% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 43049 % Primary Name: SMEATON BAY % Record Type: TAVG % Country: United States % State: AK % Latitude: 55.31670 +/- 0.00005 % Longitude: -130.78330 +/- 0.00005 % Elevation (m): 6.10 +/- 0.05 % # of Months: 14 % % IDs: coop - 508558 % ghcnd - USC00508558 % ncdc - 20021793 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 44c7c36050576a76e47f8952b08ce8b1 % Raw Data Hash: 5125519b96e6893c56af3d8e6e5f6245 % Adj Data Hash: 5125519b96e6893c56af3d8e6e5f6245 % % 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 1948 8 NaN NaN NaN NaN NaN NaN 12.649 0.394 1948 9 NaN NaN NaN NaN NaN NaN 7.994 -1.041 1948 10 NaN NaN NaN NaN NaN NaN 3.601 -0.568 1948 11 NaN NaN NaN NaN NaN NaN -0.571 0.117 1948 12 NaN NaN NaN NaN NaN NaN -7.570 -3.713 1949 1 NaN NaN NaN NaN NaN NaN -7.190 -1.321 1949 2 NaN NaN NaN NaN NaN NaN -6.304 -3.637 1949 3 NaN NaN NaN NaN NaN NaN 0.186 0.963 1949 4 NaN NaN NaN NaN NaN NaN 1.527 -1.219 1949 5 NaN NaN NaN NaN NaN NaN 6.989 -0.073 1949 6 NaN NaN NaN NaN NaN NaN 8.612 -1.875 1949 7 NaN NaN NaN NaN NaN NaN 11.016 -1.572 1949 8 13.333 -1.590 0 0 13.333 -1.590 11.457 -0.798 1949 9 12.111 0.408 0 0 12.111 0.408 9.835 0.800 1949 10 7.056 0.219 0 0 7.056 0.219 3.821 -0.347 1949 11 6.333 4.353 0 0 6.333 4.353 2.760 3.448 1949 12 -1.889 -0.701 0 0 -1.889 -0.701 -6.701 -2.844 1950 1 -10.000 -6.800 0 0 -10.000 -6.800 -14.424 -8.556 1950 2 0.444 0.443 0 0 0.444 0.443 -1.951 0.716 1950 3 2.056 0.163 0 0 2.056 0.163 -1.044 -0.267 1950 4 3.778 -1.637 0 0 3.778 -1.637 1.301 -1.445 1950 5 6.611 -3.119 0 0 6.611 -3.119 5.298 -1.764 1950 6 13.833 0.678 0 0 13.833 0.678 11.965 1.478 1950 7 13.667 -1.590 0 0 13.667 -1.590 11.729 -0.859 1950 8 14.333 -0.590 0 0 14.333 -0.590 12.470 0.215 1950 9 11.722 0.019 0 0 11.722 0.019 9.513 0.478 1950 10 NaN NaN NaN NaN NaN NaN 2.935 -1.233 1950 11 NaN NaN NaN NaN NaN NaN -4.916 -4.228 1950 12 NaN NaN NaN NaN NaN NaN -2.580 1.277 1951 1 NaN NaN NaN NaN NaN NaN -7.735 -1.867 1951 2 NaN NaN NaN NaN NaN NaN -4.049 -1.382 1951 3 NaN NaN NaN NaN NaN NaN -4.228 -3.451 1951 4 NaN NaN NaN NaN NaN NaN 2.106 -0.640 1951 5 NaN NaN NaN NaN NaN NaN 6.825 -0.237 1951 6 NaN NaN NaN NaN NaN NaN 10.756 0.269 1951 7 NaN NaN NaN NaN NaN NaN 13.447 0.859 1951 8 NaN NaN NaN NaN NaN NaN 12.785 0.530 1951 9 NaN NaN NaN NaN NaN NaN 9.762 0.727