% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 166904 % Primary Name: LITTLE JEANA STATION % Record Type: TAVG % Country: Antarctica % State: ZZ % Latitude: -81.38300 +/- 0.00050 % Longitude: 170.75000 +/- 0.00050 % Elevation (m): 53.90 +/- 0.05 % # of Months: 8 % % IDs: gsod - 999999-88703 % wban - 88703 % % Sources: US First Order Summary of the Day % Global Summary of the Day % % Site Hash: 6be2f3c2fb4671602c3b558a49c563d4 % Raw Data Hash: 4387ebf3d83911fbbc7c83faca53114e % Adj Data Hash: 944710575726b98d4a46fb768a9b0208 % % 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 1963 10 NaN NaN NaN NaN NaN NaN -28.208 0.492 1963 11 NaN NaN NaN NaN NaN NaN -13.856 1.971 1963 12 NaN NaN NaN NaN NaN NaN -7.752 -0.448 1964 1 NaN NaN NaN NaN NaN NaN -9.075 -1.356 1964 2 NaN NaN NaN NaN NaN NaN -17.613 -1.050 1964 3 NaN NaN NaN NaN NaN NaN -28.352 -0.197 1964 4 NaN NaN NaN NaN NaN NaN -31.969 1.064 1964 5 NaN NaN NaN NaN NaN NaN -37.786 -2.823 1964 6 NaN NaN NaN NaN NaN NaN -31.195 3.790 1964 7 NaN NaN NaN NaN NaN NaN -34.791 3.051 1964 8 NaN NaN NaN NaN NaN NaN -42.718 -3.093 1964 9 NaN NaN NaN NaN NaN NaN -36.656 0.259 1964 10 -27.876 -0.037 1 0 NaN NaN -28.374 0.325 1964 11 -14.087 0.879 0 0 -14.087 0.879 -14.332 1.494 1964 12 -7.235 -0.793 0 0 -7.235 -0.793 -7.568 -0.265 1965 1 -7.394 -0.535 0 0 -7.394 -0.535 -8.043 -0.324 1965 2 -15.012 0.691 1 0 NaN NaN -15.135 1.429 1965 3 NaN NaN NaN NaN NaN NaN -30.415 -2.260 1965 4 NaN NaN NaN NaN NaN NaN -31.932 1.101 1965 5 NaN NaN NaN NaN NaN NaN -39.949 -4.987 1965 6 NaN NaN NaN NaN NaN NaN -37.228 -2.243 1965 7 NaN NaN NaN NaN NaN NaN -35.494 2.348 1965 8 NaN NaN NaN NaN NaN NaN -36.811 2.815 1965 9 NaN NaN NaN NaN NaN NaN -37.731 -0.815 1965 10 -26.281 1.557 0 0 -26.281 1.557 -28.242 0.457 1965 11 NaN NaN NaN NaN NaN NaN -15.435 0.391 1965 12 -5.269 1.174 0 0 -5.269 1.174 -6.384 0.919 1966 1 -9.179 -2.320 1 0 NaN NaN -7.558 0.161 1966 2 NaN NaN NaN NaN NaN NaN -14.385 2.179 1966 3 NaN NaN NaN NaN NaN NaN -23.371 4.784 1966 4 NaN NaN NaN NaN NaN NaN -31.994 1.040 1966 5 NaN NaN NaN NaN NaN NaN -39.641 -4.679 1966 6 NaN NaN NaN NaN NaN NaN -32.119 2.866 1966 7 NaN NaN NaN NaN NaN NaN -36.297 1.545 1966 8 NaN NaN NaN NaN NaN NaN -41.627 -2.002 1966 9 NaN NaN NaN NaN NaN NaN -37.286 -0.371 1966 10 NaN NaN NaN NaN NaN NaN -28.482 0.218 1966 11 NaN NaN NaN NaN NaN NaN -15.467 0.359 1966 12 NaN NaN NaN NaN NaN NaN -7.204 0.099 1967 1 NaN NaN NaN NaN NaN NaN -5.467 2.252