% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 16257 % Primary Name: OKINAWA RYUKYU IS/YONTAN AB % Record Type: TAVG % Country: Japan % Latitude: 26.38300 +/- 0.00050 % Longitude: 127.75000 +/- 0.00050 % Elevation (m): 76.00 +/- 0.05 % # of Months: 34 % % IDs: gsod - 749331-99999 % usaf - 749331 % % Sources: Global Summary of the Day % % Site Hash: fe0148a622c4f426b22444000d2a195c % Raw Data Hash: 01833a11353bda879f2794199402748b % Adj Data Hash: e8da55a22bb354a429d7d8b52bb9b5a8 % % 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 1950 5 NaN NaN NaN NaN NaN NaN 23.252 -0.648 1950 6 NaN NaN NaN NaN NaN NaN 25.023 -1.458 1950 7 NaN NaN NaN NaN NaN NaN 28.132 -0.567 1950 8 NaN NaN NaN NaN NaN NaN 27.857 -0.584 1950 9 NaN NaN NaN NaN NaN NaN 27.612 0.115 1950 10 NaN NaN NaN NaN NaN NaN 24.792 0.292 1950 11 NaN NaN NaN NaN NaN NaN 21.724 -0.022 1950 12 NaN NaN NaN NaN NaN NaN 16.706 -1.504 1951 1 NaN NaN NaN NaN NaN NaN 16.013 0.020 1951 2 NaN NaN NaN NaN NaN NaN 16.988 0.582 1951 3 NaN NaN NaN NaN NaN NaN 17.051 -1.057 1951 4 NaN NaN NaN NaN NaN NaN 20.776 -0.249 1951 5 24.204 0.815 1 0 NaN NaN 23.080 -0.820 1951 6 25.494 -0.475 0 0 25.494 -0.475 25.722 -0.759 1951 7 27.608 -0.581 0 0 27.608 -0.581 28.240 -0.459 1951 8 27.708 -0.223 0 0 27.708 -0.223 28.136 -0.305 1951 9 26.911 -0.075 0 0 26.911 -0.075 27.825 0.328 1951 10 23.998 0.009 0 0 23.998 0.009 24.612 0.112 1951 11 20.224 -1.012 0 0 20.224 -1.012 21.311 -0.435 1951 12 18.333 0.634 0 0 18.333 0.634 19.045 0.835 1952 1 16.013 0.530 0 0 16.013 0.530 16.427 0.434 1952 2 17.347 1.452 1 0 NaN NaN 17.240 0.834 1952 3 18.742 1.145 0 0 18.742 1.145 18.806 0.698 1952 4 21.069 0.555 0 0 21.069 0.555 21.402 0.377 1952 5 24.973 1.584 0 0 24.973 1.584 25.260 1.360 1952 6 26.691 0.721 0 0 26.691 0.721 26.932 0.451 1952 7 27.987 -0.201 0 0 27.987 -0.201 28.578 -0.121 1952 8 27.715 -0.216 0 0 27.715 -0.216 28.380 -0.062 1952 9 27.035 0.049 0 0 27.035 0.049 28.204 0.707 1952 10 24.167 0.178 0 0 24.167 0.178 24.463 -0.037 1952 11 23.059 1.823 0 0 23.059 1.823 23.792 2.045 1952 12 17.842 0.143 0 0 17.842 0.143 18.169 -0.041 1953 1 15.568 0.086 0 0 15.568 0.086 15.755 -0.238 1953 2 16.856 0.961 1 0 NaN NaN 17.205 0.798 1953 3 18.165 0.568 0 0 18.165 0.568 18.338 0.231 1953 4 18.881 -1.632 0 0 18.881 -1.632 19.301 -1.724 1953 5 21.989 -1.400 0 0 21.989 -1.400 22.663 -1.237 1953 6 27.430 1.460 0 0 27.430 1.460 27.550 1.069 1953 7 28.199 0.011 0 0 28.199 0.011 29.103 0.404 1953 8 28.251 0.320 0 0 28.251 0.320 28.575 0.133 1953 9 26.861 -0.125 0 0 26.861 -0.125 27.639 0.142 1953 10 24.498 0.509 0 0 24.498 0.509 24.877 0.377 1953 11 21.759 0.523 0 0 21.759 0.523 22.544 0.798 1953 12 19.020 1.321 0 0 19.020 1.321 19.606 1.397 1954 1 17.668 2.186 0 0 17.668 2.186 17.931 1.937 1954 2 15.569 -0.327 1 0 NaN NaN 16.789 0.383 1954 3 NaN NaN NaN NaN NaN NaN 17.307 -0.801 1954 4 NaN NaN NaN NaN NaN NaN 21.726 0.702 1954 5 NaN NaN NaN NaN NaN NaN 25.340 1.440 1954 6 NaN NaN NaN NaN NaN NaN 26.610 0.129 1954 7 NaN NaN NaN NaN NaN NaN 29.019 0.320 1954 8 NaN NaN NaN NaN NaN NaN 28.184 -0.258 1954 9 NaN NaN NaN NaN NaN NaN 27.589 0.092 1954 10 NaN NaN NaN NaN NaN NaN 23.968 -0.533 1954 11 NaN NaN NaN NaN NaN NaN 22.397 0.650 1954 12 NaN NaN NaN NaN NaN NaN 17.887 -0.323 1955 1 NaN NaN NaN NaN NaN NaN 14.787 -1.207 1955 2 NaN NaN NaN NaN NaN NaN 17.206 0.800