% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 2984 % Primary Name: CAMP CHARCOT % Record Type: TAVG % Country: Antarctica % Latitude: -69.40000 +/- 0.05000 % Longitude: 139.00000 +/- 0.05000 % Elevation (m): 2400.00 +/- 0.50 % # of Months: 21 % % IDs: hadcru - 896430 % wmssc - 896430 % % Sources: Hadley Centre Data Release % World Monthly Surface Station Climatology % % Site Hash: 04d3c0a6eb14b671f762fcaea9f56c2e % Raw Data Hash: 0d32a9d150b75d752bb8c7260bc3f202 % Adj Data Hash: 48f48272dda300d9c90e05723930aecb % % 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 4 NaN NaN NaN NaN NaN NaN -41.017 1.223 1956 5 NaN NaN NaN NaN NaN NaN -42.853 1.126 1956 6 NaN NaN NaN NaN NaN NaN -44.590 -0.245 1956 7 NaN NaN NaN NaN NaN NaN -45.536 -0.976 1956 8 NaN NaN NaN NaN NaN NaN -46.944 -2.218 1956 9 NaN NaN NaN NaN NaN NaN -41.047 2.584 1956 10 NaN NaN NaN NaN NaN NaN -39.962 -0.752 1956 11 NaN NaN NaN NaN NaN NaN -29.160 0.866 1956 12 NaN NaN NaN NaN NaN NaN -20.412 1.925 1957 1 NaN NaN NaN NaN NaN NaN -20.711 0.957 1957 2 NaN NaN NaN NaN NaN NaN -28.018 0.316 1957 3 NaN NaN NaN NaN NaN NaN -36.062 0.538 1957 4 -40.600 1.687 0 0 -40.600 1.687 -40.610 1.630 1957 5 -41.500 2.527 0 0 -41.500 2.527 -42.518 1.462 1957 6 -47.200 -2.808 0 0 -47.200 -2.808 -45.823 -1.478 1957 7 -48.700 -4.093 0 0 -48.700 -4.093 -47.873 -3.314 1957 8 -46.400 -1.626 0 0 -46.400 -1.626 -45.910 -1.183 1957 9 -43.900 -0.222 0 0 -43.900 -0.222 -43.132 0.499 1957 10 -37.400 1.857 0 0 -37.400 1.857 -38.077 1.132 1957 11 -30.300 -0.227 0 0 -30.300 -0.227 -28.975 1.050 1957 12 -21.300 1.084 0 0 -21.300 1.084 -20.770 1.566 1958 1 -22.400 -0.684 0 0 -22.400 -0.684 -21.389 0.280 1958 2 -39.600 -11.219 1 0 NaN NaN -28.123 0.211 1958 3 -34.400 2.248 0 0 -34.400 2.248 -34.210 2.391 1958 4 -38.500 3.787 0 0 -38.500 3.787 -38.756 3.484 1958 5 -41.400 2.627 0 0 -41.400 2.627 -41.927 2.053 1958 6 -49.800 -5.408 1 0 NaN NaN -48.804 -4.459 1958 7 -41.700 2.907 0 0 -41.700 2.907 -43.740 0.819 1958 8 -43.200 1.574 0 0 -43.200 1.574 -44.950 -0.223 1958 9 -51.600 -7.922 1 0 NaN NaN -49.049 -5.418 1958 10 -39.700 -0.443 0 0 -39.700 -0.443 -40.318 -1.109 1958 11 -30.500 -0.427 0 0 -30.500 -0.427 -29.949 0.076 1958 12 -23.700 -1.316 0 0 -23.700 -1.316 -23.020 -0.684 1959 1 NaN NaN NaN NaN NaN NaN -22.434 -0.765 1959 2 NaN NaN NaN NaN NaN NaN -28.118 0.216 1959 3 NaN NaN NaN NaN NaN NaN -36.929 -0.329 1959 4 NaN NaN NaN NaN NaN NaN -40.354 1.886 1959 5 NaN NaN NaN NaN NaN NaN -45.253 -1.273 1959 6 NaN NaN NaN NaN NaN NaN -45.652 -1.307 1959 7 NaN NaN NaN NaN NaN NaN -44.485 0.074 1959 8 NaN NaN NaN NaN NaN NaN -47.427 -2.700 1959 9 NaN NaN NaN NaN NaN NaN -47.169 -3.538 1959 10 NaN NaN NaN NaN NaN NaN -41.014 -1.805 1959 11 NaN NaN NaN NaN NaN NaN -31.370 -1.344 1959 12 NaN NaN NaN NaN NaN NaN -21.667 0.670