% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 38829 % Primary Name: RIVERTON, WY. % Record Type: TAVG % Country: United States % State: WY % Latitude: 43.06925 +/- 0.00575 % Longitude: -108.46843 +/- 0.00893 % Elevation (m): 1691.22 +/- 7.27 % # of Months: 18 % % Alternate Names: RIVERTON % % IDs: ghcnm - 42572672000 % gsod - 726720-99999 % icao - KRIW % usaf - 726720 % wmo - 72672 % % Sources: Global Summary of the Day % Global Historical Climatology Network - Monthly v2 % World Meteorological Organization Metadata % % Site Hash: bb048cc006f2f8a3efb8bdc2141b631c % Raw Data Hash: d604f1430b62443b826a4be52a396629 % Adj Data Hash: b65c0e3de5877508780bcd9290479fe5 % % 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 2004 5 NaN NaN NaN NaN NaN NaN 8.848 0.088 2004 6 NaN NaN NaN NaN NaN NaN 12.629 -1.041 2004 7 NaN NaN NaN NaN NaN NaN 17.346 -0.513 2004 8 NaN NaN NaN NaN NaN NaN 15.069 -1.587 2004 9 NaN NaN NaN NaN NaN NaN 10.937 -0.558 2004 10 NaN NaN NaN NaN NaN NaN 6.389 0.901 2004 11 NaN NaN NaN NaN NaN NaN -2.115 0.455 2004 12 NaN NaN NaN NaN NaN NaN -4.480 2.478 2005 1 NaN NaN NaN NaN NaN NaN -4.611 3.957 2005 2 NaN NaN NaN NaN NaN NaN -3.754 1.976 2005 3 NaN NaN NaN NaN NaN NaN -1.475 1.106 2005 4 NaN NaN NaN NaN NaN NaN 3.473 0.590 2005 5 10.993 -0.030 1 0 NaN NaN 8.517 -0.242 2005 6 NaN NaN NaN NaN NaN NaN 12.180 -1.489 2005 7 24.718 4.595 1 0 NaN NaN 19.444 1.586 2005 8 22.379 3.459 1 0 NaN NaN 16.192 -0.464 2005 9 18.322 4.562 1 0 NaN NaN 11.558 0.063 2005 10 12.017 4.266 1 0 NaN NaN 7.443 1.955 2005 11 NaN NaN NaN NaN NaN NaN -0.889 1.681 2005 12 0.813 5.507 1 0 NaN NaN -6.975 -0.017 2006 1 -2.030 4.273 0 0 -2.030 4.273 -5.094 3.473 2006 2 -5.403 -1.937 0 0 -5.403 -1.937 -6.249 -0.519 2006 3 2.525 2.842 1 0 NaN NaN -2.801 -0.220 2006 4 NaN NaN NaN NaN NaN NaN 4.961 2.078 2006 5 NaN NaN NaN NaN NaN NaN 10.128 1.369 2006 6 NaN NaN NaN NaN NaN NaN 15.560 1.890 2006 7 26.083 5.960 1 0 NaN NaN 20.628 2.770 2006 8 21.446 2.527 0 0 21.446 2.527 16.874 0.218 2006 9 13.327 -0.432 0 0 13.327 -0.432 10.450 -1.045 2006 10 6.487 -1.264 0 0 6.487 -1.264 5.341 -0.146 2006 11 1.352 1.657 0 0 1.352 1.657 -1.587 0.983 2006 12 -4.337 0.357 0 0 -4.337 0.357 -5.577 1.381 2007 1 -9.604 -3.301 0 0 -9.604 -3.301 -9.778 -1.211 2007 2 -1.196 2.269 0 0 -1.196 2.269 -2.943 2.787 2007 3 5.742 6.059 0 0 5.742 6.059 1.706 4.287 2007 4 NaN NaN NaN NaN NaN NaN 4.210 1.327 2007 5 NaN NaN NaN NaN NaN NaN 9.851 1.092 2007 6 NaN NaN NaN NaN NaN NaN 15.230 1.560 2007 7 NaN NaN NaN NaN NaN NaN 20.959 3.101 2007 8 NaN NaN NaN NaN NaN NaN 18.078 1.422 2007 9 NaN NaN NaN NaN NaN NaN 11.948 0.453 2007 10 NaN NaN NaN NaN NaN NaN 6.948 1.460 2007 11 NaN NaN NaN NaN NaN NaN -0.393 2.176 2007 12 NaN NaN NaN NaN NaN NaN -9.037 -2.080 2008 1 NaN NaN NaN NaN NaN NaN -10.486 -1.919 2008 2 NaN NaN NaN NaN NaN NaN -5.062 0.668 2008 3 NaN NaN NaN NaN NaN NaN -4.052 -1.471