% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 22792 % Primary Name: GRYTVIKEN/FLAT BLUF % Record Type: TAVG % Country: South Georgia and South Sandwich Islands [United Kingdom] % Latitude: -54.26700 +/- 0.00050 % Longitude: -36.50000 +/- 0.00050 % Elevation (m): 10.00 +/- 0.05 % # of Months: 25 % % IDs: gsod - 889020-99999 % usaf - 889020 % % Sources: Global Summary of the Day % % Site Hash: 2339717034ef5dbf2f465df7028e7bb8 % Raw Data Hash: f1351a814bb6e12d8a29cf6724f9a8fc % Adj Data Hash: 141997be93c6da1a4afcf53f02e3736a % % 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 1987 6 NaN NaN NaN NaN NaN NaN -1.507 -0.421 1987 7 NaN NaN NaN NaN NaN NaN -2.922 -1.219 1987 8 NaN NaN NaN NaN NaN NaN -1.789 -0.211 1987 9 NaN NaN NaN NaN NaN NaN -1.742 -1.382 1987 10 NaN NaN NaN NaN NaN NaN -0.112 -1.209 1987 11 NaN NaN NaN NaN NaN NaN 3.145 0.776 1987 12 NaN NaN NaN NaN NaN NaN 4.144 0.843 1988 1 NaN NaN NaN NaN NaN NaN 4.709 0.290 1988 2 NaN NaN NaN NaN NaN NaN 5.403 0.516 1988 3 NaN NaN NaN NaN NaN NaN 5.803 1.639 1988 4 NaN NaN NaN NaN NaN NaN 0.846 -1.244 1988 5 NaN NaN NaN NaN NaN NaN 0.299 0.317 1988 6 -1.199 -0.206 0 0 -1.199 -0.206 -0.609 0.478 1988 7 -1.021 0.589 1 0 NaN NaN -0.314 1.389 1988 8 -2.855 -1.370 1 0 NaN NaN -2.463 -0.885 1988 9 -1.452 -1.185 0 0 -1.452 -1.185 -0.808 -0.447 1988 10 0.048 -1.142 0 0 0.048 -1.142 0.080 -1.017 1988 11 2.524 0.062 0 0 2.524 0.062 2.367 -0.002 1988 12 4.209 0.815 0 0 4.209 0.815 3.684 0.383 1989 1 5.282 0.770 0 0 5.282 0.770 4.637 0.218 1989 2 4.575 -0.404 0 0 4.575 -0.404 4.367 -0.520 1989 3 5.608 1.351 0 0 5.608 1.351 5.247 1.083 1989 4 1.630 -0.553 0 0 1.630 -0.553 1.628 -0.463 1989 5 2.676 2.601 0 0 2.676 2.601 2.647 2.664 1989 6 1.304 2.297 0 0 1.304 2.297 1.365 2.451 1989 7 0.274 1.884 1 0 NaN NaN 0.286 1.989 1989 8 -0.414 1.072 0 0 -0.414 1.072 -0.184 1.394 1989 9 0.556 0.823 0 0 0.556 0.823 0.621 0.981 1989 10 3.440 2.251 1 0 NaN NaN 2.455 1.358 1989 11 3.043 0.581 0 0 3.043 0.581 2.669 0.300 1989 12 4.961 1.566 0 0 4.961 1.566 4.024 0.722 1990 1 3.833 -0.678 1 0 NaN NaN 5.350 0.932 1990 2 6.425 1.445 0 0 6.425 1.445 5.973 1.085 1990 3 5.869 1.612 0 0 5.869 1.612 5.465 1.301 1990 4 1.485 -0.698 0 0 1.485 -0.698 1.668 -0.422 1990 5 -1.683 -1.758 0 0 -1.683 -1.758 -1.156 -1.138 1990 6 8.101 9.095 1 0 NaN NaN 1.015 2.101 1990 7 NaN NaN NaN NaN NaN NaN 0.062 1.765 1990 8 NaN NaN NaN NaN NaN NaN -0.778 0.800 1990 9 NaN NaN NaN NaN NaN NaN -0.025 0.335 1990 10 NaN NaN NaN NaN NaN NaN 2.108 1.011 1990 11 NaN NaN NaN NaN NaN NaN 3.518 1.149 1990 12 NaN NaN NaN NaN NaN NaN 3.114 -0.187 1991 1 NaN NaN NaN NaN NaN NaN 5.481 1.062 1991 2 NaN NaN NaN NaN NaN NaN 5.424 0.537 1991 3 NaN NaN NaN NaN NaN NaN 3.689 -0.475 1991 4 NaN NaN NaN NaN NaN NaN 2.731 0.641 1991 5 NaN NaN NaN NaN NaN NaN 0.346 0.364 1991 6 NaN NaN NaN NaN NaN NaN -2.102 -1.016