% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 32644 % Primary Name: BAKER RANGER STATION % Record Type: TAVG % Country: United States % State: UT % Latitude: 37.86670 +/- 0.00005 % Longitude: -109.36670 +/- 0.00005 % Elevation (m): 2148.84 +/- 0.15 % # of Months: 22 % % Alternate Names: Missing Station ID - 420400 % % IDs: coop - 420400 % ghcnd - USC00420400 % ncdc - 12005479 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 04a9a6cd0426d1517d064d90e26dc974 % Raw Data Hash: 86bc0fbe54e750150b056664a8c02af0 % Adj Data Hash: 4c6232346f9d213ac39e0ccf417e7b1b % % 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 1923 1 NaN NaN NaN NaN NaN NaN 1.253 3.406 1923 2 NaN NaN NaN NaN NaN NaN 0.052 -0.986 1923 3 NaN NaN NaN NaN NaN NaN 1.903 -2.639 1923 4 NaN NaN NaN NaN NaN NaN 8.374 -0.903 1923 5 NaN NaN NaN NaN NaN NaN 15.062 0.157 1923 6 NaN NaN NaN NaN NaN NaN 18.794 -1.615 1923 7 NaN NaN NaN NaN NaN NaN 24.498 0.386 1923 8 NaN NaN NaN NaN NaN NaN 21.260 -1.386 1923 9 NaN NaN NaN NaN NaN NaN 16.733 -1.430 1923 10 NaN NaN NaN NaN NaN NaN 10.017 -1.566 1923 11 NaN NaN NaN NaN NaN NaN 4.937 0.783 1923 12 NaN NaN NaN NaN NaN NaN -0.822 0.269 1924 1 -6.827 -2.728 0 0 -6.827 -2.728 -5.277 -3.124 1924 2 1.831 2.740 1 0 NaN NaN 3.043 2.005 1924 3 -1.352 -3.948 1 0 NaN NaN 1.529 -3.013 1924 4 5.005 -2.325 0 0 5.005 -2.325 8.491 -0.785 1924 5 9.787 -3.172 1 0 NaN NaN 15.193 0.288 1924 6 NaN NaN NaN NaN NaN NaN 20.980 0.571 1924 7 NaN NaN NaN NaN NaN NaN 23.779 -0.333 1924 8 17.309 -3.390 1 0 NaN NaN 22.457 -0.189 1924 9 14.035 -2.181 1 0 NaN NaN 17.406 -0.756 1924 10 NaN NaN NaN NaN NaN NaN 10.927 -0.655 1924 11 2.059 -0.148 0 0 2.059 -0.148 4.573 0.419 1924 12 -6.054 -3.017 1 0 NaN NaN -4.439 -3.349 1925 1 -5.647 -1.547 0 0 -5.647 -1.547 -6.528 -4.375 1925 2 -0.291 0.617 0 0 -0.291 0.617 1.975 0.937 1925 3 NaN NaN NaN NaN NaN NaN 5.363 0.821 1925 4 NaN NaN NaN NaN NaN NaN 10.508 1.231 1925 5 NaN NaN NaN NaN NaN NaN 17.014 2.109 1925 6 16.055 -2.407 1 0 NaN NaN 19.086 -1.323 1925 7 20.117 -2.049 1 0 NaN NaN 24.547 0.435 1925 8 17.642 -3.057 1 0 NaN NaN 21.257 -1.388 1925 9 12.115 -4.101 1 0 NaN NaN 17.290 -0.872 1925 10 9.235 -0.401 1 0 NaN NaN 11.124 -0.458 1925 11 NaN NaN NaN NaN NaN NaN 3.622 -0.532 1925 12 -0.746 2.291 1 0 NaN NaN 0.296 1.386 1926 1 -4.808 -0.709 0 0 -4.808 -0.709 -2.064 0.089 1926 2 -2.496 -1.587 1 0 NaN NaN 3.298 2.260 1926 3 NaN NaN NaN NaN NaN NaN 5.119 0.577 1926 4 11.019 3.689 1 0 NaN NaN 10.351 1.074 1926 5 15.179 2.221 1 0 NaN NaN 14.954 0.048 1926 6 22.717 4.254 1 0 NaN NaN 21.114 0.705 1926 7 NaN NaN NaN NaN NaN NaN 23.403 -0.709 1926 8 NaN NaN NaN NaN NaN NaN 23.184 0.539 1926 9 NaN NaN NaN NaN NaN NaN 18.280 0.117 1926 10 NaN NaN NaN NaN NaN NaN 13.054 1.471 1926 11 NaN NaN NaN NaN NaN NaN 6.069 1.915 1926 12 NaN NaN NaN NaN NaN NaN -1.680 -0.589 1927 1 NaN NaN NaN NaN NaN NaN 0.206 2.359 1927 2 NaN NaN NaN NaN NaN NaN 3.222 2.184 1927 3 NaN NaN NaN NaN NaN NaN 3.962 -0.581 1927 4 NaN NaN NaN NaN NaN NaN 9.645 0.369 1927 5 NaN NaN NaN NaN NaN NaN 15.070 0.164 1927 6 NaN NaN NaN NaN NaN NaN 19.672 -0.737