% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 33293 % Primary Name: JEFFERSON BARRACKS % Record Type: TAVG % Country: United States % State: MO % Latitude: 38.51670 +/- 0.00005 % Longitude: -90.26670 +/- 0.00005 % Elevation (m): 149.35 +/- 0.15 % # of Months: 9 % % Alternate Names: Missing Station ID - 234272 % % IDs: coop - 234272 % ghcnd - USC00234272 % ncdc - 12002963 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 06d460cd726570b8e187fdeb9d9b2d36 % Raw Data Hash: 2c9fef234493ee1cb77d388f2b6f800a % Adj Data Hash: 521199550b3903831d969b50c778eb1e % % 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 1941 2 NaN NaN NaN NaN NaN NaN 0.020 -2.022 1941 3 NaN NaN NaN NaN NaN NaN 4.406 -2.798 1941 4 NaN NaN NaN NaN NaN NaN 15.694 1.848 1941 5 NaN NaN NaN NaN NaN NaN 20.176 1.297 1941 6 NaN NaN NaN NaN NaN NaN 24.324 0.676 1941 7 NaN NaN NaN NaN NaN NaN 26.608 0.837 1941 8 NaN NaN NaN NaN NaN NaN 26.166 1.373 1941 9 NaN NaN NaN NaN NaN NaN 22.671 1.691 1941 10 NaN NaN NaN NaN NaN NaN 17.288 2.851 1941 11 NaN NaN NaN NaN NaN NaN 7.675 0.030 1941 12 NaN NaN NaN NaN NaN NaN 4.522 2.386 1942 1 NaN NaN NaN NaN NaN NaN -0.851 -0.341 1942 2 1.013 -1.817 1 0 NaN NaN 0.583 -1.459 1942 3 9.805 1.813 0 0 9.805 1.813 8.438 1.234 1942 4 15.515 0.881 0 0 15.515 0.881 15.082 1.236 1942 5 18.251 -1.417 0 0 18.251 -1.417 18.137 -0.743 1942 6 NaN NaN NaN NaN NaN NaN 23.727 0.080 1942 7 NaN NaN NaN NaN NaN NaN 25.957 0.186 1942 8 NaN NaN NaN NaN NaN NaN 23.629 -1.163 1942 9 21.183 -0.584 0 0 21.183 -0.584 20.302 -0.678 1942 10 16.229 1.004 0 0 16.229 1.004 14.937 0.500 1942 11 11.280 2.846 1 0 NaN NaN 9.585 1.940 1942 12 1.410 -1.515 0 0 1.410 -1.515 0.970 -1.167 1943 1 1.868 1.590 0 0 1.868 1.590 0.879 1.390 1943 2 NaN NaN NaN NaN NaN NaN 4.079 2.037 1943 3 NaN NaN NaN NaN NaN NaN 4.500 -2.703 1943 4 NaN NaN NaN NaN NaN NaN 13.393 -0.453 1943 5 NaN NaN NaN NaN NaN NaN 18.507 -0.372 1943 6 NaN NaN NaN NaN NaN NaN 25.146 1.499 1943 7 NaN NaN NaN NaN NaN NaN 26.444 0.673 1943 8 NaN NaN NaN NaN NaN NaN 26.128 1.335 1943 9 NaN NaN NaN NaN NaN NaN 18.976 -2.003 1943 10 NaN NaN NaN NaN NaN NaN 13.883 -0.555 1943 11 NaN NaN NaN NaN NaN NaN 6.575 -1.071 1943 12 NaN NaN NaN NaN NaN NaN 0.660 -1.476 1944 1 NaN NaN NaN NaN NaN NaN 1.861 2.372