% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 17568 % Primary Name: KROH % Record Type: TAVG % Country: Malaysia % Latitude: 5.72000 +/- 0.00500 % Longitude: 101.00000 +/- 0.00500 % Elevation (m): 368.68 +/- 206.20 % # of Months: 18 % % IDs: ca - 349 % % Sources: Colonial Archive % % Site Hash: 126321e389e2613099677d5559236c71 % Raw Data Hash: 5a70f5c447f4adf1dbb62b7a94a285da % Adj Data Hash: 5a70f5c447f4adf1dbb62b7a94a285da % % 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 1931 1 NaN NaN NaN NaN NaN NaN 24.904 0.031 1931 2 NaN NaN NaN NaN NaN NaN 25.960 0.249 1931 3 NaN NaN NaN NaN NaN NaN 26.868 0.491 1931 4 NaN NaN NaN NaN NaN NaN 26.936 0.324 1931 5 NaN NaN NaN NaN NaN NaN 26.750 0.273 1931 6 NaN NaN NaN NaN NaN NaN 25.879 -0.019 1931 7 NaN NaN NaN NaN NaN NaN 25.217 -0.308 1931 8 NaN NaN NaN NaN NaN NaN 25.875 0.287 1931 9 NaN NaN NaN NaN NaN NaN 25.539 -0.020 1931 10 NaN NaN NaN NaN NaN NaN 25.072 -0.140 1931 11 NaN NaN NaN NaN NaN NaN 24.778 -0.185 1931 12 NaN NaN NaN NaN NaN NaN 24.434 -0.225 1932 1 24.350 -0.651 0 0 24.350 -0.651 24.008 -0.865 1932 2 25.700 -0.139 0 0 25.700 -0.139 25.372 -0.340 1932 3 25.900 -0.605 0 0 25.900 -0.605 25.719 -0.658 1932 4 26.250 -0.490 0 0 26.250 -0.490 26.135 -0.477 1932 5 26.400 -0.204 0 0 26.400 -0.204 26.430 -0.047 1932 6 25.350 -0.675 0 0 25.350 -0.675 25.483 -0.415 1932 7 25.250 -0.402 0 0 25.250 -0.402 25.219 -0.306 1932 8 25.750 0.034 0 0 25.750 0.034 25.634 0.046 1932 9 24.850 -0.837 0 0 24.850 -0.837 25.347 -0.212 1932 10 25.500 0.160 0 0 25.500 0.160 25.198 -0.014 1932 11 24.850 -0.240 0 0 24.850 -0.240 24.802 -0.160 1932 12 24.750 -0.036 0 0 24.750 -0.036 24.439 -0.219 1933 1 24.650 -0.351 0 0 24.650 -0.351 24.656 -0.218 1933 2 25.650 -0.189 0 0 25.650 -0.189 25.112 -0.599 1933 3 26.550 0.045 0 0 26.550 0.045 26.011 -0.367 1933 4 26.300 -0.440 0 0 26.300 -0.440 26.050 -0.562 1933 5 26.600 -0.004 0 0 26.600 -0.004 26.426 -0.050 1933 6 25.350 -0.675 0 0 25.350 -0.675 25.660 -0.238 1933 7 NaN NaN NaN NaN NaN NaN 25.194 -0.331 1933 8 NaN NaN NaN NaN NaN NaN 25.635 0.047 1933 9 NaN NaN NaN NaN NaN NaN 25.476 -0.083 1933 10 NaN NaN NaN NaN NaN NaN 25.022 -0.190 1933 11 NaN NaN NaN NaN NaN NaN 24.481 -0.482 1933 12 NaN NaN NaN NaN NaN NaN 24.216 -0.443 1934 1 NaN NaN NaN NaN NaN NaN 24.198 -0.675 1934 2 NaN NaN NaN NaN NaN NaN 24.653 -1.058 1934 3 NaN NaN NaN NaN NaN NaN 25.532 -0.845 1934 4 NaN NaN NaN NaN NaN NaN 25.920 -0.693 1934 5 NaN NaN NaN NaN NaN NaN 26.016 -0.460 1934 6 NaN NaN NaN NaN NaN NaN 25.511 -0.386