% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 13481 % Primary Name: FANANU % Record Type: TAVG % Country: Federated States of Micronesia % State: FM % Latitude: 8.55000 +/- 0.00005 % Longitude: 151.90920 +/- 0.00005 % Elevation (m): 0.91 +/- 0.15 % # of Months: 14 % % Alternate Names: Missing Station ID - 914251 % % IDs: coop - 914251 % ghcnd - FMC00914251 % ncdc - 30001523 % nws - FNUP8 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 586e512fa1cde84a7bdb4765ae5a2833 % Raw Data Hash: 8c50c6f52b1cb805fddec3a0dede64de % Adj Data Hash: 7539f12602f6f93e18f1908c492dab18 % % 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 2002 10 NaN NaN NaN NaN NaN NaN 28.886 0.658 2002 11 NaN NaN NaN NaN NaN NaN 29.027 0.689 2002 12 NaN NaN NaN NaN NaN NaN 28.586 0.469 2003 1 NaN NaN NaN NaN NaN NaN 28.356 0.416 2003 2 NaN NaN NaN NaN NaN NaN 28.434 0.541 2003 3 NaN NaN NaN NaN NaN NaN 28.654 0.705 2003 4 NaN NaN NaN NaN NaN NaN 28.405 0.495 2003 5 NaN NaN NaN NaN NaN NaN 28.437 0.150 2003 6 NaN NaN NaN NaN NaN NaN 28.588 0.186 2003 7 NaN NaN NaN NaN NaN NaN 28.441 0.294 2003 8 NaN NaN NaN NaN NaN NaN 28.846 0.647 2003 9 NaN NaN NaN NaN NaN NaN 28.809 0.467 2003 10 29.889 1.344 0 0 29.889 1.344 29.197 0.969 2003 11 28.833 0.179 0 0 28.833 0.179 28.755 0.417 2003 12 28.333 -0.101 0 0 28.333 -0.101 28.347 0.230 2004 1 28.722 0.466 0 0 28.722 0.466 28.547 0.607 2004 2 28.778 0.568 0 0 28.778 0.568 28.620 0.726 2004 3 29.111 0.846 0 0 29.111 0.846 28.914 0.966 2004 4 29.056 0.829 0 0 29.056 0.829 28.607 0.698 2004 5 29.270 0.667 1 0 NaN NaN 28.974 0.688 2004 6 28.278 -0.441 0 0 28.278 -0.441 28.486 0.084 2004 7 NaN NaN NaN NaN NaN NaN 28.916 0.770 2004 8 NaN NaN NaN NaN NaN NaN 28.727 0.528 2004 9 NaN NaN NaN NaN NaN NaN 29.109 0.768 2004 10 29.667 1.122 0 0 29.667 1.122 29.198 0.970 2004 11 29.889 1.234 0 0 29.889 1.234 29.446 1.108 2004 12 NaN NaN NaN NaN NaN NaN 28.894 0.777 2005 1 29.278 1.021 0 0 29.278 1.021 28.691 0.752 2005 2 NaN NaN NaN NaN NaN NaN 28.715 0.822 2005 3 NaN NaN NaN NaN NaN NaN 28.735 0.786 2005 4 NaN NaN NaN NaN NaN NaN 28.695 0.786 2005 5 29.778 1.174 0 0 29.778 1.174 29.235 0.948 2005 6 29.833 1.114 0 0 29.833 1.114 29.281 0.879 2005 7 NaN NaN NaN NaN NaN NaN 28.942 0.796 2005 8 NaN NaN NaN NaN NaN NaN 28.857 0.659 2005 9 NaN NaN NaN NaN NaN NaN 28.911 0.569 2005 10 NaN NaN NaN NaN NaN NaN 29.000 0.772 2005 11 NaN NaN NaN NaN NaN NaN 29.362 1.025 2005 12 NaN NaN NaN NaN NaN NaN 29.025 0.908 2006 1 NaN NaN NaN NaN NaN NaN 28.581 0.641 2006 2 NaN NaN NaN NaN NaN NaN 28.531 0.638 2006 3 NaN NaN NaN NaN NaN NaN 28.524 0.576 2006 4 NaN NaN NaN NaN NaN NaN 28.617 0.708 2006 5 NaN NaN NaN NaN NaN NaN 28.535 0.248 2006 6 NaN NaN NaN NaN NaN NaN 29.022 0.620