% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 25460 % Primary Name: MORSE FIELD HAWAII % Record Type: TAVG % Country: United States % State: HI % Latitude: 18.91600 +/- 0.00050 % Longitude: -155.68300 +/- 0.00050 % Elevation (m): 12.00 +/- 0.05 % # of Months: 24 % % IDs: gsod - 749154-99999 % usaf - 749154 % % Sources: Global Summary of the Day % % Site Hash: fd48c32df777e77306bfe3dfaceae7a7 % Raw Data Hash: e6547ad9241468e06fe4e7cf327fd431 % Adj Data Hash: f3c5ffda1a96a13247ce91e690f13e49 % % 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 1939 1 NaN NaN NaN NaN NaN NaN 21.965 -0.207 1939 2 NaN NaN NaN NaN NaN NaN 21.380 -0.020 1939 3 NaN NaN NaN NaN NaN NaN 20.433 -0.654 1939 4 NaN NaN NaN NaN NaN NaN 20.698 -0.497 1939 5 NaN NaN NaN NaN NaN NaN 21.657 -0.347 1939 6 NaN NaN NaN NaN NaN NaN 21.688 -1.127 1939 7 NaN NaN NaN NaN NaN NaN 22.786 -0.768 1939 8 NaN NaN NaN NaN NaN NaN 23.561 -0.529 1939 9 NaN NaN NaN NaN NaN NaN 23.637 -0.591 1939 10 NaN NaN NaN NaN NaN NaN 23.777 -0.498 1939 11 NaN NaN NaN NaN NaN NaN 23.201 -0.899 1939 12 NaN NaN NaN NaN NaN NaN 23.107 0.005 1940 1 24.359 -1.014 1 0 NaN NaN 22.930 0.758 1940 2 24.656 0.056 1 0 NaN NaN 22.025 0.625 1940 3 25.147 0.859 0 0 25.147 0.859 21.662 0.575 1940 4 26.156 1.760 0 0 26.156 1.760 22.053 0.858 1940 5 26.792 1.587 0 0 26.792 1.587 22.751 0.747 1940 6 26.498 0.482 0 0 26.498 0.482 23.026 0.210 1940 7 27.204 0.450 0 0 27.204 0.450 23.929 0.376 1940 8 27.568 0.277 0 0 27.568 0.277 24.403 0.313 1940 9 27.602 0.174 0 0 27.602 0.174 24.255 0.027 1940 10 27.728 0.252 0 0 27.728 0.252 24.649 0.374 1940 11 26.263 -1.037 0 0 26.263 -1.037 24.521 0.422 1940 12 25.403 -0.900 0 0 25.403 -0.900 23.422 0.320 1941 1 25.342 -0.031 0 0 25.342 -0.031 22.874 0.702 1941 2 24.756 0.155 1 0 NaN NaN 21.259 -0.141 1941 3 24.470 0.181 0 0 24.470 0.181 20.599 -0.489 1941 4 25.207 0.812 0 0 25.207 0.812 21.175 -0.020 1941 5 25.728 0.522 0 0 25.728 0.522 21.726 -0.279 1941 6 27.015 0.999 0 0 27.015 0.999 23.100 0.285 1941 7 27.188 0.434 0 0 27.188 0.434 23.595 0.042 1941 8 28.133 0.842 0 0 28.133 0.842 24.743 0.653 1941 9 27.443 0.015 0 0 27.443 0.015 24.445 0.217 1941 10 26.405 -1.071 0 0 26.405 -1.071 24.259 -0.016 1941 11 26.067 -1.234 0 0 26.067 -1.234 24.155 0.055 1941 12 24.406 -1.897 1 0 NaN NaN 22.554 -0.548 1942 1 NaN NaN NaN NaN NaN NaN 22.474 0.301 1942 2 NaN NaN NaN NaN NaN NaN 21.537 0.137 1942 3 NaN NaN NaN NaN NaN NaN 19.901 -1.187 1942 4 NaN NaN NaN NaN NaN NaN 20.340 -0.855 1942 5 NaN NaN NaN NaN NaN NaN 22.047 0.042 1942 6 NaN NaN NaN NaN NaN NaN 22.898 0.083 1942 7 NaN NaN NaN NaN NaN NaN 23.834 0.280 1942 8 NaN NaN NaN NaN NaN NaN 24.396 0.306 1942 9 NaN NaN NaN NaN NaN NaN 24.460 0.233 1942 10 NaN NaN NaN NaN NaN NaN 24.688 0.413 1942 11 NaN NaN NaN NaN NaN NaN 24.974 0.875 1942 12 NaN NaN NaN NaN NaN NaN 24.147 1.045