% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 30674 % Primary Name: SHONGOPOVI % Record Type: TAVG % Country: United States % State: AZ % Latitude: 35.80000 +/- 0.00005 % Longitude: -110.53330 +/- 0.00005 % Elevation (m): 1866.90 +/- 0.05 % # of Months: 18 % % IDs: coop - 27829 % ghcnd - USC00027829 % ncdc - 20001283 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: e585a25ba9b1f00cb6c31bea28762645 % Raw Data Hash: 01a2cdc62f71527987060fdcde11ad5f % Adj Data Hash: cdfa455a2b17ee4f33a7a8c18619464d % % 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 1956 10 NaN NaN NaN NaN NaN NaN 12.854 0.348 1956 11 NaN NaN NaN NaN NaN NaN 2.964 -2.078 1956 12 NaN NaN NaN NaN NaN NaN -0.008 0.095 1957 1 NaN NaN NaN NaN NaN NaN 0.370 0.967 1957 2 NaN NaN NaN NaN NaN NaN 5.942 3.281 1957 3 NaN NaN NaN NaN NaN NaN 6.429 0.473 1957 4 NaN NaN NaN NaN NaN NaN 9.106 -1.136 1957 5 NaN NaN NaN NaN NaN NaN 12.579 -2.863 1957 6 NaN NaN NaN NaN NaN NaN 21.193 0.206 1957 7 NaN NaN NaN NaN NaN NaN 24.162 -0.318 1957 8 NaN NaN NaN NaN NaN NaN 22.475 -0.621 1957 9 NaN NaN NaN NaN NaN NaN 19.321 0.225 1957 10 10.087 -4.353 1 0 NaN NaN 11.857 -0.649 1957 11 4.111 -2.865 0 0 4.111 -2.865 2.702 -2.340 1957 12 4.722 2.890 0 0 4.722 2.890 1.964 2.066 1958 1 2.944 1.607 0 0 2.944 1.607 0.429 1.026 1958 2 6.500 1.904 0 0 6.500 1.904 5.193 2.532 1958 3 4.722 -3.168 0 0 4.722 -3.168 3.302 -2.654 1958 4 10.444 -1.732 0 0 10.444 -1.732 9.197 -1.045 1958 5 19.667 2.290 0 0 19.667 2.290 17.477 2.035 1958 6 NaN NaN NaN NaN NaN NaN 22.072 1.085 1958 7 24.889 -1.526 0 0 24.889 -1.526 24.623 0.143 1958 8 25.278 0.247 0 0 25.278 0.247 24.452 1.356 1958 9 20.722 -0.309 0 0 20.722 -0.309 19.196 0.100 1958 10 15.611 1.170 0 0 15.611 1.170 13.701 1.195 1958 11 7.222 0.246 0 0 7.222 0.246 4.935 -0.107 1958 12 6.778 4.946 0 0 6.778 4.946 3.375 3.477 1959 1 4.444 3.107 0 0 4.444 3.107 1.091 1.688 1959 2 4.333 -0.263 0 0 4.333 -0.263 2.048 -0.613 1959 3 8.556 0.665 0 0 8.556 0.665 6.022 0.067 1959 4 13.611 1.434 0 0 13.611 1.434 11.961 1.719 1959 5 NaN NaN NaN NaN NaN NaN 14.775 -0.667 1959 6 NaN NaN NaN NaN NaN NaN 22.308 1.321 1959 7 NaN NaN NaN NaN NaN NaN 25.962 1.482 1959 8 NaN NaN NaN NaN NaN NaN 22.496 -0.599 1959 9 NaN NaN NaN NaN NaN NaN 19.136 0.040 1959 10 NaN NaN NaN NaN NaN NaN 12.959 0.453 1959 11 NaN NaN NaN NaN NaN NaN 5.308 0.266 1959 12 NaN NaN NaN NaN NaN NaN 1.431 1.534 1960 1 NaN NaN NaN NaN NaN NaN -2.827 -2.230 1960 2 NaN NaN NaN NaN NaN NaN 0.949 -1.712 1960 3 NaN NaN NaN NaN NaN NaN 7.989 2.033 1960 4 NaN NaN NaN NaN NaN NaN 11.407 1.165