% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39420 % Primary Name: WALDO LAKE % Record Type: TAVG % Country: United States % State: OR % Latitude: 43.66670 +/- 0.00005 % Longitude: -122.08330 +/- 0.00005 % Elevation (m): 1673.96 +/- 0.15 % # of Months: 18 % % Alternate Names: Missing Station ID - 358968 % % IDs: coop - 358968 % ghcnd - USC00358968 % ncdc - 20015987 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 6e0f3f0af84295900d36b762ae19f739 % Raw Data Hash: 74d6299ae9e197eaeb9a24b71bd6e78a % Adj Data Hash: c35db3dd859a1c43c1abaf47a723b8e0 % % 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 1912 8 NaN NaN NaN NaN NaN NaN 15.999 -1.347 1912 9 NaN NaN NaN NaN NaN NaN 14.446 -0.853 1912 10 NaN NaN NaN NaN NaN NaN 8.396 -2.282 1912 11 NaN NaN NaN NaN NaN NaN 6.541 0.299 1912 12 NaN NaN NaN NaN NaN NaN 3.635 -0.216 1913 1 NaN NaN NaN NaN NaN NaN 1.626 -1.485 1913 2 NaN NaN NaN NaN NaN NaN 3.561 -1.569 1913 3 NaN NaN NaN NaN NaN NaN 4.753 -1.229 1913 4 NaN NaN NaN NaN NaN NaN 7.452 -0.599 1913 5 NaN NaN NaN NaN NaN NaN 11.238 -0.098 1913 6 NaN NaN NaN NaN NaN NaN 13.689 -0.788 1913 7 NaN NaN NaN NaN NaN NaN 16.919 -0.454 1913 8 16.050 3.192 1 0 NaN NaN 17.819 0.474 1913 9 NaN NaN NaN NaN NaN NaN 14.903 -0.395 1913 10 5.069 -1.122 0 0 5.069 -1.122 10.144 -0.534 1913 11 2.238 0.484 1 0 NaN NaN 6.665 0.422 1913 12 -0.602 0.034 0 0 -0.602 0.034 3.500 -0.351 1914 1 -1.751 -0.374 0 0 -1.751 -0.374 5.179 2.068 1914 2 -5.556 -6.197 1 0 NaN NaN 5.362 0.232 1914 3 -0.176 -1.671 1 0 NaN NaN 7.816 1.834 1914 4 3.313 -0.250 0 0 3.313 -0.250 8.734 0.683 1914 5 13.563 6.714 1 0 NaN NaN 12.685 1.349 1914 6 NaN NaN NaN NaN NaN NaN 13.032 -1.446 1914 7 16.365 3.479 1 0 NaN NaN 17.625 0.251 1914 8 16.701 3.842 0 0 16.701 3.842 17.007 -0.338 1914 9 9.614 -1.196 1 0 NaN NaN 13.789 -1.510 1914 10 6.753 0.563 0 0 6.753 0.563 11.707 1.029 1914 11 3.393 1.639 1 0 NaN NaN 6.536 0.294 1914 12 -2.768 -2.132 0 0 -2.768 -2.132 0.867 -2.984 1915 1 -0.811 0.566 0 0 -0.811 0.566 2.495 -0.615 1915 2 NaN NaN NaN NaN NaN NaN 5.667 0.538 1915 3 2.593 1.098 0 0 2.593 1.098 7.887 1.905 1915 4 NaN NaN NaN NaN NaN NaN 9.407 1.357 1915 5 4.754 -2.095 0 0 4.754 -2.095 10.605 -0.731 1915 6 NaN NaN NaN NaN NaN NaN 13.604 -0.874 1915 7 NaN NaN NaN NaN NaN NaN 16.940 -0.433 1915 8 NaN NaN NaN NaN NaN NaN 18.723 1.377 1915 9 NaN NaN NaN NaN NaN NaN 14.610 -0.688 1915 10 NaN NaN NaN NaN NaN NaN 10.843 0.165 1915 11 NaN NaN NaN NaN NaN NaN 5.666 -0.577 1915 12 NaN NaN NaN NaN NaN NaN 3.937 0.085 1916 1 NaN NaN NaN NaN NaN NaN -1.593 -4.703 1916 2 NaN NaN NaN NaN NaN NaN 6.641 1.511 1916 3 NaN NaN NaN NaN NaN NaN 5.556 -0.427 1916 4 NaN NaN NaN NaN NaN NaN 8.219 0.169 1916 5 NaN NaN NaN NaN NaN NaN 9.091 -2.245