% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 164329 % Primary Name: SIOUX FALLS WFO AP % Record Type: TAVG % Country: United States % State: SD % Latitude: 43.58780 +/- 0.00005 % Longitude: -96.73000 +/- 0.00005 % Elevation (m): 435.86 +/- 0.15 % # of Months: 29 % % Alternate Names: Missing Station ID - 397666 % % IDs: coop - 397666 % ghcnd - USC00397666 % ncdc - 30001529 % nws - FSDS2 % % Sources: Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: d6950f1f1cce365888e0164af7b1bf1e % Raw Data Hash: a639839c2d467c36323200df13048724 % Adj Data Hash: a639839c2d467c36323200df13048724 % % 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 2010 1 NaN NaN NaN NaN NaN NaN -13.264 -1.421 2010 2 NaN NaN NaN NaN NaN NaN -10.094 -1.900 2010 3 NaN NaN NaN NaN NaN NaN 1.425 3.437 2010 4 NaN NaN NaN NaN NaN NaN 11.724 4.682 2010 5 NaN NaN NaN NaN NaN NaN 14.378 0.120 2010 6 NaN NaN NaN NaN NaN NaN 19.912 0.227 2010 7 NaN NaN NaN NaN NaN NaN 23.110 0.718 2010 8 NaN NaN NaN NaN NaN NaN 23.733 2.498 2010 9 NaN NaN NaN NaN NaN NaN 14.870 -0.852 2010 10 NaN NaN NaN NaN NaN NaN 11.717 2.380 2010 11 NaN NaN NaN NaN NaN NaN 1.146 1.006 2010 12 NaN NaN NaN NaN NaN NaN -9.986 -2.358 2011 1 -11.889 -0.961 0 0 -11.889 -0.961 -13.967 -2.124 2011 2 -8.167 -0.889 0 0 -8.167 -0.889 -9.057 -0.863 2011 3 -1.167 -0.070 0 0 -1.167 -0.070 -3.962 -1.949 2011 4 6.889 -1.069 0 0 6.889 -1.069 6.556 -0.486 2011 5 14.167 -1.008 0 0 14.167 -1.008 13.398 -0.860 2011 6 20.000 -0.601 0 0 20.000 -0.601 19.541 -0.144 2011 7 25.715 2.407 0 0 25.715 2.407 25.290 2.898 2011 8 22.056 -0.095 0 0 22.056 -0.095 21.778 0.543 2011 9 15.500 -1.138 0 0 15.500 -1.138 15.113 -0.609 2011 10 12.000 1.747 0 0 12.000 1.747 12.216 2.879 2011 11 2.667 1.611 0 0 2.667 1.611 2.237 2.097 2011 12 -2.794 3.919 0 0 -2.794 3.919 -3.051 4.578 2012 1 -4.297 6.631 0 0 -4.297 6.631 -5.984 5.860 2012 2 NaN NaN NaN NaN NaN NaN -3.424 4.770 2012 3 9.966 11.063 0 0 9.966 11.063 7.151 9.164 2012 4 10.962 3.004 0 0 10.962 3.004 10.165 3.123 2012 5 17.058 1.884 0 0 17.058 1.884 16.743 2.485 2012 6 22.895 2.294 0 0 22.895 2.294 21.797 2.111 2012 7 27.498 4.191 0 0 27.498 4.191 26.064 3.672 2012 8 22.515 0.364 0 0 22.515 0.364 21.386 0.151 2012 9 17.418 0.780 0 0 17.418 0.780 16.020 0.298 2012 10 8.024 -2.229 0 0 8.024 -2.229 8.354 -0.984 2012 11 2.277 1.221 0 0 2.277 1.221 1.976 1.836 2012 12 -5.629 1.083 0 0 -5.629 1.083 -6.403 1.225 2013 1 -7.906 3.021 0 0 -7.906 3.021 -9.515 2.329 2013 2 NaN NaN NaN NaN NaN NaN -7.764 0.430 2013 3 -2.631 -1.534 0 0 -2.631 -1.534 -4.787 -2.774 2013 4 4.005 -3.953 0 0 4.005 -3.953 2.701 -4.341 2013 5 NaN NaN NaN NaN NaN NaN 13.359 -0.900 2013 6 19.878 -0.723 0 0 19.878 -0.723 19.562 -0.123 2013 7 22.973 -0.335 0 0 22.973 -0.335 22.601 0.209 2013 8 22.490 0.340 0 0 22.490 0.340 21.991 0.756 2013 9 NaN NaN NaN NaN NaN NaN 18.556 2.834 2013 10 NaN NaN NaN NaN NaN NaN 9.124 -0.213