% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 3407 % Primary Name: CLAREMONT HIGH SCHOOL % Record Type: TAVG % Country: Australia % Latitude: -42.80000 +/- 0.00005 % Longitude: 147.26670 +/- 0.00005 % Elevation (m): 18.30 +/- 0.50 % # of Months: 19 % % IDs: ghcnd - ASN00094124 % % Sources: Global Historical Climatology Network - Daily % % Site Hash: 53e0e3349fece104cf71a7d0eccb4ea2 % Raw Data Hash: 5f1356fec4a98d1cc068d8883b2e9d51 % Adj Data Hash: bae35edbc972e595614d7b519edb2200 % % 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 9 NaN NaN NaN NaN NaN NaN 7.583 0.337 1966 10 NaN NaN NaN NaN NaN NaN 9.206 0.180 1966 11 NaN NaN NaN NaN NaN NaN 11.354 0.584 1966 12 NaN NaN NaN NaN NaN NaN 11.913 -0.596 1967 1 NaN NaN NaN NaN NaN NaN 13.202 -1.062 1967 2 NaN NaN NaN NaN NaN NaN 14.881 0.576 1967 3 NaN NaN NaN NaN NaN NaN 12.315 -0.300 1967 4 NaN NaN NaN NaN NaN NaN 9.906 0.223 1967 5 NaN NaN NaN NaN NaN NaN 7.823 0.552 1967 6 NaN NaN NaN NaN NaN NaN 6.218 0.748 1967 7 NaN NaN NaN NaN NaN NaN 4.989 0.193 1967 8 NaN NaN NaN NaN NaN NaN 5.324 -0.190 1967 9 10.026 -0.029 1 0 NaN NaN 6.773 -0.473 1967 10 NaN NaN NaN NaN NaN NaN 9.102 0.077 1967 11 NaN NaN NaN NaN NaN NaN 9.666 -1.103 1967 12 14.893 -0.426 0 0 14.893 -0.426 11.217 -1.292 1968 1 NaN NaN NaN NaN NaN NaN 14.278 0.014 1968 2 18.664 1.550 1 0 NaN NaN 15.176 0.871 1968 3 15.917 0.494 0 0 15.917 0.494 13.357 0.743 1968 4 NaN NaN NaN NaN NaN NaN 9.915 0.232 1968 5 NaN NaN NaN NaN NaN NaN 6.053 -1.219 1968 6 6.936 -1.343 0 0 6.936 -1.343 4.807 -0.663 1968 7 7.260 -0.345 1 0 NaN NaN 4.588 -0.209 1968 8 NaN NaN NaN NaN NaN NaN 5.463 -0.051 1968 9 11.086 1.031 1 0 NaN NaN 6.888 -0.358 1968 10 11.807 -0.028 1 0 NaN NaN 7.904 -1.122 1968 11 12.770 -0.808 1 0 NaN NaN 8.963 -1.806 1968 12 15.107 -0.211 1 0 NaN NaN 12.112 -0.398 1969 1 NaN NaN NaN NaN NaN NaN 14.327 0.063 1969 2 17.342 0.228 1 0 NaN NaN 15.364 1.059 1969 3 16.395 0.971 0 0 16.395 0.971 13.217 0.603 1969 4 12.707 0.215 0 0 12.707 0.215 9.435 -0.249 1969 5 9.765 -0.316 0 0 9.765 -0.316 7.203 -0.069 1969 6 6.950 -1.329 0 0 6.950 -1.329 4.684 -0.786 1969 7 8.435 0.829 0 0 8.435 0.829 5.747 0.950 1969 8 8.875 0.552 1 0 NaN NaN 6.387 0.874 1969 9 8.820 -1.235 1 0 NaN NaN 5.609 -1.637 1969 10 NaN NaN NaN NaN NaN NaN 8.975 -0.051 1969 11 14.618 1.040 0 0 14.618 1.040 11.669 0.900 1969 12 NaN NaN NaN NaN NaN NaN 10.641 -1.869 1970 1 NaN NaN NaN NaN NaN NaN 14.906 0.642 1970 2 NaN NaN NaN NaN NaN NaN 13.337 -0.968 1970 3 NaN NaN NaN NaN NaN NaN 12.879 0.264 1970 4 NaN NaN NaN NaN NaN NaN 10.813 1.130 1970 5 NaN NaN NaN NaN NaN NaN 6.441 -0.830 1970 6 NaN NaN NaN NaN NaN NaN 5.834 0.364 1970 7 NaN NaN NaN NaN NaN NaN 5.087 0.291 1970 8 NaN NaN NaN NaN NaN NaN 4.750 -0.764 1970 9 NaN NaN NaN NaN NaN NaN 5.329 -1.917 1970 10 NaN NaN NaN NaN NaN NaN 8.251 -0.775 1970 11 NaN NaN NaN NaN NaN NaN 11.350 0.581