% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 3703 % Primary Name: BENDOC FORESTRY % Record Type: TAVG % Country: Australia % Latitude: -37.15000 +/- 0.00005 % Longitude: 148.88330 +/- 0.00005 % Elevation (m): 914.40 +/- 0.50 % # of Months: 23 % % IDs: ghcnd - ASN00084077 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 71f182aacb551f840fc3c659b9b56404 % Raw Data Hash: 4c59eca73a0ef27d241f694f98202005 % Adj Data Hash: f6d40509a414a6bb5d1955d53cf432d4 % % 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 2 NaN NaN NaN NaN NaN NaN 16.991 -0.867 1964 3 NaN NaN NaN NaN NaN NaN 16.189 -0.480 1964 4 NaN NaN NaN NaN NaN NaN 14.707 0.745 1964 5 NaN NaN NaN NaN NaN NaN 10.924 -0.651 1964 6 NaN NaN NaN NaN NaN NaN 10.481 0.642 1964 7 NaN NaN NaN NaN NaN NaN 8.840 -0.140 1964 8 NaN NaN NaN NaN NaN NaN 9.922 0.263 1964 9 NaN NaN NaN NaN NaN NaN 11.128 0.089 1964 10 NaN NaN NaN NaN NaN NaN 11.368 -1.202 1964 11 NaN NaN NaN NaN NaN NaN 14.242 0.111 1964 12 NaN NaN NaN NaN NaN NaN 14.009 -1.915 1965 1 NaN NaN NaN NaN NaN NaN 14.954 -2.584 1965 2 18.030 3.921 1 0 NaN NaN 17.700 -0.158 1965 3 13.542 0.622 1 0 NaN NaN 16.496 -0.173 1965 4 NaN NaN NaN NaN NaN NaN 12.304 -1.658 1965 5 NaN NaN NaN NaN NaN NaN 11.780 0.206 1965 6 NaN NaN NaN NaN NaN NaN 9.539 -0.300 1965 7 3.447 -1.784 1 0 NaN NaN 8.397 -0.583 1965 8 5.413 -0.498 1 0 NaN NaN 10.166 0.507 1965 9 8.219 0.928 0 0 8.219 0.928 12.137 1.098 1965 10 11.442 2.621 1 0 NaN NaN 13.614 1.044 1965 11 11.324 0.941 0 0 11.324 0.941 13.590 -0.542 1965 12 NaN NaN NaN NaN NaN NaN 16.796 0.872 1966 1 16.495 2.705 1 0 NaN NaN 18.018 0.480 1966 2 14.810 0.700 0 0 14.810 0.700 16.771 -1.087 1966 3 13.124 0.203 1 0 NaN NaN 16.960 0.291 1966 4 10.402 0.188 1 0 NaN NaN 13.280 -0.682 1966 5 NaN NaN NaN NaN NaN NaN 11.230 -0.344 1966 6 3.955 -2.136 0 0 3.955 -2.136 9.097 -0.741 1966 7 2.684 -2.547 1 0 NaN NaN 8.288 -0.693 1966 8 3.954 -1.957 0 0 3.954 -1.957 9.177 -0.482 1966 9 6.968 -0.323 0 0 6.968 -0.323 10.948 -0.091 1966 10 9.590 0.768 1 0 NaN NaN 11.997 -0.573 1966 11 NaN NaN NaN NaN NaN NaN 14.290 0.159 1966 12 NaN NaN NaN NaN NaN NaN 15.333 -0.591 1967 1 15.451 1.661 1 0 NaN NaN 16.804 -0.735 1967 2 NaN NaN NaN NaN NaN NaN 18.385 0.527 1967 3 13.526 0.605 1 0 NaN NaN 16.215 -0.454 1967 4 NaN NaN NaN NaN NaN NaN 14.256 0.294 1967 5 7.148 -0.678 1 0 NaN NaN 11.801 0.227 1967 6 5.253 -0.837 1 0 NaN NaN 10.873 1.034 1967 7 3.787 -1.444 1 0 NaN NaN 8.930 -0.051 1967 8 4.724 -1.186 1 0 NaN NaN 9.426 -0.233 1967 9 3.350 -3.941 1 0 NaN NaN 10.379 -0.660 1967 10 NaN NaN NaN NaN NaN NaN 13.155 0.585 1967 11 NaN NaN NaN NaN NaN NaN 13.884 -0.247 1967 12 NaN NaN NaN NaN NaN NaN 14.322 -1.602 1968 1 NaN NaN NaN NaN NaN NaN 17.851 0.312 1968 2 NaN NaN NaN NaN NaN NaN 19.975 2.117 1968 3 NaN NaN NaN NaN NaN NaN 18.274 1.605 1968 4 NaN NaN NaN NaN NaN NaN 15.605 1.643 1968 5 NaN NaN NaN NaN NaN NaN 10.999 -0.575 1968 6 NaN NaN NaN NaN NaN NaN 9.352 -0.486 1968 7 NaN NaN NaN NaN NaN NaN 8.406 -0.574 1968 8 NaN NaN NaN NaN NaN NaN 9.668 0.009 1968 9 NaN NaN NaN NaN NaN NaN 10.414 -0.625