% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 29022 % Primary Name: COLUMBIA FORT JACKSON % Record Type: TAVG % Country: United States % State: SC % Latitude: 34.01670 +/- 0.00005 % Longitude: -80.93330 +/- 0.00005 % Elevation (m): 75.90 +/- 0.05 % # of Months: 18 % % Alternate Names: COLUMBIA FT JACKSON % % IDs: coop - 381934 % ghcnd - USC00381934 % ncdc - 20017445 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 4a9454d49edf59ded51b2d100855876b % Raw Data Hash: a72c9a9c6bcfc62ebb0f38faa5b7570e % Adj Data Hash: a0f6251f474cb414e12b8622dd13a203 % % 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 1955 11 NaN NaN NaN NaN NaN NaN 10.692 -0.177 1955 12 NaN NaN NaN NaN NaN NaN 4.813 -1.642 1956 1 NaN NaN NaN NaN NaN NaN 4.520 -0.941 1956 2 NaN NaN NaN NaN NaN NaN 8.725 1.835 1956 3 NaN NaN NaN NaN NaN NaN 11.161 0.105 1956 4 NaN NaN NaN NaN NaN NaN 15.351 -0.849 1956 5 NaN NaN NaN NaN NaN NaN 21.263 0.621 1956 6 NaN NaN NaN NaN NaN NaN 24.748 0.485 1956 7 NaN NaN NaN NaN NaN NaN 26.291 0.150 1956 8 NaN NaN NaN NaN NaN NaN 26.582 0.819 1956 9 NaN NaN NaN NaN NaN NaN 21.472 -1.043 1956 10 NaN NaN NaN NaN NaN NaN 16.743 0.632 1956 11 12.056 0.043 0 0 12.056 0.043 10.468 -0.400 1956 12 NaN NaN NaN NaN NaN NaN 11.523 5.068 1957 1 8.556 1.950 0 0 8.556 1.950 7.170 1.709 1957 2 12.333 4.299 0 0 12.333 4.299 10.389 3.499 1957 3 11.833 -0.367 0 0 11.833 -0.367 10.432 -0.624 1957 4 18.389 1.045 0 0 18.389 1.045 17.900 1.700 1957 5 22.444 0.659 0 0 22.444 0.659 20.962 0.320 1957 6 25.667 0.260 0 0 25.667 0.260 24.661 0.398 1957 7 26.778 -0.507 0 0 26.778 -0.507 25.960 -0.180 1957 8 26.111 -0.796 0 0 26.111 -0.796 25.254 -0.509 1957 9 24.611 0.952 0 0 24.611 0.952 23.364 0.849 1957 10 15.833 -1.421 0 0 15.833 -1.421 13.893 -2.217 1957 11 12.333 0.321 0 0 12.333 0.321 12.045 1.177 1957 12 8.000 0.401 0 0 8.000 0.401 7.156 0.701 1958 1 3.889 -2.716 0 0 3.889 -2.716 2.805 -2.657 1958 2 -17.778 -25.812 1 0 NaN NaN 2.713 -4.177 1958 3 10.222 -1.978 0 0 10.222 -1.978 8.592 -2.464 1958 4 -17.778 -35.122 1 0 NaN NaN 16.027 -0.174 1958 5 21.056 -0.730 0 0 21.056 -0.730 20.755 0.113 1958 6 NaN NaN NaN NaN NaN NaN 24.610 0.347 1958 7 NaN NaN NaN NaN NaN NaN 26.201 0.061 1958 8 NaN NaN NaN NaN NaN NaN 26.069 0.306 1958 9 NaN NaN NaN NaN NaN NaN 22.485 -0.030 1958 10 NaN NaN NaN NaN NaN NaN 15.158 -0.952 1958 11 NaN NaN NaN NaN NaN NaN 13.323 2.455 1958 12 NaN NaN NaN NaN NaN NaN 4.576 -1.879 1959 1 NaN NaN NaN NaN NaN NaN 5.308 -0.154 1959 2 NaN NaN NaN NaN NaN NaN 7.850 0.960 1959 3 NaN NaN NaN NaN NaN NaN 9.908 -1.148 1959 4 NaN NaN NaN NaN NaN NaN 17.255 1.055 1959 5 NaN NaN NaN NaN NaN NaN 21.791 1.149