% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 35102 % Primary Name: NEW BOSTON 3 NE % Record Type: TAVG % Country: United States % State: MO % Latitude: 39.98330 +/- 0.00005 % Longitude: -92.81670 +/- 0.00005 % Elevation (m): 292.90 +/- 0.05 % # of Months: 16 % % Alternate Names: NEW BOSTON % % IDs: coop - 235999 % ghcnd - USC00235999 % ncdc - 20012046 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 419697e261fccef8abbac4c053324706 % Raw Data Hash: 3f36d62145002026d685d3395d1904ca % Adj Data Hash: c9bfad4bd5076eabe9b00f253d68dcc4 % % 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 1892 1 NaN NaN NaN NaN NaN NaN -5.976 -2.417 1892 2 NaN NaN NaN NaN NaN NaN 1.948 2.213 1892 3 NaN NaN NaN NaN NaN NaN 2.369 -2.759 1892 4 NaN NaN NaN NaN NaN NaN 11.071 -1.387 1892 5 NaN NaN NaN NaN NaN NaN 14.999 -3.111 1892 6 NaN NaN NaN NaN NaN NaN 23.075 0.076 1892 7 NaN NaN NaN NaN NaN NaN 24.268 -1.386 1892 8 NaN NaN NaN NaN NaN NaN 23.876 -0.638 1892 9 NaN NaN NaN NaN NaN NaN 20.010 -0.078 1892 10 NaN NaN NaN NaN NaN NaN 14.179 0.421 1892 11 NaN NaN NaN NaN NaN NaN 3.858 -2.198 1892 12 NaN NaN NaN NaN NaN NaN -2.829 -2.565 1893 1 -7.115 -2.335 0 0 -7.115 -2.335 -7.456 -3.897 1893 2 -6.736 -5.250 0 0 -6.736 -5.250 -3.620 -3.355 1893 3 -1.380 -5.286 0 0 -1.380 -5.286 3.440 -1.687 1893 4 6.858 -4.379 0 0 6.858 -4.379 11.830 -0.628 1893 5 16.326 -0.563 0 0 16.326 -0.563 16.240 -1.870 1893 6 24.333 2.556 0 0 24.333 2.556 22.788 -0.211 1893 7 26.048 1.615 0 0 26.048 1.615 25.376 -0.278 1893 8 NaN NaN NaN NaN NaN NaN 22.455 -2.059 1893 9 20.944 2.078 0 0 20.944 2.078 21.078 0.991 1893 10 11.792 -0.745 0 0 11.792 -0.745 14.399 0.641 1893 11 3.803 -1.032 0 0 3.803 -1.032 4.428 -1.627 1893 12 -0.591 0.893 0 0 -0.591 0.893 0.436 0.699 1894 1 -2.755 2.025 0 0 -2.755 2.025 -2.832 0.727 1894 2 -4.268 -2.782 1 0 NaN NaN -3.132 -2.867 1894 3 7.210 3.303 0 0 7.210 3.303 7.706 2.578 1894 4 NaN NaN NaN NaN NaN NaN 13.670 1.212 1894 5 NaN NaN NaN NaN NaN NaN 17.720 -0.390 1894 6 28.747 6.969 1 0 NaN NaN 23.741 0.742 1894 7 NaN NaN NaN NaN NaN NaN 24.837 -0.817 1894 8 NaN NaN NaN NaN NaN NaN 25.286 0.772 1894 9 NaN NaN NaN NaN NaN NaN 20.185 0.098 1894 10 NaN NaN NaN NaN NaN NaN 14.349 0.591 1894 11 NaN NaN NaN NaN NaN NaN 4.291 -1.765 1894 12 -0.323 1.161 0 0 -0.323 1.161 1.693 1.956 1895 1 NaN NaN NaN NaN NaN NaN -6.351 -2.792 1895 2 NaN NaN NaN NaN NaN NaN -5.374 -5.109 1895 3 NaN NaN NaN NaN NaN NaN 4.313 -0.814 1895 4 NaN NaN NaN NaN NaN NaN 14.653 2.194 1895 5 NaN NaN NaN NaN NaN NaN 18.017 -0.093 1895 6 NaN NaN NaN NaN NaN NaN 22.283 -0.715 1895 7 NaN NaN NaN NaN NaN NaN 23.127 -2.527 1895 8 NaN NaN NaN NaN NaN NaN 23.668 -0.846 1895 9 NaN NaN NaN NaN NaN NaN 22.044 1.957 1895 10 NaN NaN NaN NaN NaN NaN 10.969 -2.789 1895 11 NaN NaN NaN NaN NaN NaN 4.523 -1.533 1895 12 NaN NaN NaN NaN NaN NaN -0.227 0.037