% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 166910 % Primary Name: LITTLE AMERICA % Record Type: TAVG % Country: Antarctica % State: ZZ % Latitude: -78.20000 +/- 0.00500 % Longitude: -162.25000 +/- 0.00500 % Elevation (m): 32.00 +/- 0.05 % # of Months: 36 % % IDs: ghcnd - AYW00067601 % gsod - 999999-67601 % ncdc - 20028964 % wban - 67601 % % Sources: US First Order Summary of the Day % Global Historical Climatology Network - Daily % Global Summary of the Day % Multi-network Metadata System % % Site Hash: c7c3e8d9f9db4f14f003bedae73890f5 % Raw Data Hash: 6988e8a8f0c70440324e4d6e42866c68 % Adj Data Hash: 1b4db9f19417ebcd90f3bc688062fb53 % % 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 2 -13.188 -0.514 1 0 NaN NaN -10.933 1.208 1956 3 -18.334 3.504 0 0 -18.334 3.504 -17.951 3.354 1956 4 -30.448 -3.701 0 0 -30.448 -3.701 -28.847 -2.633 1956 5 -28.498 0.588 0 0 -28.498 0.588 -28.477 0.076 1956 6 -35.085 -5.740 0 0 -35.085 -5.740 -33.755 -4.943 1956 7 -30.833 1.870 0 0 -30.833 1.870 -30.586 1.584 1956 8 -41.013 -5.241 0 0 -41.013 -5.241 -40.443 -5.204 1956 9 -30.017 3.265 0 0 -30.017 3.265 -29.886 2.862 1956 10 -29.455 -4.533 0 0 -29.455 -4.533 -28.716 -4.328 1956 11 -17.372 -3.374 0 0 -17.372 -3.374 -15.957 -2.492 1956 12 -5.171 2.347 0 0 -5.171 2.347 -4.598 2.387 1957 1 -6.088 1.286 0 0 -6.088 1.286 -5.754 1.087 1957 2 -12.086 0.588 0 0 -12.086 0.588 -10.825 1.315 1957 3 -25.948 -4.110 0 0 -25.948 -4.110 -24.847 -3.542 1957 4 -32.775 -6.028 0 0 -32.775 -6.028 -31.427 -5.213 1957 5 -30.753 -1.667 0 0 -30.753 -1.667 -30.659 -2.106 1957 6 -23.892 5.454 0 0 -23.892 5.454 -24.330 4.482 1957 7 -35.537 -2.834 0 0 -35.537 -2.834 -35.112 -2.942 1957 8 -34.557 1.215 0 0 -34.557 1.215 -33.715 1.525 1957 9 -34.188 -0.907 0 0 -34.188 -0.907 -33.363 -0.615 1957 10 -19.510 5.412 0 0 -19.510 5.412 -20.437 3.951 1957 11 -12.553 1.444 0 0 -12.553 1.444 -12.141 1.323 1957 12 -4.502 3.016 0 0 -4.502 3.016 -4.140 2.845 1958 1 -7.724 -0.351 0 0 -7.724 -0.351 -6.816 0.025 1958 2 -9.482 3.192 0 0 -9.482 3.192 -8.073 4.067 1958 3 -24.780 -2.941 0 0 -24.780 -2.941 -23.690 -2.385 1958 4 -21.254 5.493 0 0 -21.254 5.493 -20.846 5.368 1958 5 -29.135 -0.049 0 0 -29.135 -0.049 -29.147 -0.594 1958 6 -28.358 0.987 0 0 -28.358 0.987 -28.403 0.410 1958 7 -37.174 -4.471 0 0 -37.174 -4.471 -36.612 -4.442 1958 8 -35.653 0.119 0 0 -35.653 0.119 -35.800 -0.561 1958 9 -35.348 -2.067 0 0 -35.348 -2.067 -34.940 -2.192 1958 10 -27.127 -2.206 0 0 -27.127 -2.206 -26.855 -2.467 1958 11 -14.017 -0.019 0 0 -14.017 -0.019 -13.565 -0.101 1958 12 -7.271 0.247 0 0 -7.271 0.247 -7.100 -0.115 1959 1 -9.538 -2.164 1 0 NaN NaN -7.533 -0.692 1959 2 NaN NaN NaN NaN NaN NaN -10.911 1.230 1959 3 NaN NaN NaN NaN NaN NaN -19.690 1.616 1959 4 NaN NaN NaN NaN NaN NaN -21.843 4.371 1959 5 NaN NaN NaN NaN NaN NaN -30.363 -1.810 1959 6 NaN NaN NaN NaN NaN NaN -28.700 0.112 1959 7 NaN NaN NaN NaN NaN NaN -30.264 1.906 1959 8 NaN NaN NaN NaN NaN NaN -38.786 -3.547 1959 9 NaN NaN NaN NaN NaN NaN -32.960 -0.212 1959 10 NaN NaN NaN NaN NaN NaN -30.301 -5.913 1959 11 NaN NaN NaN NaN NaN NaN -15.598 -2.134 1959 12 NaN NaN NaN NaN NaN NaN -6.512 0.472 1960 1 NaN NaN NaN NaN NaN NaN -8.534 -1.693