% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 2795 % Primary Name: FALEASAO TAU % Record Type: TAVG % Country: American Samoa [United States] % State: PI % Latitude: -14.21667 +/- 0.00833 % Longitude: -168.53333 +/- 0.00833 % Elevation (m): 6.10 +/- 0.05 % # of Months: 9 % % IDs: coop - 914188 % % Sources: US Cooperative Summary of the Day % US Cooperative Summary of the Month % % Site Hash: cb5248447515edb5ced9e519a930908c % Raw Data Hash: f1992cb926bad610e62dea7fa1077091 % Adj Data Hash: f15ac6a186334b488dd1ff0cca1f1623 % % 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 1954 6 NaN NaN NaN NaN NaN NaN 27.094 0.120 1954 7 NaN NaN NaN NaN NaN NaN 26.585 0.077 1954 8 NaN NaN NaN NaN NaN NaN 26.790 0.339 1954 9 NaN NaN NaN NaN NaN NaN 27.015 0.418 1954 10 NaN NaN NaN NaN NaN NaN 26.824 0.285 1954 11 NaN NaN NaN NaN NaN NaN 26.445 -0.381 1954 12 NaN NaN NaN NaN NaN NaN 27.033 0.078 1955 1 NaN NaN NaN NaN NaN NaN 26.863 -0.349 1955 2 NaN NaN NaN NaN NaN NaN 27.159 -0.183 1955 3 NaN NaN NaN NaN NaN NaN 26.863 -0.647 1955 4 NaN NaN NaN NaN NaN NaN 27.107 -0.348 1955 5 NaN NaN NaN NaN NaN NaN 27.081 -0.230 1955 6 27.500 0.641 0 0 27.500 0.641 27.285 0.310 1955 7 27.111 0.718 0 0 27.111 0.718 26.957 0.449 1955 8 27.444 1.109 0 0 27.444 1.109 26.942 0.491 1955 9 26.944 0.463 0 0 26.944 0.463 26.895 0.298 1955 10 25.500 -0.923 0 0 25.500 -0.923 26.409 -0.129 1955 11 26.611 -0.100 0 0 26.611 -0.100 26.793 -0.033 1955 12 25.944 -0.895 0 0 25.944 -0.895 26.581 -0.374 1956 1 NaN NaN NaN NaN NaN NaN 26.940 -0.272 1956 2 NaN NaN NaN NaN NaN NaN 27.034 -0.309 1956 3 NaN NaN NaN NaN NaN NaN 27.401 -0.109 1956 4 NaN NaN NaN NaN NaN NaN 27.321 -0.134 1956 5 26.333 -0.862 1 0 NaN NaN 26.883 -0.428 1956 6 NaN NaN NaN NaN NaN NaN 26.369 -0.605 1956 7 NaN NaN NaN NaN NaN NaN 26.092 -0.416 1956 8 NaN NaN NaN NaN NaN NaN 26.278 -0.173 1956 9 NaN NaN NaN NaN NaN NaN 26.255 -0.342 1956 10 NaN NaN NaN NaN NaN NaN 26.465 -0.074 1956 11 NaN NaN NaN NaN NaN NaN 26.550 -0.277 1956 12 NaN NaN NaN NaN NaN NaN 26.481 -0.474 1957 1 NaN NaN NaN NaN NaN NaN 26.836 -0.376 1957 2 NaN NaN NaN NaN NaN NaN 27.105 -0.237 1957 3 NaN NaN NaN NaN NaN NaN 27.255 -0.255 1957 4 NaN NaN NaN NaN NaN NaN 27.320 -0.135 1957 5 NaN NaN NaN NaN NaN NaN 27.219 -0.091 1957 6 NaN NaN NaN NaN NaN NaN 27.081 0.106 1957 7 25.056 -1.337 1 0 NaN NaN 26.291 -0.217 1957 8 NaN NaN NaN NaN NaN NaN 26.641 0.190 1957 9 NaN NaN NaN NaN NaN NaN 26.838 0.241 1957 10 NaN NaN NaN NaN NaN NaN 26.614 0.075 1957 11 NaN NaN NaN NaN NaN NaN 27.058 0.231 1957 12 NaN NaN NaN NaN NaN NaN 27.307 0.352 1958 1 NaN NaN NaN NaN NaN NaN 27.609 0.397 1958 2 NaN NaN NaN NaN NaN NaN 27.539 0.196 1958 3 NaN NaN NaN NaN NaN NaN 27.860 0.351 1958 4 NaN NaN NaN NaN NaN NaN 28.046 0.591 1958 5 NaN NaN NaN NaN NaN NaN 27.528 0.218 1958 6 NaN NaN NaN NaN NaN NaN 26.805 -0.170 1958 7 NaN NaN NaN NaN NaN NaN 26.434 -0.074