% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 2881 % Primary Name: KOMSOMOLSKAYA % Record Type: TAVG % Country: Antarctica % Latitude: -78.10000 +/- 0.05000 % Longitude: 97.50000 +/- 0.05000 % Elevation (m): 3540.00 +/- 0.50 % # of Months: 18 % % IDs: hadcru - 895940 % wmssc - 895940 % % Sources: Hadley Centre Data Release % World Monthly Surface Station Climatology % % Site Hash: 8c6fda686065b9bf3b1cbba497fb4f2b % Raw Data Hash: b138500767b824c55aa231f03cab596d % Adj Data Hash: b138500767b824c55aa231f03cab596d % % 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 1956 11 NaN NaN NaN NaN NaN NaN -40.922 1.107 1956 12 NaN NaN NaN NaN NaN NaN -29.510 2.494 1957 1 NaN NaN NaN NaN NaN NaN -30.860 1.256 1957 2 NaN NaN NaN NaN NaN NaN -41.690 1.265 1957 3 NaN NaN NaN NaN NaN NaN -54.382 0.404 1957 4 NaN NaN NaN NaN NaN NaN -53.631 7.147 1957 5 NaN NaN NaN NaN NaN NaN -61.028 1.414 1957 6 NaN NaN NaN NaN NaN NaN -55.812 6.288 1957 7 NaN NaN NaN NaN NaN NaN -61.826 2.240 1957 8 NaN NaN NaN NaN NaN NaN -58.032 6.404 1957 9 NaN NaN NaN NaN NaN NaN -56.457 5.977 1957 10 NaN NaN NaN NaN NaN NaN -49.697 5.251 1957 11 -40.400 0.786 0 0 -40.400 0.786 -39.632 2.397 1957 12 -32.000 -0.840 0 0 -32.000 -0.840 -32.147 -0.144 1958 1 -31.400 -0.127 0 0 -31.400 -0.127 -31.460 0.655 1958 2 -45.000 -2.889 0 0 -45.000 -2.889 -44.525 -1.570 1958 3 -53.000 0.943 0 0 -53.000 0.943 -53.296 1.490 1958 4 -56.600 3.335 0 0 -56.600 3.335 -58.356 2.423 1958 5 -59.200 2.399 0 0 -59.200 2.399 -60.816 1.627 1958 6 -65.300 -4.043 0 0 -65.300 -4.043 -65.570 -3.470 1958 7 -62.000 1.223 0 0 -62.000 1.223 -63.941 0.125 1958 8 -65.700 -2.107 0 0 -65.700 -2.107 -67.576 -3.140 1958 9 -61.700 -0.109 0 0 -61.700 -0.109 -63.124 -0.690 1958 10 -55.300 -1.195 0 0 -55.300 -1.195 -56.453 -1.505 1958 11 -42.000 -0.814 0 0 -42.000 -0.814 -42.066 -0.037 1958 12 -33.600 -2.440 0 0 -33.600 -2.440 -33.238 -1.235 1959 1 -32.800 -1.527 0 0 -32.800 -1.527 -34.071 -1.956 1959 2 -40.600 1.511 0 0 -40.600 1.511 -42.161 0.794 1959 3 NaN NaN NaN NaN NaN NaN -51.689 3.097 1959 4 NaN NaN NaN NaN NaN NaN -58.326 2.453 1959 5 NaN NaN NaN NaN NaN NaN -61.607 0.835 1959 6 NaN NaN NaN NaN NaN NaN -63.118 -1.019 1959 7 NaN NaN NaN NaN NaN NaN -65.512 -1.446 1959 8 NaN NaN NaN NaN NaN NaN -65.655 -1.219 1959 9 NaN NaN NaN NaN NaN NaN -65.670 -3.236 1959 10 NaN NaN NaN NaN NaN NaN -55.362 -0.414 1959 11 -41.100 0.086 0 0 -41.100 0.086 -42.799 -0.770 1959 12 -29.200 1.960 0 0 -29.200 1.960 -30.843 1.160 1960 1 NaN NaN NaN NaN NaN NaN -34.389 -2.273 1960 2 NaN NaN NaN NaN NaN NaN -42.678 0.276 1960 3 NaN NaN NaN NaN NaN NaN -57.863 -3.077 1960 4 NaN NaN NaN NaN NaN NaN -61.645 -0.867 1960 5 NaN NaN NaN NaN NaN NaN -64.359 -1.917 1960 6 NaN NaN NaN NaN NaN NaN -64.384 -2.284 1960 7 NaN NaN NaN NaN NaN NaN -66.835 -2.769 1960 8 NaN NaN NaN NaN NaN NaN -66.550 -2.114 1960 9 NaN NaN NaN NaN NaN NaN -62.896 -0.462 1960 10 NaN NaN NaN NaN NaN NaN -56.299 -1.352 1960 11 NaN NaN NaN NaN NaN NaN -43.141 -1.112 1960 12 NaN NaN NaN NaN NaN NaN -33.120 -1.116