% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39574 % Primary Name: DREWSEY 13 W % Record Type: TAVG % Country: United States % State: OR % Latitude: 43.83330 +/- 0.00005 % Longitude: -118.63330 +/- 0.00005 % Elevation (m): 1189.90 +/- 0.05 % # of Months: 13 % % IDs: coop - 352417 % ghcnd - USC00352417 % ncdc - 20016016 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: a1f042a998fb497b6d9601b81d3fe337 % Raw Data Hash: 2a0f16d01030f4267e9a5cd26ccffb0d % Adj Data Hash: b31636c670a82cbcae624f379bda5b15 % % 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 1966 10 NaN NaN NaN NaN NaN NaN 7.344 0.063 1966 11 NaN NaN NaN NaN NaN NaN 2.879 1.822 1966 12 NaN NaN NaN NaN NaN NaN -1.593 1.247 1967 1 NaN NaN NaN NaN NaN NaN -0.572 3.472 1967 2 NaN NaN NaN NaN NaN NaN 1.591 2.411 1967 3 NaN NaN NaN NaN NaN NaN 0.603 -0.854 1967 4 NaN NaN NaN NaN NaN NaN 1.746 -3.463 1967 5 NaN NaN NaN NaN NaN NaN 9.698 -0.229 1967 6 NaN NaN NaN NaN NaN NaN 13.818 -0.373 1967 7 NaN NaN NaN NaN NaN NaN 19.988 1.439 1967 8 NaN NaN NaN NaN NaN NaN 20.204 2.535 1967 9 NaN NaN NaN NaN NaN NaN 16.219 2.865 1967 10 5.144 -2.854 1 0 NaN NaN 7.495 0.213 1967 11 3.333 1.561 0 0 3.333 1.561 1.992 0.935 1967 12 -4.222 -2.099 0 0 -4.222 -2.099 -4.138 -1.298 1968 1 -3.444 -0.117 0 0 -3.444 -0.117 -3.528 0.516 1968 2 3.167 3.271 0 0 3.167 3.271 2.850 3.670 1968 3 4.111 1.938 0 0 4.111 1.938 3.091 1.634 1968 4 5.722 -0.203 0 0 5.722 -0.203 3.466 -1.743 1968 5 9.556 -1.087 0 0 9.556 -1.087 9.671 -0.255 1968 6 16.611 1.704 0 0 16.611 1.704 14.227 0.036 1968 7 20.278 1.012 0 0 20.278 1.012 19.872 1.322 1968 8 16.667 -1.718 0 0 16.667 -1.718 15.777 -1.891 1968 9 12.944 -1.125 0 0 12.944 -1.125 13.267 -0.086 1968 10 7.167 -0.831 0 0 7.167 -0.831 6.746 -0.535 1968 11 NaN NaN NaN NaN NaN NaN 1.260 0.203 1968 12 NaN NaN NaN NaN NaN NaN -2.510 0.330 1969 1 NaN NaN NaN NaN NaN NaN -4.187 -0.143 1969 2 NaN NaN NaN NaN NaN NaN -2.423 -1.603 1969 3 NaN NaN NaN NaN NaN NaN -0.019 -1.476 1969 4 NaN NaN NaN NaN NaN NaN 5.378 0.169 1969 5 NaN NaN NaN NaN NaN NaN 11.885 1.959 1969 6 NaN NaN NaN NaN NaN NaN 14.215 0.024 1969 7 NaN NaN NaN NaN NaN NaN 17.960 -0.590 1969 8 NaN NaN NaN NaN NaN NaN 17.390 -0.279 1969 9 NaN NaN NaN NaN NaN NaN 14.063 0.710 1969 10 NaN NaN NaN NaN NaN NaN 5.168 -2.113