% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 2656 % Primary Name: IN AMGUEL % Record Type: TAVG % Country: Algeria % Latitude: 23.81700 +/- 0.00050 % Longitude: 5.15000 +/- 0.00050 % Elevation (m): 1006.10 +/- 0.05 % # of Months: 29 % % IDs: gsod - 606780-99999 % usaf - 606780 % % Sources: Global Summary of the Day % % Site Hash: f430d383aba69096b99b510180b74843 % Raw Data Hash: cb8dff28f30fa09a5f0efcb5900d6b88 % Adj Data Hash: 7ad4588c4288aedc3cf20ab50c883857 % % 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 1963 10 NaN NaN NaN NaN NaN NaN 24.104 -1.589 1963 11 NaN NaN NaN NaN NaN NaN 20.075 -0.354 1963 12 NaN NaN NaN NaN NaN NaN 17.482 1.531 1964 1 NaN NaN NaN NaN NaN NaN 15.323 0.140 1964 2 NaN NaN NaN NaN NaN NaN 17.876 0.111 1964 3 NaN NaN NaN NaN NaN NaN 23.401 2.253 1964 4 NaN NaN NaN NaN NaN NaN 24.197 -0.835 1964 5 NaN NaN NaN NaN NaN NaN 28.764 -0.399 1964 6 NaN NaN NaN NaN NaN NaN 32.207 -0.243 1964 7 NaN NaN NaN NaN NaN NaN 32.632 -0.132 1964 8 NaN NaN NaN NaN NaN NaN 32.068 -0.032 1964 9 NaN NaN NaN NaN NaN NaN 28.687 -1.477 1964 10 21.323 -3.888 1 0 NaN NaN 24.396 -1.297 1964 11 17.611 -2.336 1 0 NaN NaN 18.984 -1.444 1964 12 18.621 3.151 1 0 NaN NaN 16.623 0.672 1965 1 17.243 2.541 1 0 NaN NaN 16.234 1.051 1965 2 14.819 -2.465 1 0 NaN NaN 18.532 0.767 1965 3 19.571 -1.095 1 0 NaN NaN 21.196 0.048 1965 4 22.358 -2.193 1 0 NaN NaN 22.816 -2.217 1965 5 30.118 1.435 1 0 NaN NaN 28.818 -0.346 1965 6 24.956 -7.013 1 0 NaN NaN 30.711 -1.740 1965 7 30.631 -1.653 1 0 NaN NaN 32.228 -0.536 1965 8 30.431 -1.188 1 0 NaN NaN 31.178 -0.923 1965 9 28.909 -0.774 1 0 NaN NaN 30.007 -0.157 1965 10 27.734 2.522 1 0 NaN NaN 27.083 1.390 1965 11 20.500 0.553 1 0 NaN NaN 20.631 0.203 1965 12 14.787 -0.683 1 0 NaN NaN 15.749 -0.202 1966 1 16.459 1.756 1 0 NaN NaN 17.152 1.969 1966 2 18.704 1.420 1 0 NaN NaN 19.590 1.824 1966 3 19.744 -0.923 0 0 19.744 -0.923 20.017 -1.131 1966 4 25.450 0.899 0 0 25.450 0.899 25.396 0.363 1966 5 27.278 -1.405 0 0 27.278 -1.405 27.828 -1.336 1966 6 32.230 0.261 0 0 32.230 0.261 33.189 0.738 1966 7 32.754 0.471 0 0 32.754 0.471 33.121 0.356 1966 8 32.004 0.384 0 0 32.004 0.384 32.131 0.031 1966 9 29.318 -0.365 0 0 29.318 -0.365 29.942 -0.222 1966 10 24.657 -0.554 0 0 24.657 -0.554 25.553 -0.139 1966 11 19.973 0.026 0 0 19.973 0.026 20.562 0.133 1966 12 15.261 -0.209 1 0 NaN NaN 15.959 0.008 1967 1 12.308 -2.395 1 0 NaN NaN 13.829 -1.354 1967 2 16.551 -0.733 1 0 NaN NaN 18.336 0.571 1967 3 NaN NaN NaN NaN NaN NaN 21.342 0.194 1967 4 NaN NaN NaN NaN NaN NaN 25.331 0.299 1967 5 NaN NaN NaN NaN NaN NaN 29.703 0.539 1967 6 NaN NaN NaN NaN NaN NaN 32.313 -0.138 1967 7 NaN NaN NaN NaN NaN NaN 31.176 -1.589 1967 8 NaN NaN NaN NaN NaN NaN 31.390 -0.710 1967 9 NaN NaN NaN NaN NaN NaN 30.714 0.550 1967 10 NaN NaN NaN NaN NaN NaN 25.145 -0.547 1967 11 NaN NaN NaN NaN NaN NaN 20.445 0.017 1967 12 NaN NaN NaN NaN NaN NaN 14.949 -1.002 1968 1 NaN NaN NaN NaN NaN NaN 13.441 -1.743 1968 2 NaN NaN NaN NaN NaN NaN 19.126 1.361