% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 167757 % Primary Name: UMIAT AFS % Record Type: TAVG % Country: United States % State: AK % Latitude: 69.36670 +/- 0.00005 % Longitude: -152.13330 +/- 0.00005 % Elevation (m): 103.90 +/- 0.05 % # of Months: 15 % % IDs: ghcnd - USW00026537 % ncdc - 20022425 % wban - 26537 % % Sources: US First Order Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 45042a8ec1dc6bbce45321a64034393b % Raw Data Hash: 82894848fecc369b290bf6f7e650fa1e % Adj Data Hash: cba7ddcfa7a6fff23b701a70c3f4e592 % % 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 1952 7 NaN NaN NaN NaN NaN NaN 10.814 0.624 1952 8 NaN NaN NaN NaN NaN NaN 7.725 0.153 1952 9 NaN NaN NaN NaN NaN NaN -0.656 -1.040 1952 10 NaN NaN NaN NaN NaN NaN -9.167 2.112 1952 11 NaN NaN NaN NaN NaN NaN -15.643 5.503 1952 12 NaN NaN NaN NaN NaN NaN -27.263 1.355 1953 1 NaN NaN NaN NaN NaN NaN -31.151 -2.072 1953 2 NaN NaN NaN NaN NaN NaN -32.285 -1.397 1953 3 NaN NaN NaN NaN NaN NaN -28.650 -0.905 1953 4 NaN NaN NaN NaN NaN NaN -16.122 2.294 1953 5 NaN NaN NaN NaN NaN NaN -3.277 1.031 1953 6 NaN NaN NaN NaN NaN NaN 7.784 1.489 1953 7 10.168 0.532 0 0 10.168 0.532 9.967 -0.224 1953 8 5.992 -1.025 0 0 5.992 -1.025 6.563 -1.009 1953 9 1.178 1.349 0 0 1.178 1.349 1.686 1.302 1953 10 -12.315 -0.480 0 0 -12.315 -0.480 -12.569 -1.290 1953 11 -20.713 0.987 0 0 -20.713 0.987 -20.028 1.118 1953 12 -33.253 -4.081 0 0 -33.253 -4.081 -31.531 -2.914 1954 1 -30.616 -0.982 0 0 -30.616 -0.982 -29.906 -0.826 1954 2 -31.763 -0.320 1 0 NaN NaN -34.111 -3.223 1954 3 -22.578 5.723 1 0 NaN NaN -24.061 3.684 1954 4 -17.042 1.929 0 0 -17.042 1.929 -16.874 1.541 1954 5 -7.908 -3.046 0 0 -7.908 -3.046 -5.572 -1.265 1954 6 4.625 -1.115 0 0 4.625 -1.115 5.368 -0.927 1954 7 11.245 1.609 0 0 11.245 1.609 10.363 0.172 1954 8 12.950 5.933 1 0 NaN NaN 10.938 3.366 1954 9 NaN NaN NaN NaN NaN NaN 2.505 2.121 1954 10 NaN NaN NaN NaN NaN NaN -8.767 2.512 1954 11 NaN NaN NaN NaN NaN NaN -18.985 2.160 1954 12 NaN NaN NaN NaN NaN NaN -32.920 -4.303 1955 1 NaN NaN NaN NaN NaN NaN -26.848 2.231 1955 2 -47.284 -15.841 1 0 NaN NaN -36.598 -5.710 1955 3 NaN NaN NaN NaN NaN NaN -29.268 -1.522 1955 4 NaN NaN NaN NaN NaN NaN -20.156 -1.741 1955 5 NaN NaN NaN NaN NaN NaN -5.307 -1.000 1955 6 NaN NaN NaN NaN NaN NaN 5.339 -0.956 1955 7 NaN NaN NaN NaN NaN NaN 10.789 0.599 1955 8 NaN NaN NaN NaN NaN NaN 5.624 -1.947 1955 9 NaN NaN NaN NaN NaN NaN -0.094 -0.478 1955 10 NaN NaN NaN NaN NaN NaN -12.979 -1.699 1955 11 NaN NaN NaN NaN NaN NaN -26.185 -5.039 1955 12 NaN NaN NaN NaN NaN NaN -30.844 -2.227 1956 1 NaN NaN NaN NaN NaN NaN -31.202 -2.123 1956 2 NaN NaN NaN NaN NaN NaN -36.072 -5.184