% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 4283 % Primary Name: SANDY HOLLOW (MT DANGER VINEYA % Record Type: TAVG % Country: Australia % Latitude: -32.33330 +/- 0.00005 % Longitude: 150.56670 +/- 0.00005 % Elevation (m): 133.00 +/- 0.50 % # of Months: 25 % % IDs: ghcnd - ASN00061317 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 32e3d5e3ccd21e32f17561bbd37c4c13 % Raw Data Hash: ce98534a091a0dc910dd4429bdeb6342 % Adj Data Hash: bdf0cd6dc58a8d707d1662020e8b28b2 % % 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 1971 2 NaN NaN NaN NaN NaN NaN 19.010 -0.481 1971 3 NaN NaN NaN NaN NaN NaN 18.386 0.506 1971 4 NaN NaN NaN NaN NaN NaN 14.125 -0.184 1971 5 NaN NaN NaN NaN NaN NaN 10.110 -0.464 1971 6 NaN NaN NaN NaN NaN NaN 7.971 -0.316 1971 7 NaN NaN NaN NaN NaN NaN 6.357 -0.714 1971 8 NaN NaN NaN NaN NaN NaN 8.566 0.118 1971 9 NaN NaN NaN NaN NaN NaN 11.004 0.071 1971 10 NaN NaN NaN NaN NaN NaN 13.711 -0.053 1971 11 NaN NaN NaN NaN NaN NaN 14.376 -2.056 1971 12 NaN NaN NaN NaN NaN NaN 18.136 -0.654 1972 1 NaN NaN NaN NaN NaN NaN 17.637 -2.214 1972 2 22.398 -0.260 1 0 NaN NaN 17.845 -1.646 1972 3 20.660 -0.386 0 0 20.660 -0.386 17.127 -0.752 1972 4 16.263 -1.213 0 0 16.263 -1.213 13.528 -0.782 1972 5 14.081 0.341 0 0 14.081 0.341 11.157 0.584 1972 6 10.580 -0.874 0 0 10.580 -0.874 8.701 0.414 1972 7 8.998 -1.239 0 0 8.998 -1.239 7.108 0.038 1972 8 11.848 0.233 0 0 11.848 0.233 9.641 1.193 1972 9 16.215 2.115 0 0 16.215 2.115 12.673 1.739 1972 10 18.187 1.256 0 0 18.187 1.256 14.359 0.595 1972 11 19.275 -0.324 0 0 19.275 -0.324 16.012 -0.420 1972 12 24.173 2.216 0 0 24.173 2.216 20.381 1.591 1973 1 NaN NaN NaN NaN NaN NaN 21.452 1.602 1973 2 NaN NaN NaN NaN NaN NaN 19.542 0.050 1973 3 22.025 0.979 1 0 NaN NaN 18.636 0.757 1973 4 17.750 0.274 0 0 17.750 0.274 15.423 1.113 1973 5 NaN NaN NaN NaN NaN NaN 11.437 0.864 1973 6 11.488 0.034 1 0 NaN NaN 9.128 0.841 1973 7 13.026 2.789 0 0 13.026 2.789 9.434 2.364 1973 8 NaN NaN NaN NaN NaN NaN 9.133 0.685 1973 9 16.375 2.275 0 0 16.375 2.275 12.092 1.158 1973 10 18.367 1.436 1 0 NaN NaN 14.541 0.777 1973 11 NaN NaN NaN NaN NaN NaN 16.124 -0.308 1973 12 23.492 1.535 0 0 23.492 1.535 19.080 0.290 1974 1 NaN NaN NaN NaN NaN NaN 19.388 -0.462 1974 2 23.238 0.580 1 0 NaN NaN 18.577 -0.915 1974 3 19.932 -1.114 1 0 NaN NaN 18.315 0.436 1974 4 19.100 1.624 0 0 19.100 1.624 15.805 1.495 1974 5 14.532 0.792 1 0 NaN NaN 11.564 0.991 1974 6 NaN NaN NaN NaN NaN NaN 8.638 0.351 1974 7 10.516 0.279 1 0 NaN NaN 7.608 0.538 1974 8 10.808 -0.808 1 0 NaN NaN 8.050 -0.399 1974 9 NaN NaN NaN NaN NaN NaN 9.813 -1.121 1974 10 NaN NaN NaN NaN NaN NaN 12.906 -0.858 1974 11 19.444 -0.155 1 0 NaN NaN 14.506 -1.926 1974 12 NaN NaN NaN NaN NaN NaN 18.416 -0.374 1975 1 NaN NaN NaN NaN NaN NaN 19.547 -0.303 1975 2 NaN NaN NaN NaN NaN NaN 18.999 -0.492 1975 3 NaN NaN NaN NaN NaN NaN 17.386 -0.493 1975 4 NaN NaN NaN NaN NaN NaN 13.683 -0.626 1975 5 NaN NaN NaN NaN NaN NaN 11.238 0.665 1975 6 NaN NaN NaN NaN NaN NaN 8.892 0.605 1975 7 NaN NaN NaN NaN NaN NaN 8.514 1.443 1975 8 NaN NaN NaN NaN NaN NaN 8.965 0.517 1975 9 NaN NaN NaN NaN NaN NaN 11.952 1.018 1975 10 NaN NaN NaN NaN NaN NaN 13.239 -0.526 1975 11 NaN NaN NaN NaN NaN NaN 16.928 0.496