% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 5059 % Primary Name: GROSE ISLAND % Record Type: TAVG % Country: Australia % Latitude: -12.65000 +/- 0.00005 % Longitude: 130.36670 +/- 0.00005 % Elevation (m): 2.70 +/- 0.05 % # of Months: 26 % % IDs: ghcnd - ASN00014187 % gsod - 949999-00066 % wban - 66 % % Sources: Global Historical Climatology Network - Daily % Global Summary of the Day % % Site Hash: e186b5705b4114e1fcf7324582b4ca27 % Raw Data Hash: a5e3f1e0100537120028496276a38827 % Adj Data Hash: 6035e0f6a9b742864629dea33d42bb29 % % 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 1968 10 NaN NaN NaN NaN NaN NaN 27.562 0.037 1968 11 NaN NaN NaN NaN NaN NaN 28.510 0.190 1968 12 NaN NaN NaN NaN NaN NaN 28.601 0.210 1969 1 NaN NaN NaN NaN NaN NaN 28.245 0.037 1969 2 NaN NaN NaN NaN NaN NaN 27.549 -0.623 1969 3 NaN NaN NaN NaN NaN NaN 28.049 0.012 1969 4 NaN NaN NaN NaN NaN NaN 27.192 -0.289 1969 5 NaN NaN NaN NaN NaN NaN 26.288 0.213 1969 6 NaN NaN NaN NaN NaN NaN 23.800 -0.694 1969 7 NaN NaN NaN NaN NaN NaN 24.755 0.803 1969 8 NaN NaN NaN NaN NaN NaN 25.055 0.229 1969 9 NaN NaN NaN NaN NaN NaN 25.522 -0.775 1969 10 27.717 -0.446 0 0 27.717 -0.446 26.703 -0.822 1969 11 29.577 0.619 0 0 29.577 0.619 28.757 0.436 1969 12 29.104 0.075 0 0 29.104 0.075 28.793 0.402 1970 1 28.865 0.019 0 0 28.865 0.019 28.952 0.744 1970 2 28.732 -0.078 1 0 NaN NaN 28.704 0.532 1970 3 29.182 0.507 1 0 NaN NaN 28.596 0.559 1970 4 29.229 1.110 1 0 NaN NaN 27.887 0.407 1970 5 27.615 0.901 0 0 27.615 0.901 26.644 0.568 1970 6 26.676 1.545 1 0 NaN NaN 25.638 1.144 1970 7 24.110 -0.480 1 0 NaN NaN 23.450 -0.502 1970 8 24.920 -0.545 0 0 24.920 -0.545 24.275 -0.551 1970 9 27.526 0.592 1 0 NaN NaN 26.862 0.566 1970 10 28.953 0.790 0 0 28.953 0.790 28.031 0.506 1970 11 29.352 0.394 1 0 NaN NaN 28.385 0.065 1970 12 29.037 0.008 0 0 29.037 0.008 28.383 -0.008 1971 1 28.492 -0.354 1 0 NaN NaN 28.850 0.642 1971 2 28.202 -0.608 0 0 28.202 -0.608 28.146 -0.025 1971 3 27.537 -1.138 1 0 NaN NaN 27.481 -0.556 1971 4 27.598 -0.521 0 0 27.598 -0.521 26.956 -0.524 1971 5 26.060 -0.654 1 0 NaN NaN 25.106 -0.969 1971 6 24.148 -0.984 0 0 24.148 -0.984 23.172 -1.322 1971 7 24.079 -0.512 1 0 NaN NaN 23.382 -0.570 1971 8 25.802 0.337 1 0 NaN NaN 25.637 0.810 1971 9 28.098 1.164 0 0 28.098 1.164 27.364 1.068 1971 10 29.433 1.270 1 0 NaN NaN 28.276 0.751 1971 11 29.174 0.216 1 0 NaN NaN 28.343 0.023 1971 12 NaN NaN NaN NaN NaN NaN 27.959 -0.432 1972 1 NaN NaN NaN NaN NaN NaN 28.754 0.546 1972 2 NaN NaN NaN NaN NaN NaN 28.343 0.171 1972 3 NaN NaN NaN NaN NaN NaN 27.624 -0.413 1972 4 NaN NaN NaN NaN NaN NaN 27.395 -0.086 1972 5 NaN NaN NaN NaN NaN NaN 25.133 -0.943 1972 6 NaN NaN NaN NaN NaN NaN 24.377 -0.117 1972 7 NaN NaN NaN NaN NaN NaN 23.427 -0.525 1972 8 NaN NaN NaN NaN NaN NaN 25.638 0.811 1972 9 NaN NaN NaN NaN NaN NaN 26.017 -0.279 1972 10 NaN NaN NaN NaN NaN NaN 27.512 -0.013 1972 11 NaN NaN NaN NaN NaN NaN 28.590 0.270