% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 5055 % Primary Name: MANTON DAM % Record Type: TAVG % Country: Australia % Latitude: -12.83810 +/- 0.00005 % Longitude: 131.13060 +/- 0.00005 % Elevation (m): 41.00 +/- 0.50 % # of Months: 9 % % IDs: ghcnd - ASN00014035 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: f3a9edc858f4a01fb9c41530bfc94c0e % Raw Data Hash: 40af534c01ed96d84bb55949e985cdfc % Adj Data Hash: 7d58f713f43558b2c76ff3960daa6526 % % 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 1964 1 NaN NaN NaN NaN NaN NaN 28.027 -0.075 1964 2 NaN NaN NaN NaN NaN NaN 29.417 1.386 1964 3 NaN NaN NaN NaN NaN NaN 27.808 -0.366 1964 4 NaN NaN NaN NaN NaN NaN 27.930 0.560 1964 5 NaN NaN NaN NaN NaN NaN 25.447 0.166 1964 6 NaN NaN NaN NaN NaN NaN 22.416 -0.774 1964 7 NaN NaN NaN NaN NaN NaN 23.104 0.318 1964 8 NaN NaN NaN NaN NaN NaN 24.969 0.261 1964 9 NaN NaN NaN NaN NaN NaN 28.770 1.307 1964 10 NaN NaN NaN NaN NaN NaN 29.769 0.276 1964 11 NaN NaN NaN NaN NaN NaN 29.050 -0.752 1964 12 NaN NaN NaN NaN NaN NaN 28.395 -0.561 1965 1 29.387 0.515 1 0 NaN NaN 28.351 0.249 1965 2 29.522 0.722 0 0 29.522 0.722 29.122 1.091 1965 3 26.913 -2.030 0 0 26.913 -2.030 27.198 -0.976 1965 4 NaN NaN NaN NaN NaN NaN 26.302 -1.068 1965 5 26.930 0.879 0 0 26.930 0.879 25.537 0.256 1965 6 25.441 1.481 0 0 25.441 1.481 23.418 0.227 1965 7 NaN NaN NaN NaN NaN NaN 20.236 -2.550 1965 8 25.295 -0.182 1 0 NaN NaN 24.157 -0.550 1965 9 NaN NaN NaN NaN NaN NaN 27.240 -0.223 1965 10 29.738 -0.524 0 0 29.738 -0.524 29.345 -0.148 1965 11 30.943 0.372 1 0 NaN NaN 30.584 0.783 1965 12 29.110 -0.615 0 0 29.110 -0.615 28.418 -0.537 1966 1 NaN NaN NaN NaN NaN NaN 27.863 -0.239 1966 2 NaN NaN NaN NaN NaN NaN 27.954 -0.077 1966 3 NaN NaN NaN NaN NaN NaN 28.131 -0.043 1966 4 NaN NaN NaN NaN NaN NaN 28.181 0.810 1966 5 NaN NaN NaN NaN NaN NaN 25.088 -0.194 1966 6 NaN NaN NaN NaN NaN NaN 24.127 0.936 1966 7 NaN NaN NaN NaN NaN NaN 22.226 -0.560 1966 8 NaN NaN NaN NaN NaN NaN 24.728 0.020 1966 9 NaN NaN NaN NaN NaN NaN 27.815 0.352 1966 10 NaN NaN NaN NaN NaN NaN 28.132 -1.361 1966 11 NaN NaN NaN NaN NaN NaN 29.652 -0.150 1966 12 NaN NaN NaN NaN NaN NaN 28.743 -0.212