% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 35199 % Primary Name: BLOOMINGTON 2 S % Record Type: TAVG % Country: United States % State: NE % Latitude: 40.06670 +/- 0.00005 % Longitude: -99.03330 +/- 0.00005 % Elevation (m): 573.00 +/- 0.05 % # of Months: 18 % % IDs: coop - 250953 % ghcnd - USC00250953 % ncdc - 20012936 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: ff4bb43ca685be2516a63202809ecb5d % Raw Data Hash: 5bea72363cddc93917a041e2fc701e43 % Adj Data Hash: c64991890e6311b52f620772c4a53aa5 % % 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 1906 12 NaN NaN NaN NaN NaN NaN 1.858 2.573 1907 1 NaN NaN NaN NaN NaN NaN -4.160 -1.031 1907 2 NaN NaN NaN NaN NaN NaN 1.504 1.399 1907 3 NaN NaN NaN NaN NaN NaN 7.898 3.763 1907 4 NaN NaN NaN NaN NaN NaN 7.681 -3.329 1907 5 NaN NaN NaN NaN NaN NaN 13.200 -3.594 1907 6 NaN NaN NaN NaN NaN NaN 21.436 -1.193 1907 7 NaN NaN NaN NaN NaN NaN 25.222 -0.605 1907 8 NaN NaN NaN NaN NaN NaN 24.672 -0.059 1907 9 NaN NaN NaN NaN NaN NaN 19.446 0.051 1907 10 NaN NaN NaN NaN NaN NaN 13.419 0.584 1907 11 NaN NaN NaN NaN NaN NaN 3.628 -0.825 1907 12 -1.200 -0.555 1 0 NaN NaN -1.039 -0.325 1908 1 0.774 3.834 0 0 0.774 3.834 0.069 3.199 1908 2 -0.062 -0.238 0 0 -0.062 -0.238 0.976 0.871 1908 3 6.756 2.551 0 0 6.756 2.551 5.961 1.826 1908 4 12.367 1.286 0 0 12.367 1.286 12.079 1.070 1908 5 NaN NaN NaN NaN NaN NaN 15.596 -1.198 1908 6 20.257 -2.442 0 0 20.257 -2.442 21.347 -1.282 1908 7 22.435 -3.462 0 0 22.435 -3.462 23.786 -2.042 1908 8 21.697 -3.105 0 0 21.697 -3.105 23.281 -1.450 1908 9 22.174 2.709 0 0 22.174 2.709 20.416 1.021 1908 10 12.542 -0.363 0 0 12.542 -0.363 12.040 -0.794 1908 11 5.332 0.808 0 0 5.332 0.808 4.722 0.268 1908 12 0.937 1.581 0 0 0.937 1.581 0.615 1.330 1909 1 -3.766 -0.706 0 0 -3.766 -0.706 -3.348 -0.218 1909 2 0.451 0.275 1 0 NaN NaN 0.558 0.452 1909 3 3.710 -0.495 0 0 3.710 -0.495 2.857 -1.277 1909 4 9.165 -1.915 0 0 9.165 -1.915 9.526 -1.484 1909 5 16.413 -0.452 0 0 16.413 -0.452 15.482 -1.313 1909 6 21.865 -0.834 0 0 21.865 -0.834 21.659 -0.970 1909 7 NaN NaN NaN NaN NaN NaN 24.960 -0.868 1909 8 NaN NaN NaN NaN NaN NaN 26.025 1.293 1909 9 NaN NaN NaN NaN NaN NaN 18.906 -0.489 1909 10 NaN NaN NaN NaN NaN NaN 12.681 -0.153 1909 11 NaN NaN NaN NaN NaN NaN 6.217 1.764 1909 12 NaN NaN NaN NaN NaN NaN -7.314 -6.600 1910 1 NaN NaN NaN NaN NaN NaN -4.019 -0.889 1910 2 NaN NaN NaN NaN NaN NaN -1.508 -1.613 1910 3 NaN NaN NaN NaN NaN NaN 11.055 6.921 1910 4 NaN NaN NaN NaN NaN NaN 12.995 1.985 1910 5 NaN NaN NaN NaN NaN NaN 14.126 -2.668 1910 6 NaN NaN NaN NaN NaN NaN 21.823 -0.806