% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 36254 % Primary Name: HUALAPAI VALLEY FITTS % Record Type: TAVG % Country: United States % State: NV % Latitude: 40.90000 +/- 0.00833 % Longitude: -119.30000 +/- 0.00833 % Elevation (m): 1260.00 +/- 0.05 % # of Months: 11 % % Alternate Names: HUALAPAI VALLEY FITT % % IDs: coop - 263816 % ghcnd - USC00263816 % ncdc - 20019269 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 8c5d644e4162cb8ccda9524c8e60ad62 % Raw Data Hash: 8768f068bec2fdf1dc62a22e77fd39a1 % Adj Data Hash: 8768f068bec2fdf1dc62a22e77fd39a1 % % 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 1968 3 NaN NaN NaN NaN NaN NaN 4.630 1.089 1968 4 NaN NaN NaN NaN NaN NaN 6.116 -1.023 1968 5 NaN NaN NaN NaN NaN NaN 12.157 -0.140 1968 6 NaN NaN NaN NaN NaN NaN 17.506 0.402 1968 7 NaN NaN NaN NaN NaN NaN 23.349 1.630 1968 8 NaN NaN NaN NaN NaN NaN 17.429 -2.961 1968 9 NaN NaN NaN NaN NaN NaN 15.797 -0.233 1968 10 NaN NaN NaN NaN NaN NaN 9.937 0.285 1968 11 NaN NaN NaN NaN NaN NaN 2.694 -0.195 1968 12 NaN NaN NaN NaN NaN NaN -2.298 -0.814 1969 1 NaN NaN NaN NaN NaN NaN -0.751 1.269 1969 2 NaN NaN NaN NaN NaN NaN -0.254 -1.512 1969 3 3.944 -0.392 0 0 3.944 -0.392 1.811 -1.730 1969 4 8.667 0.733 0 0 8.667 0.733 7.261 0.123 1969 5 15.444 2.352 0 0 15.444 2.352 14.829 2.532 1969 6 17.389 -0.511 0 0 17.389 -0.511 16.137 -0.968 1969 7 22.500 -0.014 0 0 22.500 -0.014 22.097 0.378 1969 8 21.000 -0.186 0 0 21.000 -0.186 20.841 0.450 1969 9 18.111 1.286 0 0 18.111 1.286 17.385 1.355 1969 10 7.333 -3.113 0 0 7.333 -3.113 6.999 -2.653 1969 11 3.222 -0.462 0 0 3.222 -0.462 2.948 0.059 1969 12 0.833 1.522 0 0 0.833 1.522 -0.279 1.205 1970 1 0.222 1.447 0 0 0.222 1.447 -0.108 1.912 1970 2 NaN NaN NaN NaN NaN NaN 4.370 3.111 1970 3 NaN NaN NaN NaN NaN NaN 2.935 -0.606 1970 4 NaN NaN NaN NaN NaN NaN 3.690 -3.448 1970 5 NaN NaN NaN NaN NaN NaN 12.715 0.418 1970 6 NaN NaN NaN NaN NaN NaN 17.060 -0.044 1970 7 NaN NaN NaN NaN NaN NaN 22.513 0.794 1970 8 NaN NaN NaN NaN NaN NaN 21.426 1.035 1970 9 NaN NaN NaN NaN NaN NaN 13.951 -2.079 1970 10 NaN NaN NaN NaN NaN NaN 8.161 -1.491 1970 11 NaN NaN NaN NaN NaN NaN 4.342 1.452 1970 12 NaN NaN NaN NaN NaN NaN -2.824 -1.340 1971 1 NaN NaN NaN NaN NaN NaN -0.129 1.891