% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 15489 % Primary Name: SEBAPO % Record Type: TAVG % Country: Indonesia % Latitude: -1.50000 +/- 0.00833 % Longitude: 103.25000 +/- 0.00833 % Elevation (m): 67.20 +/- 43.57 % # of Months: 13 % % IDs: wwr - 96D27 % % Sources: World Weather Records % % Site Hash: 921619c1e19184071b05eb68111200f9 % Raw Data Hash: d0379fb3cc42085563fa032783e409cc % Adj Data Hash: d0379fb3cc42085563fa032783e409cc % % 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 1996 1 NaN NaN NaN NaN NaN NaN 26.144 0.044 1996 2 NaN NaN NaN NaN NaN NaN 26.452 -0.043 1996 3 NaN NaN NaN NaN NaN NaN 27.350 0.438 1996 4 NaN NaN NaN NaN NaN NaN 27.129 0.099 1996 5 NaN NaN NaN NaN NaN NaN 28.056 0.615 1996 6 NaN NaN NaN NaN NaN NaN 27.669 0.461 1996 7 NaN NaN NaN NaN NaN NaN 27.306 0.407 1996 8 NaN NaN NaN NaN NaN NaN 26.952 0.084 1996 9 NaN NaN NaN NaN NaN NaN 27.000 0.180 1996 10 NaN NaN NaN NaN NaN NaN 26.711 0.087 1996 11 NaN NaN NaN NaN NaN NaN 27.079 0.513 1996 12 NaN NaN NaN NaN NaN NaN 26.654 0.440 1997 1 26.000 0.441 0 0 26.000 0.441 26.381 0.282 1997 2 26.800 0.846 0 0 26.800 0.846 27.161 0.666 1997 3 26.300 -0.071 0 0 26.300 -0.071 27.221 0.309 1997 4 26.600 0.111 0 0 26.600 0.111 27.091 0.061 1997 5 27.200 0.300 0 0 27.200 0.300 28.053 0.613 1997 6 NaN NaN NaN NaN NaN NaN 27.930 0.722 1997 7 26.800 0.442 0 0 26.800 0.442 27.451 0.553 1997 8 27.500 1.173 0 0 27.500 1.173 27.892 1.024 1997 9 NaN NaN NaN NaN NaN NaN 27.335 0.514 1997 10 NaN NaN NaN NaN NaN NaN 27.104 0.480 1997 11 NaN NaN NaN NaN NaN NaN 27.358 0.792 1997 12 NaN NaN NaN NaN NaN NaN 27.301 1.087 1998 1 NaN NaN NaN NaN NaN NaN 27.529 1.429 1998 2 27.400 1.446 0 0 27.400 1.446 28.128 1.634 1998 3 27.600 1.229 0 0 27.600 1.229 28.465 1.553 1998 4 27.700 1.211 0 0 27.700 1.211 28.382 1.353 1998 5 28.000 1.100 0 0 28.000 1.100 28.801 1.360 1998 6 NaN NaN NaN NaN NaN NaN 28.034 0.826 1998 7 NaN NaN NaN NaN NaN NaN 27.323 0.424 1998 8 NaN NaN NaN NaN NaN NaN 26.961 0.094 1998 9 NaN NaN NaN NaN NaN NaN 27.378 0.557 1998 10 NaN NaN NaN NaN NaN NaN 27.278 0.655 1998 11 NaN NaN NaN NaN NaN NaN 27.416 0.850 1998 12 NaN NaN NaN NaN NaN NaN 26.710 0.496 1999 1 27.100 1.541 0 0 27.100 1.541 26.705 0.606 1999 2 26.800 0.846 0 0 26.800 0.846 27.093 0.599 1999 3 NaN NaN NaN NaN NaN NaN 27.166 0.255 1999 4 NaN NaN NaN NaN NaN NaN 27.501 0.471 1999 5 NaN NaN NaN NaN NaN NaN 27.530 0.089 1999 6 NaN NaN NaN NaN NaN NaN 27.378 0.171 1999 7 NaN NaN NaN NaN NaN NaN 26.838 -0.061 1999 8 NaN NaN NaN NaN NaN NaN 26.981 0.114 1999 9 NaN NaN NaN NaN NaN NaN 26.995 0.175 1999 10 NaN NaN NaN NaN NaN NaN 26.554 -0.070 1999 11 NaN NaN NaN NaN NaN NaN 26.842 0.276 1999 12 NaN NaN NaN NaN NaN NaN 26.614 0.400 2000 1 NaN NaN NaN NaN NaN NaN 26.085 -0.014 2000 2 NaN NaN NaN NaN NaN NaN 26.640 0.145