% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 18635 % Primary Name: NEW PLYMOUTH % Record Type: TAVG % Country: New Zealand % Latitude: -39.10000 +/- 0.05000 % Longitude: 174.10000 +/- 0.05000 % Elevation (m): 58.00 +/- 0.50 % # of Months: 16 % % IDs: wmssc - 933070 % % Sources: World Monthly Surface Station Climatology % % Site Hash: 6b13c0f2c8da97e45838b6818dbff5e6 % Raw Data Hash: 654040b834b67e391b89d183b09542e2 % Adj Data Hash: 654040b834b67e391b89d183b09542e2 % % 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 1960 1 NaN NaN NaN NaN NaN NaN 17.420 0.331 1960 2 NaN NaN NaN NaN NaN NaN 17.263 -0.126 1960 3 NaN NaN NaN NaN NaN NaN 14.783 -1.045 1960 4 NaN NaN NaN NaN NaN NaN 12.039 -0.605 1960 5 NaN NaN NaN NaN NaN NaN 10.229 0.572 1960 6 NaN NaN NaN NaN NaN NaN 7.350 0.154 1960 7 NaN NaN NaN NaN NaN NaN 6.427 0.030 1960 8 NaN NaN NaN NaN NaN NaN 6.778 -0.667 1960 9 NaN NaN NaN NaN NaN NaN 9.666 0.360 1960 10 NaN NaN NaN NaN NaN NaN 11.755 0.537 1960 11 NaN NaN NaN NaN NaN NaN 13.305 -0.151 1960 12 NaN NaN NaN NaN NaN NaN 14.338 -1.071 1961 1 18.300 -0.744 0 0 18.300 -0.744 16.971 -0.118 1961 2 17.700 -1.644 0 0 17.700 -1.644 17.119 -0.271 1961 3 15.900 -1.883 0 0 15.900 -1.883 14.993 -0.835 1961 4 14.100 -0.499 0 0 14.100 -0.499 12.044 -0.601 1961 5 12.600 0.987 0 0 12.600 0.987 9.323 -0.334 1961 6 10.400 1.250 0 0 10.400 1.250 6.839 -0.357 1961 7 9.400 1.048 0 0 9.400 1.048 6.019 -0.378 1961 8 9.800 0.401 0 0 9.800 0.401 6.691 -0.753 1961 9 11.300 0.039 0 0 11.300 0.039 8.879 -0.428 1961 10 13.900 0.727 0 0 13.900 0.727 12.235 1.017 1961 11 14.500 -0.911 0 0 14.500 -0.911 13.682 0.226 1961 12 17.800 0.436 0 0 17.800 0.436 16.636 1.227 1962 1 19.200 0.156 0 0 19.200 0.156 18.493 1.404 1962 2 NaN NaN NaN NaN NaN NaN 17.367 -0.023 1962 3 17.300 -0.483 0 0 17.300 -0.483 16.065 0.238 1962 4 15.200 0.601 0 0 15.200 0.601 12.968 0.323 1962 5 14.100 2.487 0 0 14.100 2.487 11.266 1.608 1962 6 NaN NaN NaN NaN NaN NaN 8.117 0.921 1962 7 NaN NaN NaN NaN NaN NaN 7.094 0.697 1962 8 NaN NaN NaN NaN NaN NaN 7.930 0.485 1962 9 NaN NaN NaN NaN NaN NaN 9.256 -0.051 1962 10 NaN NaN NaN NaN NaN NaN 12.587 1.369 1962 11 NaN NaN NaN NaN NaN NaN 13.437 -0.018 1962 12 NaN NaN NaN NaN NaN NaN 15.230 -0.179 1963 1 NaN NaN NaN NaN NaN NaN 17.117 0.027 1963 2 NaN NaN NaN NaN NaN NaN 18.404 1.014 1963 3 NaN NaN NaN NaN NaN NaN 15.581 -0.247 1963 4 NaN NaN NaN NaN NaN NaN 11.419 -1.226 1963 5 NaN NaN NaN NaN NaN NaN 9.357 -0.301