% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 42623 % Primary Name: PORT CRESCENT % Record Type: TAVG % Country: United States % State: WA % Latitude: 48.11670 +/- 0.00005 % Longitude: -123.68330 +/- 0.00005 % Elevation (m): 78.94 +/- 0.15 % # of Months: 8 % % Alternate Names: Missing Station ID - 456642 % % IDs: coop - 456642 % ghcnd - USC00456642 % ncdc - 12005967 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 04c3098e9d20e32cf2dc7e94159bdb80 % Raw Data Hash: 54b6a6f360ce1486e20ad7a467e46940 % Adj Data Hash: ba0cd590ce034f0adcff944b295c4e71 % % 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 1915 5 NaN NaN NaN NaN NaN NaN 10.409 0.453 1915 6 NaN NaN NaN NaN NaN NaN 12.111 0.011 1915 7 NaN NaN NaN NaN NaN NaN 14.248 0.213 1915 8 NaN NaN NaN NaN NaN NaN 15.742 1.391 1915 9 NaN NaN NaN NaN NaN NaN 13.459 0.028 1915 10 NaN NaN NaN NaN NaN NaN 10.643 0.396 1915 11 NaN NaN NaN NaN NaN NaN 5.725 -1.277 1915 12 NaN NaN NaN NaN NaN NaN 5.068 -0.047 1916 1 NaN NaN NaN NaN NaN NaN -1.288 -5.266 1916 2 NaN NaN NaN NaN NaN NaN 5.451 0.114 1916 3 NaN NaN NaN NaN NaN NaN 4.934 -0.594 1916 4 NaN NaN NaN NaN NaN NaN 6.897 -0.356 1916 5 9.137 -0.939 0 0 9.137 -0.939 8.521 -1.435 1916 6 NaN NaN NaN NaN NaN NaN 11.516 -0.585 1916 7 14.016 -0.139 1 0 NaN NaN 13.058 -0.977 1916 8 NaN NaN NaN NaN NaN NaN 14.199 -0.152 1916 9 NaN NaN NaN NaN NaN NaN 13.094 -0.337 1916 10 7.429 -2.938 0 0 7.429 -2.938 8.568 -1.680 1916 11 NaN NaN NaN NaN NaN NaN 5.142 -1.859 1916 12 NaN NaN NaN NaN NaN NaN 3.243 -1.872 1917 1 2.557 -1.541 0 0 2.557 -1.541 2.484 -1.495 1917 2 2.644 -2.812 1 0 NaN NaN 3.650 -1.686 1917 3 3.603 -2.044 0 0 3.603 -2.044 3.021 -2.507 1917 4 NaN NaN NaN NaN NaN NaN 5.685 -1.568 1917 5 9.013 -1.063 0 0 9.013 -1.063 8.697 -1.259 1917 6 10.919 -1.301 0 0 10.919 -1.301 10.650 -1.450 1917 7 NaN NaN NaN NaN NaN NaN 13.152 -0.883 1917 8 NaN NaN NaN NaN NaN NaN 14.493 0.142 1917 9 NaN NaN NaN NaN NaN NaN 13.216 -0.215 1917 10 NaN NaN NaN NaN NaN NaN 10.451 0.204 1917 11 NaN NaN NaN NaN NaN NaN 9.168 2.166 1917 12 NaN NaN NaN NaN NaN NaN 6.941 1.827 1918 1 NaN NaN NaN NaN NaN NaN 5.540 1.562 1918 2 NaN NaN NaN NaN NaN NaN 4.168 -1.168 1918 3 NaN NaN NaN NaN NaN NaN 4.645 -0.883 1918 4 NaN NaN NaN NaN NaN NaN 7.194 -0.059 1918 5 NaN NaN NaN NaN NaN NaN 8.827 -1.129 1918 6 NaN NaN NaN NaN NaN NaN 12.643 0.543