% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 43130 % Primary Name: WIDE BAY % Record Type: TAVG % Country: United States % State: AK % Latitude: 57.36670 +/- 0.00005 % Longitude: -156.41670 +/- 0.00005 % Elevation (m): 6.10 +/- 0.05 % # of Months: 9 % % IDs: coop - 509845 % ghcnd - USC00509845 % ncdc - 20021849 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 4c67def79e1a274b89bcfca04879397f % Raw Data Hash: ff0ca259b129ff38c3d629e52b704210 % Adj Data Hash: 1152801d228ab7c323789e8006c50e4d % % 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 1962 2 NaN NaN NaN NaN NaN NaN -1.750 4.032 1962 3 NaN NaN NaN NaN NaN NaN -4.617 -0.442 1962 4 NaN NaN NaN NaN NaN NaN -0.113 -0.043 1962 5 NaN NaN NaN NaN NaN NaN 4.478 -0.620 1962 6 NaN NaN NaN NaN NaN NaN 8.621 -0.290 1962 7 NaN NaN NaN NaN NaN NaN 12.639 1.218 1962 8 NaN NaN NaN NaN NaN NaN 12.471 0.830 1962 9 NaN NaN NaN NaN NaN NaN 8.107 -0.671 1962 10 NaN NaN NaN NaN NaN NaN 2.054 -0.286 1962 11 NaN NaN NaN NaN NaN NaN -0.596 1.565 1962 12 NaN NaN NaN NaN NaN NaN -7.285 -0.673 1963 1 NaN NaN NaN NaN NaN NaN -1.966 4.477 1963 2 1.216 7.033 1 0 NaN NaN -4.664 1.117 1963 3 -1.611 2.600 0 0 -1.611 2.600 -2.287 1.888 1963 4 -0.889 -0.784 0 0 -0.889 -0.784 -1.328 -1.258 1963 5 5.111 0.049 0 0 5.111 0.049 5.484 0.386 1963 6 7.500 -1.375 0 0 7.500 -1.375 8.143 -0.768 1963 7 11.667 0.282 0 0 11.667 0.282 11.582 0.161 1963 8 11.222 -0.383 0 0 11.222 -0.383 11.831 0.190 1963 9 10.778 2.036 0 0 10.778 2.036 10.603 1.826 1963 10 4.533 2.230 1 0 NaN NaN 1.268 -1.071 1963 11 NaN NaN NaN NaN NaN NaN -6.749 -4.589 1963 12 NaN NaN NaN NaN NaN NaN -2.961 3.652 1964 1 NaN NaN NaN NaN NaN NaN -5.298 1.146 1964 2 NaN NaN NaN NaN NaN NaN -6.832 -1.051 1964 3 NaN NaN NaN NaN NaN NaN -5.545 -1.369 1964 4 NaN NaN NaN NaN NaN NaN -1.081 -1.012 1964 5 NaN NaN NaN NaN NaN NaN 3.706 -1.392 1964 6 NaN NaN NaN NaN NaN NaN 9.819 0.908 1964 7 NaN NaN NaN NaN NaN NaN 10.994 -0.427 1964 8 NaN NaN NaN NaN NaN NaN 10.796 -0.845 1964 9 NaN NaN NaN NaN NaN NaN 9.466 0.688 1964 10 NaN NaN NaN NaN NaN NaN 2.559 0.220