% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 26210 % Primary Name: COLLEGEPORT % Record Type: TAVG % Country: United States % State: TX % Latitude: 28.71670 +/- 0.00005 % Longitude: -96.18330 +/- 0.00005 % Elevation (m): 4.27 +/- 0.15 % # of Months: 23 % % Alternate Names: Missing Station ID - 411885 % % IDs: coop - 411885 % ghcnd - USC00411885 % ncdc - 12005109 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 7ca6e3f5948c9c85be1b358283838181 % Raw Data Hash: eec037baaa01feb9a580b42f42581f0c % Adj Data Hash: cb706f278dabb951596d7e2c837d5197 % % 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 1911 1 NaN NaN NaN NaN NaN NaN 19.040 3.572 1911 2 NaN NaN NaN NaN NaN NaN 19.176 3.255 1911 3 NaN NaN NaN NaN NaN NaN 20.127 2.005 1911 4 NaN NaN NaN NaN NaN NaN 21.791 0.719 1911 5 NaN NaN NaN NaN NaN NaN 22.879 -1.204 1911 6 NaN NaN NaN NaN NaN NaN 27.536 0.685 1911 7 NaN NaN NaN NaN NaN NaN 26.929 -1.066 1911 8 NaN NaN NaN NaN NaN NaN 28.379 0.214 1911 9 NaN NaN NaN NaN NaN NaN 28.974 1.841 1911 10 NaN NaN NaN NaN NaN NaN 24.069 0.121 1911 11 NaN NaN NaN NaN NaN NaN 18.432 -1.809 1911 12 NaN NaN NaN NaN NaN NaN 16.301 -0.948 1912 1 14.158 1.425 1 0 NaN NaN 13.672 -1.797 1912 2 10.879 -2.307 0 0 10.879 -2.307 13.635 -2.287 1912 3 14.302 -1.085 0 0 14.302 -1.085 16.256 -1.867 1912 4 20.140 1.804 0 0 20.140 1.804 21.070 -0.002 1912 5 23.542 2.194 0 0 23.542 2.194 23.922 -0.161 1912 6 25.078 0.963 0 0 25.078 0.963 25.284 -1.567 1912 7 NaN NaN NaN NaN NaN NaN 27.670 -0.325 1912 8 28.592 3.162 1 0 NaN NaN 28.339 0.175 1912 9 25.361 0.964 1 0 NaN NaN 28.058 0.925 1912 10 20.052 -1.161 0 0 20.052 -1.161 24.232 0.284 1912 11 14.782 -2.724 0 0 14.782 -2.724 18.860 -1.381 1912 12 10.744 -3.770 0 0 10.744 -3.770 16.173 -1.076 1913 1 10.834 -1.899 1 0 NaN NaN 15.790 0.321 1913 2 11.932 -1.254 1 0 NaN NaN 14.657 -1.264 1913 3 13.815 -1.572 0 0 13.815 -1.572 16.718 -1.405 1913 4 17.264 -1.072 0 0 17.264 -1.072 19.453 -1.618 1913 5 NaN NaN NaN NaN NaN NaN 22.802 -1.281 1913 6 23.422 -0.694 1 0 NaN NaN 25.730 -1.121 1913 7 27.995 2.736 1 0 NaN NaN 27.643 -0.352 1913 8 NaN NaN NaN NaN NaN NaN 27.929 -0.235 1913 9 NaN NaN NaN NaN NaN NaN 25.760 -1.373 1913 10 NaN NaN NaN NaN NaN NaN 22.483 -1.465 1913 11 NaN NaN NaN NaN NaN NaN 22.610 2.369 1913 12 11.000 -3.514 0 0 11.000 -3.514 16.864 -0.385 1914 1 12.232 -0.501 1 0 NaN NaN 16.789 1.321 1914 2 11.052 -2.134 1 0 NaN NaN 14.143 -1.779 1914 3 NaN NaN NaN NaN NaN NaN 15.527 -2.596 1914 4 17.940 -0.396 0 0 17.940 -0.396 19.896 -1.176 1914 5 18.881 -2.466 1 0 NaN NaN 23.455 -0.628 1914 6 27.363 3.247 1 0 NaN NaN 27.478 0.627 1914 7 NaN NaN NaN NaN NaN NaN 28.283 0.289 1914 8 NaN NaN NaN NaN NaN NaN 27.679 -0.486 1914 9 NaN NaN NaN NaN NaN NaN 26.846 -0.287 1914 10 NaN NaN NaN NaN NaN NaN 23.680 -0.268 1914 11 NaN NaN NaN NaN NaN NaN 20.091 -0.150 1914 12 NaN NaN NaN NaN NaN NaN 14.055 -3.194 1915 1 NaN NaN NaN NaN NaN NaN 14.302 -1.167 1915 2 NaN NaN NaN NaN NaN NaN 16.349 0.427 1915 3 NaN NaN NaN NaN NaN NaN 13.851 -4.272 1915 4 NaN NaN NaN NaN NaN NaN 19.847 -1.225 1915 5 NaN NaN NaN NaN NaN NaN 23.767 -0.316 1915 6 NaN NaN NaN NaN NaN NaN 27.815 0.963