% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 38009 % Primary Name: ALOHA RANCH % Record Type: TAVG % Country: United States % State: OR % Latitude: 42.36670 +/- 0.00005 % Longitude: -122.76670 +/- 0.00005 % Elevation (m): 396.24 +/- 0.15 % # of Months: 19 % % Alternate Names: Missing Station ID - 350138 % % IDs: coop - 350138 % ghcnd - USC00350138 % ncdc - 12004296 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 1cfc8f4ce7371345207e461e3331b23b % Raw Data Hash: e37195cb5b058fd3e9a365c11b65dea6 % Adj Data Hash: e3fce440890afe5acf0ca5b283cea65f % % 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 1914 4 NaN NaN NaN NaN NaN NaN 6.265 0.512 1914 5 NaN NaN NaN NaN NaN NaN 11.581 1.676 1914 6 NaN NaN NaN NaN NaN NaN 12.725 -1.151 1914 7 NaN NaN NaN NaN NaN NaN 18.652 0.761 1914 8 NaN NaN NaN NaN NaN NaN 17.708 0.374 1914 9 NaN NaN NaN NaN NaN NaN 12.420 -1.950 1914 10 NaN NaN NaN NaN NaN NaN 9.015 0.159 1914 11 NaN NaN NaN NaN NaN NaN 3.241 -0.272 1914 12 NaN NaN NaN NaN NaN NaN -2.973 -3.353 1915 1 NaN NaN NaN NaN NaN NaN -0.363 -0.160 1915 2 NaN NaN NaN NaN NaN NaN 2.530 0.493 1915 3 NaN NaN NaN NaN NaN NaN 4.705 1.545 1915 4 12.638 2.814 1 0 NaN NaN 7.245 1.492 1915 5 NaN NaN NaN NaN NaN NaN 8.575 -1.330 1915 6 NaN NaN NaN NaN NaN NaN 12.675 -1.201 1915 7 NaN NaN NaN NaN NaN NaN 17.238 -0.653 1915 8 NaN NaN NaN NaN NaN NaN 19.175 1.842 1915 9 NaN NaN NaN NaN NaN NaN 13.136 -1.234 1915 10 12.697 -0.230 0 0 12.697 -0.230 9.124 0.267 1915 11 6.509 -1.074 0 0 6.509 -1.074 2.702 -0.810 1915 12 5.429 0.979 0 0 5.429 0.979 0.729 0.349 1916 1 2.113 -1.755 0 0 2.113 -1.755 -3.882 -3.679 1916 2 8.943 2.836 0 0 8.943 2.836 4.384 2.347 1916 3 8.848 1.618 0 0 8.848 1.618 3.842 0.682 1916 4 NaN NaN NaN NaN NaN NaN 6.131 0.377 1916 5 11.326 -2.649 1 0 NaN NaN 7.691 -2.214 1916 6 16.625 -1.322 0 1 16.625 -1.322 12.464 -1.413 1916 7 18.566 -3.395 0 0 18.566 -3.395 15.700 -2.191 1916 8 20.498 -0.905 0 0 20.498 -0.905 17.036 -0.297 1916 9 17.247 -1.193 1 0 NaN NaN 14.378 0.008 1916 10 10.033 -2.894 1 0 NaN NaN 7.423 -1.434 1916 11 NaN NaN NaN NaN NaN NaN 0.959 -2.553 1916 12 0.161 -4.289 0 0 0.161 -4.289 -2.793 -3.173 1917 1 0.407 -3.461 0 0 0.407 -3.461 -3.625 -3.422 1917 2 3.016 -3.091 0 0 3.016 -3.091 -0.357 -2.394 1917 3 3.747 -3.484 0 0 3.747 -3.484 -1.040 -4.201 1917 4 NaN NaN NaN NaN NaN NaN 4.024 -1.729 1917 5 11.692 -2.284 0 0 11.692 -2.284 7.983 -1.922 1917 6 15.422 -2.525 1 0 NaN NaN 12.684 -1.193 1917 7 NaN NaN NaN NaN NaN NaN 19.580 1.689 1917 8 NaN NaN NaN NaN NaN NaN 18.346 1.013 1917 9 NaN NaN NaN NaN NaN NaN 14.559 0.189 1917 10 NaN NaN NaN NaN NaN NaN 9.853 0.997 1917 11 NaN NaN NaN NaN NaN NaN 4.483 0.970 1917 12 NaN NaN NaN NaN NaN NaN 2.622 2.242 1918 1 NaN NaN NaN NaN NaN NaN 1.489 1.692 1918 2 NaN NaN NaN NaN NaN NaN 1.351 -0.687 1918 3 NaN NaN NaN NaN NaN NaN 3.034 -0.126 1918 4 NaN NaN NaN NaN NaN NaN 5.590 -0.163 1918 5 NaN NaN NaN NaN NaN NaN 8.433 -1.473 1918 6 NaN NaN NaN NaN NaN NaN 16.502 2.625