% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 26608 % Primary Name: ROCKSPRINGS 5 W % Record Type: TAVG % Country: United States % State: TX % Latitude: 30.01670 +/- 0.00005 % Longitude: -100.30000 +/- 0.00005 % Elevation (m): 729.10 +/- 0.05 % # of Months: 15 % % IDs: coop - 417711 % ghcnd - USC00417711 % ncdc - 20024584 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 775fb8542644420dd0c788eb14bcb1b2 % Raw Data Hash: 182947a9b138d4a9401e77840363fab1 % Adj Data Hash: 0fc196cb5eb9affe570b7b64d94f625b % % 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 1954 2 NaN NaN NaN NaN NaN NaN 14.122 2.919 1954 3 NaN NaN NaN NaN NaN NaN 15.358 -0.099 1954 4 NaN NaN NaN NaN NaN NaN 22.032 2.221 1954 5 NaN NaN NaN NaN NaN NaN 22.647 -0.653 1954 6 NaN NaN NaN NaN NaN NaN 27.528 0.733 1954 7 NaN NaN NaN NaN NaN NaN 28.742 0.556 1954 8 NaN NaN NaN NaN NaN NaN 28.996 1.149 1954 9 NaN NaN NaN NaN NaN NaN 27.037 1.939 1954 10 NaN NaN NaN NaN NaN NaN 21.116 1.364 1954 11 NaN NaN NaN NaN NaN NaN 13.894 0.040 1954 12 NaN NaN NaN NaN NaN NaN 12.511 2.494 1955 1 NaN NaN NaN NaN NaN NaN 9.462 0.544 1955 2 9.389 0.265 0 0 9.389 0.265 11.334 0.131 1955 3 14.778 1.400 0 0 14.778 1.400 16.518 1.060 1955 4 20.278 2.547 0 0 20.278 2.547 22.398 2.588 1955 5 22.944 1.724 0 0 22.944 1.724 24.552 1.253 1955 6 25.111 0.395 0 0 25.111 0.395 26.873 0.077 1955 7 25.889 -0.218 0 0 25.889 -0.218 27.901 -0.285 1955 8 26.333 0.566 0 0 26.333 0.566 27.990 0.143 1955 9 24.222 1.204 0 0 24.222 1.204 26.298 1.200 1955 10 17.833 0.160 0 0 17.833 0.160 19.791 0.039 1955 11 12.056 0.281 0 0 12.056 0.281 13.743 -0.111 1955 12 9.056 1.118 0 0 9.056 1.118 10.741 0.725 1956 1 7.167 0.328 0 0 7.167 0.328 9.335 0.417 1956 2 9.000 -0.124 0 0 9.000 -0.124 11.888 0.685 1956 3 12.500 -0.878 0 0 12.500 -0.878 16.302 0.845 1956 4 NaN NaN NaN NaN NaN NaN 20.133 0.323 1956 5 NaN NaN NaN NaN NaN NaN 25.050 1.751 1956 6 27.375 2.659 1 0 NaN NaN 28.780 1.984 1956 7 NaN NaN NaN NaN NaN NaN 28.755 0.569 1956 8 NaN NaN NaN NaN NaN NaN 28.750 0.903 1956 9 NaN NaN NaN NaN NaN NaN 25.753 0.655 1956 10 NaN NaN NaN NaN NaN NaN 21.713 1.961 1956 11 NaN NaN NaN NaN NaN NaN 13.011 -0.843 1956 12 NaN NaN NaN NaN NaN NaN 11.797 1.780 1957 1 NaN NaN NaN NaN NaN NaN 10.465 1.546 1957 2 NaN NaN NaN NaN NaN NaN 15.480 4.277 1957 3 NaN NaN NaN NaN NaN NaN 15.653 0.195 1957 4 NaN NaN NaN NaN NaN NaN 18.323 -1.488 1957 5 NaN NaN NaN NaN NaN NaN 21.842 -1.458 1957 6 NaN NaN NaN NaN NaN NaN 26.310 -0.486