% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 40904 % Primary Name: LA GRANDE 16 WSW % Record Type: TAVG % Country: United States % State: OR % Latitude: 45.25000 +/- 0.00500 % Longitude: -118.40000 +/- 0.00500 % Elevation (m): 1054.90 +/- 0.05 % # of Months: 19 % % IDs: coop - 354626 % ghcnd - USC00354626 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % % Site Hash: 88338dcbd20c40206e92526568bd0bf3 % Raw Data Hash: cf6450ad99b5e81a29e9c65404e2eb1a % Adj Data Hash: 90471dcfb4462ba1a24f38f83eaef1f9 % % 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 1959 8 NaN NaN NaN NaN NaN NaN 18.454 -1.602 1959 9 NaN NaN NaN NaN NaN NaN 14.646 -1.203 1959 10 NaN NaN NaN NaN NaN NaN 10.141 0.440 1959 11 NaN NaN NaN NaN NaN NaN 1.911 -1.696 1959 12 NaN NaN NaN NaN NaN NaN 0.479 0.107 1960 1 NaN NaN NaN NaN NaN NaN -4.867 -3.655 1960 2 NaN NaN NaN NaN NaN NaN 2.477 0.109 1960 3 NaN NaN NaN NaN NaN NaN 4.560 -0.438 1960 4 NaN NaN NaN NaN NaN NaN 8.502 -0.110 1960 5 NaN NaN NaN NaN NaN NaN 11.618 -1.470 1960 6 NaN NaN NaN NaN NaN NaN 16.905 -0.201 1960 7 NaN NaN NaN NaN NaN NaN 23.224 2.313 1960 8 14.222 -2.993 0 0 14.222 -2.993 18.425 -1.631 1960 9 12.056 -0.953 0 0 12.056 -0.953 16.252 0.403 1960 10 7.056 0.194 0 0 7.056 0.194 10.683 0.981 1960 11 0.944 0.178 0 0 0.944 0.178 4.040 0.434 1960 12 -4.000 -1.532 0 0 -4.000 -1.532 -0.908 -1.280 1961 1 -3.500 0.553 0 0 -3.500 0.553 0.974 2.186 1961 2 1.778 2.250 0 0 1.778 2.250 6.545 4.177 1961 3 2.611 0.453 0 0 2.611 0.453 5.578 0.580 1961 4 3.611 -2.161 0 0 3.611 -2.161 8.019 -0.593 1961 5 10.222 -0.025 0 0 10.222 -0.025 12.636 -0.451 1961 6 15.833 1.569 0 0 15.833 1.569 19.457 2.352 1961 7 17.333 -0.737 0 0 17.333 -0.737 22.323 1.412 1961 8 20.667 3.451 0 0 20.667 3.451 22.955 2.900 1961 9 NaN NaN NaN NaN NaN NaN 14.002 -1.846 1961 10 10.000 3.139 0 0 10.000 3.139 9.133 -0.568 1961 11 1.556 0.789 0 0 1.556 0.789 0.981 -2.626 1961 12 NaN NaN NaN NaN NaN NaN 0.982 0.610 1962 1 NaN NaN NaN NaN NaN NaN -1.867 -0.655 1962 2 NaN NaN NaN NaN NaN NaN 2.619 0.251 1962 3 2.333 0.175 0 0 2.333 0.175 3.402 -1.596 1962 4 9.278 3.505 0 0 9.278 3.505 9.904 1.291 1962 5 8.722 -1.525 0 0 8.722 -1.525 11.007 -2.080 1962 6 12.611 -1.654 0 0 12.611 -1.654 15.891 -1.214 1962 7 NaN NaN NaN NaN NaN NaN 20.207 -0.704 1962 8 NaN NaN NaN NaN NaN NaN 18.766 -1.289 1962 9 NaN NaN NaN NaN NaN NaN 16.517 0.669 1962 10 NaN NaN NaN NaN NaN NaN 10.056 0.354 1962 11 NaN NaN NaN NaN NaN NaN 5.165 1.558 1962 12 NaN NaN NaN NaN NaN NaN 2.691 2.319 1963 1 NaN NaN NaN NaN NaN NaN -4.064 -2.852 1963 2 NaN NaN NaN NaN NaN NaN 5.120 2.752 1963 3 NaN NaN NaN NaN NaN NaN 5.243 0.245 1963 4 NaN NaN NaN NaN NaN NaN 6.923 -1.690 1963 5 NaN NaN NaN NaN NaN NaN 13.252 0.165 1963 6 NaN NaN NaN NaN NaN NaN 16.440 -0.665