% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 28444 % Primary Name: GRANITE HILL % Record Type: TAVG % Country: United States % State: GA % Latitude: 33.30000 +/- 0.00005 % Longitude: -82.93330 +/- 0.00005 % Elevation (m): 158.50 +/- 0.15 % # of Months: 20 % % Alternate Names: Missing Station ID - 93840 % % IDs: coop - 93840 % ghcnd - USC00093840 % ncdc - 12001454 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: bafef1e8523d4fb4bf8a40e67636c9d8 % Raw Data Hash: 8474ba34df8f3f8acb474654b0f17d6d % Adj Data Hash: 47d36f42d84e032a938d3adf7e9dc481 % % 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 1910 12 NaN NaN NaN NaN NaN NaN 5.565 -2.946 1911 1 NaN NaN NaN NaN NaN NaN 9.725 2.243 1911 2 NaN NaN NaN NaN NaN NaN 11.352 2.311 1911 3 NaN NaN NaN NaN NaN NaN 13.793 0.712 1911 4 NaN NaN NaN NaN NaN NaN 17.461 -0.317 1911 5 NaN NaN NaN NaN NaN NaN 22.568 0.577 1911 6 NaN NaN NaN NaN NaN NaN 27.240 1.842 1911 7 NaN NaN NaN NaN NaN NaN 25.635 -1.270 1911 8 NaN NaN NaN NaN NaN NaN 26.351 -0.293 1911 9 NaN NaN NaN NaN NaN NaN 26.799 2.960 1911 10 NaN NaN NaN NaN NaN NaN 20.155 2.444 1911 11 NaN NaN NaN NaN NaN NaN 10.901 -1.603 1911 12 12.367 4.071 1 0 NaN NaN 9.571 1.060 1912 1 NaN NaN NaN NaN NaN NaN 4.663 -2.819 1912 2 NaN NaN NaN NaN NaN NaN 5.729 -3.312 1912 3 11.795 -1.070 0 0 11.795 -1.070 11.861 -1.220 1912 4 18.247 0.685 0 0 18.247 0.685 18.514 0.736 1912 5 22.215 0.440 0 0 22.215 0.440 22.419 0.429 1912 6 23.635 -1.548 0 0 23.635 -1.548 24.065 -1.334 1912 7 25.810 -0.879 0 0 25.810 -0.879 26.384 -0.521 1912 8 26.240 -0.187 0 0 26.240 -0.187 26.396 -0.248 1912 9 24.917 1.294 0 0 24.917 1.294 25.723 1.884 1912 10 18.771 1.276 0 0 18.771 1.276 18.357 0.646 1912 11 10.870 -1.418 0 0 10.870 -1.418 11.224 -1.280 1912 12 9.476 1.181 0 0 9.476 1.181 9.513 1.002 1913 1 11.640 4.375 0 0 11.640 4.375 11.419 3.937 1913 2 9.012 0.188 1 0 NaN NaN 9.079 0.038 1913 3 14.294 1.429 1 0 NaN NaN 13.423 0.342 1913 4 16.570 -0.992 0 0 16.570 -0.992 16.935 -0.843 1913 5 21.690 -0.084 0 0 21.690 -0.084 22.010 0.019 1913 6 NaN NaN NaN NaN NaN NaN 24.652 -0.747 1913 7 NaN NaN NaN NaN NaN NaN 27.407 0.502 1913 8 25.550 -0.877 1 0 NaN NaN 26.427 -0.217 1913 9 21.810 -1.813 0 0 21.810 -1.813 22.727 -1.112 1913 10 16.647 -0.849 1 0 NaN NaN 16.527 -1.185 1913 11 13.327 1.039 0 0 13.327 1.039 12.707 0.202 1913 12 NaN NaN NaN NaN NaN NaN 8.931 0.419 1914 1 NaN NaN NaN NaN NaN NaN 7.998 0.516 1914 2 NaN NaN NaN NaN NaN NaN 7.126 -1.915 1914 3 NaN NaN NaN NaN NaN NaN 10.692 -2.389 1914 4 NaN NaN NaN NaN NaN NaN 18.293 0.515 1914 5 NaN NaN NaN NaN NaN NaN 22.431 0.440 1914 6 NaN NaN NaN NaN NaN NaN 27.877 2.478 1914 7 NaN NaN NaN NaN NaN NaN 26.972 0.067 1914 8 NaN NaN NaN NaN NaN NaN 26.032 -0.612 1914 9 NaN NaN NaN NaN NaN NaN 22.817 -1.022 1914 10 NaN NaN NaN NaN NaN NaN 17.320 -0.391 1914 11 NaN NaN NaN NaN NaN NaN 11.650 -0.855