% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 4 % Primary Name: AWS: ALLISON (8900) % Record Type: TAVG % Country: Antarctica % Latitude: -89.80000 +/- 0.05000 % Longitude: -60.00000 +/- 0.05000 % Elevation (m): 2835.00 +/- 0.50 % # of Months: 12 % % IDs: wmssc - 899038 % % Sources: World Monthly Surface Station Climatology % % Site Hash: 8a6873885ac0688780706f3f4159ee41 % Raw Data Hash: 23e5ec6a7d0166a6d94aa503ab0fba04 % Adj Data Hash: 23e5ec6a7d0166a6d94aa503ab0fba04 % % 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 1985 2 NaN NaN NaN NaN NaN NaN -40.061 -1.171 1985 3 NaN NaN NaN NaN NaN NaN -51.244 0.107 1985 4 NaN NaN NaN NaN NaN NaN -54.224 0.986 1985 5 NaN NaN NaN NaN NaN NaN -56.915 -1.211 1985 6 NaN NaN NaN NaN NaN NaN -52.980 3.128 1985 7 NaN NaN NaN NaN NaN NaN -60.063 -2.204 1985 8 NaN NaN NaN NaN NaN NaN -56.563 1.335 1985 9 NaN NaN NaN NaN NaN NaN -59.079 -2.307 1985 10 NaN NaN NaN NaN NaN NaN -49.556 -0.380 1985 11 NaN NaN NaN NaN NaN NaN -38.762 -1.800 1985 12 NaN NaN NaN NaN NaN NaN -30.075 -3.001 1986 1 NaN NaN NaN NaN NaN NaN -26.663 0.843 1986 2 -33.400 5.978 0 0 -33.400 5.978 -34.620 4.270 1986 3 -51.200 0.639 0 0 -51.200 0.639 -50.924 0.427 1986 4 -53.200 2.498 0 0 -53.200 2.498 -52.011 3.199 1986 5 -59.900 -3.708 0 0 -59.900 -3.708 -57.813 -2.110 1986 6 -59.200 -2.604 0 0 -59.200 -2.604 -59.974 -3.865 1986 7 NaN NaN NaN NaN NaN NaN -58.390 -0.531 1986 8 NaN NaN NaN NaN NaN NaN -57.115 0.782 1986 9 NaN NaN NaN NaN NaN NaN -62.124 -5.352 1986 10 NaN NaN NaN NaN NaN NaN -50.641 -1.465 1986 11 NaN NaN NaN NaN NaN NaN -37.894 -0.932 1986 12 NaN NaN NaN NaN NaN NaN -28.777 -1.703 1987 1 -24.700 3.295 0 0 -24.700 3.295 -26.406 1.100 1987 2 -38.700 0.678 0 0 -38.700 0.678 -39.225 -0.335 1987 3 -50.500 1.339 0 0 -50.500 1.339 -50.978 0.372 1987 4 -58.100 -2.402 0 0 -58.100 -2.402 -56.442 -1.232 1987 5 -58.900 -2.708 0 0 -58.900 -2.708 -56.843 -1.139 1987 6 -55.900 0.696 0 0 -55.900 0.696 -54.487 1.621 1987 7 -61.400 -3.053 0 0 -61.400 -3.053 -59.521 -1.662 1987 8 NaN NaN NaN NaN NaN NaN -62.603 -4.705 1987 9 NaN NaN NaN NaN NaN NaN -58.344 -1.572 1987 10 NaN NaN NaN NaN NaN NaN -50.374 -1.198 1987 11 NaN NaN NaN NaN NaN NaN -38.681 -1.719 1987 12 NaN NaN NaN NaN NaN NaN -28.211 -1.137 1988 1 NaN NaN NaN NaN NaN NaN -27.272 0.235 1988 2 NaN NaN NaN NaN NaN NaN -40.056 -1.166 1988 3 NaN NaN NaN NaN NaN NaN -48.819 2.532 1988 4 NaN NaN NaN NaN NaN NaN -55.118 0.092 1988 5 NaN NaN NaN NaN NaN NaN -56.851 -1.148 1988 6 NaN NaN NaN NaN NaN NaN -55.092 1.016 1988 7 NaN NaN NaN NaN NaN NaN -59.023 -1.164