% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 33166 % Primary Name: POPES CREEK % Record Type: TAVG % Country: United States % State: MD % Latitude: 38.40000 +/- 0.00833 % Longitude: -77.00000 +/- 0.00833 % Elevation (m): 6.10 +/- 0.15 % # of Months: 11 % % Alternate Names: Missing Station ID - 187205 % % IDs: coop - 187205 % ghcnd - USC00187205 % ncdc - 12002352 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: ca83ae2c7c7a2802613562fd794efea9 % Raw Data Hash: a7d0658c5020e75141020479fd37e7f7 % Adj Data Hash: c1817295f0879d2366c3fc1ef61eed60 % % 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 1893 7 NaN NaN NaN NaN NaN NaN 25.395 0.124 1893 8 NaN NaN NaN NaN NaN NaN 23.947 -0.715 1893 9 NaN NaN NaN NaN NaN NaN 20.159 -0.867 1893 10 NaN NaN NaN NaN NaN NaN 13.807 -0.592 1893 11 NaN NaN NaN NaN NaN NaN 7.900 -1.056 1893 12 NaN NaN NaN NaN NaN NaN 4.431 0.698 1894 1 NaN NaN NaN NaN NaN NaN 3.940 1.919 1894 2 NaN NaN NaN NaN NaN NaN 3.181 -0.148 1894 3 NaN NaN NaN NaN NaN NaN 10.387 2.276 1894 4 NaN NaN NaN NaN NaN NaN 12.893 -0.909 1894 5 NaN NaN NaN NaN NaN NaN 19.708 1.012 1894 6 NaN NaN NaN NaN NaN NaN 23.394 0.466 1894 7 25.396 0.228 1 0 NaN NaN 25.467 0.195 1894 8 23.552 -1.007 0 0 23.552 -1.007 23.305 -1.357 1894 9 22.027 1.105 0 0 22.027 1.105 22.212 1.186 1894 10 14.916 0.622 0 0 14.916 0.622 14.364 -0.034 1894 11 6.708 -2.143 0 0 6.708 -2.143 7.721 -1.235 1894 12 NaN NaN NaN NaN NaN NaN 3.821 0.088 1895 1 0.113 -1.804 0 0 0.113 -1.804 0.607 -1.414 1895 2 NaN NaN NaN NaN NaN NaN -2.982 -6.311 1895 3 NaN NaN NaN NaN NaN NaN 6.816 -1.295 1895 4 11.905 -1.793 0 0 11.905 -1.793 13.308 -0.493 1895 5 17.308 -1.285 1 0 NaN NaN 17.107 -1.590 1895 6 24.138 1.314 0 0 24.138 1.314 23.825 0.897 1895 7 23.521 -1.647 0 0 23.521 -1.647 23.355 -1.917 1895 8 26.161 1.603 0 0 26.161 1.603 25.279 0.616 1895 9 NaN NaN NaN NaN NaN NaN 23.286 2.260 1895 10 NaN NaN NaN NaN NaN NaN 11.369 -3.029 1895 11 NaN NaN NaN NaN NaN NaN 9.247 0.292 1895 12 NaN NaN NaN NaN NaN NaN 3.785 0.052 1896 1 NaN NaN NaN NaN NaN NaN 1.218 -0.803 1896 2 NaN NaN NaN NaN NaN NaN 3.019 -0.310 1896 3 NaN NaN NaN NaN NaN NaN 5.702 -2.409 1896 4 NaN NaN NaN NaN NaN NaN 15.217 1.415 1896 5 NaN NaN NaN NaN NaN NaN 21.223 2.527 1896 6 NaN NaN NaN NaN NaN NaN 22.406 -0.521 1896 7 NaN NaN NaN NaN NaN NaN 25.479 0.208 1896 8 NaN NaN NaN NaN NaN NaN 25.004 0.341