% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 5012 % Primary Name: ROPER VALLEY % Record Type: TAVG % Country: Australia % Latitude: -14.92890 +/- 0.00005 % Longitude: 134.00780 +/- 0.00005 % Elevation (m): 69.00 +/- 0.50 % # of Months: 17 % % IDs: ghcnd - ASN00014617 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 65cc5286f1eca3dfe4557da23082622d % Raw Data Hash: 8a7cd08d52d9ccb8a697b1880dd499e7 % Adj Data Hash: 8dfcef0997314023103e90a8b3173020 % % 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 1994 6 NaN NaN NaN NaN NaN NaN 21.608 -0.407 1994 7 NaN NaN NaN NaN NaN NaN 20.987 -0.430 1994 8 NaN NaN NaN NaN NaN NaN 22.085 -1.160 1994 9 NaN NaN NaN NaN NaN NaN 25.847 -0.489 1994 10 NaN NaN NaN NaN NaN NaN 29.969 0.376 1994 11 NaN NaN NaN NaN NaN NaN 31.779 0.578 1994 12 NaN NaN NaN NaN NaN NaN 31.174 0.202 1995 1 NaN NaN NaN NaN NaN NaN 30.224 0.309 1995 2 NaN NaN NaN NaN NaN NaN 29.596 0.303 1995 3 NaN NaN NaN NaN NaN NaN 28.442 -0.305 1995 4 NaN NaN NaN NaN NaN NaN 27.483 0.254 1995 5 NaN NaN NaN NaN NaN NaN 24.960 0.508 1995 6 20.953 -1.356 1 0 NaN NaN 22.503 0.488 1995 7 22.856 1.145 0 0 22.856 1.145 22.320 0.903 1995 8 NaN NaN NaN NaN NaN NaN 23.176 -0.068 1995 9 28.948 2.318 0 0 28.948 2.318 28.186 1.850 1995 10 30.016 0.129 1 0 NaN NaN 29.353 -0.241 1995 11 32.063 0.568 1 0 NaN NaN 31.765 0.565 1995 12 31.025 -0.241 0 0 31.025 -0.241 31.289 0.317 1996 1 30.878 0.669 0 0 30.878 0.669 30.595 0.680 1996 2 29.908 0.321 1 0 NaN NaN 30.157 0.863 1996 3 29.308 0.268 0 0 29.308 0.268 28.911 0.164 1996 4 27.578 0.055 0 0 27.578 0.055 27.265 0.036 1996 5 NaN NaN NaN NaN NaN NaN 24.303 -0.149 1996 6 24.178 1.868 0 0 24.178 1.868 24.260 2.244 1996 7 NaN NaN NaN NaN NaN NaN 22.394 0.976 1996 8 25.062 1.524 0 0 25.062 1.524 24.655 1.411 1996 9 26.272 -0.358 1 0 NaN NaN 26.634 0.298 1996 10 30.504 0.617 1 0 NaN NaN 30.225 0.632 1996 11 31.585 0.091 1 0 NaN NaN 31.189 -0.011 1996 12 29.333 -1.932 1 0 NaN NaN 31.134 0.162 1997 1 29.590 -0.619 1 0 NaN NaN 29.134 -0.781 1997 2 NaN NaN NaN NaN NaN NaN 29.274 -0.020 1997 3 NaN NaN NaN NaN NaN NaN 28.402 -0.345 1997 4 NaN NaN NaN NaN NaN NaN 27.193 -0.036 1997 5 NaN NaN NaN NaN NaN NaN 24.940 0.488 1997 6 NaN NaN NaN NaN NaN NaN 22.274 0.259 1997 7 NaN NaN NaN NaN NaN NaN 21.621 0.204 1997 8 NaN NaN NaN NaN NaN NaN 23.818 0.573 1997 9 NaN NaN NaN NaN NaN NaN 27.944 1.608 1997 10 NaN NaN NaN NaN NaN NaN 30.292 0.699 1997 11 NaN NaN NaN NaN NaN NaN 31.587 0.386 1997 12 NaN NaN NaN NaN NaN NaN 30.406 -0.566 1998 1 NaN NaN NaN NaN NaN NaN 30.128 0.213