% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 25561 % Primary Name: KOHALA SUGAR % Record Type: TAVG % Country: United States % State: HI % Latitude: 20.25000 +/- 0.00500 % Longitude: -155.75000 +/- 0.00500 % Elevation (m): 78.44 +/- 198.03 % # of Months: 12 % % Alternate Names: Missing Station ID - 514683 % % IDs: coop - 514683 % ghcnd - USC00514683 % ncdc - 30015332 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 0785ad7f7c9fb0c6ce704ca7aa662638 % Raw Data Hash: 263ac26d34e6ec5fc373462e30b33311 % Adj Data Hash: 2297affe884bee2e7e6a72af5d8057a2 % % 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 1904 1 NaN NaN NaN NaN NaN NaN 20.182 -0.250 1904 2 NaN NaN NaN NaN NaN NaN 19.414 -0.760 1904 3 NaN NaN NaN NaN NaN NaN 19.872 -0.450 1904 4 NaN NaN NaN NaN NaN NaN 20.251 -0.401 1904 5 NaN NaN NaN NaN NaN NaN 21.114 -0.475 1904 6 NaN NaN NaN NaN NaN NaN 22.133 -0.274 1904 7 NaN NaN NaN NaN NaN NaN 22.607 -0.308 1904 8 NaN NaN NaN NaN NaN NaN 22.907 -0.407 1904 9 NaN NaN NaN NaN NaN NaN 23.086 -0.293 1904 10 NaN NaN NaN NaN NaN NaN 22.711 -0.301 1904 11 NaN NaN NaN NaN NaN NaN 21.418 -0.849 1904 12 NaN NaN NaN NaN NaN NaN 20.498 -0.533 1905 1 19.713 -1.509 0 0 19.713 -1.509 19.100 -1.332 1905 2 20.729 -0.235 1 0 NaN NaN 19.318 -0.856 1905 3 21.509 0.397 0 0 21.509 0.397 20.027 -0.295 1905 4 21.388 -0.054 0 0 21.388 -0.054 20.402 -0.250 1905 5 22.285 -0.094 0 0 22.285 -0.094 21.651 0.062 1905 6 22.937 -0.261 0 0 22.937 -0.261 22.084 -0.323 1905 7 23.486 -0.219 1 0 NaN NaN 22.898 -0.017 1905 8 24.243 0.139 1 0 NaN NaN 23.461 0.147 1905 9 23.793 -0.377 1 0 NaN NaN 23.362 -0.018 1905 10 23.280 -0.522 1 0 NaN NaN 22.710 -0.301 1905 11 22.519 -0.539 0 0 22.519 -0.539 22.272 0.005 1905 12 21.429 -0.393 0 0 21.429 -0.393 20.711 -0.320 1906 1 NaN NaN NaN NaN NaN NaN 20.300 -0.132 1906 2 NaN NaN NaN NaN NaN NaN 20.167 -0.007 1906 3 NaN NaN NaN NaN NaN NaN 19.791 -0.531 1906 4 NaN NaN NaN NaN NaN NaN 20.728 0.076 1906 5 NaN NaN NaN NaN NaN NaN 21.412 -0.177 1906 6 NaN NaN NaN NaN NaN NaN 22.662 0.255 1906 7 NaN NaN NaN NaN NaN NaN 22.738 -0.177 1906 8 NaN NaN NaN NaN NaN NaN 23.143 -0.170 1906 9 NaN NaN NaN NaN NaN NaN 23.229 -0.150 1906 10 NaN NaN NaN NaN NaN NaN 23.194 0.183 1906 11 NaN NaN NaN NaN NaN NaN 22.211 -0.056 1906 12 NaN NaN NaN NaN NaN NaN 20.849 -0.183