% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 43508 % Primary Name: STUYAHOK % Record Type: TAVG % Country: United States % State: AK % Latitude: 62.16670 +/- 0.00005 % Longitude: -161.83330 +/- 0.00005 % Elevation (m): 25.84 +/- 10.00 % # of Months: 21 % % Alternate Names: Missing Station ID - 508785 % % IDs: coop - 508785 % ghcnd - USC00508785 % ncdc - 20022168 % ncdc - 30015307 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 61fa86bc31d58e92319c45e433c40ef2 % Raw Data Hash: 7b802d4082a8d7638bd764b569029d16 % Adj Data Hash: 5cf623289ede218747b02381aa071046 % % 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 1937 7 NaN NaN NaN NaN NaN NaN 13.577 1.056 1937 8 NaN NaN NaN NaN NaN NaN 11.027 -0.139 1937 9 NaN NaN NaN NaN NaN NaN 8.634 2.097 1937 10 NaN NaN NaN NaN NaN NaN 0.429 2.804 1937 11 NaN NaN NaN NaN NaN NaN -5.423 4.134 1937 12 NaN NaN NaN NaN NaN NaN -15.829 1.130 1938 1 NaN NaN NaN NaN NaN NaN -21.897 -5.458 1938 2 NaN NaN NaN NaN NaN NaN -18.104 -2.793 1938 3 NaN NaN NaN NaN NaN NaN -10.753 0.963 1938 4 NaN NaN NaN NaN NaN NaN 1.820 6.236 1938 5 NaN NaN NaN NaN NaN NaN 6.138 1.165 1938 6 NaN NaN NaN NaN NaN NaN 10.792 0.346 1938 7 13.789 2.123 0 0 13.789 2.123 13.020 0.499 1938 8 11.503 1.192 0 0 11.503 1.192 11.680 0.514 1938 9 5.837 0.155 0 0 5.837 0.155 6.775 0.238 1938 10 1.276 4.506 0 0 1.276 4.506 1.260 3.635 1938 11 -7.208 3.204 0 0 -7.208 3.204 -5.351 4.206 1938 12 -14.870 2.944 0 0 -14.870 2.944 -14.156 2.803 1939 1 -23.529 -6.235 0 0 -23.529 -6.235 -22.278 -5.839 1939 2 -12.914 3.251 1 0 NaN NaN -11.196 4.115 1939 3 -13.281 -0.710 0 0 -13.281 -0.710 -14.539 -2.823 1939 4 NaN NaN NaN NaN NaN NaN -3.212 1.204 1939 5 2.416 -1.701 0 0 2.416 -1.701 3.102 -1.871 1939 6 9.735 0.144 0 0 9.735 0.144 10.731 0.285 1939 7 9.018 -2.648 0 0 9.018 -2.648 11.998 -0.522 1939 8 7.848 -2.463 0 0 7.848 -2.463 10.461 -0.705 1939 9 4.737 -0.945 0 0 4.737 -0.945 6.657 0.121 1939 10 -4.679 -1.449 0 0 -4.679 -1.449 -4.029 -1.653 1939 11 -17.620 -7.208 0 0 -17.620 -7.208 -16.022 -6.465 1939 12 -17.378 0.436 0 0 -17.378 0.436 -18.211 -1.251 1940 1 -12.742 4.552 0 0 -12.742 4.552 -12.255 4.184 1940 2 NaN NaN NaN NaN NaN NaN -12.526 2.785 1940 3 -11.167 1.404 1 0 NaN NaN -11.394 0.322 1940 4 2.105 7.375 0 0 2.105 7.375 3.498 7.913 1940 5 6.998 2.880 1 0 NaN NaN 8.424 3.451 1940 6 NaN NaN NaN NaN NaN NaN 13.062 2.617 1940 7 NaN NaN NaN NaN NaN NaN 13.133 0.612 1940 8 NaN NaN NaN NaN NaN NaN 12.478 1.312 1940 9 NaN NaN NaN NaN NaN NaN 7.182 0.646 1940 10 NaN NaN NaN NaN NaN NaN -1.566 0.809 1940 11 NaN NaN NaN NaN NaN NaN -5.019 4.538 1940 12 NaN NaN NaN NaN NaN NaN -15.608 1.352 1941 1 NaN NaN NaN NaN NaN NaN -20.654 -4.215 1941 2 NaN NaN NaN NaN NaN NaN -9.705 5.606 1941 3 NaN NaN NaN NaN NaN NaN -11.088 0.628 1941 4 NaN NaN NaN NaN NaN NaN -1.148 3.267 1941 5 NaN NaN NaN NaN NaN NaN 5.436 0.464