% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39658 % Primary Name: DREWSEY 12 WNW % Record Type: TAVG % Country: United States % State: OR % Latitude: 43.91670 +/- 0.00005 % Longitude: -118.58330 +/- 0.00005 % Elevation (m): 1177.10 +/- 0.05 % # of Months: 15 % % IDs: coop - 352419 % ghcnd - USC00352419 % ncdc - 20016029 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 366dd81233fc206852db796d38b62d96 % Raw Data Hash: 9403f23a46d347b925a02e19c9967a57 % Adj Data Hash: 5ab7ed679542ad93454146a069843f62 % % 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 8.833 1.552 1964 11 NaN NaN NaN NaN NaN NaN 0.199 -0.858 1964 12 NaN NaN NaN NaN NaN NaN -2.125 0.715 1965 1 NaN NaN NaN NaN NaN NaN -2.396 1.648 1965 2 NaN NaN NaN NaN NaN NaN 1.097 1.918 1965 3 NaN NaN NaN NaN NaN NaN -0.000 -1.457 1965 4 NaN NaN NaN NaN NaN NaN 5.999 0.790 1965 5 NaN NaN NaN NaN NaN NaN 8.804 -1.123 1965 6 NaN NaN NaN NaN NaN NaN 13.353 -0.838 1965 7 NaN NaN NaN NaN NaN NaN 18.043 -0.507 1965 8 NaN NaN NaN NaN NaN NaN 16.687 -0.982 1965 9 NaN NaN NaN NaN NaN NaN 10.555 -2.799 1965 10 7.664 -0.401 1 0 NaN NaN 9.674 2.393 1965 11 4.000 2.160 0 0 4.000 2.160 2.900 1.844 1965 12 -2.368 -0.312 1 0 NaN NaN -3.372 -0.532 1966 1 NaN NaN NaN NaN NaN NaN -2.148 1.895 1966 2 NaN NaN NaN NaN NaN NaN -1.141 -0.321 1966 3 NaN NaN NaN NaN NaN NaN 1.463 0.007 1966 4 NaN NaN NaN NaN NaN NaN 5.378 0.169 1966 5 NaN NaN NaN NaN NaN NaN 11.611 1.685 1966 6 NaN NaN NaN NaN NaN NaN 12.547 -1.644 1966 7 NaN NaN NaN NaN NaN NaN 17.937 -0.613 1966 8 NaN NaN NaN NaN NaN NaN 17.879 0.211 1966 9 NaN NaN NaN NaN NaN NaN 15.252 1.898 1966 10 6.583 -1.482 1 0 NaN NaN 7.344 0.063 1966 11 4.222 2.382 0 0 4.222 2.382 2.879 1.822 1966 12 -1.944 0.111 0 0 -1.944 0.111 -1.593 1.247 1967 1 -0.611 2.648 0 0 -0.611 2.648 -0.572 3.472 1967 2 1.444 1.481 0 0 1.444 1.481 1.591 2.411 1967 3 2.333 0.093 0 0 2.333 0.093 0.603 -0.854 1967 4 3.389 -2.604 0 0 3.389 -2.604 1.746 -3.463 1967 5 10.944 0.234 0 0 10.944 0.234 9.698 -0.229 1967 6 15.611 0.636 0 0 15.611 0.636 13.818 -0.373 1967 7 20.778 1.444 0 0 20.778 1.444 19.988 1.439 1967 8 20.167 1.714 0 0 20.167 1.714 20.204 2.535 1967 9 16.556 2.418 0 0 16.556 2.418 16.219 2.865 1967 10 NaN NaN NaN NaN NaN NaN 7.495 0.213 1967 11 NaN NaN NaN NaN NaN NaN 1.992 0.935 1967 12 NaN NaN NaN NaN NaN NaN -4.138 -1.298 1968 1 NaN NaN NaN NaN NaN NaN -3.528 0.516 1968 2 NaN NaN NaN NaN NaN NaN 2.850 3.670 1968 3 NaN NaN NaN NaN NaN NaN 3.091 1.634 1968 4 NaN NaN NaN NaN NaN NaN 3.466 -1.743 1968 5 NaN NaN NaN NaN NaN NaN 9.671 -0.255 1968 6 NaN NaN NaN NaN NaN NaN 14.227 0.036 1968 7 NaN NaN NaN NaN NaN NaN 19.872 1.322 1968 8 NaN NaN NaN NaN NaN NaN 15.777 -1.891 1968 9 NaN NaN NaN NaN NaN NaN 13.267 -0.086