% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 165671 % Primary Name: MILE 50 - KANDIK RIVER % Record Type: TAVG % Country: United States % State: AK % Latitude: 65.56640 +/- 0.00005 % Longitude: -141.52060 +/- 0.00005 % Elevation (m): 374.90 +/- 0.15 % # of Months: 19 % % Alternate Names: Missing Station ID - 504210 % % IDs: coop - 504210 % ghcnd - USC00504210 % ncdc - 30015692 % nws - DIKA2 % % Sources: Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 09d025e02f085ba54d0426e950d8666e % Raw Data Hash: 4dee1db76cba9eacd303870c1c4ebcf9 % Adj Data Hash: 3ae518a12695b3772a7d2647731775ac % % 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 2010 7 NaN NaN NaN NaN NaN NaN 12.371 1.021 2010 8 NaN NaN NaN NaN NaN NaN 10.379 1.847 2010 9 NaN NaN NaN NaN NaN NaN 2.292 0.763 2010 10 NaN NaN NaN NaN NaN NaN -7.931 2.064 2010 11 NaN NaN NaN NaN NaN NaN -16.220 5.909 2010 12 NaN NaN NaN NaN NaN NaN -31.623 -2.442 2011 1 NaN NaN NaN NaN NaN NaN -29.949 1.761 2011 2 NaN NaN NaN NaN NaN NaN -25.889 1.491 2011 3 NaN NaN NaN NaN NaN NaN -21.822 -0.747 2011 4 NaN NaN NaN NaN NaN NaN -8.676 0.433 2011 5 NaN NaN NaN NaN NaN NaN 4.982 2.673 2011 6 NaN NaN NaN NaN NaN NaN 9.751 0.185 2011 7 13.300 0.218 1 0 NaN NaN 12.349 0.999 2011 8 10.039 -0.225 0 0 10.039 -0.225 8.819 0.287 2011 9 6.025 2.764 0 0 6.025 2.764 3.794 2.265 2011 10 -4.205 4.058 0 0 -4.205 4.058 -6.496 3.499 2011 11 -27.203 -6.806 0 0 -27.203 -6.806 -27.198 -5.069 2011 12 -17.971 9.478 0 0 -17.971 9.478 -21.695 7.486 2012 1 -33.642 -3.663 0 0 -33.642 -3.663 -35.485 -3.774 2012 2 -15.395 10.253 1 0 NaN NaN -19.758 7.622 2012 3 NaN NaN NaN NaN NaN NaN -23.549 -2.473 2012 4 NaN NaN NaN NaN NaN NaN -4.779 4.329 2012 5 NaN NaN NaN NaN NaN NaN 2.865 0.556 2012 6 NaN NaN NaN NaN NaN NaN 11.943 2.377 2012 7 NaN NaN NaN NaN NaN NaN 12.166 0.816 2012 8 NaN NaN NaN NaN NaN NaN 9.674 1.142 2012 9 6.715 3.454 1 0 NaN NaN 4.051 2.522 2012 10 -8.387 -0.124 0 0 -8.387 -0.124 -10.479 -0.484 2012 11 -30.378 -9.981 0 0 -30.378 -9.981 -29.150 -7.020 2012 12 -29.211 -1.762 0 0 -29.211 -1.762 -32.553 -3.372 2013 1 -18.922 11.057 1 0 NaN NaN -27.757 3.954 2013 2 -17.550 8.098 1 0 NaN NaN -23.481 3.899 2013 3 -18.745 0.599 0 0 -18.745 0.599 -21.676 -0.600 2013 4 -12.828 -5.451 0 0 -12.828 -5.451 -13.968 -4.859 2013 5 2.160 -1.881 0 0 2.160 -1.881 1.288 -1.021 2013 6 12.465 1.167 1 0 NaN NaN 12.651 3.085 2013 7 14.913 1.831 0 0 14.913 1.831 12.852 1.502 2013 8 NaN NaN NaN NaN NaN NaN 10.936 2.404 2013 9 NaN NaN NaN NaN NaN NaN 2.362 0.833 2013 10 NaN NaN NaN NaN NaN NaN -3.567 6.427