% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 4922 % Primary Name: LIVERPOOL CREEK JTTRE % Record Type: TAVG % Country: Australia % Latitude: -17.71670 +/- 0.00005 % Longitude: 145.85000 +/- 0.00005 % Elevation (m): 90.00 +/- 0.50 % # of Months: 19 % % IDs: ghcnd - ASN00032137 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 46526f9f542a5c8c1006bfeee9dc9a19 % Raw Data Hash: 86ac71ad4aaa0cf2a65ca73f43e84f76 % Adj Data Hash: 95aaf17fb173ab1bae980d824ae167fb % % 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 1978 11 NaN NaN NaN NaN NaN NaN 24.597 -0.412 1978 12 NaN NaN NaN NaN NaN NaN 25.843 0.208 1979 1 NaN NaN NaN NaN NaN NaN 25.118 -0.667 1979 2 NaN NaN NaN NaN NaN NaN 25.590 -0.204 1979 3 NaN NaN NaN NaN NaN NaN 25.455 0.394 1979 4 NaN NaN NaN NaN NaN NaN 22.954 -0.468 1979 5 NaN NaN NaN NaN NaN NaN 22.270 0.293 1979 6 NaN NaN NaN NaN NaN NaN 20.260 0.069 1979 7 NaN NaN NaN NaN NaN NaN 19.136 -0.441 1979 8 NaN NaN NaN NaN NaN NaN 19.929 -0.387 1979 9 NaN NaN NaN NaN NaN NaN 21.722 0.184 1979 10 NaN NaN NaN NaN NaN NaN 23.665 0.379 1979 11 24.343 -0.679 0 0 24.343 -0.679 25.016 0.008 1979 12 25.771 0.122 0 0 25.771 0.122 26.093 0.458 1980 1 NaN NaN NaN NaN NaN NaN 26.859 1.074 1980 2 NaN NaN NaN NaN NaN NaN 26.821 1.027 1980 3 23.956 -1.117 0 0 23.956 -1.117 25.091 0.031 1980 4 NaN NaN NaN NaN NaN NaN 23.738 0.315 1980 5 NaN NaN NaN NaN NaN NaN 22.678 0.701 1980 6 NaN NaN NaN NaN NaN NaN 20.792 0.601 1980 7 NaN NaN NaN NaN NaN NaN 19.932 0.354 1980 8 NaN NaN NaN NaN NaN NaN 20.406 0.090 1980 9 NaN NaN NaN NaN NaN NaN 21.275 -0.263 1980 10 NaN NaN NaN NaN NaN NaN 23.577 0.291 1980 11 NaN NaN NaN NaN NaN NaN 24.991 -0.017 1980 12 NaN NaN NaN NaN NaN NaN 25.630 -0.005 1981 1 25.018 -0.781 1 0 NaN NaN 24.563 -1.221 1981 2 NaN NaN NaN NaN NaN NaN 26.648 0.854 1981 3 25.758 0.684 1 0 NaN NaN 25.632 0.571 1981 4 24.672 1.236 0 2 24.672 1.236 24.020 0.598 1981 5 22.604 0.614 1 0 NaN NaN 22.221 0.244 1981 6 19.568 -0.636 0 0 19.568 -0.636 20.239 0.048 1981 7 20.871 1.280 0 0 20.871 1.280 21.137 1.559 1981 8 21.694 1.364 0 0 21.694 1.364 21.756 1.440 1981 9 21.522 -0.029 0 0 21.522 -0.029 21.478 -0.060 1981 10 23.226 -0.073 0 0 23.226 -0.073 22.840 -0.446 1981 11 26.896 1.874 1 0 NaN NaN 25.987 0.979 1981 12 NaN NaN NaN NaN NaN NaN 26.812 1.177 1982 1 27.944 2.145 1 0 NaN NaN 26.623 0.838 1982 2 27.512 1.705 1 0 NaN NaN 26.276 0.483 1982 3 27.279 2.205 0 0 27.279 2.205 25.794 0.733 1982 4 25.070 1.634 1 0 NaN NaN 23.263 -0.160 1982 5 NaN NaN NaN NaN NaN NaN 21.658 -0.319 1982 6 NaN NaN NaN NaN NaN NaN 18.099 -2.092 1982 7 18.433 -1.159 1 0 NaN NaN 18.420 -1.157 1982 8 19.921 -0.408 0 0 19.921 -0.408 19.210 -1.106 1982 9 NaN NaN NaN NaN NaN NaN 21.103 -0.434 1982 10 NaN NaN NaN NaN NaN NaN 21.857 -1.429 1982 11 NaN NaN NaN NaN NaN NaN 24.078 -0.930 1982 12 NaN NaN NaN NaN NaN NaN 25.877 0.242 1983 1 NaN NaN NaN NaN NaN NaN 26.842 1.058 1983 2 NaN NaN NaN NaN NaN NaN 26.797 1.003 1983 3 NaN NaN NaN NaN NaN NaN 25.596 0.536 1983 4 NaN NaN NaN NaN NaN NaN 24.791 1.369 1983 5 NaN NaN NaN NaN NaN NaN 23.520 1.543 1983 6 NaN NaN NaN NaN NaN NaN 20.402 0.211 1983 7 NaN NaN NaN NaN NaN NaN 19.266 -0.312 1983 8 NaN NaN NaN NaN NaN NaN 20.476 0.160