% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 33896 % Primary Name: PRAIRIE VILLAGE % Record Type: TAVG % Country: United States % State: KS % Latitude: 39.00000 +/- 0.00005 % Longitude: -94.63330 +/- 0.00005 % Elevation (m): 281.03 +/- 0.15 % # of Months: 12 % % Alternate Names: Missing Station ID - 146543 % % IDs: coop - 146543 % ghcnd - USC00146543 % ncdc - 20007724 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 1a203f95b3200973025ca2b3b360929f % Raw Data Hash: 87b72f6539b845bedbe338f73d79ddfc % Adj Data Hash: 635d7530eee54b6230c9e4a54500bfe1 % % 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 1947 9 NaN NaN NaN NaN NaN NaN 21.997 1.909 1947 10 NaN NaN NaN NaN NaN NaN 18.424 4.666 1947 11 NaN NaN NaN NaN NaN NaN 3.757 -2.299 1947 12 NaN NaN NaN NaN NaN NaN 1.957 2.221 1948 1 NaN NaN NaN NaN NaN NaN -5.841 -2.281 1948 2 NaN NaN NaN NaN NaN NaN -1.462 -1.197 1948 3 NaN NaN NaN NaN NaN NaN 3.301 -1.826 1948 4 NaN NaN NaN NaN NaN NaN 15.268 2.810 1948 5 NaN NaN NaN NaN NaN NaN 17.362 -0.749 1948 6 NaN NaN NaN NaN NaN NaN 22.520 -0.478 1948 7 NaN NaN NaN NaN NaN NaN 25.283 -0.371 1948 8 NaN NaN NaN NaN NaN NaN 24.609 0.095 1948 9 16.850 -3.846 1 0 NaN NaN 21.364 1.277 1948 10 13.313 -1.054 0 0 13.313 -1.054 13.181 -0.577 1948 11 7.452 0.787 0 0 7.452 0.787 7.077 1.021 1948 12 2.185 1.840 0 0 2.185 1.840 1.056 1.319 1949 1 -3.576 -0.626 1 0 NaN NaN -4.729 -1.170 1949 2 NaN NaN NaN NaN NaN NaN -1.283 -1.018 1949 3 5.673 -0.064 0 0 5.673 -0.064 4.502 -0.625 1949 4 11.945 -1.122 0 0 11.945 -1.122 11.716 -0.742 1949 5 19.916 1.197 0 0 19.916 1.197 19.322 1.212 1949 6 24.658 1.051 0 0 24.658 1.051 23.871 0.873 1949 7 27.098 0.835 1 0 NaN NaN 26.000 0.346 1949 8 NaN NaN NaN NaN NaN NaN 23.771 -0.743 1949 9 NaN NaN NaN NaN NaN NaN 16.700 -3.388 1949 10 NaN NaN NaN NaN NaN NaN 15.177 1.419 1949 11 NaN NaN NaN NaN NaN NaN 8.414 2.358 1949 12 NaN NaN NaN NaN NaN NaN 1.749 2.013 1950 1 NaN NaN NaN NaN NaN NaN -1.895 1.664 1950 2 NaN NaN NaN NaN NaN NaN 0.597 0.862 1950 3 4.064 -1.672 1 0 NaN NaN 3.060 -2.067 1950 4 10.407 -2.661 0 0 10.407 -2.661 9.953 -2.506 1950 5 NaN NaN NaN NaN NaN NaN 18.284 0.174 1950 6 NaN NaN NaN NaN NaN NaN 22.458 -0.540 1950 7 NaN NaN NaN NaN NaN NaN 22.114 -3.540 1950 8 NaN NaN NaN NaN NaN NaN 21.160 -3.354 1950 9 NaN NaN NaN NaN NaN NaN 18.741 -1.346 1950 10 NaN NaN NaN NaN NaN NaN 17.229 3.471 1950 11 NaN NaN NaN NaN NaN NaN 3.831 -2.225 1950 12 NaN NaN NaN NaN NaN NaN -2.102 -1.839 1951 1 NaN NaN NaN NaN NaN NaN -2.204 1.355 1951 2 NaN NaN NaN NaN NaN NaN 0.081 0.346 1951 3 NaN NaN NaN NaN NaN NaN 2.429 -2.699 1951 4 NaN NaN NaN NaN NaN NaN 10.022 -2.436