% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 41230 % Primary Name: POWDER RIVER % Record Type: TAVG % Country: United States % State: MT % Latitude: 45.71670 +/- 0.00005 % Longitude: -105.08330 +/- 0.00005 % Elevation (m): 899.16 +/- 0.15 % # of Months: 13 % % Alternate Names: Missing Station ID - 246688 % % IDs: coop - 246688 % ghcnd - USC00246688 % ncdc - 12003160 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: d0f322dd34622d081d07edda105ca48b % Raw Data Hash: f0b54831a9cd7185657b343c39a3cffb % Adj Data Hash: b5068e9f1e96b578b82697f54b96bd22 % % 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 1892 2 NaN NaN NaN NaN NaN NaN -5.442 -0.463 1892 3 NaN NaN NaN NaN NaN NaN -0.639 0.045 1892 4 NaN NaN NaN NaN NaN NaN 4.195 -2.019 1892 5 NaN NaN NaN NaN NaN NaN 8.569 -3.923 1892 6 NaN NaN NaN NaN NaN NaN 15.545 -2.158 1892 7 NaN NaN NaN NaN NaN NaN 21.703 -0.236 1892 8 NaN NaN NaN NaN NaN NaN 20.611 -0.351 1892 9 NaN NaN NaN NaN NaN NaN 16.115 1.508 1892 10 NaN NaN NaN NaN NaN NaN 10.198 2.065 1892 11 NaN NaN NaN NaN NaN NaN -0.994 -0.700 1892 12 NaN NaN NaN NaN NaN NaN -8.983 -3.321 1893 1 NaN NaN NaN NaN NaN NaN -8.589 0.492 1893 2 -11.800 -7.137 0 0 -11.800 -7.137 -10.642 -5.663 1893 3 -3.244 -2.876 0 0 -3.244 -2.876 -4.736 -4.052 1893 4 4.463 -2.067 0 0 4.463 -2.067 3.422 -2.791 1893 5 12.276 -0.533 0 0 12.276 -0.533 11.439 -1.054 1893 6 18.593 0.574 0 0 18.593 0.574 17.934 0.231 1893 7 23.492 1.237 0 0 23.492 1.237 22.727 0.788 1893 8 22.632 1.354 0 0 22.632 1.354 21.169 0.206 1893 9 15.925 1.002 0 0 15.925 1.002 14.898 0.290 1893 10 6.290 -2.158 0 0 6.290 -2.158 7.193 -0.940 1893 11 -2.528 -2.551 0 0 -2.528 -2.551 -2.828 -2.534 1893 12 -4.946 0.399 0 0 -4.946 0.399 -5.455 0.206 1894 1 NaN NaN NaN NaN NaN NaN -12.134 -3.053 1894 2 -12.382 -7.719 0 0 -12.382 -7.719 -9.929 -4.950 1894 3 -2.273 -1.905 0 0 -2.273 -1.905 -2.801 -2.117 1894 4 NaN NaN NaN NaN NaN NaN 7.934 1.720 1894 5 NaN NaN NaN NaN NaN NaN 13.908 1.415 1894 6 NaN NaN NaN NaN NaN NaN 18.856 1.153 1894 7 NaN NaN NaN NaN NaN NaN 22.684 0.745 1894 8 NaN NaN NaN NaN NaN NaN 22.277 1.315 1894 9 NaN NaN NaN NaN NaN NaN 13.069 -1.538 1894 10 NaN NaN NaN NaN NaN NaN 8.493 0.361 1894 11 NaN NaN NaN NaN NaN NaN 0.525 0.818 1894 12 NaN NaN NaN NaN NaN NaN -4.496 1.166 1895 1 NaN NaN NaN NaN NaN NaN -12.760 -3.680 1895 2 NaN NaN NaN NaN NaN NaN -9.096 -4.116 1895 3 NaN NaN NaN NaN NaN NaN -1.458 -0.774