% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 34239 % Primary Name: GOLD HILL % Record Type: TAVG % Country: United States % State: NV % Latitude: 39.28330 +/- 0.00005 % Longitude: -119.65000 +/- 0.00005 % Elevation (m): 1981.20 +/- 0.15 % # of Months: 23 % % Alternate Names: Missing Station ID - 263290 % % IDs: coop - 263290 % ghcnd - USC00263290 % ncdc - 12003370 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: a325ed7bf6b683bce0e9045235b9aff0 % Raw Data Hash: 5a2c7f0ffe18eb370b778fea7294e8a0 % Adj Data Hash: 0e99cda407be2ab1040aa0c8edcb32d9 % % 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 9 NaN NaN NaN NaN NaN NaN 17.877 1.004 1892 10 NaN NaN NaN NaN NaN NaN 9.925 -0.656 1892 11 NaN NaN NaN NaN NaN NaN 4.780 0.865 1892 12 NaN NaN NaN NaN NaN NaN -1.125 -0.692 1893 1 NaN NaN NaN NaN NaN NaN 0.392 1.107 1893 2 NaN NaN NaN NaN NaN NaN 0.603 -1.877 1893 3 NaN NaN NaN NaN NaN NaN 3.437 -1.625 1893 4 NaN NaN NaN NaN NaN NaN 6.299 -2.304 1893 5 NaN NaN NaN NaN NaN NaN 12.566 -1.074 1893 6 NaN NaN NaN NaN NaN NaN 17.798 -0.709 1893 7 NaN NaN NaN NaN NaN NaN 22.393 -0.547 1893 8 NaN NaN NaN NaN NaN NaN 21.842 0.395 1893 9 16.015 -2.061 1 0 NaN NaN 14.897 -1.976 1893 10 14.900 3.116 0 0 14.900 3.116 10.128 -0.453 1893 11 8.743 3.625 0 0 8.743 3.625 3.826 -0.089 1893 12 5.948 5.178 0 0 5.948 5.178 1.463 1.896 1894 1 2.077 1.589 0 0 2.077 1.589 -0.845 -0.131 1894 2 -0.259 -3.942 0 0 -0.259 -3.942 -1.059 -3.539 1894 3 4.955 -1.311 0 0 4.955 -1.311 4.201 -0.861 1894 4 9.688 -0.117 0 0 9.688 -0.117 9.399 0.796 1894 5 12.911 -1.932 0 0 12.911 -1.932 14.466 0.826 1894 6 13.498 -6.212 0 0 13.498 -6.212 14.854 -3.653 1894 7 22.139 -2.004 0 0 22.139 -2.004 23.244 0.304 1894 8 22.435 -0.214 0 0 22.435 -0.214 22.412 0.965 1894 9 17.187 -0.889 0 0 17.187 -0.889 15.955 -0.918 1894 10 13.202 1.418 0 0 13.202 1.418 11.341 0.760 1894 11 11.977 6.859 1 0 NaN NaN 6.204 2.289 1894 12 -0.511 -1.282 0 0 -0.511 -1.282 -2.016 -1.583 1895 1 -0.255 -0.744 1 0 NaN NaN -2.154 -1.440 1895 2 4.113 0.430 0 0 4.113 0.430 1.752 -0.728 1895 3 4.929 -1.336 0 0 4.929 -1.336 4.355 -0.707 1895 4 9.547 -0.259 0 0 9.547 -0.259 9.474 0.872 1895 5 12.645 -2.198 0 0 12.645 -2.198 14.235 0.595 1895 6 17.605 -2.105 0 0 17.605 -2.105 17.550 -0.957 1895 7 NaN NaN NaN NaN NaN NaN 21.962 -0.979 1895 8 NaN NaN NaN NaN NaN NaN 21.371 -0.076 1895 9 NaN NaN NaN NaN NaN NaN 15.381 -1.491 1895 10 NaN NaN NaN NaN NaN NaN 11.294 0.714 1895 11 NaN NaN NaN NaN NaN NaN 2.352 -1.563 1895 12 1.176 0.405 0 0 1.176 0.405 -1.865 -1.432 1896 1 NaN NaN NaN NaN NaN NaN 2.383 3.097 1896 2 NaN NaN NaN NaN NaN NaN 3.830 1.350 1896 3 NaN NaN NaN NaN NaN NaN 4.617 -0.446 1896 4 NaN NaN NaN NaN NaN NaN 5.163 -3.440 1896 5 NaN NaN NaN NaN NaN NaN 10.719 -2.921 1896 6 NaN NaN NaN NaN NaN NaN 19.953 1.446 1896 7 NaN NaN NaN NaN NaN NaN 23.265 0.325 1896 8 NaN NaN NaN NaN NaN NaN 20.831 -0.616 1896 9 NaN NaN NaN NaN NaN NaN 16.025 -0.848 1896 10 NaN NaN NaN NaN NaN NaN 11.815 1.234 1896 11 NaN NaN NaN NaN NaN NaN 3.470 -0.445 1896 12 NaN NaN NaN NaN NaN NaN 2.378 2.810