% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 11310 % Primary Name: VALDIVIA (PI % Record Type: TAVG % Country: Chile % Latitude: -39.62000 +/- 0.00500 % Longitude: -73.07000 +/- 0.00500 % Elevation (m): 50.00 +/- 0.50 % # of Months: 18 % % IDs: ca - 304000000044 % % Sources: Colonial Archive % % Site Hash: ecc9c38efdd1b663923e47120721be02 % Raw Data Hash: 38e606aa8f5f0595d394fb7ac928fb8c % Adj Data Hash: 38e606aa8f5f0595d394fb7ac928fb8c % % 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 1967 5 NaN NaN NaN NaN NaN NaN 10.281 0.870 1967 6 NaN NaN NaN NaN NaN NaN 4.942 -2.343 1967 7 NaN NaN NaN NaN NaN NaN 5.969 -0.988 1967 8 NaN NaN NaN NaN NaN NaN 6.719 -0.774 1967 9 NaN NaN NaN NaN NaN NaN 8.357 -0.399 1967 10 NaN NaN NaN NaN NaN NaN 10.826 0.284 1967 11 NaN NaN NaN NaN NaN NaN 13.344 0.338 1967 12 NaN NaN NaN NaN NaN NaN 15.823 1.020 1968 1 NaN NaN NaN NaN NaN NaN 16.268 0.380 1968 2 NaN NaN NaN NaN NaN NaN 15.810 0.151 1968 3 NaN NaN NaN NaN NaN NaN 13.855 -0.089 1968 4 NaN NaN NaN NaN NaN NaN 11.144 0.119 1968 5 9.900 0.369 0 0 9.900 0.369 10.478 1.066 1968 6 8.550 1.144 0 0 8.550 1.144 8.019 0.734 1968 7 NaN NaN NaN NaN NaN NaN 7.513 0.556 1968 8 NaN NaN NaN NaN NaN NaN 8.318 0.826 1968 9 9.950 1.075 0 0 9.950 1.075 9.788 1.032 1968 10 9.650 -1.012 0 0 9.650 -1.012 9.837 -0.705 1968 11 14.000 0.874 0 0 14.000 0.874 14.234 1.228 1968 12 13.850 -1.072 0 0 13.850 -1.072 14.070 -0.733 1969 1 16.150 0.142 0 0 16.150 0.142 15.878 -0.010 1969 2 14.500 -1.279 0 0 14.500 -1.279 14.136 -1.524 1969 3 13.300 -0.764 0 0 13.300 -0.764 13.439 -0.505 1969 4 11.000 -0.144 0 0 11.000 -0.144 10.870 -0.155 1969 5 9.550 0.019 0 0 9.550 0.019 9.732 0.321 1969 6 7.250 -0.156 0 0 7.250 -0.156 6.808 -0.478 1969 7 8.700 1.623 0 0 8.700 1.623 8.022 1.065 1969 8 7.900 0.288 0 0 7.900 0.288 7.596 0.103 1969 9 9.450 0.575 0 0 9.450 0.575 8.769 0.013 1969 10 9.450 -1.212 0 0 9.450 -1.212 9.140 -1.402 1969 11 12.950 -0.176 0 0 12.950 -0.176 12.896 -0.110 1969 12 15.350 0.428 0 0 15.350 0.428 15.584 0.782 1970 1 NaN NaN NaN NaN NaN NaN 15.809 -0.079 1970 2 NaN NaN NaN NaN NaN NaN 15.985 0.325 1970 3 NaN NaN NaN NaN NaN NaN 13.949 0.005 1970 4 NaN NaN NaN NaN NaN NaN 11.564 0.539 1970 5 NaN NaN NaN NaN NaN NaN 9.908 0.496 1970 6 NaN NaN NaN NaN NaN NaN 7.129 -0.156 1970 7 NaN NaN NaN NaN NaN NaN 7.643 0.685 1970 8 NaN NaN NaN NaN NaN NaN 6.957 -0.535 1970 9 NaN NaN NaN NaN NaN NaN 9.165 0.410 1970 10 NaN NaN NaN NaN NaN NaN 10.041 -0.501 1970 11 NaN NaN NaN NaN NaN NaN 13.042 0.036 1970 12 NaN NaN NaN NaN NaN NaN 13.517 -1.285