% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 37516 % Primary Name: HOLSTEIN RANGER STATION % Record Type: TAVG % Country: United States % State: UT % Latitude: 41.95000 +/- 0.00500 % Longitude: -113.45000 +/- 0.00500 % Elevation (m): 1981.20 +/- 0.15 % # of Months: 11 % % Alternate Names: HOLSTEIN RS % Missing Station ID - 424035 % % IDs: coop - 424035 % ghcnd - USC00424035 % ncdc - 12005540 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: d6576cc95e38b715a963cf3e4147ac3c % Raw Data Hash: b603c07bc0c0e9e037350111dd88bb3b % Adj Data Hash: 456ff88842cae3d0427798c28d3c4c79 % % 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 1915 7 NaN NaN NaN NaN NaN NaN 19.302 -1.608 1915 8 NaN NaN NaN NaN NaN NaN 21.202 1.490 1915 9 NaN NaN NaN NaN NaN NaN 12.847 -1.750 1915 10 NaN NaN NaN NaN NaN NaN 9.908 1.677 1915 11 NaN NaN NaN NaN NaN NaN 1.030 -0.219 1915 12 NaN NaN NaN NaN NaN NaN -3.291 0.109 1916 1 NaN NaN NaN NaN NaN NaN -7.265 -2.490 1916 2 NaN NaN NaN NaN NaN NaN -1.384 0.373 1916 3 NaN NaN NaN NaN NaN NaN 2.465 1.082 1916 4 NaN NaN NaN NaN NaN NaN 7.145 0.965 1916 5 NaN NaN NaN NaN NaN NaN 8.801 -2.630 1916 6 NaN NaN NaN NaN NaN NaN 13.865 -2.197 1916 7 18.762 -0.203 1 0 NaN NaN 20.385 -0.525 1916 8 16.215 -1.552 0 0 16.215 -1.552 18.541 -1.171 1916 9 12.470 -0.183 1 0 NaN NaN 14.172 -0.425 1916 10 4.127 -2.160 1 0 NaN NaN 6.858 -1.373 1916 11 NaN NaN NaN NaN NaN NaN -1.647 -2.895 1916 12 -6.611 -1.267 0 0 -6.611 -1.267 -5.943 -2.544 1917 1 NaN NaN NaN NaN NaN NaN -9.704 -4.929 1917 2 -3.500 0.202 1 0 NaN NaN -4.469 -2.712 1917 3 NaN NaN NaN NaN NaN NaN -5.063 -6.445 1917 4 0.782 -3.455 0 0 0.782 -3.455 3.093 -3.088 1917 5 NaN NaN NaN NaN NaN NaN 9.438 -1.993 1917 6 11.904 -2.214 1 0 NaN NaN 13.806 -2.256 1917 7 18.779 -0.186 1 0 NaN NaN 21.969 1.059 1917 8 16.717 -1.050 1 0 NaN NaN 19.002 -0.710 1917 9 12.675 0.022 0 0 12.675 0.022 15.148 0.551 1917 10 NaN NaN NaN NaN NaN NaN 9.281 1.049 1917 11 NaN NaN NaN NaN NaN NaN 3.791 2.543 1917 12 NaN NaN NaN NaN NaN NaN 2.433 5.832 1918 1 NaN NaN NaN NaN NaN NaN -1.843 2.932 1918 2 NaN NaN NaN NaN NaN NaN -2.267 -0.510 1918 3 NaN NaN NaN NaN NaN NaN 2.609 1.226 1918 4 NaN NaN NaN NaN NaN NaN 4.958 -1.222 1918 5 NaN NaN NaN NaN NaN NaN 10.056 -1.375 1918 6 NaN NaN NaN NaN NaN NaN 19.079 3.017 1918 7 NaN NaN NaN NaN NaN NaN 20.733 -0.177 1918 8 NaN NaN NaN NaN NaN NaN 17.275 -2.437 1918 9 NaN NaN NaN NaN NaN NaN 15.116 0.519