% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 167518 % Primary Name: ST LOUIS LAMBERT % Record Type: TAVG % Country: United States % State: MO % Latitude: 38.75000 +/- 0.00005 % Longitude: -90.38330 +/- 0.00005 % Elevation (m): 166.10 +/- 0.05 % # of Months: 17 % % IDs: ghcnd - USW00093910 % gsod - 999999-93910 % ncdc - 20011883 % wban - 93910 % % Sources: US First Order Summary of the Day % Global Historical Climatology Network - Daily % Global Summary of the Day % Multi-network Metadata System % % Site Hash: 7f808835f0c4516c18cf267acbfd9859 % Raw Data Hash: 5b46bd31002c0f2d1623a8fc84ab134f % Adj Data Hash: ac8b7cbf96edff2e2d814dac58d9e1f3 % % 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 1944 3 NaN NaN NaN NaN NaN NaN 3.327 -1.896 1944 4 NaN NaN NaN NaN NaN NaN 11.006 -1.386 1944 5 NaN NaN NaN NaN NaN NaN 19.974 2.033 1944 6 NaN NaN NaN NaN NaN NaN 25.064 2.091 1944 7 NaN NaN NaN NaN NaN NaN 24.816 -0.176 1944 8 NaN NaN NaN NaN NaN NaN 24.101 0.227 1944 9 NaN NaN NaN NaN NaN NaN 20.297 0.126 1944 10 NaN NaN NaN NaN NaN NaN 14.096 0.534 1944 11 NaN NaN NaN NaN NaN NaN 7.524 1.317 1944 12 NaN NaN NaN NaN NaN NaN -3.383 -3.478 1945 1 NaN NaN NaN NaN NaN NaN -4.688 -1.615 1945 2 NaN NaN NaN NaN NaN NaN 0.449 0.739 1945 3 12.653 6.250 0 0 12.653 6.250 10.811 5.588 1945 4 13.562 -0.010 0 0 13.562 -0.010 12.856 0.464 1945 5 15.870 -3.250 0 0 15.870 -3.250 14.824 -3.117 1945 6 20.852 -3.301 0 0 20.852 -3.301 20.653 -2.320 1945 7 24.344 -1.827 0 0 24.344 -1.827 23.358 -1.634 1945 8 24.661 -0.392 0 0 24.661 -0.392 23.481 -0.393 1945 9 20.535 -0.816 0 0 20.535 -0.816 20.349 0.178 1945 10 14.002 -0.740 0 0 14.002 -0.740 12.848 -0.714 1945 11 7.760 0.373 0 0 7.760 0.373 6.551 0.344 1945 12 -2.485 -3.759 0 0 -2.485 -3.759 -3.559 -3.653 1946 1 1.190 3.083 0 0 1.190 3.083 -1.352 1.721 1946 2 4.602 3.712 1 0 NaN NaN 1.990 2.279 1946 3 13.745 7.342 0 0 13.745 7.342 11.983 6.759 1946 4 15.388 1.817 0 0 15.388 1.817 14.073 1.681 1946 5 16.606 -2.514 0 0 16.606 -2.514 15.628 -2.312 1946 6 24.387 0.234 0 0 24.387 0.234 23.145 0.172 1946 7 26.258 0.087 0 0 26.258 0.087 24.805 -0.186 1946 8 NaN NaN NaN NaN NaN NaN 21.232 -2.642 1946 9 NaN NaN NaN NaN NaN NaN 19.673 -0.498 1946 10 NaN NaN NaN NaN NaN NaN 15.866 2.304 1946 11 NaN NaN NaN NaN NaN NaN 7.968 1.761 1946 12 NaN NaN NaN NaN NaN NaN 3.100 3.006 1947 1 NaN NaN NaN NaN NaN NaN -0.101 2.971 1947 2 NaN NaN NaN NaN NaN NaN -3.797 -3.507 1947 3 NaN NaN NaN NaN NaN NaN 1.266 -3.958 1947 4 NaN NaN NaN NaN NaN NaN 11.956 -0.436 1947 5 NaN NaN NaN NaN NaN NaN 15.833 -2.108 1947 6 NaN NaN NaN NaN NaN NaN 21.595 -1.378 1947 7 NaN NaN NaN NaN NaN NaN 22.905 -2.087