% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 88376 % Primary Name: LAVERTON COMPARISON % Record Type: TAVG % Country: Australia % Latitude: -37.86330 +/- 0.00005 % Longitude: 144.74560 +/- 0.00005 % Elevation (m): 36.60 +/- 39.14 % # of Months: 16 % % IDs: ghcnd - ASN00087177 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 7f6831c3ecd083701f004b999184e4f9 % Raw Data Hash: 9e5352b2f159f316c0b24c3328e5e9f6 % Adj Data Hash: c01095181ea9ab0c06f4f7b545fb8895 % % 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 1996 3 NaN NaN NaN NaN NaN NaN 17.170 -0.284 1996 4 NaN NaN NaN NaN NaN NaN 12.304 -1.583 1996 5 NaN NaN NaN NaN NaN NaN 11.434 0.489 1996 6 NaN NaN NaN NaN NaN NaN 9.178 0.330 1996 7 NaN NaN NaN NaN NaN NaN 8.116 0.150 1996 8 NaN NaN NaN NaN NaN NaN 9.320 0.426 1996 9 NaN NaN NaN NaN NaN NaN 10.562 -0.115 1996 10 NaN NaN NaN NaN NaN NaN 13.178 0.510 1996 11 NaN NaN NaN NaN NaN NaN 13.713 -1.011 1996 12 NaN NaN NaN NaN NaN NaN 15.308 -1.670 1997 1 NaN NaN NaN NaN NaN NaN 20.666 1.498 1997 2 NaN NaN NaN NaN NaN NaN 22.520 3.272 1997 3 17.003 -1.255 0 0 17.003 -1.255 16.446 -1.008 1997 4 14.955 0.263 0 0 14.955 0.263 13.902 0.014 1997 5 12.287 0.538 0 0 12.287 0.538 11.197 0.253 1997 6 10.348 0.696 0 0 10.348 0.696 9.343 0.495 1997 7 8.406 -0.364 0 0 8.406 -0.364 7.433 -0.533 1997 8 9.759 0.061 1 0 NaN NaN 8.674 -0.220 1997 9 11.345 -0.137 0 0 11.345 -0.137 10.704 0.027 1997 10 13.939 0.465 1 0 NaN NaN 13.157 0.488 1997 11 16.095 0.566 1 0 NaN NaN 15.654 0.930 1997 12 17.877 0.094 0 0 17.877 0.094 17.405 0.426 1998 1 20.508 0.536 0 0 20.508 0.536 20.211 1.044 1998 2 NaN NaN NaN NaN NaN NaN 19.262 0.015 1998 3 18.016 -0.242 0 0 18.016 -0.242 17.763 0.309 1998 4 14.065 -0.627 0 0 14.065 -0.627 12.932 -0.955 1998 5 12.156 0.407 0 0 12.156 0.407 11.287 0.343 1998 6 9.883 0.231 0 0 9.883 0.231 8.786 -0.061 1998 7 8.381 -0.390 0 0 8.381 -0.390 7.361 -0.605 1998 8 NaN NaN NaN NaN NaN NaN 9.786 0.893 1998 9 NaN NaN NaN NaN NaN NaN 12.071 1.394 1998 10 NaN NaN NaN NaN NaN NaN 11.958 -0.711 1998 11 NaN NaN NaN NaN NaN NaN 14.085 -0.639 1998 12 NaN NaN NaN NaN NaN NaN 17.615 0.637 1999 1 NaN NaN NaN NaN NaN NaN 21.107 1.940 1999 2 NaN NaN NaN NaN NaN NaN 20.545 1.298 1999 3 NaN NaN NaN NaN NaN NaN 17.135 -0.319 1999 4 NaN NaN NaN NaN NaN NaN 12.554 -1.334 1999 5 NaN NaN NaN NaN NaN NaN 12.064 1.120 1999 6 NaN NaN NaN NaN NaN NaN 9.468 0.621 1999 7 NaN NaN NaN NaN NaN NaN 9.311 1.345