% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39061 % Primary Name: RIVERTON 19 N % Record Type: TAVG % Country: United States % State: WY % Latitude: 43.30000 +/- 0.00005 % Longitude: -108.36670 +/- 0.00005 % Elevation (m): 1524.90 +/- 0.05 % # of Months: 19 % % Alternate Names: RIVERTON 20 N % % IDs: coop - 487780 % ghcnd - USC00487780 % ncdc - 20022840 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 0cc9cd58e28ac9292f5a8a075f036231 % Raw Data Hash: 745bcc6adbff440f08e7f6c798064cec % Adj Data Hash: 5a6a52b50c5615cd9405b85dc154d2c6 % % 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 1950 9 NaN NaN NaN NaN NaN NaN 10.217 -1.278 1950 10 NaN NaN NaN NaN NaN NaN 8.699 3.212 1950 11 NaN NaN NaN NaN NaN NaN -1.984 0.586 1950 12 NaN NaN NaN NaN NaN NaN -2.187 4.771 1951 1 NaN NaN NaN NaN NaN NaN -8.395 0.172 1951 2 NaN NaN NaN NaN NaN NaN -3.775 1.954 1951 3 NaN NaN NaN NaN NaN NaN -4.529 -1.948 1951 4 NaN NaN NaN NaN NaN NaN 2.321 -0.562 1951 5 NaN NaN NaN NaN NaN NaN 8.807 0.048 1951 6 NaN NaN NaN NaN NaN NaN 9.693 -3.976 1951 7 NaN NaN NaN NaN NaN NaN 17.504 -0.355 1951 8 NaN NaN NaN NaN NaN NaN 15.667 -0.989 1951 9 12.111 -2.199 0 0 12.111 -2.199 10.144 -1.351 1951 10 6.722 -1.580 0 0 6.722 -1.580 5.048 -0.440 1951 11 NaN NaN NaN NaN NaN NaN -4.133 -1.563 1951 12 NaN NaN NaN NaN NaN NaN -8.533 -1.575 1952 1 -10.333 -4.581 0 0 -10.333 -4.581 -9.184 -0.617 1952 2 -4.278 -1.363 0 0 -4.278 -1.363 -6.936 -1.206 1952 3 -2.833 -3.067 0 0 -2.833 -3.067 -6.614 -4.032 1952 4 NaN NaN NaN NaN NaN NaN 4.260 1.378 1952 5 11.667 0.093 0 0 11.667 0.093 9.241 0.482 1952 6 18.611 2.127 0 0 18.611 2.127 13.903 0.234 1952 7 21.389 0.715 0 0 21.389 0.715 17.280 -0.579 1952 8 20.373 0.903 1 0 NaN NaN 16.744 0.089 1952 9 15.500 1.190 0 0 15.500 1.190 13.287 1.791 1952 10 NaN NaN NaN NaN NaN NaN 8.217 2.730 1952 11 NaN NaN NaN NaN NaN NaN -5.508 -2.938 1952 12 -4.788 -0.645 1 0 NaN NaN -6.364 0.594 1953 1 -2.895 2.857 1 0 NaN NaN -1.984 6.583 1953 2 -4.722 -1.807 0 0 -4.722 -1.807 -4.771 0.959 1953 3 NaN NaN NaN NaN NaN NaN -1.359 1.222 1953 4 4.167 -1.531 0 1 4.167 -1.531 0.726 -2.156 1953 5 9.778 -1.796 0 0 9.778 -1.796 5.994 -2.766 1953 6 17.444 0.960 0 0 17.444 0.960 13.379 -0.291 1953 7 23.389 2.715 0 0 23.389 2.715 19.285 1.426 1953 8 20.611 1.141 0 0 20.611 1.141 16.705 0.050 1953 9 16.000 1.690 0 0 16.000 1.690 12.696 1.201 1953 10 NaN NaN NaN NaN NaN NaN 7.577 2.089 1953 11 NaN NaN NaN NaN NaN NaN 0.465 3.035 1953 12 NaN NaN NaN NaN NaN NaN -5.663 1.295 1954 1 NaN NaN NaN NaN NaN NaN -4.761 3.807 1954 2 NaN NaN NaN NaN NaN NaN -0.187 5.543 1954 3 NaN NaN NaN NaN NaN NaN -5.269 -2.688 1954 4 NaN NaN NaN NaN NaN NaN 4.678 1.796 1954 5 NaN NaN NaN NaN NaN NaN 9.427 0.668 1954 6 NaN NaN NaN NaN NaN NaN 12.618 -1.051 1954 7 NaN NaN NaN NaN NaN NaN 19.845 1.987 1954 8 NaN NaN NaN NaN NaN NaN 16.414 -0.242 1954 9 NaN NaN NaN NaN NaN NaN 12.504 1.009