% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 26352 % Primary Name: MORRISTON % Record Type: TAVG % Country: United States % State: FL % Latitude: 29.28330 +/- 0.00005 % Longitude: -82.45000 +/- 0.00005 % Elevation (m): 24.38 +/- 0.15 % # of Months: 22 % % Alternate Names: Missing Station ID - 85935 % % IDs: coop - 85935 % ghcnd - USC00085935 % ncdc - 12001360 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: c2e259f33f6189aef1cffb5386fd1231 % Raw Data Hash: 24025df651bef82e446e3e31105a51d1 % Adj Data Hash: 6cca5e0bfffc568554a038a0a4eb4963 % % 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 1939 3 NaN NaN NaN NaN NaN NaN 18.426 1.672 1939 4 NaN NaN NaN NaN NaN NaN 20.074 -0.040 1939 5 NaN NaN NaN NaN NaN NaN 23.182 -0.541 1939 6 NaN NaN NaN NaN NaN NaN 27.070 0.703 1939 7 NaN NaN NaN NaN NaN NaN 27.282 -0.027 1939 8 NaN NaN NaN NaN NaN NaN 26.461 -0.814 1939 9 NaN NaN NaN NaN NaN NaN 27.060 1.094 1939 10 NaN NaN NaN NaN NaN NaN 22.046 1.056 1939 11 NaN NaN NaN NaN NaN NaN 14.999 -1.271 1939 12 NaN NaN NaN NaN NaN NaN 12.851 0.084 1940 1 NaN NaN NaN NaN NaN NaN 6.336 -5.731 1940 2 NaN NaN NaN NaN NaN NaN 10.659 -2.511 1940 3 17.087 -0.663 0 0 17.087 -0.663 15.880 -0.873 1940 4 19.602 -1.509 0 0 19.602 -1.509 18.756 -1.358 1940 5 22.250 -2.470 0 0 22.250 -2.470 21.986 -1.737 1940 6 27.020 -0.344 1 0 NaN NaN 26.527 0.160 1940 7 NaN NaN NaN NaN NaN NaN 27.030 -0.279 1940 8 27.540 -0.732 0 0 27.540 -0.732 27.354 0.078 1940 9 24.510 -2.453 0 0 24.510 -2.453 24.715 -1.251 1940 10 20.562 -1.425 1 0 NaN NaN 20.056 -0.934 1940 11 17.457 0.190 0 0 17.457 0.190 16.506 0.237 1940 12 17.515 3.751 0 0 17.515 3.751 15.153 2.387 1941 1 13.137 0.073 0 0 13.137 0.073 11.575 -0.491 1941 2 NaN NaN NaN NaN NaN NaN 9.837 -3.333 1941 3 15.456 -2.294 0 0 15.456 -2.294 13.943 -2.810 1941 4 21.500 0.389 0 0 21.500 0.389 20.468 0.354 1941 5 23.353 -1.367 0 0 23.353 -1.367 23.138 -0.585 1941 6 26.981 -0.383 1 0 NaN NaN 26.499 0.132 1941 7 27.615 -0.691 0 0 27.615 -0.691 26.979 -0.329 1941 8 28.423 0.150 0 0 28.423 0.150 28.070 0.794 1941 9 26.802 -0.161 0 0 26.802 -0.161 26.783 0.817 1941 10 25.019 3.032 0 0 25.019 3.032 24.092 3.101 1941 11 18.178 0.912 0 0 18.178 0.912 16.803 0.534 1941 12 16.955 3.191 0 0 16.955 3.191 14.345 1.578 1942 1 13.042 -0.022 0 0 13.042 -0.022 10.951 -1.115 1942 2 13.170 -0.996 1 0 NaN NaN 9.742 -3.428 1942 3 NaN NaN NaN NaN NaN NaN 15.610 -1.143 1942 4 NaN NaN NaN NaN NaN NaN 19.552 -0.562 1942 5 NaN NaN NaN NaN NaN NaN 23.371 -0.352 1942 6 NaN NaN NaN NaN NaN NaN 26.556 0.189 1942 7 NaN NaN NaN NaN NaN NaN 28.085 0.777 1942 8 NaN NaN NaN NaN NaN NaN 27.109 -0.167 1942 9 NaN NaN NaN NaN NaN NaN 26.292 0.326 1942 10 NaN NaN NaN NaN NaN NaN 20.962 -0.029 1942 11 NaN NaN NaN NaN NaN NaN 17.306 1.036 1942 12 NaN NaN NaN NaN NaN NaN 14.111 1.344 1943 1 NaN NaN NaN NaN NaN NaN 13.209 1.143 1943 2 NaN NaN NaN NaN NaN NaN 11.985 -1.185