% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 34133 % Primary Name: NEW HARTFORD % Record Type: TAVG % Country: United States % State: MO % Latitude: 39.19940 +/- 0.00005 % Longitude: -91.27030 +/- 0.00005 % Elevation (m): 185.01 +/- 0.15 % # of Months: 23 % % Alternate Names: Missing Station ID - 236021 % % IDs: coop - 236021 % ghcnd - USC00236021 % ncdc - 12002986 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 376af0eb653222ef7f74687489e062b8 % Raw Data Hash: f7f8e7a95fc354c7e0d203adb39de94f % Adj Data Hash: 151937cbd14156cf312b44e0c3c28854 % % 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 3 NaN NaN NaN NaN NaN NaN 2.452 -2.591 1892 4 NaN NaN NaN NaN NaN NaN 10.967 -1.379 1892 5 NaN NaN NaN NaN NaN NaN 15.064 -2.771 1892 6 NaN NaN NaN NaN NaN NaN 23.121 0.268 1892 7 NaN NaN NaN NaN NaN NaN 23.809 -1.525 1892 8 NaN NaN NaN NaN NaN NaN 23.633 -0.564 1892 9 NaN NaN NaN NaN NaN NaN 19.346 -0.629 1892 10 NaN NaN NaN NaN NaN NaN 13.864 0.290 1892 11 NaN NaN NaN NaN NaN NaN 3.431 -2.738 1892 12 NaN NaN NaN NaN NaN NaN -2.325 -2.219 1893 1 NaN NaN NaN NaN NaN NaN -7.891 -4.526 1893 2 NaN NaN NaN NaN NaN NaN -3.497 -3.129 1893 3 5.491 -0.225 1 0 NaN NaN 3.703 -1.340 1893 4 12.796 -0.223 0 0 12.796 -0.223 11.537 -0.810 1893 5 17.186 -1.322 0 0 17.186 -1.322 15.870 -1.965 1893 6 23.222 -0.305 0 0 23.222 -0.305 22.496 -0.358 1893 7 26.344 0.337 0 0 26.344 0.337 25.304 -0.031 1893 8 24.301 -0.569 0 0 24.301 -0.569 22.389 -1.808 1893 9 23.093 2.444 0 0 23.093 2.444 20.939 0.964 1893 10 14.588 0.340 0 0 14.588 0.340 13.516 -0.058 1893 11 4.407 -2.435 0 0 4.407 -2.435 4.599 -1.570 1893 12 1.241 0.674 0 0 1.241 0.674 0.227 0.333 1894 1 -0.609 2.083 0 0 -0.609 2.083 -2.199 1.167 1894 2 NaN NaN NaN NaN NaN NaN -2.975 -2.606 1894 3 9.278 3.561 0 0 9.278 3.561 7.944 2.901 1894 4 13.130 0.110 0 0 13.130 0.110 13.014 0.668 1894 5 17.490 -1.018 0 0 17.490 -1.018 17.065 -0.770 1894 6 27.222 3.695 1 0 NaN NaN 24.186 1.333 1894 7 26.481 0.474 0 0 26.481 0.474 25.019 -0.315 1894 8 24.247 -0.623 0 0 24.247 -0.623 24.392 0.195 1894 9 21.704 1.056 0 0 21.704 1.056 19.981 0.007 1894 10 NaN NaN NaN NaN NaN NaN 13.933 0.359 1894 11 4.540 -2.302 0 0 4.540 -2.302 4.014 -2.155 1894 12 2.593 2.025 0 0 2.593 2.025 1.904 2.010 1895 1 NaN NaN NaN NaN NaN NaN -6.368 -3.003 1895 2 -8.909 -9.214 0 0 -8.909 -9.214 -6.325 -5.956 1895 3 3.730 -1.986 1 0 NaN NaN 4.198 -0.845 1895 4 11.877 -1.142 0 0 11.877 -1.142 13.848 1.502 1895 5 NaN NaN NaN NaN NaN NaN 17.633 -0.202 1895 6 NaN NaN NaN NaN NaN NaN 23.142 0.289 1895 7 NaN NaN NaN NaN NaN NaN 23.460 -1.875 1895 8 NaN NaN NaN NaN NaN NaN 23.774 -0.423 1895 9 NaN NaN NaN NaN NaN NaN 21.745 1.771 1895 10 NaN NaN NaN NaN NaN NaN 10.345 -3.229 1895 11 NaN NaN NaN NaN NaN NaN 4.705 -1.465 1895 12 NaN NaN NaN NaN NaN NaN 0.600 0.706 1896 1 NaN NaN NaN NaN NaN NaN -1.389 1.977 1896 2 NaN NaN NaN NaN NaN NaN 0.282 0.651 1896 3 NaN NaN NaN NaN NaN NaN 2.377 -2.666 1896 4 NaN NaN NaN NaN NaN NaN 16.482 4.135