% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 15360 % Primary Name: PG.WONOLANGUN % Record Type: TAVG % Country: Indonesia % Latitude: -7.23333 +/- 0.00833 % Longitude: 113.20000 +/- 0.00833 % Elevation (m): 0.60 +/- 10.00 % # of Months: 16 % % IDs: wwr - 96L06 % % Sources: World Weather Records % % Site Hash: 8616cdbfd5a1ef0283212807735d29e1 % Raw Data Hash: 313e42ac10438987ba3591a1ec0e8537 % Adj Data Hash: be457987c08dd6cb2a2c974b3b059cb5 % % 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 2 NaN NaN NaN NaN NaN NaN 26.720 -0.060 1997 3 NaN NaN NaN NaN NaN NaN 27.707 0.767 1997 4 NaN NaN NaN NaN NaN NaN 27.490 0.313 1997 5 NaN NaN NaN NaN NaN NaN 27.764 0.469 1997 6 NaN NaN NaN NaN NaN NaN 27.345 0.553 1997 7 NaN NaN NaN NaN NaN NaN 26.503 0.195 1997 8 NaN NaN NaN NaN NaN NaN 26.388 -0.213 1997 9 NaN NaN NaN NaN NaN NaN 27.330 -0.035 1997 10 NaN NaN NaN NaN NaN NaN 28.634 0.698 1997 11 NaN NaN NaN NaN NaN NaN 29.460 1.418 1997 12 NaN NaN NaN NaN NaN NaN 28.012 0.901 1998 1 NaN NaN NaN NaN NaN NaN 28.174 1.397 1998 2 28.400 1.294 0 0 28.400 1.294 27.827 1.048 1998 3 NaN NaN NaN NaN NaN NaN 27.689 0.749 1998 4 NaN NaN NaN NaN NaN NaN 28.009 0.833 1998 5 29.100 1.480 0 0 29.100 1.480 28.514 1.220 1998 6 28.200 1.082 0 0 28.200 1.082 27.715 0.923 1998 7 27.700 1.066 0 0 27.700 1.066 27.507 1.199 1998 8 28.500 1.573 0 0 28.500 1.573 28.030 1.430 1998 9 29.500 1.808 0 0 29.500 1.808 28.314 0.949 1998 10 29.600 1.338 0 0 29.600 1.338 28.347 0.411 1998 11 NaN NaN NaN NaN NaN NaN 27.780 -0.262 1998 12 NaN NaN NaN NaN NaN NaN 27.178 0.067 1999 1 27.200 0.097 0 0 27.200 0.097 26.739 -0.037 1999 2 26.100 -1.006 0 0 26.100 -1.006 26.983 0.204 1999 3 27.200 -0.066 0 0 27.200 -0.066 27.058 0.118 1999 4 27.300 -0.203 0 0 27.300 -0.203 27.261 0.084 1999 5 NaN NaN NaN NaN NaN NaN 27.499 0.205 1999 6 27.100 -0.018 0 0 27.100 -0.018 27.222 0.430 1999 7 NaN NaN NaN NaN NaN NaN 26.552 0.245 1999 8 NaN NaN NaN NaN NaN NaN 27.136 0.536 1999 9 28.200 0.508 0 0 28.200 0.508 27.809 0.443 1999 10 28.900 0.638 0 0 28.900 0.638 28.442 0.507 1999 11 28.000 -0.368 0 0 28.000 -0.368 28.069 0.027 1999 12 27.400 -0.037 0 0 27.400 -0.037 27.342 0.231 2000 1 NaN NaN NaN NaN NaN NaN 26.854 0.078 2000 2 NaN NaN NaN NaN NaN NaN 26.890 0.111 2000 3 NaN NaN NaN NaN NaN NaN 27.214 0.274 2000 4 NaN NaN NaN NaN NaN NaN 27.284 0.107 2000 5 NaN NaN NaN NaN NaN NaN 27.726 0.432 2000 6 NaN NaN NaN NaN NaN NaN 26.753 -0.039 2000 7 NaN NaN NaN NaN NaN NaN 26.951 0.644 2000 8 NaN NaN NaN NaN NaN NaN 27.225 0.624 2000 9 NaN NaN NaN NaN NaN NaN 28.324 0.959 2000 10 NaN NaN NaN NaN NaN NaN 28.419 0.483 2000 11 NaN NaN NaN NaN NaN NaN 28.089 0.047 2000 12 NaN NaN NaN NaN NaN NaN 27.877 0.766