0 9.652 0.552 16.795 1.449 1949 10 2.774 -0.098 0 0 2.774 -0.098 8.366 -0.753 1949 11 1.190 5.351 0 0 1.190 5.351 4.777 2.691 1949 12 -8.973 0.250 0 0 -8.973 0.250 -3.389 -0.412 1950 1 -9.198 0.939 0 0 -9.198 0.939 -2.864 1.027 1950 2 -6.309 1.156 0 0 -6.309 1.156 0.921 2.139 1950 3 -2.350 1.466 0 0 -2.350 1.466 2.470 0.039 1950 4 2.937 2.230 0 0 2.937 2.230 8.367 1.413 1950 5 4.721 -1.122 0 0 4.721 -1.122 11.254 -0.835 1950 6 NaN NaN NaN NaN NaN NaN 17.505 0.032 1950 7 12.631 -1.892 0 0 12.631 -1.892 20.261 -0.508 1950 8 11.315 -1.823 0 0 11.315 -1.823 18.742 -0.643 1950 9 7.455 -1.645 0 0 7.455 -1.645 14.565 -0.782 1950 10 NaN NaN NaN NaN NaN NaN 13.040 3.921 1950 11 NaN NaN NaN NaN NaN NaN 3.907 1.822 1950 12 NaN NaN NaN NaN NaN NaN 0.546 3.523 1951 1 NaN NaN NaN NaN NaN NaN -2.753 1.138 1951 2 NaN NaN NaN NaN NaN NaN -1.114 0.104 1951 3 NaN NaN NaN NaN NaN NaN 1.838 -0.592 1951 4 NaN NaN NaN NaN NaN NaN 6.990 0.037 1951 5 NaN NaN NaN NaN NaN NaN 12.610 0.521 1951 6 NaN NaN NaN NaN NaN NaN 16.544 -0.929 1951 7 NaN NaN NaN NaN NaN NaN 22.589 1.821 1951 8 NaN NaN NaN NaN NaN NaN 19.745 0.360 1951 9 NaN NaN NaN NaN NaN NaN 15.843 0.496