% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 43318 % Primary Name: MOOSE PASS 6 NW % Record Type: TAVG % Country: United States % State: AK % Latitude: 60.53330 +/- 0.00005 % Longitude: -149.51670 +/- 0.00005 % Elevation (m): 200.90 +/- 0.05 % # of Months: 9 % % IDs: coop - 505895 % ghcnd - USC00505895 % ncdc - 20021990 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 75581771a7f5ce60a4e7acb967a92896 % Raw Data Hash: 6f1a8488d503c311f8c4e6386c5885df % Adj Data Hash: 3ad5a3a4ce916754a99ceff8df899818 % % 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 1978 5 NaN NaN NaN NaN NaN NaN 5.718 1.036 1978 6 NaN NaN NaN NaN NaN NaN 8.428 -0.359 1978 7 NaN NaN NaN NaN NaN NaN 10.916 -0.336 1978 8 NaN NaN NaN NaN NaN NaN 12.419 1.755 1978 9 NaN NaN NaN NaN NaN NaN 7.763 0.866 1978 10 NaN NaN NaN NaN NaN NaN 2.336 1.593 1978 11 NaN NaN NaN NaN NaN NaN -2.850 1.396 1978 12 NaN NaN NaN NaN NaN NaN -5.826 2.675 1979 1 NaN NaN NaN NaN NaN NaN -5.668 3.750 1979 2 NaN NaN NaN NaN NaN NaN -12.979 -6.099 1979 3 NaN NaN NaN NaN NaN NaN -1.972 2.952 1979 4 NaN NaN NaN NaN NaN NaN 1.762 1.721 1979 5 6.722 2.952 0 0 6.722 2.952 5.852 1.169 1979 6 10.222 2.347 0 0 10.222 2.347 9.090 0.303 1979 7 13.778 3.438 0 0 13.778 3.438 12.824 1.572 1979 8 12.833 3.082 0 0 12.833 3.082 12.261 1.598 1979 9 8.444 2.459 0 0 8.444 2.459 9.105 2.207 1979 10 3.222 3.392 0 0 3.222 3.392 3.753 3.011 1979 11 -1.556 3.603 0 0 -1.556 3.603 0.385 4.632 1979 12 -17.000 -7.587 0 0 -17.000 -7.587 -12.031 -3.530 1980 1 -14.944 -4.614 0 0 -14.944 -4.614 -11.307 -1.889 1980 2 NaN NaN NaN NaN NaN NaN -2.389 4.490 1980 3 NaN NaN NaN NaN NaN NaN -3.267 1.656 1980 4 NaN NaN NaN NaN NaN NaN 2.254 2.213 1980 5 NaN NaN NaN NaN NaN NaN 4.911 0.229 1980 6 NaN NaN NaN NaN NaN NaN 8.855 0.067 1980 7 NaN NaN NaN NaN NaN NaN 11.451 0.199 1980 8 NaN NaN NaN NaN NaN NaN 10.007 -0.657 1980 9 NaN NaN NaN NaN NaN NaN 7.020 0.123 1980 10 NaN NaN NaN NaN NaN NaN 2.274 1.531 1980 11 NaN NaN NaN NaN NaN NaN -1.361 2.886 1980 12 NaN NaN NaN NaN NaN NaN -14.932 -6.431 1981 1 NaN NaN NaN NaN NaN NaN -0.670 8.748