% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 38989 % Primary Name: VIEWPOINT RANCH % Record Type: TAVG % Country: United States % State: OR % Latitude: 43.23330 +/- 0.00005 % Longitude: -120.51670 +/- 0.00005 % Elevation (m): 1330.10 +/- 0.05 % # of Months: 28 % % Alternate Names: VIEWPOINT RCH % % IDs: coop - 358895 % ghcnd - USC00358895 % ncdc - 20015901 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 539912838e7686ce18416b4bb1df6308 % Raw Data Hash: c914cd2a857c4754b069624bc7d3253a % Adj Data Hash: d3bc0b5d2a536111853497cccbac20de % % 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 1964 10 NaN NaN NaN NaN NaN NaN 10.312 2.290 1964 11 NaN NaN NaN NaN NaN NaN 1.244 -1.197 1964 12 NaN NaN NaN NaN NaN NaN -0.182 0.782 1965 1 NaN NaN NaN NaN NaN NaN -0.437 1.461 1965 2 NaN NaN NaN NaN NaN NaN 2.484 1.862 1965 3 NaN NaN NaN NaN NaN NaN 1.434 -0.490 1965 4 NaN NaN NaN NaN NaN NaN 6.025 0.816 1965 5 NaN NaN NaN NaN NaN NaN 8.575 -1.303 1965 6 NaN NaN NaN NaN NaN NaN 13.019 -1.163 1965 7 NaN NaN NaN NaN NaN NaN 17.832 -0.791 1965 8 NaN NaN NaN NaN NaN NaN 16.039 -1.465 1965 9 NaN NaN NaN NaN NaN NaN 10.890 -2.690 1965 10 9.787 1.349 1 0 NaN NaN 10.819 2.797 1965 11 3.667 0.811 0 0 3.667 0.811 3.586 1.144 1965 12 -1.500 -0.951 0 0 -1.500 -0.951 -1.930 -0.966 1966 1 -0.667 0.817 0 0 -0.667 0.817 -1.457 0.441 1966 2 -0.500 -1.537 0 0 -0.500 -1.537 -0.533 -1.155 1966 3 2.722 0.384 0 0 2.722 0.384 2.137 0.213 1966 4 7.833 2.210 0 0 7.833 2.210 6.264 1.056 1966 5 12.333 2.041 0 0 12.333 2.041 12.124 2.246 1966 6 13.667 -0.931 0 0 13.667 -0.931 12.691 -1.491 1966 7 17.775 -1.263 1 0 NaN NaN 17.337 -1.286 1966 8 18.389 0.470 0 0 18.389 0.470 17.841 0.336 1966 9 NaN NaN NaN NaN NaN NaN 14.782 1.202 1966 10 8.167 -0.271 0 0 8.167 -0.271 8.669 0.646 1966 11 3.278 0.422 0 0 3.278 0.422 3.561 1.119 1966 12 0.833 1.383 0 0 0.833 1.383 0.214 1.178 1967 1 -0.167 1.317 0 0 -0.167 1.317 0.415 2.314 1967 2 2.611 1.574 0 0 2.611 1.574 2.829 2.207 1967 3 2.333 -0.005 0 0 2.333 -0.005 0.532 -1.392 1967 4 2.444 -3.179 0 0 2.444 -3.179 0.761 -4.448 1967 5 10.444 0.152 0 0 10.444 0.152 10.027 0.149 1967 6 15.111 0.514 0 0 15.111 0.514 13.487 -0.696 1967 7 20.778 1.740 0 0 20.778 1.740 20.112 1.489 1967 8 19.722 1.803 0 0 19.722 1.803 20.002 2.497 1967 9 16.556 2.560 0 0 16.556 2.560 15.923 2.342 1967 10 9.593 1.156 1 0 NaN NaN 8.757 0.734 1967 11 3.889 1.033 0 0 3.889 1.033 3.863 1.421 1967 12 -2.778 -2.228 0 0 -2.778 -2.228 -3.440 -2.476 1968 1 -1.278 0.206 0 0 -1.278 0.206 -1.554 0.344 1968 2 2.833 1.797 0 0 2.833 1.797 4.234 3.612 1968 3 NaN NaN NaN NaN NaN NaN 3.336 1.413 1968 4 NaN NaN NaN NaN NaN NaN 3.959 -1.249 1968 5 NaN NaN NaN NaN NaN NaN 9.660 -0.218 1968 6 NaN NaN NaN NaN NaN NaN 14.213 0.030 1968 7 NaN NaN NaN NaN NaN NaN 20.508 1.885 1968 8 NaN NaN NaN NaN NaN NaN 15.287 -2.218 1968 9 NaN NaN NaN NaN NaN NaN 13.427 -0.154 1968 10 NaN NaN NaN NaN NaN NaN 8.359 0.336 1968 11 NaN NaN NaN NaN NaN NaN 2.325 -0.116 1968 12 NaN NaN NaN NaN NaN NaN -1.613 -0.649 1969 1 NaN NaN NaN NaN NaN NaN -1.807 0.091 1969 2 NaN NaN NaN NaN NaN NaN -0.989 -1.611