% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 15399 % Primary Name: STA. KLIMATOLOGI CILEDUG % Record Type: TAVG % Country: Indonesia % Latitude: -6.26667 +/- 0.00833 % Longitude: 106.66667 +/- 0.00833 % Elevation (m): 24.68 +/- 18.63 % # of Months: 15 % % IDs: wwr - 96I29 % % Sources: World Weather Records % % Site Hash: 1790cfa6336c1c4220cefe122ccb6e22 % Raw Data Hash: 8a33fe83d17943cf2fd7e53e3344d645 % Adj Data Hash: 8a33fe83d17943cf2fd7e53e3344d645 % % 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 4 NaN NaN NaN NaN NaN NaN 27.418 0.084 1997 5 NaN NaN NaN NaN NaN NaN 28.030 0.538 1997 6 NaN NaN NaN NaN NaN NaN 27.554 0.602 1997 7 NaN NaN NaN NaN NaN NaN 26.840 0.337 1997 8 NaN NaN NaN NaN NaN NaN 26.928 0.435 1997 9 NaN NaN NaN NaN NaN NaN 27.152 0.569 1997 10 NaN NaN NaN NaN NaN NaN 27.747 1.176 1997 11 NaN NaN NaN NaN NaN NaN 27.906 1.186 1997 12 NaN NaN NaN NaN NaN NaN 27.759 1.300 1998 1 NaN NaN NaN NaN NaN NaN 27.936 1.670 1998 2 NaN NaN NaN NaN NaN NaN 27.845 1.277 1998 3 NaN NaN NaN NaN NaN NaN 28.209 1.137 1998 4 28.000 0.447 0 0 28.000 0.447 28.316 0.982 1998 5 NaN NaN NaN NaN NaN NaN 28.829 1.336 1998 6 27.100 -0.070 0 0 27.100 -0.070 27.643 0.690 1998 7 27.300 0.579 0 0 27.300 0.579 27.038 0.535 1998 8 NaN NaN NaN NaN NaN NaN 27.026 0.534 1998 9 NaN NaN NaN NaN NaN NaN 27.177 0.594 1998 10 NaN NaN NaN NaN NaN NaN 26.760 0.189 1998 11 27.800 0.862 0 0 27.800 0.862 27.114 0.395 1998 12 27.800 1.123 0 0 27.800 1.123 27.031 0.572 1999 1 26.300 -0.184 0 0 26.300 -0.184 26.411 0.146 1999 2 NaN NaN NaN NaN NaN NaN 26.820 0.252 1999 3 27.400 0.109 0 0 27.400 0.109 27.684 0.611 1999 4 NaN NaN NaN NaN NaN NaN 28.092 0.758 1999 5 27.300 -0.411 0 0 27.300 -0.411 27.562 0.070 1999 6 27.000 -0.170 0 0 27.000 -0.170 27.274 0.322 1999 7 26.800 0.079 0 0 26.800 0.079 26.529 0.026 1999 8 27.300 0.590 0 0 27.300 0.590 26.544 0.052 1999 9 28.000 1.199 0 0 28.000 1.199 27.095 0.512 1999 10 27.300 0.511 0 0 27.300 0.511 26.524 -0.047 1999 11 27.300 0.362 0 0 27.300 0.362 26.865 0.145 1999 12 26.800 0.123 0 0 26.800 0.123 26.596 0.138 2000 1 NaN NaN NaN NaN NaN NaN 26.508 0.242 2000 2 NaN NaN NaN NaN NaN NaN 26.968 0.400 2000 3 NaN NaN NaN NaN NaN NaN 27.632 0.560 2000 4 NaN NaN NaN NaN NaN NaN 27.723 0.388 2000 5 NaN NaN NaN NaN NaN NaN 28.127 0.634 2000 6 NaN NaN NaN NaN NaN NaN 27.018 0.065 2000 7 NaN NaN NaN NaN NaN NaN 26.974 0.471 2000 8 NaN NaN NaN NaN NaN NaN 26.595 0.103 2000 9 NaN NaN NaN NaN NaN NaN 27.348 0.765 2000 10 NaN NaN NaN NaN NaN NaN 27.044 0.473 2000 11 NaN NaN NaN NaN NaN NaN 26.950 0.231 2000 12 NaN NaN NaN NaN NaN NaN 27.360 0.901