% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 41675 % Primary Name: FRASER % Record Type: TAVG % Country: United States % State: ID % Latitude: 46.38330 +/- 0.00005 % Longitude: -116.08330 +/- 0.00005 % Elevation (m): 923.92 +/- 116.13 % # of Months: 22 % % Alternate Names: Missing Station ID - 103345 % % IDs: coop - 103345 % ghcnd - USC00103345 % ncdc - 12001576 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: e6cd4cb33f67e6c6f807511af1765709 % Raw Data Hash: 539cb54d350c866c81fd3c75648db13c % Adj Data Hash: d98951e09553f3d4dd377a23840efecc % % 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 1893 4 NaN NaN NaN NaN NaN NaN 2.929 -2.348 1893 5 NaN NaN NaN NaN NaN NaN 8.609 -1.254 1893 6 NaN NaN NaN NaN NaN NaN 11.388 -2.546 1893 7 NaN NaN NaN NaN NaN NaN 17.141 -1.050 1893 8 NaN NaN NaN NaN NaN NaN 17.463 -0.056 1893 9 NaN NaN NaN NaN NaN NaN 11.828 -1.249 1893 10 NaN NaN NaN NaN NaN NaN 5.434 -1.628 1893 11 NaN NaN NaN NaN NaN NaN 0.078 -0.785 1893 12 NaN NaN NaN NaN NaN NaN -0.331 2.205 1894 1 NaN NaN NaN NaN NaN NaN -4.026 -0.129 1894 2 NaN NaN NaN NaN NaN NaN -4.531 -3.798 1894 3 NaN NaN NaN NaN NaN NaN -0.339 -1.634 1894 4 6.983 0.084 0 0 6.983 0.084 4.932 -0.346 1894 5 12.413 0.928 0 0 12.413 0.928 10.530 0.668 1894 6 14.015 -1.542 0 0 14.015 -1.542 11.927 -2.008 1894 7 NaN NaN NaN NaN NaN NaN 18.490 0.300 1894 8 18.862 -0.280 1 0 NaN NaN 18.893 1.373 1894 9 12.171 -2.528 1 0 NaN NaN 10.990 -2.087 1894 10 7.506 -1.178 1 0 NaN NaN 6.820 -0.241 1894 11 4.990 2.505 0 0 4.990 2.505 3.612 2.749 1894 12 -2.148 -1.235 0 0 -2.148 -1.235 -3.472 -0.937 1895 1 -1.529 0.746 0 0 -1.529 0.746 -4.730 -0.833 1895 2 0.791 -0.098 1 0 NaN NaN -0.348 0.386 1895 3 2.634 -0.283 0 0 2.634 -0.283 0.296 -0.999 1895 4 8.482 1.582 0 0 8.482 1.582 6.329 1.051 1895 5 11.226 -0.259 1 0 NaN NaN 9.233 -0.630 1895 6 14.944 -0.612 1 0 NaN NaN 12.379 -1.555 1895 7 17.778 -2.035 0 0 17.778 -2.035 16.848 -1.342 1895 8 18.453 -0.689 0 0 18.453 -0.689 16.923 -0.597 1895 9 NaN NaN NaN NaN NaN NaN 9.597 -3.480 1895 10 NaN NaN NaN NaN NaN NaN 8.221 1.159 1895 11 NaN NaN NaN NaN NaN NaN 0.524 -0.339 1895 12 -1.852 -0.938 0 0 -1.852 -0.938 -2.696 -0.161 1896 1 NaN NaN NaN NaN NaN NaN -1.385 2.513 1896 2 NaN NaN NaN NaN NaN NaN 1.717 2.450 1896 3 0.645 -2.272 0 0 0.645 -2.272 -0.008 -1.304 1896 4 4.828 -2.071 0 0 4.828 -2.071 3.205 -2.072 1896 5 7.723 -3.762 0 0 7.723 -3.762 6.742 -3.120 1896 6 14.940 -0.617 0 0 14.940 -0.617 13.585 -0.350 1896 7 19.803 -0.010 1 0 NaN NaN 19.938 1.747 1896 8 NaN NaN NaN NaN NaN NaN 17.426 -0.094 1896 9 NaN NaN NaN NaN NaN NaN 11.602 -1.475 1896 10 NaN NaN NaN NaN NaN NaN 7.884 0.823 1896 11 NaN NaN NaN NaN NaN NaN -2.633 -3.497 1896 12 NaN NaN NaN NaN NaN NaN 0.815 3.351 1897 1 NaN NaN NaN NaN NaN NaN -4.360 -0.463 1897 2 NaN NaN NaN NaN NaN NaN -0.724 0.009 1897 3 NaN NaN NaN NaN NaN NaN -2.957 -4.252 1897 4 NaN NaN NaN NaN NaN NaN 6.237 0.959 1897 5 NaN NaN NaN NaN NaN NaN 13.401 3.539 1897 6 NaN NaN NaN NaN NaN NaN 12.766 -1.168 1897 7 NaN NaN NaN NaN NaN NaN 15.736 -2.454