% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 35495 % Primary Name: HOLBROOK % Record Type: TAVG % Country: United States % State: NE % Latitude: 40.30470 +/- 0.00005 % Longitude: -100.01000 +/- 0.00005 % Elevation (m): 673.91 +/- 0.15 % # of Months: 12 % % Alternate Names: Missing Station ID - 253900 % % IDs: coop - 253900 % ghcnd - USC00253900 % ncdc - 12003276 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 5e27508af52ce0c96f13099156b930a1 % Raw Data Hash: af183c98f586d34c66de92e4940b77e7 % Adj Data Hash: 2394e003338984d6b90de8a7c2500a0f % % 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 1905 1 NaN NaN NaN NaN NaN NaN -8.606 -3.272 1905 2 NaN NaN NaN NaN NaN NaN -8.703 -6.737 1905 3 NaN NaN NaN NaN NaN NaN 4.949 2.838 1905 4 NaN NaN NaN NaN NaN NaN 7.857 -1.381 1905 5 NaN NaN NaN NaN NaN NaN 12.931 -2.358 1905 6 NaN NaN NaN NaN NaN NaN 20.168 -0.746 1905 7 NaN NaN NaN NaN NaN NaN 21.057 -3.023 1905 8 NaN NaN NaN NaN NaN NaN 23.108 0.145 1905 9 NaN NaN NaN NaN NaN NaN 18.135 0.654 1905 10 NaN NaN NaN NaN NaN NaN 9.118 -1.782 1905 11 NaN NaN NaN NaN NaN NaN 4.141 1.596 1905 12 NaN NaN NaN NaN NaN NaN -1.400 1.344 1906 1 0.802 5.475 1 0 NaN NaN -1.712 3.621 1906 2 -1.427 -0.121 1 0 NaN NaN -1.094 0.872 1906 3 -3.489 -6.261 0 0 -3.489 -6.261 -4.570 -6.682 1906 4 11.768 1.870 0 0 11.768 1.870 11.208 1.971 1906 5 16.539 0.590 0 0 16.539 0.590 15.560 0.271 1906 6 19.953 -1.621 0 0 19.953 -1.621 18.837 -2.078 1906 7 21.998 -2.742 0 0 21.998 -2.742 20.871 -3.209 1906 8 22.873 -0.752 0 0 22.873 -0.752 22.100 -0.864 1906 9 17.968 -0.173 0 0 17.968 -0.173 17.343 -0.137 1906 10 8.773 -2.787 0 0 8.773 -2.787 9.314 -1.585 1906 11 2.133 -1.072 0 0 2.133 -1.072 1.720 -0.825 1906 12 0.021 2.105 0 0 0.021 2.105 -0.450 2.294 1907 1 NaN NaN NaN NaN NaN NaN -7.760 -2.426 1907 2 NaN NaN NaN NaN NaN NaN -0.551 1.415 1907 3 NaN NaN NaN NaN NaN NaN 5.266 3.154 1907 4 NaN NaN NaN NaN NaN NaN 5.835 -3.402 1907 5 NaN NaN NaN NaN NaN NaN 11.759 -3.530 1907 6 NaN NaN NaN NaN NaN NaN 19.324 -1.591 1907 7 NaN NaN NaN NaN NaN NaN 22.998 -1.082 1907 8 NaN NaN NaN NaN NaN NaN 22.879 -0.084 1907 9 NaN NaN NaN NaN NaN NaN 16.840 -0.641 1907 10 NaN NaN NaN NaN NaN NaN 11.882 0.983 1907 11 NaN NaN NaN NaN NaN NaN 2.152 -0.393 1907 12 NaN NaN NaN NaN NaN NaN -1.962 0.783