% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 15301 % Primary Name: KARANG KEMIRI % Record Type: TAVG % Country: Indonesia % Latitude: -8.55000 +/- 0.00833 % Longitude: 109.55000 +/- 0.00833 % Elevation (m): 0.00 +/- 10.00 % # of Months: 24 % % IDs: wwr - 96K24 % % Sources: World Weather Records % % Site Hash: 951e971ba265d586f4b241bd78f22aa0 % Raw Data Hash: 5995af91b51a85538c86abd842e794e8 % Adj Data Hash: 5995af91b51a85538c86abd842e794e8 % % 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 26.884 0.132 1997 2 NaN NaN NaN NaN NaN NaN 27.249 0.258 1997 3 NaN NaN NaN NaN NaN NaN 27.934 0.669 1997 4 NaN NaN NaN NaN NaN NaN 27.725 0.337 1997 5 NaN NaN NaN NaN NaN NaN 27.490 0.362 1997 6 NaN NaN NaN NaN NaN NaN 26.648 0.430 1997 7 NaN NaN NaN NaN NaN NaN 25.166 -0.328 1997 8 NaN NaN NaN NaN NaN NaN 25.092 -0.297 1997 9 NaN NaN NaN NaN NaN NaN 25.406 -0.287 1997 10 NaN NaN NaN NaN NaN NaN 26.633 0.676 1997 11 NaN NaN NaN NaN NaN NaN 27.475 0.929 1997 12 NaN NaN NaN NaN NaN NaN 27.686 1.040 1998 1 27.700 0.955 0 0 27.700 0.955 27.988 1.236 1998 2 26.900 -0.084 0 0 26.900 -0.084 27.822 0.831 1998 3 27.800 0.543 0 0 27.800 0.543 28.070 0.806 1998 4 28.000 0.620 0 0 28.000 0.620 28.199 0.811 1998 5 28.100 0.980 0 0 28.100 0.980 28.310 1.183 1998 6 NaN NaN NaN NaN NaN NaN 27.374 1.156 1998 7 27.200 1.714 0 0 27.200 1.714 26.834 1.341 1998 8 27.500 2.119 0 0 27.500 2.119 26.974 1.585 1998 9 26.400 0.714 0 0 26.400 0.714 26.246 0.553 1998 10 27.400 1.450 0 0 27.400 1.450 26.696 0.739 1998 11 26.900 0.361 0 0 26.900 0.361 26.631 0.085 1998 12 27.200 0.561 0 0 27.200 0.561 27.037 0.391 1999 1 27.100 0.355 0 0 27.100 0.355 27.084 0.332 1999 2 27.100 0.116 0 0 27.100 0.116 27.364 0.373 1999 3 27.300 0.043 0 0 27.300 0.043 27.509 0.244 1999 4 27.300 -0.080 0 0 27.300 -0.080 27.566 0.178 1999 5 NaN NaN NaN NaN NaN NaN 27.307 0.179 1999 6 26.500 0.290 0 0 26.500 0.290 26.556 0.338 1999 7 25.700 0.214 0 0 25.700 0.214 25.622 0.129 1999 8 NaN NaN NaN NaN NaN NaN 25.581 0.193 1999 9 27.000 1.314 0 0 27.000 1.314 26.464 0.771 1999 10 NaN NaN NaN NaN NaN NaN 26.212 0.254 1999 11 26.700 0.161 0 0 26.700 0.161 26.717 0.171 1999 12 27.300 0.661 0 0 27.300 0.661 27.146 0.500 2000 1 27.000 0.255 0 0 27.000 0.255 27.169 0.417 2000 2 27.700 0.716 0 0 27.700 0.716 27.546 0.555 2000 3 27.300 0.043 0 0 27.300 0.043 27.485 0.220 2000 4 27.300 -0.080 0 0 27.300 -0.080 27.541 0.153 2000 5 NaN NaN NaN NaN NaN NaN 27.514 0.387 2000 6 NaN NaN NaN NaN NaN NaN 26.383 0.165 2000 7 NaN NaN NaN NaN NaN NaN 26.097 0.604 2000 8 NaN NaN NaN NaN NaN NaN 26.029 0.641 2000 9 NaN NaN NaN NaN NaN NaN 26.716 1.023 2000 10 NaN NaN NaN NaN NaN NaN 26.531 0.574 2000 11 NaN NaN NaN NaN NaN NaN 26.502 -0.044 2000 12 NaN NaN NaN NaN NaN NaN 27.331 0.685 2001 1 NaN NaN NaN NaN NaN NaN 27.061 0.309 2001 2 NaN NaN NaN NaN NaN NaN 27.088 0.097 2001 3 NaN NaN NaN NaN NaN NaN 27.250 -0.015 2001 4 NaN NaN NaN NaN NaN NaN 27.729 0.341