% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 43167 % Primary Name: SHAW ISLAND % Record Type: TAVG % Country: United States % State: AK % Latitude: 58.20000 +/- 0.00500 % Longitude: -136.25000 +/- 0.00500 % Elevation (m): 2.44 +/- 0.15 % # of Months: 26 % % Alternate Names: Missing Station ID - 508397 % % IDs: coop - 508397 % ghcnd - USC00508397 % ncdc - 30015299 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 95811c6c04947487095e31401182459b % Raw Data Hash: 99cdf5a46f3c8446be5bef0d0f8f8d83 % Adj Data Hash: 7695fa72345f045ae5267e3a94e6eb5f % % 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 1924 11 NaN NaN NaN NaN NaN NaN -1.355 1.044 1924 12 NaN NaN NaN NaN NaN NaN -8.203 -2.251 1925 1 NaN NaN NaN NaN NaN NaN -13.146 -4.711 1925 2 NaN NaN NaN NaN NaN NaN -7.954 -2.539 1925 3 NaN NaN NaN NaN NaN NaN -3.969 -0.378 1925 4 NaN NaN NaN NaN NaN NaN -0.367 -0.697 1925 5 NaN NaN NaN NaN NaN NaN 4.649 0.447 1925 6 NaN NaN NaN NaN NaN NaN 7.184 -0.558 1925 7 NaN NaN NaN NaN NaN NaN 9.371 -0.364 1925 8 NaN NaN NaN NaN NaN NaN 9.253 -0.156 1925 9 NaN NaN NaN NaN NaN NaN 6.985 0.495 1925 10 NaN NaN NaN NaN NaN NaN 3.766 1.595 1925 11 5.820 3.718 0 0 5.820 3.718 0.400 2.799 1925 12 2.803 4.253 0 0 2.803 4.253 -1.659 4.292 1926 1 4.135 8.070 0 0 4.135 8.070 -1.628 6.807 1926 2 NaN NaN NaN NaN NaN NaN -2.527 2.888 1926 3 4.661 3.752 0 0 4.661 3.752 0.412 4.003 1926 4 6.872 2.041 0 0 6.872 2.041 2.392 2.062 1926 5 9.172 0.469 0 0 9.172 0.469 5.053 0.850 1926 6 13.137 0.894 1 0 NaN NaN 9.410 1.668 1926 7 13.082 -1.153 0 0 13.082 -1.153 10.233 0.498 1926 8 12.621 -1.289 0 0 12.621 -1.289 10.379 0.970 1926 9 NaN NaN NaN NaN NaN NaN 6.414 -0.076 1926 10 7.032 0.360 0 0 7.032 0.360 3.638 1.467 1926 11 4.207 2.105 0 0 4.207 2.105 -1.402 0.997 1926 12 1.144 2.595 0 0 1.144 2.595 -4.670 1.281 1927 1 0.292 4.226 0 0 0.292 4.226 -8.209 0.226 1927 2 0.691 1.606 1 0 NaN NaN -3.679 1.736 1927 3 2.214 1.305 0 0 2.214 1.305 -2.412 1.179 1927 4 1.851 -2.979 0 0 1.851 -2.979 -2.987 -3.317 1927 5 7.264 -1.439 0 0 7.264 -1.439 3.800 -0.402 1927 6 10.795 -1.448 0 0 10.795 -1.448 8.426 0.684 1927 7 12.406 -1.829 0 0 12.406 -1.829 10.963 1.228 1927 8 11.920 -1.989 0 0 11.920 -1.989 10.706 1.297 1927 9 9.856 -1.135 0 0 9.856 -1.135 6.691 0.201 1927 10 5.668 -1.004 1 0 NaN NaN 1.832 -0.339 1927 11 NaN NaN NaN NaN NaN NaN -7.097 -4.698 1927 12 -0.962 0.488 0 0 -0.962 0.488 -8.854 -2.902 1928 1 1.294 5.229 0 0 1.294 5.229 -6.189 2.246 1928 2 2.500 3.414 1 0 NaN NaN -2.257 3.158 1928 3 1.185 0.275 0 0 1.185 0.275 -4.431 -0.840 1928 4 NaN NaN NaN NaN NaN NaN -0.453 -0.783 1928 5 NaN NaN NaN NaN NaN NaN 3.399 -0.803 1928 6 NaN NaN NaN NaN NaN NaN 8.715 0.973 1928 7 NaN NaN NaN NaN NaN NaN 9.744 0.009 1928 8 NaN NaN NaN NaN NaN NaN 8.643 -0.766 1928 9 NaN NaN NaN NaN NaN NaN 6.519 0.029 1928 10 NaN NaN NaN NaN NaN NaN 2.620 0.449 1928 11 NaN NaN NaN NaN NaN NaN -0.160 2.239 1928 12 NaN NaN NaN NaN NaN NaN -3.068 2.884 1929 1 NaN NaN NaN NaN NaN NaN -6.746 1.690 1929 2 NaN NaN NaN NaN NaN NaN -4.031 1.384 1929 3 NaN NaN NaN NaN NaN NaN -2.699 0.892