% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 21487 % Primary Name: LUGA % Record Type: TAVG % Country: Russia % Latitude: 58.73300 +/- 0.00050 % Longitude: 29.88300 +/- 0.00050 % Elevation (m): 103.90 +/- 0.05 % # of Months: 12 % % IDs: gsod - 261680-99999 % usaf - 261680 % % Sources: Global Summary of the Day % % Site Hash: 5b48aa9d713ab0daeb7c2e65bf18bee8 % Raw Data Hash: ea1200e3517cfba15db216c957137fae % Adj Data Hash: a08e2801b75e974e6a953821fefe3d1f % % 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 1948 9 NaN NaN NaN NaN NaN NaN 10.474 0.101 1948 10 NaN NaN NaN NaN NaN NaN 4.948 0.310 1948 11 NaN NaN NaN NaN NaN NaN 0.119 1.027 1948 12 NaN NaN NaN NaN NaN NaN -2.206 3.480 1949 1 NaN NaN NaN NaN NaN NaN -3.303 5.778 1949 2 NaN NaN NaN NaN NaN NaN -4.274 4.142 1949 3 NaN NaN NaN NaN NaN NaN -2.598 1.289 1949 4 NaN NaN NaN NaN NaN NaN 4.824 1.251 1949 5 NaN NaN NaN NaN NaN NaN 13.190 2.637 1949 6 NaN NaN NaN NaN NaN NaN 14.737 -0.578 1949 7 NaN NaN NaN NaN NaN NaN 16.235 -0.696 1949 8 NaN NaN NaN NaN NaN NaN 14.339 -1.173 1949 9 11.247 1.015 1 0 NaN NaN 12.399 2.026 1949 10 5.027 0.529 0 0 5.027 0.529 5.485 0.847 1949 11 1.082 2.131 0 0 1.082 2.131 1.371 2.279 1949 12 -1.492 4.335 0 0 -1.492 4.335 -1.650 4.036 1950 1 -15.627 -6.406 1 0 NaN NaN -15.886 -6.806 1950 2 -5.650 2.905 0 0 -5.650 2.905 -5.959 2.456 1950 3 -2.393 1.634 0 0 -2.393 1.634 -2.631 1.256 1950 4 7.333 3.900 0 0 7.333 3.900 7.670 4.097 1950 5 10.538 0.125 1 0 NaN NaN 10.777 0.223 1950 6 13.227 -1.949 1 0 NaN NaN 14.330 -0.985 1950 7 NaN NaN NaN NaN NaN NaN 14.963 -1.968 1950 8 NaN NaN NaN NaN NaN NaN 14.314 -1.199 1950 9 NaN NaN NaN NaN NaN NaN 11.368 0.996 1950 10 NaN NaN NaN NaN NaN NaN 5.459 0.821 1950 11 -0.230 0.818 0 0 -0.230 0.818 0.372 1.281 1950 12 1.308 7.134 1 0 NaN NaN -3.042 2.644 1951 1 NaN NaN NaN NaN NaN NaN -9.968 -0.887 1951 2 NaN NaN NaN NaN NaN NaN -8.509 -0.094 1951 3 NaN NaN NaN NaN NaN NaN -5.639 -1.752 1951 4 NaN NaN NaN NaN NaN NaN 6.168 2.595 1951 5 NaN NaN NaN NaN NaN NaN 7.736 -2.817 1951 6 NaN NaN NaN NaN NaN NaN 14.788 -0.527 1951 7 NaN NaN NaN NaN NaN NaN 15.556 -1.374 1951 8 NaN NaN NaN NaN NaN NaN 17.334 1.821 1951 9 NaN NaN NaN NaN NaN NaN 11.603 1.231 1951 10 NaN NaN NaN NaN NaN NaN 4.389 -0.249 1951 11 NaN NaN NaN NaN NaN NaN -2.020 -1.112 1951 12 NaN NaN NaN NaN NaN NaN -1.209 4.478