% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 43298 % Primary Name: ST MATTHEW ISLAND ALASKA % Record Type: TAVG % Country: United States % State: AK % Latitude: 60.35000 +/- 0.00500 % Longitude: -172.70000 +/- 0.00500 % Elevation (m): 29.00 +/- 0.05 % # of Months: 28 % % IDs: gsod - 749231-99999 % usaf - 749231 % % Sources: Global Summary of the Day % % Site Hash: e84b087172124e870f661e3b27b3f86c % Raw Data Hash: 0677bb35bbb975baaf955eca20d49a9e % Adj Data Hash: e459a83ef7ffcc81b1015f214b68020f % % 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 1941 10 NaN NaN NaN NaN NaN NaN 3.147 1.809 1941 11 NaN NaN NaN NaN NaN NaN 0.769 2.197 1941 12 NaN NaN NaN NaN NaN NaN -5.401 1.242 1942 1 NaN NaN NaN NaN NaN NaN -1.807 6.174 1942 2 NaN NaN NaN NaN NaN NaN -6.534 4.645 1942 3 NaN NaN NaN NaN NaN NaN -9.401 0.475 1942 4 NaN NaN NaN NaN NaN NaN -2.882 3.401 1942 5 NaN NaN NaN NaN NaN NaN 0.071 0.916 1942 6 NaN NaN NaN NaN NaN NaN 2.856 -0.145 1942 7 NaN NaN NaN NaN NaN NaN 6.481 -0.434 1942 8 NaN NaN NaN NaN NaN NaN 8.639 0.489 1942 9 NaN NaN NaN NaN NaN NaN 7.719 1.627 1942 10 1.654 0.658 1 0 NaN NaN 0.851 -0.487 1942 11 -1.785 -0.015 0 0 -1.785 -0.015 -1.465 -0.037 1942 12 -12.124 -5.137 0 0 -12.124 -5.137 -12.345 -5.702 1943 1 -12.468 -4.144 0 0 -12.468 -4.144 -10.282 -2.301 1943 2 -14.379 -2.858 0 0 -14.379 -2.858 -12.657 -1.479 1943 3 -6.509 3.710 0 0 -6.509 3.710 -7.520 2.357 1943 4 -5.609 1.016 0 0 -5.609 1.016 -6.227 0.056 1943 5 0.909 2.096 0 0 0.909 2.096 1.001 1.846 1943 6 5.015 2.357 0 0 5.015 2.357 4.628 1.627 1943 7 7.572 0.999 0 0 7.572 0.999 7.379 0.464 1943 8 8.636 0.828 0 0 8.636 0.828 8.712 0.562 1943 9 8.796 3.047 1 0 NaN NaN 5.404 -0.688 1943 10 NaN NaN NaN NaN NaN NaN 2.226 0.888 1943 11 NaN NaN NaN NaN NaN NaN 1.175 2.602 1943 12 NaN NaN NaN NaN NaN NaN -8.852 -2.209 1944 1 NaN NaN NaN NaN NaN NaN -10.322 -2.341 1944 2 NaN NaN NaN NaN NaN NaN -9.086 2.092 1944 3 NaN NaN NaN NaN NaN NaN -10.970 -1.094 1944 4 NaN NaN NaN NaN NaN NaN -7.749 -1.466 1944 5 NaN NaN NaN NaN NaN NaN -0.885 -0.041 1944 6 NaN NaN NaN NaN NaN NaN 2.525 -0.475 1944 7 6.432 -0.141 0 0 6.432 -0.141 6.680 -0.235 1944 8 7.885 0.078 0 0 7.885 0.078 8.247 0.096 1944 9 6.420 0.671 0 0 6.420 0.671 6.628 0.536 1944 10 1.955 0.960 0 0 1.955 0.960 1.801 0.463 1944 11 -3.028 -1.258 0 0 -3.028 -1.258 -1.716 -0.289 1944 12 -5.767 1.219 0 0 -5.767 1.219 -5.651 0.993 1945 1 -8.362 -0.038 0 0 -8.362 -0.038 -5.295 2.686 1945 2 -11.149 0.372 0 0 -11.149 0.372 -10.259 0.919 1945 3 -15.679 -5.460 0 0 -15.679 -5.460 -14.701 -4.824 1945 4 -3.869 2.757 0 0 -3.869 2.757 -4.599 1.684 1945 5 -1.351 -0.164 0 0 -1.351 -0.164 -1.220 -0.375 1945 6 3.248 0.591 0 0 3.248 0.591 2.743 -0.257 1945 7 6.939 0.366 0 0 6.939 0.366 7.078 0.162 1945 8 8.500 0.692 0 0 8.500 0.692 8.517 0.366 1945 9 6.550 0.801 0 0 6.550 0.801 7.076 0.984 1945 10 2.973 1.978 1 0 NaN NaN 0.176 -1.162 1945 11 NaN NaN NaN NaN NaN NaN -2.563 -1.136 1945 12 NaN NaN NaN NaN NaN NaN -7.876 -1.232 1946 1 NaN NaN NaN NaN NaN NaN -5.789 2.192 1946 2 NaN NaN NaN NaN NaN NaN -14.376 -3.198 1946 3 NaN NaN NaN NaN NaN NaN -16.557 -6.680 1946 4 NaN NaN NaN NaN NaN NaN -7.953 -1.670 1946 5 NaN NaN NaN NaN NaN NaN -1.329 -0.484 1946 6 NaN NaN NaN NaN NaN NaN 1.729 -1.271 1946 7 NaN NaN NaN NaN NaN NaN 6.101 -0.815 1946 8 NaN NaN NaN NaN NaN NaN 6.743 -1.407 1946 9 NaN NaN NaN NaN NaN NaN 5.899 -0.192 1946 10 NaN NaN NaN NaN NaN NaN 2.388 1.050