% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 3011 % Primary Name: LOUBET COAST % Record Type: TAVG % Country: Antarctica % Latitude: -66.90000 +/- 0.05000 % Longitude: -66.80000 +/- 0.05000 % Elevation (m): 7.00 +/- 0.50 % # of Months: 30 % % IDs: hadcru - 889560 % wmssc - 889560 % % Sources: Hadley Centre Data Release % World Monthly Surface Station Climatology % % Site Hash: 77e90f9ab116abe6e6357922c0578c75 % Raw Data Hash: f624c2c9088b8522da0767112baa588f % Adj Data Hash: f624c2c9088b8522da0767112baa588f % % 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 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 NaN NaN NaN NaN NaN NaN -6.668 2.413 1955 10 NaN NaN NaN NaN NaN NaN -4.372 1.924 1955 11 NaN NaN NaN NaN NaN NaN -3.574 -0.484 1955 12 NaN NaN NaN NaN NaN NaN -0.572 0.299 1956 1 NaN NaN NaN NaN NaN NaN 1.370 1.425 1956 2 NaN NaN NaN NaN NaN NaN 0.434 0.873 1956 3 NaN NaN NaN NaN NaN NaN -0.271 1.350 1956 4 NaN NaN NaN NaN NaN NaN -0.344 3.544 1956 5 NaN NaN NaN NaN NaN NaN -1.251 5.036 1956 6 NaN NaN NaN NaN NaN NaN -3.242 5.794 1956 7 -7.800 4.170 0 0 -7.800 4.170 -7.787 3.260 1956 8 -6.400 5.908 0 0 -6.400 5.908 -5.269 6.115 1956 9 -9.900 0.105 0 0 -9.900 0.105 -7.150 1.931 1956 10 -5.100 2.120 0 0 -5.100 2.120 -3.470 2.826 1956 11 -2.700 1.314 0 0 -2.700 1.314 -1.309 1.781 1956 12 -1.700 0.094 0 0 -1.700 0.094 -0.232 0.639 1957 1 -0.100 0.878 0 0 -0.100 0.878 1.072 1.127 1957 2 -0.300 1.064 0 0 -0.300 1.064 0.728 1.168 1957 3 -2.900 -0.355 0 0 -2.900 -0.355 -1.085 0.536 1957 4 -2.400 2.411 0 0 -2.400 2.411 -1.307 2.581 1957 5 -5.700 1.511 0 0 -5.700 1.511 -5.672 0.615 1957 6 -14.100 -4.140 0 0 -14.100 -4.140 -15.451 -6.415 1957 7 -15.800 -3.830 0 0 -15.800 -3.830 -15.577 -4.531 1957 8 -14.900 -2.592 0 0 -14.900 -2.592 -13.733 -2.349 1957 9 -7.200 2.805 0 0 -7.200 2.805 -5.253 3.828 1957 10 -9.500 -2.280 0 0 -9.500 -2.280 -9.065 -2.769 1957 11 -1.800 2.214 0 0 -1.800 2.214 -1.050 2.040 1957 12 -1.300 0.494 0 0 -1.300 0.494 -0.737 0.133 1958 1 -0.300 0.678 0 0 -0.300 0.678 0.529 0.584 1958 2 -1.500 -0.136 0 0 -1.500 -0.136 -0.129 0.311 1958 3 -3.200 -0.655 0 0 -3.200 -0.655 -1.980 -0.359 1958 4 -5.200 -0.389 0 0 -5.200 -0.389 -3.937 -0.049 1958 5 -10.700 -3.489 0 0 -10.700 -3.489 -10.155 -3.867 1958 6 -14.500 -4.540 0 0 -14.500 -4.540 -15.082 -6.046 1958 7 -15.900 -3.930 0 0 -15.900 -3.930 -15.820 -4.773 1958 8 -18.800 -6.492 0 0 -18.800 -6.492 -17.569 -6.185 1958 9 -15.400 -5.395 0 0 -15.400 -5.395 -13.579 -4.498 1958 10 -6.800 0.420 0 0 -6.800 0.420 -5.826 0.470 1958 11 -1.900 2.114 0 0 -1.900 2.114 -1.106 1.984 1958 12 -2.700 -0.906 0 0 -2.700 -0.906 -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 1959 7 NaN NaN NaN NaN NaN NaN -19.495 -8.449 1959 8 NaN NaN NaN NaN NaN NaN -12.846 -1.462 1959 9 NaN NaN NaN NaN NaN NaN -10.529 -1.448 1959 10 NaN NaN NaN NaN NaN NaN -5.033 1.263 1959 11 NaN NaN NaN NaN NaN NaN -4.510 -1.420 1959 12 NaN NaN NaN NaN NaN NaN 0.001 0.872