% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 173208 % Primary Name: CHARLOTTE AMALIE EST % Record Type: TAVG % Country: Virgin Islands [United States] % State: VI % Latitude: 18.33330 +/- 0.00005 % Longitude: -64.90000 +/- 0.00005 % Elevation (m): 60.00 +/- 0.05 % # of Months: 16 % % Alternate Names: Missing Station ID - 671620 % % IDs: coop - 671620 % ghcnd - VQC00671620 % ncdc - 20024061 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: b14b45732c9668901fb4e7f6d50cf4ca % Raw Data Hash: 0c0ba127c9f7912eeab18a339d67e6e7 % Adj Data Hash: a98210efd44e64e41c931ae92d8f1ab1 % % 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 1947 7 NaN NaN NaN NaN NaN NaN 27.983 0.031 1947 8 NaN NaN NaN NaN NaN NaN 28.148 0.048 1947 9 NaN NaN NaN NaN NaN NaN 27.531 -0.352 1947 10 NaN NaN NaN NaN NaN NaN 27.512 0.137 1947 11 NaN NaN NaN NaN NaN NaN 26.604 -0.003 1947 12 NaN NaN NaN NaN NaN NaN 25.442 0.091 1948 1 NaN NaN NaN NaN NaN NaN 25.082 0.338 1948 2 NaN NaN NaN NaN NaN NaN 25.070 0.214 1948 3 NaN NaN NaN NaN NaN NaN 25.133 -0.144 1948 4 NaN NaN NaN NaN NaN NaN 25.556 -0.274 1948 5 NaN NaN NaN NaN NaN NaN 27.346 0.472 1948 6 NaN NaN NaN NaN NaN NaN 28.121 0.401 1948 7 28.531 -0.273 0 0 28.531 -0.273 28.058 0.106 1948 8 29.385 0.434 0 0 29.385 0.434 28.351 0.251 1948 9 28.733 -0.001 0 0 28.733 -0.001 27.758 -0.125 1948 10 28.298 0.073 0 0 28.298 0.073 27.177 -0.197 1948 11 27.362 -0.098 0 0 27.362 -0.098 26.730 0.122 1948 12 26.492 0.289 0 0 26.492 0.289 25.416 0.065 1949 1 24.845 -0.751 0 0 24.845 -0.751 24.134 -0.611 1949 2 NaN NaN NaN NaN NaN NaN 24.454 -0.402 1949 3 25.492 -0.636 1 0 NaN NaN 25.028 -0.248 1949 4 26.572 -0.109 0 0 26.572 -0.109 25.783 -0.046 1949 5 26.965 -0.761 0 0 26.965 -0.761 26.695 -0.179 1949 6 27.953 -0.619 0 0 27.953 -0.619 27.356 -0.364 1949 7 NaN NaN NaN NaN NaN NaN 27.350 -0.602 1949 8 29.250 0.299 0 0 29.250 0.299 28.203 0.103 1949 9 28.183 -0.551 0 0 28.183 -0.551 27.478 -0.406 1949 10 28.598 0.372 1 0 NaN NaN 27.039 -0.335 1949 11 27.462 0.002 0 0 27.462 0.002 26.329 -0.279 1949 12 26.044 -0.159 0 0 26.044 -0.159 24.685 -0.666 1950 1 NaN NaN NaN NaN NaN NaN 23.625 -1.119 1950 2 NaN NaN NaN NaN NaN NaN 24.134 -0.722 1950 3 NaN NaN NaN NaN NaN NaN 24.699 -0.578 1950 4 NaN NaN NaN NaN NaN NaN 24.915 -0.915 1950 5 NaN NaN NaN NaN NaN NaN 26.109 -0.765 1950 6 NaN NaN NaN NaN NaN NaN 27.320 -0.400 1950 7 NaN NaN NaN NaN NaN NaN 27.639 -0.313 1950 8 NaN NaN NaN NaN NaN NaN 27.859 -0.241 1950 9 NaN NaN NaN NaN NaN NaN 27.659 -0.224 1950 10 NaN NaN NaN NaN NaN NaN 27.169 -0.205 1950 11 NaN NaN NaN NaN NaN NaN 26.336 -0.272 1950 12 NaN NaN NaN NaN NaN NaN 25.147 -0.204