% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 3039 % Primary Name: ROUX IS ANTARCTICA IS % Record Type: TAVG % Country: Antarctica % Latitude: -65.10000 +/- 0.00050 % Longitude: -65.03300 +/- 0.00050 % Elevation (m): 0.00 +/- 10.00 % # of Months: 24 % % IDs: gsod - 889560-99999 % usaf - 889560 % % Sources: Global Summary of the Day % % Site Hash: 9967a419e4bfc9a294930e24627c1899 % Raw Data Hash: b2457a3cd32ec3388b477493bd86a4c6 % Adj Data Hash: fc274c400c6f9df0d5f251bc3e3d81a3 % % 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 1955 7 NaN NaN NaN NaN NaN NaN -11.300 3.170 1955 8 NaN NaN NaN NaN NaN NaN -11.432 2.695 1955 9 NaN NaN NaN NaN NaN NaN -8.832 2.215 1955 10 NaN NaN NaN NaN NaN NaN -6.245 1.895 1955 11 NaN NaN NaN NaN NaN NaN -5.599 -0.330 1955 12 NaN NaN NaN NaN NaN NaN -3.709 -0.321 1956 1 NaN NaN NaN NaN NaN NaN -1.968 0.889 1956 2 NaN NaN NaN NaN NaN NaN -3.007 0.756 1956 3 NaN NaN NaN NaN NaN NaN -4.289 1.403 1956 4 NaN NaN NaN NaN NaN NaN -5.581 2.745 1956 5 NaN NaN NaN NaN NaN NaN -6.881 3.791 1956 6 NaN NaN NaN NaN NaN NaN -7.354 5.609 1956 7 -7.199 5.029 0 0 -7.199 5.029 -10.638 3.832 1956 8 -6.278 5.607 0 0 -6.278 5.607 -8.311 5.816 1956 9 -9.037 -0.233 0 0 -9.037 -0.233 -8.871 2.176 1956 10 -4.714 1.183 0 0 -4.714 1.183 -5.515 2.625 1956 11 -2.738 0.289 1 0 NaN NaN -3.524 1.745 1956 12 -1.435 -0.290 0 0 -1.435 -0.290 -2.758 0.629 1957 1 0.177 0.791 0 0 0.177 0.791 -2.375 0.482 1957 2 -0.282 1.239 1 0 NaN NaN -2.854 0.909 1957 3 -2.814 0.636 0 0 -2.814 0.636 -4.883 0.808 1957 4 -2.431 3.652 0 0 -2.431 3.652 -5.989 2.337 1957 5 -5.805 2.624 0 0 -5.805 2.624 -9.456 1.215 1957 6 -14.133 -3.412 0 0 -14.133 -3.412 -17.335 -4.372 1957 7 -16.529 -4.301 0 0 -16.529 -4.301 -17.691 -3.221 1957 8 -14.860 -2.975 0 0 -14.860 -2.975 -15.479 -1.352 1957 9 -6.917 1.888 0 0 -6.917 1.888 -7.719 3.327 1957 10 -9.557 -3.660 0 0 -9.557 -3.660 -10.290 -2.150 1957 11 -1.857 1.169 0 0 -1.857 1.169 -3.690 1.579 1957 12 -1.385 -0.240 0 0 -1.385 -0.240 -3.330 0.057 1958 1 -0.285 0.330 0 0 -0.285 0.330 -2.545 0.312 1958 2 -1.393 0.128 0 0 -1.393 0.128 -4.140 -0.377 1958 3 -3.152 0.297 0 0 -3.152 0.297 -6.048 -0.356 1958 4 -5.020 1.064 0 0 -5.020 1.064 -8.417 -0.091 1958 5 -10.989 -2.560 0 0 -10.989 -2.560 -14.795 -4.124 1958 6 -14.780 -4.059 0 0 -14.780 -4.059 -19.446 -6.483 1958 7 NaN NaN NaN NaN NaN NaN -20.720 -6.250 1958 8 NaN NaN NaN NaN NaN NaN -19.126 -4.999 1958 9 NaN NaN NaN NaN NaN NaN -15.041 -3.995 1958 10 NaN NaN NaN NaN NaN NaN -7.694 0.446 1958 11 NaN NaN NaN NaN NaN NaN -3.755 1.514 1958 12 NaN NaN NaN NaN NaN NaN -4.138 -0.750 1959 1 NaN NaN NaN NaN NaN NaN -4.246 -1.389 1959 2 NaN NaN NaN NaN NaN NaN -5.898 -2.135 1959 3 NaN NaN NaN NaN NaN NaN -5.743 -0.051 1959 4 NaN NaN NaN NaN NaN NaN -13.510 -5.184 1959 5 NaN NaN NaN NaN NaN NaN -15.592 -4.921 1959 6 NaN NaN NaN NaN NaN NaN -13.364 -0.401