% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 43281 % Primary Name: SILVER SALMON CREEK % Record Type: TAVG % Country: United States % State: AK % Latitude: 59.96670 +/- 0.00005 % Longitude: -152.66670 +/- 0.00005 % Elevation (m): 46.00 +/- 0.05 % # of Months: 13 % % IDs: coop - 508477 % ghcnd - USC00508477 % ncdc - 20021955 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: b760a98ff72978ee7cc563c520eba745 % Raw Data Hash: 0d2a3e7c6ec9e278001e7881f5a84f9f % Adj Data Hash: 0d2a3e7c6ec9e278001e7881f5a84f9f % % 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 1965 8 NaN NaN NaN NaN NaN NaN 9.884 -0.744 1965 9 NaN NaN NaN NaN NaN NaN 9.535 2.332 1965 10 NaN NaN NaN NaN NaN NaN -2.819 -3.339 1965 11 NaN NaN NaN NaN NaN NaN -5.390 -0.456 1965 12 NaN NaN NaN NaN NaN NaN -12.577 -2.568 1966 1 NaN NaN NaN NaN NaN NaN -10.109 0.531 1966 2 NaN NaN NaN NaN NaN NaN -8.783 -0.077 1966 3 NaN NaN NaN NaN NaN NaN -12.802 -5.964 1966 4 NaN NaN NaN NaN NaN NaN -0.838 0.333 1966 5 NaN NaN NaN NaN NaN NaN 2.825 -1.430 1966 6 NaN NaN NaN NaN NaN NaN 9.026 0.582 1966 7 NaN NaN NaN NaN NaN NaN 10.934 0.033 1966 8 11.000 -1.969 0 0 11.000 -1.969 10.296 -0.331 1966 9 8.944 -0.600 0 0 8.944 -0.600 8.137 0.934 1966 10 1.167 -1.696 0 0 1.167 -1.696 -1.370 -1.891 1966 11 -3.667 -1.074 0 0 -3.667 -1.074 -5.507 -0.573 1966 12 -6.889 0.779 0 0 -6.889 0.779 -11.844 -1.835 1967 1 -9.000 -0.702 0 0 -9.000 -0.702 -12.869 -2.230 1967 2 -7.333 -0.969 0 0 -7.333 -0.969 -9.738 -1.032 1967 3 -4.000 0.497 0 0 -4.000 0.497 -6.186 0.653 1967 4 NaN NaN NaN NaN NaN NaN -0.226 0.945 1967 5 7.167 0.570 0 0 7.167 0.570 5.623 1.368 1967 6 NaN NaN NaN NaN NaN NaN 9.058 0.613 1967 7 15.389 2.146 0 0 15.389 2.146 12.583 1.682 1967 8 13.056 0.086 0 0 13.056 0.086 12.036 1.408 1967 9 10.056 0.511 0 0 10.056 0.511 8.288 1.085 1967 10 4.611 1.749 0 0 4.611 1.749 0.609 0.089 1967 11 NaN NaN NaN NaN NaN NaN -2.076 2.858 1967 12 NaN NaN NaN NaN NaN NaN -10.283 -0.274 1968 1 NaN NaN NaN NaN NaN NaN -12.259 -1.619 1968 2 NaN NaN NaN NaN NaN NaN -7.171 1.535 1968 3 NaN NaN NaN NaN NaN NaN -4.737 2.101 1968 4 NaN NaN NaN NaN NaN NaN -1.717 -0.547 1968 5 NaN NaN NaN NaN NaN NaN 5.375 1.120 1968 6 NaN NaN NaN NaN NaN NaN 8.951 0.507 1968 7 NaN NaN NaN NaN NaN NaN 11.939 1.038 1968 8 NaN NaN NaN NaN NaN NaN 11.992 1.365 1968 9 NaN NaN NaN NaN NaN NaN 6.441 -0.762 1968 10 NaN NaN NaN NaN NaN NaN -0.913 -1.433