% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 3029 % Primary Name: HORSE SHOE IS ANTARCTICA IS % Record Type: TAVG % Country: Antarctica % Latitude: -66.33300 +/- 0.00050 % Longitude: -66.78300 +/- 0.00050 % Elevation (m): 0.00 +/- 10.00 % # of Months: 32 % % IDs: gsod - 889590-99999 % usaf - 889590 % % Sources: Global Summary of the Day % % Site Hash: 24c6cf2392027dc16ff00005da44a103 % Raw Data Hash: b3985fcb8e36035b6658e4b2b1228000 % Adj Data Hash: 53886141f6f8c0cde91e3c4a2ab383aa % % 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 1954 9 NaN NaN NaN NaN NaN NaN -11.267 -2.186 1954 10 NaN NaN NaN NaN NaN NaN -4.432 1.863 1954 11 NaN NaN NaN NaN NaN NaN -2.136 0.954 1954 12 NaN NaN NaN NaN NaN NaN -0.533 0.338 1955 1 NaN NaN NaN NaN NaN NaN 0.453 0.508 1955 2 NaN NaN NaN NaN NaN NaN -0.203 0.237 1955 3 NaN NaN NaN NaN NaN NaN -0.801 0.820 1955 4 NaN NaN NaN NaN NaN NaN -2.493 1.395 1955 5 NaN NaN NaN NaN NaN NaN -4.879 1.409 1955 6 NaN NaN NaN NaN NaN NaN -9.798 -0.762 1955 7 NaN NaN NaN NaN NaN NaN -8.117 2.929 1955 8 NaN NaN NaN NaN NaN NaN -8.731 2.654 1955 9 -7.584 2.758 0 0 -7.584 2.758 -6.668 2.413 1955 10 -5.366 2.192 0 0 -5.366 2.192 -4.372 1.924 1955 11 -8.278 -3.926 1 0 NaN NaN -3.574 -0.484 1955 12 NaN NaN NaN NaN NaN NaN -0.572 0.299 1956 1 2.877 4.194 1 0 NaN NaN 1.370 1.425 1956 2 0.049 1.751 1 0 NaN NaN 0.434 0.873 1956 3 -1.822 1.061 0 0 -1.822 1.061 -0.271 1.350 1956 4 -1.559 3.590 0 0 -1.559 3.590 -0.344 3.544 1956 5 NaN NaN NaN NaN NaN NaN -1.251 5.036 1956 6 -4.213 6.085 0 0 -4.213 6.085 -3.242 5.794 1956 7 -9.491 2.817 0 0 -9.491 2.817 -7.787 3.260 1956 8 -5.609 7.036 0 0 -5.609 7.036 -5.269 6.115 1956 9 -7.746 2.596 0 0 -7.746 2.596 -7.150 1.931 1956 10 -3.824 3.733 0 0 -3.824 3.733 -3.470 2.826 1956 11 -1.659 2.692 0 0 -1.659 2.692 -1.309 1.781 1956 12 -0.081 2.052 0 0 -0.081 2.052 -0.232 0.639 1957 1 1.740 3.057 0 0 1.740 3.057 1.072 1.127 1957 2 0.613 2.315 0 0 0.613 2.315 0.728 1.168 1957 3 -2.434 0.449 0 0 -2.434 0.449 -1.085 0.536 1957 4 -2.737 2.412 0 0 -2.737 2.412 -1.307 2.581 1957 5 -8.332 -0.783 0 0 -8.332 -0.783 -5.672 0.615 1957 6 -19.880 -9.582 0 0 -19.880 -9.582 -15.451 -6.415 1957 7 -17.982 -5.674 0 0 -17.982 -5.674 -15.577 -4.531 1957 8 -15.504 -2.858 0 0 -15.504 -2.858 -13.733 -2.349 1957 9 -6.159 4.184 0 0 -6.159 4.184 -5.253 3.828 1957 10 -10.799 -3.242 0 0 -10.799 -3.242 -9.065 -2.769 1957 11 -1.609 2.742 0 0 -1.609 2.742 -1.050 2.040 1957 12 -1.100 1.032 0 0 -1.100 1.032 -0.737 0.133 1958 1 0.631 1.947 0 0 0.631 1.947 0.529 0.584 1958 2 -0.454 1.247 0 0 -0.454 1.247 -0.129 0.311 1958 3 -3.837 -0.954 0 0 -3.837 -0.954 -1.980 -0.359 1958 4 -6.126 -0.977 0 0 -6.126 -0.977 -3.937 -0.049 1958 5 -13.767 -6.218 0 0 -13.767 -6.218 -10.155 -3.867 1958 6 -17.894 -7.597 0 0 -17.894 -7.597 -15.082 -6.046 1958 7 NaN NaN NaN NaN NaN NaN -15.820 -4.773 1958 8 NaN NaN NaN NaN NaN NaN -17.569 -6.185 1958 9 NaN NaN NaN NaN NaN NaN -13.579 -4.498 1958 10 NaN NaN NaN NaN NaN NaN -5.826 0.470 1958 11 NaN NaN NaN NaN NaN NaN -1.106 1.984 1958 12 NaN NaN NaN NaN NaN NaN -1.790 -0.920 1959 1 NaN NaN NaN NaN NaN NaN -1.369 -1.314 1959 2 NaN NaN NaN NaN NaN NaN -3.061 -2.621 1959 3 NaN NaN NaN NaN NaN NaN -1.128 0.493 1959 4 NaN NaN NaN NaN NaN NaN -10.979 -7.092 1959 5 NaN NaN NaN NaN NaN NaN -12.392 -6.105 1959 6 NaN NaN NaN NaN NaN NaN -7.487 1.549