% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 43005 % Primary Name: KISKA ISLAND ALEUTIAN IS % Record Type: TAVG % Country: United States % State: AK % Latitude: 51.98300 +/- 0.00050 % Longitude: 177.55000 +/- 0.00050 % Elevation (m): 91.00 +/- 0.05 % # of Months: 26 % % IDs: gsod - 749392-99999 % usaf - 749392 % % Sources: Global Summary of the Day % % Site Hash: d41d4ef0f10206474e9121902baf7be1 % Raw Data Hash: 233469471b152b92d148559931b6fa28 % Adj Data Hash: b098f22dd5de96f42048601b5537ddec % % 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 1942 9 NaN NaN NaN NaN NaN NaN 8.907 0.423 1942 10 NaN NaN NaN NaN NaN NaN 5.716 0.220 1942 11 NaN NaN NaN NaN NaN NaN 4.074 1.011 1942 12 NaN NaN NaN NaN NaN NaN 1.249 -0.116 1943 1 NaN NaN NaN NaN NaN NaN 2.356 1.250 1943 2 NaN NaN NaN NaN NaN NaN 0.835 0.406 1943 3 NaN NaN NaN NaN NaN NaN 2.437 1.423 1943 4 NaN NaN NaN NaN NaN NaN 1.336 -0.643 1943 5 NaN NaN NaN NaN NaN NaN 4.067 0.190 1943 6 NaN NaN NaN NaN NaN NaN 6.415 0.428 1943 7 NaN NaN NaN NaN NaN NaN 8.548 0.292 1943 8 NaN NaN NaN NaN NaN NaN 10.413 0.926 1943 9 8.383 0.541 1 0 NaN NaN 8.440 -0.044 1943 10 6.057 1.203 0 0 6.057 1.203 6.059 0.562 1943 11 1.619 -0.802 0 0 1.619 -0.802 2.281 -0.781 1943 12 -0.582 -1.305 0 0 -0.582 -1.305 0.153 -1.212 1944 1 -1.713 -2.177 0 0 -1.713 -2.177 -0.374 -1.480 1944 2 -0.836 -0.622 1 0 NaN NaN -0.215 -0.644 1944 3 0.108 -0.264 0 0 0.108 -0.264 0.763 -0.251 1944 4 0.813 -0.524 0 0 0.813 -0.524 1.357 -0.622 1944 5 2.973 -0.261 0 0 2.973 -0.261 3.583 -0.294 1944 6 5.835 0.490 0 0 5.835 0.490 6.204 0.217 1944 7 7.118 -0.495 1 0 NaN NaN 7.837 -0.419 1944 8 8.962 0.117 0 0 8.962 0.117 9.203 -0.285 1944 9 7.585 -0.257 0 0 7.585 -0.257 8.264 -0.220 1944 10 6.050 1.196 0 0 6.050 1.196 6.086 0.590 1944 11 3.098 0.678 0 0 3.098 0.678 3.928 0.865 1944 12 0.557 -0.165 0 0 0.557 -0.165 1.483 0.118 1945 1 -0.278 -0.742 0 0 -0.278 -0.742 1.106 -0.000 1945 2 -0.220 -0.006 1 0 NaN NaN 0.481 0.052 1945 3 -0.892 -1.264 0 0 -0.892 -1.264 -0.255 -1.269 1945 4 2.530 1.193 0 0 2.530 1.193 3.093 1.113 1945 5 3.595 0.360 0 0 3.595 0.360 4.487 0.610 1945 6 5.244 -0.100 0 0 5.244 -0.100 6.155 0.168 1945 7 7.778 0.165 0 0 7.778 0.165 8.225 -0.031 1945 8 8.991 0.146 0 0 8.991 0.146 9.411 -0.076 1945 9 8.067 0.225 0 0 8.067 0.225 8.674 0.189 1945 10 6.102 1.248 1 0 NaN NaN 4.967 -0.530 1945 11 NaN NaN NaN NaN NaN NaN 4.018 0.955 1945 12 NaN NaN NaN NaN NaN NaN 2.050 0.685 1946 1 NaN NaN NaN NaN NaN NaN 0.863 -0.244 1946 2 NaN NaN NaN NaN NaN NaN -0.474 -0.903 1946 3 NaN NaN NaN NaN NaN NaN -0.608 -1.622 1946 4 NaN NaN NaN NaN NaN NaN 1.976 -0.003 1946 5 NaN NaN NaN NaN NaN NaN 3.196 -0.681 1946 6 NaN NaN NaN NaN NaN NaN 5.569 -0.418 1946 7 NaN NaN NaN NaN NaN NaN 7.513 -0.743 1946 8 NaN NaN NaN NaN NaN NaN 9.356 -0.131 1946 9 NaN NaN NaN NaN NaN NaN 9.044 0.560 1946 10 NaN NaN NaN NaN NaN NaN 5.656 0.160