% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 2966 % Primary Name: MAUDHEIM ANTARCTICA % Record Type: TAVG % Country: Antarctica % Latitude: -70.95000 +/- 0.00500 % Longitude: -9.10000 +/- 0.00500 % Elevation (m): 37.20 +/- 0.05 % # of Months: 18 % % IDs: gsod - 619030-99999 % usaf - 619030 % % Sources: Global Summary of the Day % % Site Hash: c845abd5acd2df16bce327401cfad828 % Raw Data Hash: 71fc97fce56cbd416625841f752ab651 % Adj Data Hash: ecc2a232ad9da1da24d47ed7f26c6009 % % 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 1949 7 NaN NaN NaN NaN NaN NaN -26.658 -1.313 1949 8 NaN NaN NaN NaN NaN NaN -26.093 -1.030 1949 9 NaN NaN NaN NaN NaN NaN -24.071 -0.656 1949 10 NaN NaN NaN NaN NaN NaN -17.762 0.084 1949 11 NaN NaN NaN NaN NaN NaN -11.603 -0.495 1949 12 NaN NaN NaN NaN NaN NaN -6.101 -0.046 1950 1 NaN NaN NaN NaN NaN NaN -5.805 -0.452 1950 2 NaN NaN NaN NaN NaN NaN -10.308 -0.970 1950 3 NaN NaN NaN NaN NaN NaN -14.174 -0.230 1950 4 NaN NaN NaN NaN NaN NaN NaN NaN 1950 5 NaN NaN NaN NaN NaN NaN -21.180 -0.705 1950 6 NaN NaN NaN NaN NaN NaN -22.216 0.422 1950 7 -30.487 -5.348 1 0 NaN NaN -25.760 -0.415 1950 8 -24.618 0.238 0 0 -24.618 0.238 -25.074 -0.011 1950 9 NaN NaN NaN NaN NaN NaN -23.550 -0.135 1950 10 -17.379 0.260 1 0 NaN NaN -17.903 -0.057 1950 11 -10.738 0.163 0 0 -10.738 0.163 -10.941 0.167 1950 12 -3.852 1.996 1 0 NaN NaN NaN NaN 1951 1 -3.737 1.410 0 0 -3.737 1.410 -4.226 1.127 1951 2 -8.097 1.035 0 0 -8.097 1.035 -8.838 0.500 1951 3 -18.123 -4.385 1 0 NaN NaN NaN NaN 1951 4 -17.093 0.213 0 0 -17.093 0.213 -16.979 0.533 1951 5 -24.636 -4.368 0 0 -24.636 -4.368 -24.000 -3.526 1951 6 -26.175 -3.743 0 0 -26.175 -3.743 -25.576 -2.938 1951 7 -23.547 1.591 0 0 -23.547 1.591 -24.893 0.453 1951 8 -27.928 -3.072 1 0 NaN NaN -24.869 0.194 1951 9 -28.012 -4.803 1 0 NaN NaN -23.830 -0.415 1951 10 -17.831 -0.191 0 0 -17.831 -0.191 -17.689 0.157 1951 11 -9.833 1.068 0 0 -9.833 1.068 -10.154 0.954 1951 12 -6.690 -0.842 1 0 NaN NaN -5.764 0.290 1952 1 -5.509 -0.363 1 0 NaN NaN -5.133 0.221 1952 2 NaN NaN NaN NaN NaN NaN -9.124 0.214 1952 3 NaN NaN NaN NaN NaN NaN NaN NaN 1952 4 NaN NaN NaN NaN NaN NaN -18.256 -0.743 1952 5 NaN NaN NaN NaN NaN NaN -22.131 -1.657 1952 6 NaN NaN NaN NaN NaN NaN -22.993 -0.355 1952 7 NaN NaN NaN NaN NaN NaN -25.246 0.099 1952 8 NaN NaN NaN NaN NaN NaN -24.390 0.673 1952 9 NaN NaN NaN NaN NaN NaN -23.056 0.359 1952 10 NaN NaN NaN NaN NaN NaN -18.240 -0.394 1952 11 NaN NaN NaN NaN NaN NaN -11.813 -0.705 1952 12 NaN NaN NaN NaN NaN NaN -6.197 -0.143 1953 1 NaN NaN NaN NaN NaN NaN NaN NaN