% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 19544 % Primary Name: CHOTA % Record Type: TAVG % Country: Peru % Latitude: -6.60000 +/- 0.05000 % Longitude: -78.70000 +/- 0.05000 % Elevation (m): 425.00 +/- 0.50 % # of Months: 11 % % IDs: wmssc - 844530 % % Sources: World Monthly Surface Station Climatology % % Site Hash: f7d993619f655daa572c690cf186b1ba % Raw Data Hash: f972e3bb9eec823c26d04dafd10e115f % Adj Data Hash: 00f5d04e619bb0c8a6456fb670531e5b % % 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 1991 10 NaN NaN NaN NaN NaN NaN 17.193 0.412 1991 11 NaN NaN NaN NaN NaN NaN 17.613 0.458 1991 12 NaN NaN NaN NaN NaN NaN 18.595 1.141 1992 1 NaN NaN NaN NaN NaN NaN 19.161 1.431 1992 2 NaN NaN NaN NaN NaN NaN 19.009 1.159 1992 3 NaN NaN NaN NaN NaN NaN 19.841 2.044 1992 4 NaN NaN NaN NaN NaN NaN 19.771 2.392 1992 5 NaN NaN NaN NaN NaN NaN 19.581 2.560 1992 6 NaN NaN NaN NaN NaN NaN 17.628 1.311 1992 7 NaN NaN NaN NaN NaN NaN 16.184 0.137 1992 8 NaN NaN NaN NaN NaN NaN 16.844 0.417 1992 9 NaN NaN NaN NaN NaN NaN 17.237 0.411 1992 10 17.600 6.003 1 0 NaN NaN 17.360 0.579 1992 11 18.200 6.229 1 0 NaN NaN 17.634 0.479 1992 12 21.500 9.230 1 0 NaN NaN 17.585 0.132 1993 1 NaN NaN NaN NaN NaN NaN 17.737 0.007 1993 2 NaN NaN NaN NaN NaN NaN 18.420 0.571 1993 3 NaN NaN NaN NaN NaN NaN 18.023 0.226 1993 4 16.400 4.206 0 0 16.400 4.206 18.491 1.113 1993 5 12.400 0.563 0 0 12.400 0.563 18.530 1.509 1993 6 9.400 -1.733 0 0 9.400 -1.733 17.550 1.234 1993 7 8.000 -2.863 0 0 8.000 -2.863 16.596 0.549 1993 8 11.700 0.456 0 0 11.700 0.456 17.450 1.022 1993 9 13.100 1.458 0 0 13.100 1.458 17.766 0.940 1993 10 16.800 5.203 0 0 16.800 5.203 17.705 0.923 1993 11 NaN NaN NaN NaN NaN NaN 17.266 0.111 1993 12 22.400 10.130 1 0 NaN NaN 17.605 0.151 1994 1 NaN NaN NaN NaN NaN NaN 17.750 0.020 1994 2 NaN NaN NaN NaN NaN NaN 17.694 -0.155 1994 3 NaN NaN NaN NaN NaN NaN 17.686 -0.111 1994 4 NaN NaN NaN NaN NaN NaN 17.670 0.292 1994 5 NaN NaN NaN NaN NaN NaN 17.355 0.334 1994 6 NaN NaN NaN NaN NaN NaN 16.484 0.167 1994 7 NaN NaN NaN NaN NaN NaN 16.199 0.152 1994 8 NaN NaN NaN NaN NaN NaN 16.437 0.010 1994 9 NaN NaN NaN NaN NaN NaN 17.676 0.850 1994 10 NaN NaN NaN NaN NaN NaN 17.619 0.838 1994 11 NaN NaN NaN NaN NaN NaN 17.543 0.388 1994 12 NaN NaN NaN NaN NaN NaN 18.072 0.619