% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 25643 % Primary Name: COLLEGE HILLS % Record Type: TAVG % Country: United States % State: HI % Latitude: 21.31670 +/- 0.00005 % Longitude: -157.83330 +/- 0.00005 % Elevation (m): 53.34 +/- 0.15 % # of Months: 16 % % Alternate Names: Missing Station ID - 510397 % % IDs: coop - 510397 % ghcnd - USC00510397 % ncdc - 30015317 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 68bf4da08cb65ce08c14384f36dc2b90 % Raw Data Hash: 2e8afa31d06ce75278128fae7d7fcdaa % Adj Data Hash: e84ff78ed2c39a984f060dff28808198 % % 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 12 NaN NaN NaN NaN NaN NaN 21.818 -0.518 1905 1 NaN NaN NaN NaN NaN NaN 19.611 -2.000 1905 2 NaN NaN NaN NaN NaN NaN 20.627 -0.855 1905 3 NaN NaN NaN NaN NaN NaN 21.154 -0.709 1905 4 NaN NaN NaN NaN NaN NaN 21.891 -0.486 1905 5 NaN NaN NaN NaN NaN NaN 23.111 -0.396 1905 6 NaN NaN NaN NaN NaN NaN 24.155 -0.326 1905 7 NaN NaN NaN NaN NaN NaN 24.743 -0.275 1905 8 NaN NaN NaN NaN NaN NaN 25.447 0.018 1905 9 NaN NaN NaN NaN NaN NaN 25.273 -0.171 1905 10 NaN NaN NaN NaN NaN NaN 24.373 -0.357 1905 11 NaN NaN NaN NaN NaN NaN 23.840 0.078 1905 12 21.421 -0.617 0 0 21.421 -0.617 21.918 -0.418 1906 1 20.768 -0.546 0 0 20.768 -0.546 21.241 -0.370 1906 2 21.086 -0.099 0 0 21.086 -0.099 21.307 -0.175 1906 3 20.292 -1.274 0 0 20.292 -1.274 20.612 -1.251 1906 4 22.703 0.623 0 0 22.703 0.623 22.959 0.582 1906 5 NaN NaN NaN NaN NaN NaN 23.612 0.105 1906 6 NaN NaN NaN NaN NaN NaN 25.184 0.703 1906 7 NaN NaN NaN NaN NaN NaN 25.138 0.120 1906 8 NaN NaN NaN NaN NaN NaN 25.667 0.238 1906 9 NaN NaN NaN NaN NaN NaN 25.663 0.219 1906 10 24.676 0.243 0 0 24.676 0.243 25.175 0.445 1906 11 NaN NaN NaN NaN NaN NaN 23.836 0.073 1906 12 22.031 -0.008 0 0 22.031 -0.008 22.200 -0.135 1907 1 NaN NaN NaN NaN NaN NaN 21.847 0.236 1907 2 21.688 0.502 0 0 21.688 0.502 21.725 0.243 1907 3 20.927 -0.639 1 0 NaN NaN 21.069 -0.793 1907 4 21.732 -0.348 0 0 21.732 -0.348 21.303 -1.074 1907 5 22.369 -0.840 0 0 22.369 -0.840 23.295 -0.212 1907 6 23.881 -0.302 1 0 NaN NaN 24.397 -0.083 1907 7 NaN NaN NaN NaN NaN NaN 24.855 -0.163 1907 8 NaN NaN NaN NaN NaN NaN 25.243 -0.187 1907 9 25.117 -0.030 1 0 NaN NaN 25.526 0.082 1907 10 23.266 -1.167 1 0 NaN NaN 24.400 -0.330 1907 11 22.326 -1.139 1 0 NaN NaN 23.249 -0.514 1907 12 NaN NaN NaN NaN NaN NaN 22.626 0.291 1908 1 NaN NaN NaN NaN NaN NaN 21.227 -0.385 1908 2 20.274 -0.911 1 0 NaN NaN 21.464 -0.018 1908 3 NaN NaN NaN NaN NaN NaN 21.783 -0.080 1908 4 NaN NaN NaN NaN NaN NaN 22.043 -0.334 1908 5 NaN NaN NaN NaN NaN NaN 23.330 -0.177 1908 6 NaN NaN NaN NaN NaN NaN 23.648 -0.833 1908 7 NaN NaN NaN NaN NaN NaN 24.167 -0.851 1908 8 NaN NaN NaN NaN NaN NaN 24.741 -0.689 1908 9 NaN NaN NaN NaN NaN NaN 24.628 -0.816 1908 10 NaN NaN NaN NaN NaN NaN 23.830 -0.900 1908 11 NaN NaN NaN NaN NaN NaN 22.757 -1.006 1908 12 NaN NaN NaN NaN NaN NaN 21.768 -0.568 1909 1 NaN NaN NaN NaN NaN NaN 20.964 -0.648 1909 2 NaN NaN NaN NaN NaN NaN 20.712 -0.770