% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 4128 % Primary Name: BEDFORD HARBOUR 1 % Record Type: TAVG % Country: Australia % Latitude: -33.75000 +/- 0.00500 % Longitude: 120.60000 +/- 0.00500 % Elevation (m): 70.00 +/- 0.50 % # of Months: 25 % % IDs: ghcnd - ASN00009764 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: d21852b96b3bb53ac83b14e7bfb5f411 % Raw Data Hash: dd6e1e7176e6b368a4e1531b8c29dac3 % Adj Data Hash: d0e7ef63838b7546ea46209aa44eb578 % % 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 1966 8 NaN NaN NaN NaN NaN NaN 13.160 -0.568 1966 9 NaN NaN NaN NaN NaN NaN 12.823 -0.872 1966 10 NaN NaN NaN NaN NaN NaN 13.280 -0.668 1966 11 NaN NaN NaN NaN NaN NaN 16.783 1.592 1966 12 NaN NaN NaN NaN NaN NaN 15.723 -0.635 1967 1 NaN NaN NaN NaN NaN NaN 17.401 -0.178 1967 2 NaN NaN NaN NaN NaN NaN 17.727 0.031 1967 3 NaN NaN NaN NaN NaN NaN 17.035 -0.716 1967 4 NaN NaN NaN NaN NaN NaN 18.121 1.437 1967 5 NaN NaN NaN NaN NaN NaN 16.127 0.206 1967 6 NaN NaN NaN NaN NaN NaN 16.030 0.993 1967 7 NaN NaN NaN NaN NaN NaN 13.961 -0.243 1967 8 11.726 -1.841 0 0 11.726 -1.841 13.145 -0.583 1967 9 13.305 -0.229 0 0 13.305 -0.229 13.958 0.263 1967 10 16.995 3.207 0 0 16.995 3.207 15.548 1.599 1967 11 NaN NaN NaN NaN NaN NaN 15.751 0.560 1967 12 18.972 2.775 0 0 18.972 2.775 16.569 0.211 1968 1 NaN NaN NaN NaN NaN NaN 18.389 0.811 1968 2 19.662 2.126 0 0 19.662 2.126 17.461 -0.235 1968 3 17.150 -0.440 0 0 17.150 -0.440 16.280 -1.470 1968 4 15.343 -1.180 0 0 15.343 -1.180 15.412 -1.271 1968 5 12.186 -3.574 0 0 12.186 -3.574 13.769 -2.152 1968 6 12.100 -2.777 0 0 12.100 -2.777 15.032 -0.006 1968 7 10.990 -3.053 0 0 10.990 -3.053 13.778 -0.426 1968 8 10.719 -2.848 0 0 10.719 -2.848 12.397 -1.331 1968 9 13.095 -0.439 0 0 13.095 -0.439 12.868 -0.827 1968 10 15.801 2.013 0 0 15.801 2.013 14.024 0.075 1968 11 NaN NaN NaN NaN NaN NaN 14.391 -0.800 1968 12 19.283 3.086 1 0 NaN NaN 16.186 -0.172 1969 1 21.527 4.110 0 0 21.527 4.110 18.383 0.805 1969 2 19.439 1.904 0 0 19.439 1.904 17.351 -0.346 1969 3 19.304 1.714 0 0 19.304 1.714 17.863 0.113 1969 4 NaN NaN NaN NaN NaN NaN 16.972 0.289 1969 5 NaN NaN NaN NaN NaN NaN 16.131 0.210 1969 6 12.684 -2.192 0 0 12.684 -2.192 15.388 0.351 1969 7 11.331 -2.712 0 0 11.331 -2.712 14.195 -0.009 1969 8 11.803 -1.764 0 0 11.803 -1.764 13.767 0.038 1969 9 10.925 -2.609 1 0 NaN NaN 11.967 -1.728 1969 10 NaN NaN NaN NaN NaN NaN 14.897 0.948 1969 11 19.095 4.065 1 0 NaN NaN 15.812 0.621 1969 12 19.385 3.188 1 0 NaN NaN 15.730 -0.628 1970 1 19.716 2.299 1 0 NaN NaN 17.320 -0.258 1970 2 20.102 2.566 1 0 NaN NaN 18.408 0.711 1970 3 NaN NaN NaN NaN NaN NaN 18.192 0.442 1970 4 NaN NaN NaN NaN NaN NaN 15.683 -1.000 1970 5 NaN NaN NaN NaN NaN NaN 15.442 -0.479 1970 6 NaN NaN NaN NaN NaN NaN 15.056 0.019 1970 7 NaN NaN NaN NaN NaN NaN 14.555 0.351 1970 8 NaN NaN NaN NaN NaN NaN 13.130 -0.598 1970 9 NaN NaN NaN NaN NaN NaN 13.268 -0.427 1970 10 NaN NaN NaN NaN NaN NaN 13.445 -0.504 1970 11 NaN NaN NaN NaN NaN NaN 14.968 -0.223 1970 12 NaN NaN NaN NaN NaN NaN 16.637 0.279 1971 1 NaN NaN NaN NaN NaN NaN 17.817 0.239 1971 2 NaN NaN NaN NaN NaN NaN 17.855 0.158