% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 37152 % Primary Name: COLLEGE WARD UTAH STATE UNIV % Record Type: TAVG % Country: United States % State: UT % Latitude: 41.66670 +/- 0.00005 % Longitude: -111.90000 +/- 0.00005 % Elevation (m): 1368.90 +/- 0.05 % # of Months: 16 % % Alternate Names: CLG WARD UTAH ST UNIV % COLLEGE WARD UTAH ST % % IDs: coop - 421601 % ghcnd - USC00421601 % ncdc - 20026571 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: bfbeb1cfd97f37f938151ca9c97337f8 % Raw Data Hash: 45d2fd61db879a81eec64df730c1fb86 % Adj Data Hash: 45d2fd61db879a81eec64df730c1fb86 % % 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 1967 1 NaN NaN NaN NaN NaN NaN -0.533 1.632 1967 2 NaN NaN NaN NaN NaN NaN 2.518 1.876 1967 3 NaN NaN NaN NaN NaN NaN 5.232 1.221 1967 4 NaN NaN NaN NaN NaN NaN 6.136 -2.499 1967 5 NaN NaN NaN NaN NaN NaN 13.389 -0.847 1967 6 NaN NaN NaN NaN NaN NaN 16.684 -2.683 1967 7 NaN NaN NaN NaN NaN NaN 25.292 0.823 1967 8 NaN NaN NaN NaN NaN NaN 24.735 1.589 1967 9 NaN NaN NaN NaN NaN NaN 18.870 1.082 1967 10 NaN NaN NaN NaN NaN NaN 11.793 0.813 1967 11 NaN NaN NaN NaN NaN NaN 5.671 1.958 1967 12 NaN NaN NaN NaN NaN NaN -3.792 -2.603 1968 1 -7.556 -2.341 0 0 -7.556 -2.341 -3.156 -0.992 1968 2 -3.222 -0.814 0 0 -3.222 -0.814 3.429 2.787 1968 3 4.000 3.039 0 0 4.000 3.039 5.450 1.439 1968 4 5.056 -0.529 0 0 5.056 -0.529 6.253 -2.381 1968 5 11.167 -0.019 0 0 11.167 -0.019 13.398 -0.838 1968 6 16.000 -0.318 0 0 16.000 -0.318 18.719 -0.648 1968 7 21.556 0.135 0 0 21.556 0.135 25.126 0.656 1968 8 18.000 -2.096 0 0 18.000 -2.096 19.999 -3.147 1968 9 13.500 -1.239 0 0 13.500 -1.239 16.470 -1.318 1968 10 8.389 0.458 0 0 8.389 0.458 11.066 0.086 1968 11 0.833 0.170 0 0 0.833 0.170 3.365 -0.348 1968 12 -4.500 -0.261 0 0 -4.500 -0.261 -2.037 -0.848 1969 1 -2.667 2.548 0 0 -2.667 2.548 0.642 2.807 1969 2 -5.389 -2.981 0 0 -5.389 -2.981 -0.370 -1.012 1969 3 -3.722 -4.683 0 0 -3.722 -4.683 1.223 -2.788 1969 4 8.278 2.693 0 0 8.278 2.693 8.940 0.306 1969 5 NaN NaN NaN NaN NaN NaN 17.407 3.171 1969 6 NaN NaN NaN NaN NaN NaN 17.223 -2.144 1969 7 NaN NaN NaN NaN NaN NaN 24.672 0.202 1969 8 NaN NaN NaN NaN NaN NaN 24.803 1.657 1969 9 NaN NaN NaN NaN NaN NaN 19.883 2.094 1969 10 NaN NaN NaN NaN NaN NaN 8.452 -2.528 1969 11 NaN NaN NaN NaN NaN NaN 3.655 -0.058 1969 12 NaN NaN NaN NaN NaN NaN -0.014 1.175 1970 1 NaN NaN NaN NaN NaN NaN 0.502 2.667 1970 2 NaN NaN NaN NaN NaN NaN 4.359 3.717 1970 3 NaN NaN NaN NaN NaN NaN 3.008 -1.003 1970 4 NaN NaN NaN NaN NaN NaN 5.282 -3.352