% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 34111 % Primary Name: PARKVILLE % Record Type: TAVG % Country: United States % State: MO % Latitude: 39.16670 +/- 0.00005 % Longitude: -94.68330 +/- 0.00005 % Elevation (m): 249.60 +/- 81.01 % # of Months: 11 % % Alternate Names: Missing Station ID - 236524 % % IDs: coop - 236524 % ghcnd - USC00236524 % ncdc - 12002996 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: a0940b94833bf8048cfd9f4a498b908a % Raw Data Hash: 1f6924f46b94d78b7a1ccbd3a5aa0a34 % Adj Data Hash: 88bcb3c7ac4f79ee1cf65aff93199e4a % % 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 1907 7 NaN NaN NaN NaN NaN NaN 25.634 -0.409 1907 8 NaN NaN NaN NaN NaN NaN 24.728 -0.289 1907 9 NaN NaN NaN NaN NaN NaN 19.726 -0.470 1907 10 NaN NaN NaN NaN NaN NaN 13.675 -0.252 1907 11 NaN NaN NaN NaN NaN NaN 5.395 -0.505 1907 12 NaN NaN NaN NaN NaN NaN 1.175 1.485 1908 1 NaN NaN NaN NaN NaN NaN -0.273 3.280 1908 2 NaN NaN NaN NaN NaN NaN 0.586 0.646 1908 3 NaN NaN NaN NaN NaN NaN 7.231 2.030 1908 4 NaN NaN NaN NaN NaN NaN 13.029 0.555 1908 5 NaN NaN NaN NaN NaN NaN 16.864 -1.343 1908 6 NaN NaN NaN NaN NaN NaN 21.581 -1.716 1908 7 25.910 -2.040 0 0 25.910 -2.040 24.021 -2.022 1908 8 25.594 -1.331 0 0 25.594 -1.331 23.740 -1.277 1908 9 23.527 1.424 0 0 23.527 1.424 20.948 0.752 1908 10 NaN NaN NaN NaN NaN NaN 12.865 -1.062 1908 11 10.048 2.242 0 0 10.048 2.242 6.432 0.532 1908 12 3.407 1.809 0 0 3.407 1.809 1.523 1.833 1909 1 -1.029 0.617 0 0 -1.029 0.617 -3.391 0.162 1909 2 2.287 0.441 1 0 NaN NaN 1.295 1.355 1909 3 6.252 -0.856 0 0 6.252 -0.856 3.827 -1.373 1909 4 12.322 -2.060 0 0 12.322 -2.060 10.659 -1.815 1909 5 NaN NaN NaN NaN NaN NaN 16.422 -1.785 1909 6 23.237 -1.967 0 0 23.237 -1.967 22.460 -0.837 1909 7 25.029 -2.921 0 0 25.029 -2.921 25.006 -1.037 1909 8 NaN NaN NaN NaN NaN NaN 26.070 1.052 1909 9 NaN NaN NaN NaN NaN NaN 19.731 -0.464 1909 10 NaN NaN NaN NaN NaN NaN 13.614 -0.313 1909 11 NaN NaN NaN NaN NaN NaN 9.197 3.298 1909 12 NaN NaN NaN NaN NaN NaN -6.687 -6.377 1910 1 NaN NaN NaN NaN NaN NaN -3.700 -0.147 1910 2 NaN NaN NaN NaN NaN NaN -2.702 -2.642 1910 3 NaN NaN NaN NaN NaN NaN 12.378 7.178 1910 4 NaN NaN NaN NaN NaN NaN 13.725 1.250 1910 5 NaN NaN NaN NaN NaN NaN 14.706 -3.501 1910 6 NaN NaN NaN NaN NaN NaN 21.603 -1.694 1910 7 NaN NaN NaN NaN NaN NaN 25.573 -0.470