% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 16518 % Primary Name: OMINATO % Record Type: TAVG % Country: Japan % Latitude: 41.23300 +/- 0.00050 % Longitude: 141.15000 +/- 0.00050 % Elevation (m): 10.00 +/- 0.05 % # of Months: 20 % % IDs: gsod - 475170-99999 % usaf - 475170 % % Sources: Global Summary of the Day % % Site Hash: b9fc2231f9e50d7fa9228245978f9d46 % Raw Data Hash: aee144bd870c6aae66c31fb56ea555a5 % Adj Data Hash: d899954cfbdb442306ad757f0e091844 % % 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 2 NaN NaN NaN NaN NaN NaN -1.296 0.536 1987 3 NaN NaN NaN NaN NaN NaN 1.248 -0.260 1987 4 NaN NaN NaN NaN NaN NaN 7.432 0.028 1987 5 NaN NaN NaN NaN NaN NaN 13.435 0.693 1987 6 NaN NaN NaN NaN NaN NaN 17.646 1.141 1987 7 NaN NaN NaN NaN NaN NaN 20.916 0.136 1987 8 NaN NaN NaN NaN NaN NaN 21.668 -0.942 1987 9 NaN NaN NaN NaN NaN NaN 18.201 -0.412 1987 10 NaN NaN NaN NaN NaN NaN 12.938 0.473 1987 11 NaN NaN NaN NaN NaN NaN 5.854 -0.503 1987 12 NaN NaN NaN NaN NaN NaN 0.627 -0.144 1988 1 NaN NaN NaN NaN NaN NaN -1.136 1.055 1988 2 -0.032 -0.198 1 0 NaN NaN -3.310 -1.478 1988 3 NaN NaN NaN NaN NaN NaN 0.976 -0.533 1988 4 NaN NaN NaN NaN NaN NaN 7.872 0.469 1988 5 NaN NaN NaN NaN NaN NaN 12.645 -0.098 1988 6 NaN NaN NaN NaN NaN NaN 16.331 -0.174 1988 7 NaN NaN NaN NaN NaN NaN 17.553 -3.227 1988 8 NaN NaN NaN NaN NaN NaN 23.348 0.738 1988 9 NaN NaN NaN NaN NaN NaN 18.200 -0.413 1988 10 12.811 -1.652 1 0 NaN NaN 11.757 -0.708 1988 11 5.816 -2.539 1 0 NaN NaN 5.212 -1.144 1988 12 3.024 0.255 1 0 NaN NaN 1.406 0.635 1989 1 2.103 2.296 1 0 NaN NaN 0.148 2.339 1989 2 2.739 2.573 1 0 NaN NaN 0.899 2.731 1989 3 5.998 2.491 0 0 5.998 2.491 3.720 2.212 1989 4 10.204 0.802 1 0 NaN NaN 8.568 1.164 1989 5 16.776 2.036 1 0 NaN NaN 13.159 0.417 1989 6 16.960 -1.543 1 0 NaN NaN 15.239 -1.266 1989 7 23.334 0.556 1 0 NaN NaN 21.072 0.292 1989 8 25.685 1.076 1 0 NaN NaN 23.670 1.059 1989 9 20.865 0.254 0 0 20.865 0.254 18.259 -0.354 1989 10 15.421 0.957 1 0 NaN NaN 12.584 0.118 1989 11 10.233 1.878 1 0 NaN NaN 8.654 2.297 1989 12 4.119 1.350 1 0 NaN NaN 1.558 0.787 1990 1 -0.748 -0.555 1 0 NaN NaN -2.392 -0.201 1990 2 2.845 2.679 0 0 2.845 2.679 1.734 3.566 1990 3 6.507 3.001 1 0 NaN NaN 3.752 2.244 1990 4 10.101 0.699 1 0 NaN NaN 8.689 1.285 1990 5 NaN NaN NaN NaN NaN NaN 14.226 1.484 1990 6 NaN NaN NaN NaN NaN NaN 18.070 1.565 1990 7 NaN NaN NaN NaN NaN NaN 20.683 -0.097 1990 8 NaN NaN NaN NaN NaN NaN 24.081 1.470 1990 9 NaN NaN NaN NaN NaN NaN 19.276 0.663 1990 10 NaN NaN NaN NaN NaN NaN 13.903 1.437 1990 11 NaN NaN NaN NaN NaN NaN 9.465 3.109 1990 12 NaN NaN NaN NaN NaN NaN 3.772 3.001 1991 1 NaN NaN NaN NaN NaN NaN 0.057 2.248 1991 2 NaN NaN NaN NaN NaN NaN -0.858 0.974 1991 3 NaN NaN NaN NaN NaN NaN 1.663 0.155 1991 4 NaN NaN NaN NaN NaN NaN 8.713 1.310