% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 2792 % Primary Name: AMOULI TUTUILA % Record Type: TAVG % Country: American Samoa [United States] % Latitude: -14.26670 +/- 0.00005 % Longitude: -170.58330 +/- 0.00005 % Elevation (m): 6.10 +/- 0.05 % # of Months: 30 % % Alternate Names: AMOULE % % IDs: coop - 914021 % ghcnd - AQC00914021 % ncdc - 20030356 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 41b03bbb14b4535a1db32d78aa17d4a8 % Raw Data Hash: ac0b4b2bf198b8849874ed67752cc6b6 % Adj Data Hash: 322cb29ae15b1e495798ac308a76314d % % 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 4 NaN NaN NaN NaN NaN NaN 27.217 0.057 1954 5 NaN NaN NaN NaN NaN NaN 27.230 0.184 1954 6 NaN NaN NaN NaN NaN NaN 26.827 0.059 1954 7 NaN NaN NaN NaN NaN NaN 26.381 0.065 1954 8 NaN NaN NaN NaN NaN NaN 26.496 0.245 1954 9 NaN NaN NaN NaN NaN NaN 26.843 0.433 1954 10 NaN NaN NaN NaN NaN NaN 26.560 0.160 1954 11 NaN NaN NaN NaN NaN NaN 26.257 -0.424 1954 12 NaN NaN NaN NaN NaN NaN 26.850 0.049 1955 1 NaN NaN NaN NaN NaN NaN 26.720 -0.301 1955 2 NaN NaN NaN NaN NaN NaN 26.976 -0.169 1955 3 NaN NaN NaN NaN NaN NaN 26.501 -0.743 1955 4 26.889 0.809 0 0 25.956 -0.124 26.892 -0.268 1955 5 26.611 0.646 0 0 25.678 -0.287 26.902 -0.144 1955 6 26.556 0.869 0 0 25.622 -0.064 26.886 0.118 1955 7 26.222 0.987 0 0 25.289 0.054 26.604 0.288 1955 8 26.000 0.830 0 0 25.067 -0.103 26.496 0.245 1955 9 26.389 1.060 0 0 25.456 0.127 26.618 0.209 1955 10 26.833 1.514 0 0 25.900 0.581 26.525 0.125 1955 11 26.778 1.177 0 0 25.845 0.244 26.639 -0.042 1955 12 26.333 0.613 0 4 26.689 0.968 26.580 -0.221 1956 1 26.389 0.449 0 0 26.744 0.804 26.730 -0.290 1956 2 26.389 0.324 0 0 26.744 0.680 26.730 -0.415 1956 3 26.333 0.170 0 0 26.689 0.526 27.169 -0.074 1956 4 26.923 0.843 1 0 NaN NaN 27.079 -0.081 1956 5 26.000 0.035 0 0 26.355 0.390 26.646 -0.400 1956 6 23.722 -1.964 0 0 24.078 -1.609 26.176 -0.591 1956 7 23.500 -1.735 0 0 23.855 -1.379 25.798 -0.517 1956 8 23.944 -1.226 0 0 24.300 -0.870 26.080 -0.170 1956 9 24.056 -1.273 0 0 24.411 -0.918 26.053 -0.357 1956 10 24.889 -0.430 0 0 25.244 -0.075 26.345 -0.055 1956 11 24.778 -0.823 0 0 25.133 -0.468 26.404 -0.278 1956 12 24.889 -0.832 0 0 25.244 -0.476 26.407 -0.394 1957 1 25.000 -0.940 0 0 25.355 -0.585 26.555 -0.466 1957 2 25.167 -0.898 0 0 25.522 -0.542 26.938 -0.207 1957 3 25.167 -0.996 0 0 25.522 -0.641 26.994 -0.249 1957 4 25.111 -0.969 0 0 25.467 -0.613 27.050 -0.110 1957 5 24.889 -1.077 0 0 25.244 -0.721 27.035 -0.011 1957 6 24.500 -1.187 0 0 24.855 -0.831 26.936 0.169 1957 7 24.000 -1.235 0 0 24.355 -0.879 26.027 -0.289 1957 8 26.278 1.107 0 0 26.633 1.463 26.426 0.176 1957 9 26.389 1.060 0 0 26.744 1.415 26.695 0.286 1957 10 NaN NaN NaN NaN NaN NaN 26.461 0.061 1957 11 NaN NaN NaN NaN NaN NaN 26.933 0.252 1957 12 NaN NaN NaN NaN NaN NaN 27.035 0.234 1958 1 NaN NaN NaN NaN NaN NaN 27.523 0.503 1958 2 NaN NaN NaN NaN NaN NaN 27.456 0.311 1958 3 NaN NaN NaN NaN NaN NaN 27.638 0.394 1958 4 NaN NaN NaN NaN NaN NaN 27.800 0.639 1958 5 NaN NaN NaN NaN NaN NaN 27.299 0.253 1958 6 NaN NaN NaN NaN NaN NaN 26.619 -0.148 1958 7 NaN NaN NaN NaN NaN NaN 26.052 -0.263 1958 8 NaN NaN NaN NaN NaN NaN 26.404 0.153 1958 9 NaN NaN NaN NaN NaN NaN 26.247 -0.163