% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 160171 % Primary Name: CAPE KUMUKAHI AIR SAMPLE STN % Record Type: TAVG % Country: United States % State: HI % Latitude: 19.51668 +/- 0.01253 % Longitude: -154.80831 +/- 0.00836 % Elevation (m): 11.78 +/- 8.83 % # of Months: 27 % % Alternate Names: CAPE KUMUKAHI % % IDs: coop - 510298 % ghcnd - USC00510298 % ncdc - 20023212 % ncdc - 20023835 % wban - 21512 % % Sources: US First Order Summary of the Day % US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 47cf312b5e8a38ddc83c704d55fea483 % Raw Data Hash: 8a3973c06a4c05521e6c07917a80143a % Adj Data Hash: 4e52b63ee927938cbfd59c76dacd5968 % % 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 1956 11 NaN NaN NaN NaN NaN NaN 22.182 -0.085 1956 12 NaN NaN NaN NaN NaN NaN 21.204 0.172 1957 1 NaN NaN NaN NaN NaN NaN 20.451 0.019 1957 2 NaN NaN NaN NaN NaN NaN 19.076 -1.098 1957 3 NaN NaN NaN NaN NaN NaN 19.460 -0.862 1957 4 NaN NaN NaN NaN NaN NaN 20.214 -0.438 1957 5 NaN NaN NaN NaN NaN NaN 21.021 -0.568 1957 6 NaN NaN NaN NaN NaN NaN 22.343 -0.065 1957 7 NaN NaN NaN NaN NaN NaN 22.727 -0.188 1957 8 NaN NaN NaN NaN NaN NaN 22.974 -0.340 1957 9 NaN NaN NaN NaN NaN NaN 23.561 0.181 1957 10 NaN NaN NaN NaN NaN NaN 23.442 0.430 1957 11 23.667 0.347 0 0 23.667 0.347 22.683 0.415 1957 12 21.833 -0.251 0 0 21.833 -0.251 20.980 -0.052 1958 1 21.556 0.071 0 0 21.556 0.071 20.123 -0.309 1958 2 21.889 0.663 0 0 21.889 0.663 20.162 -0.012 1958 3 21.222 -0.152 0 0 21.222 -0.152 19.790 -0.532 1958 4 20.833 -0.871 0 0 20.833 -0.871 20.289 -0.363 1958 5 20.611 -2.031 0 0 20.611 -2.031 20.916 -0.673 1958 6 21.778 -1.682 0 0 21.778 -1.682 21.956 -0.451 1958 7 22.889 -1.079 0 0 22.889 -1.079 22.585 -0.330 1958 8 22.889 -1.478 0 0 22.889 -1.478 23.432 0.118 1958 9 25.278 0.846 0 0 25.278 0.846 23.346 -0.033 1958 10 24.722 0.658 0 0 24.722 0.658 22.793 -0.218 1958 11 23.889 0.569 0 0 23.889 0.569 22.289 0.021 1958 12 22.000 -0.084 0 0 22.000 -0.084 20.823 -0.209 1959 1 21.722 0.238 0 0 21.722 0.238 21.194 0.762 1959 2 21.556 0.329 0 0 21.556 0.329 20.018 -0.156 1959 3 22.444 1.070 0 0 22.444 1.070 20.799 0.477 1959 4 22.611 0.907 0 0 22.611 0.907 20.933 0.281 1959 5 23.611 0.969 0 0 23.611 0.969 21.609 0.020 1959 6 24.167 0.707 0 0 24.167 0.707 22.583 0.176 1959 7 24.667 0.699 0 0 24.667 0.699 23.195 0.280 1959 8 25.000 0.634 0 0 25.000 0.634 23.624 0.311 1959 9 24.556 0.124 0 0 24.556 0.124 23.530 0.151 1959 10 24.000 -0.064 0 0 24.000 -0.064 23.291 0.279 1959 11 22.667 -0.653 0 0 22.667 -0.653 22.588 0.321 1959 12 21.500 -0.584 0 0 21.500 -0.584 20.656 -0.375 1960 1 22.077 0.593 1 0 NaN NaN 19.936 -0.496 1960 2 NaN NaN NaN NaN NaN NaN 20.182 0.009 1960 3 NaN NaN NaN NaN NaN NaN 20.588 0.266 1960 4 NaN NaN NaN NaN NaN NaN 20.799 0.147 1960 5 NaN NaN NaN NaN NaN NaN 21.936 0.347 1960 6 NaN NaN NaN NaN NaN NaN 22.516 0.109 1960 7 NaN NaN NaN NaN NaN NaN 22.938 0.023 1960 8 NaN NaN NaN NaN NaN NaN 23.333 0.019 1960 9 NaN NaN NaN NaN NaN NaN 23.332 -0.047 1960 10 NaN NaN NaN NaN NaN NaN 23.451 0.440 1960 11 NaN NaN NaN NaN NaN NaN 22.190 -0.077 1960 12 NaN NaN NaN NaN NaN NaN 21.231 0.200 1961 1 NaN NaN NaN NaN NaN NaN 20.815 0.383