% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 157687 % Primary Name: SAN JUAN ISLE GRANDE % Record Type: TAVG % Country: Puerto Rico [United States] % State: PR % Latitude: 18.45000 +/- 0.00500 % Longitude: -66.10000 +/- 0.00500 % Elevation (m): 18.90 +/- 0.05 % # of Months: 11 % % Alternate Names: SAN JUAN WB AP % % IDs: coop - 668811 % ghcnd - RQC00668811 % ncdc - 20023994 % wban - 11636 % % Sources: US First Order Summary of the Day % US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 0a476b359586b9bd2181f36d92e30182 % Raw Data Hash: 323a14246672eef4af1af7ce0fbd129b % Adj Data Hash: 4ee68620cecb9651383fc30e73f2c026 % % 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 1 NaN NaN NaN NaN NaN NaN 23.427 -0.112 1954 2 NaN NaN NaN NaN NaN NaN 23.612 0.008 1954 3 NaN NaN NaN NaN NaN NaN 24.367 0.256 1954 4 NaN NaN NaN NaN NaN NaN 24.598 -0.180 1954 5 NaN NaN NaN NaN NaN NaN 26.313 0.336 1954 6 NaN NaN NaN NaN NaN NaN 26.757 -0.068 1954 7 NaN NaN NaN NaN NaN NaN 27.008 -0.000 1954 8 NaN NaN NaN NaN NaN NaN 27.176 0.075 1954 9 NaN NaN NaN NaN NaN NaN 26.397 -0.537 1954 10 NaN NaN NaN NaN NaN NaN 25.652 -0.763 1954 11 NaN NaN NaN NaN NaN NaN 25.191 -0.390 1954 12 NaN NaN NaN NaN NaN NaN 23.754 -0.472 1955 1 24.227 0.350 0 0 24.227 0.350 23.060 -0.479 1955 2 24.000 0.058 1 0 NaN NaN 23.466 -0.138 1955 3 23.802 -0.647 0 0 23.802 -0.647 23.324 -0.787 1955 4 24.718 -0.398 0 0 24.718 -0.398 24.163 -0.615 1955 5 26.321 0.006 0 0 26.321 0.006 26.085 0.109 1955 6 26.685 -0.478 0 0 26.685 -0.478 26.741 -0.084 1955 7 26.842 -0.504 0 0 26.842 -0.504 26.810 -0.198 1955 8 27.335 -0.104 0 0 27.335 -0.104 27.213 0.112 1955 9 NaN NaN NaN NaN NaN NaN 26.820 -0.114 1955 10 26.752 -0.002 0 0 26.752 -0.002 26.406 -0.010 1955 11 26.085 0.165 0 0 26.085 0.165 25.666 0.084 1955 12 24.219 -0.345 0 0 24.219 -0.345 24.139 -0.087 1956 1 NaN NaN NaN NaN NaN NaN 23.101 -0.438 1956 2 NaN NaN NaN NaN NaN NaN 23.200 -0.404 1956 3 NaN NaN NaN NaN NaN NaN 24.273 0.163 1956 4 NaN NaN NaN NaN NaN NaN 24.856 0.078 1956 5 NaN NaN NaN NaN NaN NaN 25.795 -0.182 1956 6 NaN NaN NaN NaN NaN NaN 26.234 -0.591 1956 7 NaN NaN NaN NaN NaN NaN 26.647 -0.361 1956 8 NaN NaN NaN NaN NaN NaN 26.840 -0.261 1956 9 NaN NaN NaN NaN NaN NaN 26.721 -0.213 1956 10 NaN NaN NaN NaN NaN NaN 26.242 -0.174 1956 11 NaN NaN NaN NaN NaN NaN 25.232 -0.350 1956 12 NaN NaN NaN NaN NaN NaN 23.885 -0.341