% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 43086 % Primary Name: UNUK RIVER % Record Type: TAVG % Country: United States % State: AK % Latitude: 56.06670 +/- 0.00005 % Longitude: -131.10000 +/- 0.00005 % Elevation (m): 44.72 +/- 250.97 % # of Months: 34 % % IDs: coop - 509648 % ghcnd - USC00509648 % ncdc - 20021814 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 418ec4a85184a96b70d0e9095f4f1d13 % Raw Data Hash: d42a8baac798619e6c9d93740c876e90 % Adj Data Hash: 9bb40fc40838ba84946db75a289a208c % % 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 1952 4 NaN NaN NaN NaN NaN NaN 0.943 -1.802 1952 5 NaN NaN NaN NaN NaN NaN 6.617 -0.445 1952 6 NaN NaN NaN NaN NaN NaN 8.792 -1.694 1952 7 NaN NaN NaN NaN NaN NaN 12.696 0.108 1952 8 NaN NaN NaN NaN NaN NaN 12.918 0.663 1952 9 NaN NaN NaN NaN NaN NaN 9.300 0.265 1952 10 NaN NaN NaN NaN NaN NaN 6.234 2.065 1952 11 NaN NaN NaN NaN NaN NaN 0.477 1.165 1952 12 NaN NaN NaN NaN NaN NaN -2.144 1.713 1953 1 NaN NaN NaN NaN NaN NaN -9.703 -3.835 1953 2 NaN NaN NaN NaN NaN NaN -0.184 2.483 1953 3 NaN NaN NaN NaN NaN NaN -0.551 0.226 1953 4 6.444 1.985 0 0 6.444 1.985 2.844 0.098 1953 5 9.167 0.392 0 0 9.167 0.392 7.824 0.762 1953 6 13.313 1.113 1 0 NaN NaN 11.002 0.515 1953 7 14.278 -0.023 0 0 14.278 -0.023 12.724 0.136 1953 8 13.333 -0.635 0 0 13.333 -0.635 12.760 0.505 1953 9 10.111 -0.637 0 0 10.111 -0.637 8.912 -0.123 1953 10 6.428 0.546 1 0 NaN NaN 5.107 0.938 1953 11 2.222 1.197 0 0 2.222 1.197 0.769 1.457 1953 12 -0.715 1.429 1 0 NaN NaN -1.225 2.632 1954 1 -6.278 -2.123 0 0 -6.278 -2.123 -8.795 -2.926 1954 2 3.500 4.454 1 0 NaN NaN -2.983 -0.317 1954 3 3.050 2.113 1 0 NaN NaN -1.354 -0.577 1954 4 1.778 -2.681 0 0 1.778 -2.681 -0.613 -3.359 1954 5 8.833 0.058 0 0 8.833 0.058 6.846 -0.215 1954 6 12.414 0.214 1 0 NaN NaN 9.560 -0.926 1954 7 NaN NaN NaN NaN NaN NaN 10.947 -1.641 1954 8 15.259 1.291 1 0 NaN NaN 13.503 1.248 1954 9 NaN NaN NaN NaN NaN NaN 9.957 0.923 1954 10 6.056 0.174 0 0 6.056 0.174 4.340 0.172 1954 11 4.833 3.808 0 0 4.833 3.808 2.980 3.668 1954 12 -2.278 -0.134 0 0 -2.278 -0.134 -2.674 1.183 1955 1 -3.361 0.795 1 0 NaN NaN -3.821 2.048 1955 2 NaN NaN NaN NaN NaN NaN -2.318 0.349 1955 3 NaN NaN NaN NaN NaN NaN -3.695 -2.918 1955 4 NaN NaN NaN NaN NaN NaN 1.496 -1.250 1955 5 6.944 -1.831 0 0 6.944 -1.831 5.062 -1.999 1955 6 10.889 -1.311 0 0 10.889 -1.311 9.134 -1.353 1955 7 14.222 -0.079 0 0 14.222 -0.079 11.863 -0.725 1955 8 11.500 -2.468 0 0 11.500 -2.468 10.381 -1.874 1955 9 10.444 -0.304 0 0 10.444 -0.304 8.574 -0.460 1955 10 3.889 -1.993 0 0 3.889 -1.993 2.769 -1.399 1955 11 -3.944 -4.970 0 0 -3.944 -4.970 -5.942 -5.254 1955 12 0.750 2.894 1 0 NaN NaN -8.319 -4.462 1956 1 NaN NaN NaN NaN NaN NaN -7.992 -2.124 1956 2 NaN NaN NaN NaN NaN NaN -5.524 -2.857 1956 3 -0.167 -1.103 0 0 -0.167 -1.103 -2.043 -1.266 1956 4 3.349 -1.110 1 0 NaN NaN 2.753 0.008 1956 5 8.844 0.069 1 0 NaN NaN 7.548 0.486 1956 6 10.810 -1.390 1 0 NaN NaN 9.146 -1.340 1956 7 15.222 0.921 0 0 15.222 0.921 13.026 0.439 1956 8 13.444 -0.524 0 0 13.444 -0.524 12.513 0.257 1956 9 NaN NaN NaN NaN NaN NaN 8.876 -0.158 1956 10 NaN NaN NaN NaN NaN NaN 2.456 -1.712 1956 11 NaN NaN NaN NaN NaN NaN -0.693 -0.005 1956 12 NaN NaN NaN NaN NaN NaN -4.287 -0.430 1957 1 NaN NaN NaN NaN NaN NaN -9.435 -3.567 1957 2 NaN NaN NaN NaN NaN NaN -4.281 -1.615 1957 3 NaN NaN NaN NaN NaN NaN -0.222 0.554 1957 4 NaN NaN NaN NaN NaN NaN 2.768 0.022 1957 5 NaN NaN NaN NaN NaN NaN 8.241 1.179 1957 6 NaN NaN NaN NaN NaN NaN 10.492 0.006 1957 7 NaN NaN NaN NaN NaN NaN 11.601 -0.987 1957 8 NaN NaN NaN NaN NaN NaN 13.382 1.127