% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39241 % Primary Name: BILL 18 NNW % Record Type: TAVG % Country: United States % State: WY % Latitude: 43.46670 +/- 0.00005 % Longitude: -105.43330 +/- 0.00005 % Elevation (m): 1414.90 +/- 0.05 % # of Months: 13 % % IDs: coop - 480737 % ghcnd - USC00480737 % ncdc - 20022859 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: a14fe969f93a7c6f515d43ac06b36471 % Raw Data Hash: 6f2e84ea587b9a75561acdae925898d3 % Adj Data Hash: 0eb81c8c8c1e70a6541a64d494b01bc0 % % 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 1960 9 NaN NaN NaN NaN NaN NaN 15.315 0.785 1960 10 NaN NaN NaN NaN NaN NaN 9.459 1.416 1960 11 NaN NaN NaN NaN NaN NaN 0.331 0.537 1960 12 NaN NaN NaN NaN NaN NaN -4.248 0.780 1961 1 NaN NaN NaN NaN NaN NaN -5.498 2.107 1961 2 NaN NaN NaN NaN NaN NaN -0.748 3.380 1961 3 NaN NaN NaN NaN NaN NaN 1.749 2.296 1961 4 NaN NaN NaN NaN NaN NaN 4.075 -1.430 1961 5 NaN NaN NaN NaN NaN NaN 11.765 0.184 1961 6 NaN NaN NaN NaN NaN NaN 19.592 2.538 1961 7 NaN NaN NaN NaN NaN NaN 22.106 0.528 1961 8 NaN NaN NaN NaN NaN NaN 23.010 2.432 1961 9 7.633 -8.025 1 0 NaN NaN 10.838 -3.692 1961 10 7.778 -1.395 0 0 7.778 -1.395 8.233 0.190 1961 11 -0.722 -1.645 0 0 -0.722 -1.645 -1.807 -1.601 1961 12 -5.500 -1.601 0 0 -5.500 -1.601 -6.854 -1.826 1962 1 -7.056 -0.580 0 0 -7.056 -0.580 -10.171 -2.567 1962 2 -2.500 0.499 0 0 -2.500 0.499 -4.185 -0.057 1962 3 -0.167 -0.748 0 0 -0.167 -0.748 -2.289 -1.741 1962 4 8.389 1.755 0 0 8.389 1.755 7.841 2.336 1962 5 12.944 0.234 0 0 12.944 0.234 12.403 0.822 1962 6 17.278 -0.906 0 0 17.278 -0.906 16.257 -0.798 1962 7 20.403 -2.304 1 0 NaN NaN 19.699 -1.879 1962 8 19.611 -2.095 0 0 19.611 -2.095 19.669 -0.909 1962 9 15.222 -0.436 0 0 15.222 -0.436 13.762 -0.767 1962 10 NaN NaN NaN NaN NaN NaN 11.068 3.025 1962 11 NaN NaN NaN NaN NaN NaN 2.976 3.182 1962 12 NaN NaN NaN NaN NaN NaN -2.705 2.323 1963 1 NaN NaN NaN NaN NaN NaN -12.896 -5.292 1963 2 NaN NaN NaN NaN NaN NaN -0.295 3.833 1963 3 NaN NaN NaN NaN NaN NaN 2.130 2.678 1963 4 NaN NaN NaN NaN NaN NaN 5.299 -0.206 1963 5 NaN NaN NaN NaN NaN NaN 12.464 0.883 1963 6 NaN NaN NaN NaN NaN NaN 17.392 0.338 1963 7 NaN NaN NaN NaN NaN NaN 22.292 0.714 1963 8 NaN NaN NaN NaN NaN NaN 21.785 1.207 1963 9 NaN NaN NaN NaN NaN NaN 17.432 2.902