% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 23662 % Primary Name: BAKUAI/PA KUEI % Record Type: TAVG % Country: Taiwan % Latitude: 24.93300 +/- 0.00050 % Longitude: 121.30000 +/- 0.00050 % Elevation (m): 141.00 +/- 0.05 % # of Months: 31 % % IDs: gsod - 467373-99999 % usaf - 467373 % % Sources: Global Summary of the Day % % Site Hash: 986a8dfaaa2043eb9c39e25564783644 % Raw Data Hash: fae5fdbffdaceb9345bb030fd7c80666 % Adj Data Hash: 208140ee7ba2470b3226ee7650faf813 % % 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 1987 1 NaN NaN NaN NaN NaN NaN 14.771 0.493 1987 2 NaN NaN NaN NaN NaN NaN 15.271 0.849 1987 3 NaN NaN NaN NaN NaN NaN 17.658 1.166 1987 4 NaN NaN NaN NaN NaN NaN 19.828 -0.338 1987 5 NaN NaN NaN NaN NaN NaN 22.957 -0.734 1987 6 NaN NaN NaN NaN NaN NaN 25.317 -0.826 1987 7 NaN NaN NaN NaN NaN NaN 28.233 0.205 1987 8 NaN NaN NaN NaN NaN NaN 28.386 0.593 1987 9 NaN NaN NaN NaN NaN NaN 25.135 -1.326 1987 10 NaN NaN NaN NaN NaN NaN 24.123 0.953 1987 11 NaN NaN NaN NaN NaN NaN 21.478 1.255 1987 12 NaN NaN NaN NaN NaN NaN 16.202 -0.472 1988 1 16.092 0.429 0 0 16.092 0.429 15.595 1.317 1988 2 16.103 0.298 0 0 16.103 0.298 14.684 0.262 1988 3 15.461 -2.415 0 0 15.461 -2.415 15.081 -1.411 1988 4 20.485 -1.065 0 0 20.485 -1.065 19.109 -1.057 1988 5 26.585 1.510 0 0 26.585 1.510 24.222 0.531 1988 6 29.768 2.242 0 0 29.768 2.242 27.074 0.931 1988 7 31.236 1.824 1 0 NaN NaN 29.019 0.991 1988 8 30.009 0.833 0 0 30.009 0.833 27.800 0.007 1988 9 27.881 0.037 0 0 27.881 0.037 26.198 -0.262 1988 10 24.878 0.324 0 0 24.878 0.324 23.268 0.098 1988 11 18.977 -2.631 1 0 NaN NaN 18.911 -1.313 1988 12 16.357 -1.702 0 0 16.357 -1.702 15.926 -0.749 1989 1 16.647 0.985 0 0 16.647 0.985 15.051 0.772 1989 2 15.732 -0.074 0 0 15.732 -0.074 14.569 0.146 1989 3 16.685 -1.191 0 0 16.685 -1.191 15.877 -0.615 1989 4 22.254 0.704 0 0 22.254 0.704 20.537 0.371 1989 5 24.600 -0.474 0 0 24.600 -0.474 23.024 -0.667 1989 6 28.079 0.553 0 0 28.079 0.553 26.121 -0.022 1989 7 30.056 0.644 0 0 30.056 0.644 28.171 0.143 1989 8 29.539 0.363 0 0 29.539 0.363 27.999 0.207 1989 9 27.587 -0.257 0 0 27.587 -0.257 26.729 0.268 1989 10 23.919 -0.635 1 0 NaN NaN 22.774 -0.396 1989 11 20.298 -1.309 0 0 20.298 -1.309 19.990 -0.233 1989 12 16.601 -1.457 0 0 16.601 -1.457 16.191 -0.484 1990 1 15.970 0.307 0 0 15.970 0.307 15.008 0.729 1990 2 17.325 1.520 0 0 17.325 1.520 15.948 1.526 1990 3 18.169 0.293 0 0 18.169 0.293 16.736 0.244 1990 4 20.811 -0.739 0 0 20.811 -0.739 19.519 -0.647 1990 5 25.254 0.179 0 0 25.254 0.179 23.440 -0.251 1990 6 27.812 0.286 0 0 27.812 0.286 25.812 -0.330 1990 7 29.558 0.146 1 0 NaN NaN 28.352 0.324 1990 8 NaN NaN NaN NaN NaN NaN 27.718 -0.074 1990 9 NaN NaN NaN NaN NaN NaN 26.489 0.028 1990 10 NaN NaN NaN NaN NaN NaN 22.901 -0.269 1990 11 NaN NaN NaN NaN NaN NaN 21.597 1.374 1990 12 NaN NaN NaN NaN NaN NaN 17.504 0.829 1991 1 NaN NaN NaN NaN NaN NaN 14.643 0.364 1991 2 NaN NaN NaN NaN NaN NaN 15.143 0.721 1991 3 NaN NaN NaN NaN NaN NaN 17.926 1.433 1991 4 NaN NaN NaN NaN NaN NaN 20.576 0.410 1991 5 NaN NaN NaN NaN NaN NaN 24.302 0.611 1991 6 NaN NaN NaN NaN NaN NaN 27.115 0.972 1991 7 NaN NaN NaN NaN NaN NaN 28.643 0.615