% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 26490 % Primary Name: WEIMAR % Record Type: TAVG % Country: United States % State: TX % Latitude: 29.70000 +/- 0.00005 % Longitude: -96.78330 +/- 0.00005 % Elevation (m): 115.88 +/- 19.39 % # of Months: 14 % % IDs: coop - 419549 % ghcnd - USC00419549 % ncdc - 20024480 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 8eca8ee3b986c060289de33559395048 % Raw Data Hash: 5994981d3a2dc983a793f3df336b761a % Adj Data Hash: 148c952357bdacd3becfa05db89cab54 % % 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 1901 2 NaN NaN NaN NaN NaN NaN 10.791 -1.856 1901 3 NaN NaN NaN NaN NaN NaN 16.115 -0.383 1901 4 NaN NaN NaN NaN NaN NaN 18.645 -1.977 1901 5 NaN NaN NaN NaN NaN NaN 23.330 -0.854 1901 6 NaN NaN NaN NaN NaN NaN 27.765 0.501 1901 7 NaN NaN NaN NaN NaN NaN 28.574 -0.055 1901 8 NaN NaN NaN NaN NaN NaN 28.986 0.501 1901 9 NaN NaN NaN NaN NaN NaN 25.281 -0.850 1901 10 NaN NaN NaN NaN NaN NaN 20.924 -0.315 1901 11 NaN NaN NaN NaN NaN NaN 16.162 0.156 1901 12 NaN NaN NaN NaN NaN NaN 10.869 -1.442 1902 1 NaN NaN NaN NaN NaN NaN 9.530 -1.349 1902 2 12.614 -1.174 0 0 12.614 -1.174 10.395 -2.252 1902 3 19.100 1.460 0 0 19.100 1.460 17.070 0.571 1902 4 22.928 1.164 1 0 NaN NaN 21.202 0.580 1902 5 26.465 1.138 0 0 26.465 1.138 25.095 0.910 1902 6 29.208 0.802 0 0 29.208 0.802 27.733 0.468 1902 7 29.463 -0.308 0 0 29.463 -0.308 27.758 -0.871 1902 8 31.368 1.741 0 0 31.368 1.741 29.085 0.600 1902 9 26.465 -0.808 0 0 26.465 -0.808 25.622 -0.509 1902 10 21.732 -0.648 0 0 21.732 -0.648 21.086 -0.152 1902 11 18.387 1.239 0 0 18.387 1.239 18.289 2.283 1902 12 NaN NaN NaN NaN NaN NaN 12.506 0.195 1903 1 11.444 -0.577 0 0 11.444 -0.577 10.446 -0.432 1903 2 NaN NaN NaN NaN NaN NaN 10.720 -1.927 1903 3 NaN NaN NaN NaN NaN NaN 16.164 -0.334 1903 4 NaN NaN NaN NaN NaN NaN 19.681 -0.942 1903 5 NaN NaN NaN NaN NaN NaN 22.517 -1.668 1903 6 NaN NaN NaN NaN NaN NaN 24.865 -2.400 1903 7 27.543 -2.228 0 0 27.543 -2.228 27.301 -1.328 1903 8 27.847 -1.780 0 0 27.847 -1.780 27.599 -0.886 1903 9 25.527 -1.746 0 0 25.527 -1.746 24.840 -1.291 1903 10 NaN NaN NaN NaN NaN NaN 19.598 -1.640 1903 11 NaN NaN NaN NaN NaN NaN 15.049 -0.957 1903 12 NaN NaN NaN NaN NaN NaN 11.608 -0.703 1904 1 NaN NaN NaN NaN NaN NaN 9.460 -1.418 1904 2 NaN NaN NaN NaN NaN NaN 14.434 1.787 1904 3 NaN NaN NaN NaN NaN NaN 18.666 2.168 1904 4 NaN NaN NaN NaN NaN NaN 20.031 -0.592 1904 5 NaN NaN NaN NaN NaN NaN 22.802 -1.383 1904 6 NaN NaN NaN NaN NaN NaN 26.573 -0.692 1904 7 NaN NaN NaN NaN NaN NaN 26.857 -1.772 1904 8 NaN NaN NaN NaN NaN NaN 27.011 -1.474 1904 9 NaN NaN NaN NaN NaN NaN 26.570 0.439