% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 15365 % Primary Name: BOROBUDUR % Record Type: TAVG % Country: Indonesia % Latitude: -7.10833 +/- 0.01667 % Longitude: 110.19167 +/- 0.18333 % Elevation (m): 329.32 +/- 358.19 % # of Months: 21 % % Alternate Names: UNGARAN % % IDs: wwr - 96K40 % % Sources: World Weather Records % % Site Hash: cb07cf2443c672abb243f9d14a197455 % Raw Data Hash: 4348a8e98afbc18b3c91912d528539d1 % Adj Data Hash: 7f0b49b2987371237ee5e06a26c78ce0 % % 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 1997 1 NaN NaN NaN NaN NaN NaN 26.079 0.028 1997 2 NaN NaN NaN NaN NaN NaN 26.567 0.445 1997 3 NaN NaN NaN NaN NaN NaN 27.059 0.695 1997 4 NaN NaN NaN NaN NaN NaN 26.969 0.368 1997 5 NaN NaN NaN NaN NaN NaN 27.122 0.420 1997 6 NaN NaN NaN NaN NaN NaN 26.585 0.479 1997 7 NaN NaN NaN NaN NaN NaN 25.283 -0.244 1997 8 NaN NaN NaN NaN NaN NaN 25.578 -0.143 1997 9 NaN NaN NaN NaN NaN NaN 26.348 -0.042 1997 10 NaN NaN NaN NaN NaN NaN 27.443 0.671 1997 11 NaN NaN NaN NaN NaN NaN 27.884 0.958 1997 12 NaN NaN NaN NaN NaN NaN 27.460 1.080 1998 1 26.800 1.707 0 0 26.800 1.707 27.612 1.561 1998 2 26.400 1.235 0 0 26.400 1.235 27.383 1.261 1998 3 26.500 1.094 0 0 26.500 1.094 27.305 0.942 1998 4 27.400 1.757 0 0 27.400 1.757 27.523 0.922 1998 5 27.300 1.556 0 0 27.300 1.556 27.950 1.248 1998 6 NaN NaN NaN NaN NaN NaN 27.186 1.080 1998 7 NaN NaN NaN NaN NaN NaN 26.703 1.176 1998 8 NaN NaN NaN NaN NaN NaN 26.991 1.271 1998 9 NaN NaN NaN NaN NaN NaN 26.796 0.406 1998 10 NaN NaN NaN NaN NaN NaN 27.196 0.425 1998 11 NaN NaN NaN NaN NaN NaN 27.019 0.093 1998 12 NaN NaN NaN NaN NaN NaN 26.845 0.465 1999 1 24.700 -0.393 1 0 NaN NaN 26.435 0.384 1999 2 25.900 0.735 0 0 25.900 0.735 26.602 0.479 1999 3 25.700 0.294 0 0 25.700 0.294 26.765 0.401 1999 4 25.800 0.157 0 0 25.800 0.157 26.921 0.320 1999 5 25.700 -0.044 0 0 25.700 -0.044 26.952 0.250 1999 6 25.100 -0.048 0 0 25.100 -0.048 26.382 0.276 1999 7 23.900 -0.669 0 0 23.900 -0.669 25.563 0.036 1999 8 24.700 -0.062 0 0 24.700 -0.062 25.783 0.063 1999 9 25.700 0.268 0 0 25.700 0.268 26.801 0.411 1999 10 26.200 0.387 0 0 26.200 0.387 26.999 0.227 1999 11 30.800 4.832 1 0 NaN NaN 27.041 0.114 1999 12 26.100 0.678 0 0 26.100 0.678 26.852 0.471 2000 1 25.500 0.407 0 0 25.500 0.407 26.370 0.319 2000 2 25.800 0.635 0 0 25.800 0.635 26.577 0.454 2000 3 25.600 0.194 0 0 25.600 0.194 26.631 0.267 2000 4 25.500 -0.143 0 0 25.500 -0.143 26.831 0.230 2000 5 NaN NaN NaN NaN NaN NaN 27.089 0.387 2000 6 NaN NaN NaN NaN NaN NaN 26.198 0.092 2000 7 NaN NaN NaN NaN NaN NaN 26.177 0.651 2000 8 NaN NaN NaN NaN NaN NaN 26.332 0.612 2000 9 NaN NaN NaN NaN NaN NaN 27.434 1.044 2000 10 NaN NaN NaN NaN NaN NaN 27.249 0.478 2000 11 NaN NaN NaN NaN NaN NaN 26.943 0.016 2000 12 NaN NaN NaN NaN NaN NaN 27.008 0.627 2001 1 NaN NaN NaN NaN NaN NaN 26.268 0.217 2001 2 NaN NaN NaN NaN NaN NaN 26.235 0.112 2001 3 NaN NaN NaN NaN NaN NaN 26.346 -0.018 2001 4 NaN NaN NaN NaN NaN NaN 26.839 0.238