% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 28641 % Primary Name: LUBBOCK 2 % Record Type: TAVG % Country: United States % State: TX % Latitude: 33.58330 +/- 0.00005 % Longitude: -101.88330 +/- 0.00005 % Elevation (m): 982.10 +/- 0.05 % # of Months: 9 % % IDs: coop - 415412 % ghcnd - USC00415412 % ncdc - 20025664 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 468b4a9437b8ddbe5a6f1212d8b5f2fd % Raw Data Hash: 0d2d990d39a37ee49695f642fef35f05 % Adj Data Hash: 6f2b39db9eff964db51ab58f2fbfc646 % % 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 1937 8 NaN NaN NaN NaN NaN NaN 26.955 1.286 1937 9 NaN NaN NaN NaN NaN NaN 22.729 0.635 1937 10 NaN NaN NaN NaN NaN NaN 17.040 0.619 1937 11 NaN NaN NaN NaN NaN NaN 9.109 -0.653 1937 12 NaN NaN NaN NaN NaN NaN 6.001 0.023 1938 1 NaN NaN NaN NaN NaN NaN 6.113 1.351 1938 2 NaN NaN NaN NaN NaN NaN 9.028 2.019 1938 3 NaN NaN NaN NaN NaN NaN 12.969 2.072 1938 4 NaN NaN NaN NaN NaN NaN 15.813 -0.300 1938 5 NaN NaN NaN NaN NaN NaN 20.958 0.134 1938 6 NaN NaN NaN NaN NaN NaN 25.283 -0.065 1938 7 NaN NaN NaN NaN NaN NaN 25.432 -1.071 1938 8 25.729 1.364 0 0 25.729 1.364 26.051 0.382 1938 9 NaN NaN NaN NaN NaN NaN 22.763 0.668 1938 10 17.092 1.975 0 0 17.092 1.975 18.091 1.671 1938 11 6.932 -1.527 0 0 6.932 -1.527 8.645 -1.117 1938 12 3.756 -0.919 0 0 3.756 -0.919 6.426 0.447 1939 1 4.390 0.932 0 0 4.390 0.932 6.155 1.394 1939 2 2.374 -3.331 1 0 NaN NaN 4.275 -2.733 1939 3 11.450 1.857 0 0 11.450 1.857 12.119 1.223 1939 4 14.805 -0.004 0 0 14.805 -0.004 16.450 0.337 1939 5 20.602 1.081 0 0 20.602 1.081 21.246 0.422 1939 6 NaN NaN NaN NaN NaN NaN 26.715 1.366 1939 7 NaN NaN NaN NaN NaN NaN 26.303 -0.200 1939 8 NaN NaN NaN NaN NaN NaN 24.969 -0.700 1939 9 NaN NaN NaN NaN NaN NaN 23.424 1.330 1939 10 NaN NaN NaN NaN NaN NaN 17.316 0.895 1939 11 NaN NaN NaN NaN NaN NaN 8.533 -1.229 1939 12 NaN NaN NaN NaN NaN NaN 7.816 1.837 1940 1 NaN NaN NaN NaN NaN NaN 1.440 -3.322 1940 2 NaN NaN NaN NaN NaN NaN 6.673 -0.336 1940 3 NaN NaN NaN NaN NaN NaN 11.998 1.102 1940 4 NaN NaN NaN NaN NaN NaN 16.173 0.061 1940 5 NaN NaN NaN NaN NaN NaN 20.562 -0.262