% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 25795 % Primary Name: COOT BAY RANGER STN % Record Type: TAVG % Country: United States % State: FL % Latitude: 25.18330 +/- 0.00005 % Longitude: -80.90000 +/- 0.00005 % Elevation (m): 0.96 +/- 10.00 % # of Months: 17 % % Alternate Names: COOT BAY RS % % IDs: coop - 81832 % ghcnd - USC00081832 % ncdc - 20004222 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 3423dae60180cfc0851a348dc1e8b9db % Raw Data Hash: 0ffd95a0dbd97edd4627090199f92bf2 % Adj Data Hash: 36d30d4de9104e11c4128ff253835d0d % % 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 1948 5 NaN NaN NaN NaN NaN NaN 26.175 0.124 1948 6 NaN NaN NaN NaN NaN NaN 27.852 0.270 1948 7 NaN NaN NaN NaN NaN NaN 28.149 -0.288 1948 8 NaN NaN NaN NaN NaN NaN 28.560 -0.119 1948 9 NaN NaN NaN NaN NaN NaN 28.339 0.100 1948 10 NaN NaN NaN NaN NaN NaN 26.212 0.052 1948 11 NaN NaN NaN NaN NaN NaN 26.356 2.741 1948 12 NaN NaN NaN NaN NaN NaN 23.751 2.681 1949 1 NaN NaN NaN NaN NaN NaN 22.261 1.936 1949 2 NaN NaN NaN NaN NaN NaN 23.242 2.843 1949 3 NaN NaN NaN NaN NaN NaN 22.581 0.192 1949 4 NaN NaN NaN NaN NaN NaN 24.825 0.796 1949 5 25.278 0.420 0 0 25.278 0.420 26.031 -0.020 1949 6 26.833 0.445 0 0 26.833 0.445 27.398 -0.183 1949 7 27.500 0.257 0 0 27.500 0.257 28.127 -0.309 1949 8 27.611 0.125 0 0 27.611 0.125 28.407 -0.272 1949 9 27.444 0.399 0 0 27.444 0.399 28.724 0.485 1949 10 25.778 0.811 0 0 25.778 0.811 27.032 0.872 1949 11 20.444 -1.977 0 0 20.444 -1.977 22.019 -1.596 1949 12 21.111 1.234 0 0 21.111 1.234 22.392 1.322 1950 1 21.000 1.868 0 0 21.000 1.868 22.982 2.657 1950 2 20.556 1.349 0 0 20.556 1.349 21.085 0.686 1950 3 21.556 0.360 0 0 21.556 0.360 22.850 0.461 1950 4 19.960 -2.876 1 0 NaN NaN 21.954 -2.075 1950 5 24.052 -0.805 1 0 NaN NaN 26.272 0.221 1950 6 26.556 0.167 0 0 26.556 0.167 27.958 0.377 1950 7 26.167 -1.076 0 0 26.167 -1.076 27.764 -0.673 1950 8 26.984 -0.502 1 0 NaN NaN 28.344 -0.336 1950 9 NaN NaN NaN NaN NaN NaN 28.118 -0.121 1950 10 NaN NaN NaN NaN NaN NaN 26.891 0.730 1950 11 NaN NaN NaN NaN NaN NaN 22.434 -1.181 1950 12 17.556 -2.321 0 0 17.556 -2.321 19.326 -1.744 1951 1 NaN NaN NaN NaN NaN NaN 19.137 -1.188 1951 2 NaN NaN NaN NaN NaN NaN 18.606 -1.794 1951 3 NaN NaN NaN NaN NaN NaN 22.041 -0.347 1951 4 NaN NaN NaN NaN NaN NaN 23.344 -0.685 1951 5 NaN NaN NaN NaN NaN NaN 25.467 -0.584 1951 6 NaN NaN NaN NaN NaN NaN 27.774 0.193 1951 7 NaN NaN NaN NaN NaN NaN 28.177 -0.259 1951 8 NaN NaN NaN NaN NaN NaN 29.178 0.499 1951 9 NaN NaN NaN NaN NaN NaN 29.203 0.964 1951 10 NaN NaN NaN NaN NaN NaN 26.560 0.400 1951 11 NaN NaN NaN NaN NaN NaN 23.017 -0.598 1951 12 NaN NaN NaN NaN NaN NaN 22.962 1.892