% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 3768 % Primary Name: SERPENTINE LODDON VALLEY H'WAY % Record Type: TAVG % Country: Australia % Latitude: -36.40930 +/- 0.00005 % Longitude: 143.97520 +/- 0.00005 % Elevation (m): 110.00 +/- 0.50 % # of Months: 24 % % IDs: ghcnd - ASN00080099 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: b65805c683fe9f76bdc12acc9227dd1c % Raw Data Hash: 95b6dd06fb7f00b13eaed27478c43ee2 % Adj Data Hash: 9fb77700f36b41bc524421de834840ca % % 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 4 NaN NaN NaN NaN NaN NaN 17.097 1.733 1968 5 NaN NaN NaN NaN NaN NaN 11.126 -0.651 1968 6 NaN NaN NaN NaN NaN NaN 8.976 -0.439 1968 7 NaN NaN NaN NaN NaN NaN 7.528 -1.002 1968 8 NaN NaN NaN NaN NaN NaN 9.288 -0.439 1968 9 NaN NaN NaN NaN NaN NaN 10.718 -1.099 1968 10 NaN NaN NaN NaN NaN NaN 14.000 -0.473 1968 11 NaN NaN NaN NaN NaN NaN 15.929 -1.471 1968 12 NaN NaN NaN NaN NaN NaN 19.277 -0.832 1969 1 NaN NaN NaN NaN NaN NaN 24.484 1.986 1969 2 NaN NaN NaN NaN NaN NaN 22.829 0.636 1969 3 NaN NaN NaN NaN NaN NaN 19.413 -0.353 1969 4 14.587 -0.285 0 0 14.587 -0.285 15.409 0.044 1969 5 10.629 -0.655 0 0 10.629 -0.655 11.032 -0.745 1969 6 7.968 -0.955 0 0 7.968 -0.955 8.892 -0.524 1969 7 8.226 0.189 0 0 8.226 0.189 9.075 0.545 1969 8 9.781 0.546 0 0 9.781 0.546 10.387 0.660 1969 9 9.168 -2.156 0 0 9.168 -2.156 9.595 -2.223 1969 10 14.968 0.988 0 0 14.968 0.988 15.426 0.954 1969 11 17.008 0.101 0 0 17.008 0.101 16.955 -0.445 1969 12 18.284 -1.333 0 0 18.284 -1.333 18.210 -1.899 1970 1 20.794 -1.211 0 0 20.794 -1.211 21.499 -0.999 1970 2 22.800 1.099 0 0 22.800 1.099 23.010 0.817 1970 3 NaN NaN NaN NaN NaN NaN 19.156 -0.609 1970 4 NaN NaN NaN NaN NaN NaN 15.829 0.464 1970 5 NaN NaN NaN NaN NaN NaN 10.898 -0.879 1970 6 8.673 -0.250 1 0 NaN NaN 9.669 0.253 1970 7 NaN NaN NaN NaN NaN NaN 8.818 0.288 1970 8 8.578 -0.656 0 0 8.578 -0.656 8.856 -0.871 1970 9 9.380 -1.944 0 0 9.380 -1.944 10.104 -1.713 1970 10 13.156 -0.824 0 0 13.156 -0.824 13.731 -0.741 1970 11 16.730 -0.177 1 0 NaN NaN 17.183 -0.217 1970 12 20.221 0.605 0 0 20.221 0.605 19.914 -0.195 1971 1 NaN NaN NaN NaN NaN NaN 22.737 0.239 1971 2 22.434 0.733 0 0 22.434 0.733 23.189 0.995 1971 3 21.203 1.930 0 0 21.203 1.930 22.073 2.307 1971 4 17.037 2.165 0 0 17.037 2.165 17.452 2.087 1971 5 11.211 -0.073 0 0 11.211 -0.073 11.783 0.006 1971 6 8.695 -0.228 0 0 8.695 -0.228 9.427 0.011 1971 7 NaN NaN NaN NaN NaN NaN 8.390 -0.140 1971 8 8.460 -0.774 1 0 NaN NaN 9.252 -0.475 1971 9 10.772 -0.553 0 0 10.772 -0.553 11.229 -0.588 1971 10 NaN NaN NaN NaN NaN NaN 13.226 -1.246 1971 11 NaN NaN NaN NaN NaN NaN 16.118 -1.282 1971 12 NaN NaN NaN NaN NaN NaN 19.451 -0.658 1972 1 NaN NaN NaN NaN NaN NaN 22.126 -0.371 1972 2 NaN NaN NaN NaN NaN NaN 22.539 0.346 1972 3 NaN NaN NaN NaN NaN NaN 18.793 -0.972 1972 4 NaN NaN NaN NaN NaN NaN 15.624 0.259 1972 5 NaN NaN NaN NaN NaN NaN 12.557 0.780 1972 6 NaN NaN NaN NaN NaN NaN 8.879 -0.537 1972 7 NaN NaN NaN NaN NaN NaN 8.785 0.255 1972 8 NaN NaN NaN NaN NaN NaN 10.983 1.256 1972 9 NaN NaN NaN NaN NaN NaN 13.034 1.217