% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 19323 % Primary Name: AIMELIK BABELTHUAP % Record Type: TAVG % Country: Palau % State: PI % Latitude: 7.45000 +/- 0.00833 % Longitude: 134.51667 +/- 0.00833 % Elevation (m): 60.00 +/- 0.05 % # of Months: 13 % % IDs: coop - 914015 % % Sources: US Cooperative Summary of the Day % US Cooperative Summary of the Month % % Site Hash: c1d7f41fe0c536052af0b281d7630bdc % Raw Data Hash: a8bc4c1ecbbcc6bd5d53912a20834768 % Adj Data Hash: b6a8dcc7e3d03865b62179fefd84f957 % % 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 1953 7 NaN NaN NaN NaN NaN NaN 27.607 0.178 1953 8 NaN NaN NaN NaN NaN NaN 27.686 0.213 1953 9 NaN NaN NaN NaN NaN NaN 27.500 -0.107 1953 10 NaN NaN NaN NaN NaN NaN 27.921 0.428 1953 11 NaN NaN NaN NaN NaN NaN 27.736 0.110 1953 12 NaN NaN NaN NaN NaN NaN 27.325 0.117 1954 1 NaN NaN NaN NaN NaN NaN 27.165 0.282 1954 2 NaN NaN NaN NaN NaN NaN 27.469 0.497 1954 3 NaN NaN NaN NaN NaN NaN 27.548 0.304 1954 4 NaN NaN NaN NaN NaN NaN 27.687 0.181 1954 5 NaN NaN NaN NaN NaN NaN 27.515 -0.322 1954 6 NaN NaN NaN NaN NaN NaN 27.340 -0.288 1954 7 25.778 -0.623 0 0 25.778 -0.623 26.921 -0.508 1954 8 26.278 -0.167 0 0 26.278 -0.167 27.278 -0.195 1954 9 25.980 -0.599 1 0 NaN NaN 27.572 -0.035 1954 10 26.389 -0.076 1 0 NaN NaN 27.169 -0.325 1954 11 23.889 -2.709 0 0 23.889 -2.709 27.104 -0.523 1954 12 NaN NaN NaN NaN NaN NaN 26.795 -0.414 1955 1 25.222 -0.633 0 0 25.222 -0.633 26.165 -0.718 1955 2 26.444 0.500 0 0 26.444 0.500 26.992 0.020 1955 3 26.500 0.284 0 0 26.500 0.284 27.125 -0.119 1955 4 26.944 0.467 0 0 26.944 0.467 27.468 -0.038 1955 5 26.944 0.136 0 0 26.944 0.136 27.505 -0.332 1955 6 26.444 -0.155 0 0 26.444 -0.155 27.136 -0.492 1955 7 25.889 -0.512 0 0 25.889 -0.512 26.980 -0.449 1955 8 26.222 -0.222 0 0 26.222 -0.222 27.192 -0.280 1955 9 NaN NaN NaN NaN NaN NaN 27.542 -0.065 1955 10 NaN NaN NaN NaN NaN NaN 27.365 -0.128 1955 11 NaN NaN NaN NaN NaN NaN 27.548 -0.078 1955 12 NaN NaN NaN NaN NaN NaN 27.305 0.096 1956 1 NaN NaN NaN NaN NaN NaN 26.465 -0.418 1956 2 NaN NaN NaN NaN NaN NaN 27.237 0.265 1956 3 NaN NaN NaN NaN NaN NaN 27.173 -0.071 1956 4 NaN NaN NaN NaN NaN NaN 27.096 -0.410 1956 5 NaN NaN NaN NaN NaN NaN 27.351 -0.486 1956 6 NaN NaN NaN NaN NaN NaN 27.499 -0.129 1956 7 NaN NaN NaN NaN NaN NaN 27.186 -0.243 1956 8 NaN NaN NaN NaN NaN NaN 26.967 -0.506