% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 168937 % Primary Name: SANTA ISABEL AIRPORT % Record Type: TAVG % Country: Puerto Rico [United States] % State: PR % Latitude: 17.96670 +/- 0.00005 % Longitude: -66.40000 +/- 0.00005 % Elevation (m): 9.10 +/- 0.05 % # of Months: 44 % % Alternate Names: PONCE SANTA ISABEL % SANTA ISABEL % SANTA ISABEL AP % % IDs: coop - 668933 % ghcnd - RQW00011637 % gsod - 999999-11637 % ncdc - 20023847 % ncdc - 20023848 % ncdc - 20023849 % wban - 11637 % % Sources: US First Order Summary of the Day % Global Historical Climatology Network - Daily % Global Summary of the Day % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: fd6c4cfe255080ad1db49697493de0e9 % Raw Data Hash: bbcb14a9a676d0c973fe476f664c640d % Adj Data Hash: 9208fcee99984907eb7c3a0685d82426 % % 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 1949 6 NaN NaN NaN NaN NaN NaN 26.540 -0.285 1949 7 NaN NaN NaN NaN NaN NaN 26.319 -0.689 1949 8 NaN NaN NaN NaN NaN NaN 27.002 -0.099 1949 9 NaN NaN NaN NaN NaN NaN 26.547 -0.387 1949 10 NaN NaN NaN NaN NaN NaN 26.063 -0.352 1949 11 NaN NaN NaN NaN NaN NaN 25.269 -0.313 1949 12 NaN NaN NaN NaN NaN NaN 23.637 -0.589 1950 1 NaN NaN NaN NaN NaN NaN 22.514 -1.025 1950 2 NaN NaN NaN NaN NaN NaN 22.840 -0.764 1950 3 NaN NaN NaN NaN NaN NaN 23.438 -0.673 1950 4 NaN NaN NaN NaN NaN NaN 23.747 -1.031 1950 5 NaN NaN NaN NaN NaN NaN 25.087 -0.889 1950 6 26.000 -0.637 0 0 26.000 -0.637 26.376 -0.449 1950 7 NaN NaN NaN NaN NaN NaN 26.507 -0.501 1950 8 NaN NaN NaN NaN NaN NaN 26.826 -0.275 1950 9 26.444 -0.302 0 0 26.444 -0.302 26.712 -0.223 1950 10 NaN NaN NaN NaN NaN NaN 26.184 -0.232 1950 11 25.222 -0.172 0 0 25.222 -0.172 25.270 -0.312 1950 12 23.611 -0.427 0 0 23.611 -0.427 23.988 -0.238 1951 1 22.889 -0.463 0 0 22.889 -0.463 23.011 -0.528 1951 2 22.389 -1.028 0 0 22.389 -1.028 22.508 -1.096 1951 3 22.444 -1.478 0 0 22.444 -1.478 22.918 -1.193 1951 4 24.889 0.298 0 0 24.889 0.298 25.168 0.389 1951 5 26.358 0.569 0 0 26.358 0.569 26.505 0.529 1951 6 26.667 0.029 0 0 26.667 0.029 26.927 0.102 1951 7 26.833 0.013 0 0 26.833 0.013 26.875 -0.133 1951 8 27.056 0.142 0 0 27.056 0.142 27.503 0.402 1951 9 26.889 0.142 0 0 26.889 0.142 26.990 0.056 1951 10 26.505 0.277 0 0 26.505 0.277 26.653 0.238 1951 11 25.740 0.346 0 0 25.740 0.346 26.118 0.536 1951 12 24.623 0.584 0 0 24.623 0.584 24.550 0.324 1952 1 23.623 0.271 0 0 23.623 0.271 23.331 -0.208 1952 2 23.443 0.026 1 0 NaN NaN 23.796 0.192 1952 3 24.278 0.355 0 0 24.278 0.355 24.507 0.396 1952 4 25.372 0.781 0 0 25.372 0.781 25.399 0.621 1952 5 26.494 0.705 0 0 26.494 0.705 26.628 0.652 1952 6 27.000 0.363 0 0 27.000 0.363 27.326 0.501 1952 7 26.722 -0.098 0 0 26.722 -0.098 26.651 -0.357 1952 8 26.944 0.031 0 0 26.944 0.031 27.269 0.168 1952 9 26.647 -0.100 0 0 26.647 -0.100 26.743 -0.191 1952 10 26.573 0.346 0 0 26.573 0.346 26.784 0.368 1952 11 25.333 -0.061 0 0 25.333 -0.061 25.610 0.028 1952 12 23.833 -0.205 0 0 23.833 -0.205 23.659 -0.567 1953 1 23.444 0.093 0 0 23.444 0.093 23.422 -0.117 1953 2 23.222 -0.195 0 0 23.222 -0.195 23.743 0.139 1953 3 23.389 -0.534 0 0 23.389 -0.534 24.223 0.112 1953 4 24.556 -0.035 0 0 24.556 -0.035 25.273 0.495 1953 5 25.722 -0.067 0 0 25.722 -0.067 26.359 0.383 1953 6 26.500 -0.137 0 0 26.500 -0.137 26.991 0.166 1953 7 27.000 0.179 0 0 27.000 0.179 27.161 0.153 1953 8 26.833 -0.080 0 0 26.833 -0.080 27.311 0.210 1953 9 26.889 0.142 0 0 26.889 0.142 27.164 0.230 1953 10 26.278 0.050 0 0 26.278 0.050 26.491 0.076 1953 11 25.944 0.550 0 0 25.944 0.550 25.903 0.321 1953 12 25.111 1.073 0 0 25.111 1.073 24.492 0.266 1954 1 23.722 0.371 0 0 23.722 0.371 23.427 -0.112 1954 2 23.833 0.416 0 0 23.833 0.416 23.612 0.008 1954 3 24.222 0.299 0 0 24.222 0.299 24.367 0.256 1954 4 23.760 -0.831 1 0 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 NaN NaN NaN NaN NaN NaN 23.060 -0.479 1955 2 NaN NaN NaN NaN NaN NaN 23.466 -0.138 1955 3 NaN NaN NaN NaN NaN NaN 23.324 -0.787 1955 4 NaN NaN NaN NaN NaN NaN 24.163 -0.615