% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 15655 % Primary Name: ZAWIDAN % Record Type: TAVG % Country: Iran % Latitude: 29.50000 +/- 0.00050 % Longitude: 60.88300 +/- 0.00050 % Elevation (m): 1438.40 +/- 0.05 % # of Months: 34 % % IDs: gsod - 408230-99999 % usaf - 408230 % % Sources: Global Summary of the Day % % Site Hash: fe8c405deea1626c0ceee4b14f1ebee7 % Raw Data Hash: 619bc8688e716d090611212ed8afd6c4 % Adj Data Hash: 1d756612e812ca9bad4df880c62750ad % % 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 1948 3 NaN NaN NaN NaN NaN NaN 15.801 -0.200 1948 4 NaN NaN NaN NaN NaN NaN 20.986 0.168 1948 5 NaN NaN NaN NaN NaN NaN 26.568 1.246 1948 6 NaN NaN NaN NaN NaN NaN 28.040 -0.760 1948 7 NaN NaN NaN NaN NaN NaN 30.107 0.236 1948 8 NaN NaN NaN NaN NaN NaN 27.490 -0.476 1948 9 NaN NaN NaN NaN NaN NaN 24.247 0.057 1948 10 NaN NaN NaN NaN NaN NaN 18.769 -0.339 1948 11 NaN NaN NaN NaN NaN NaN 12.387 -0.906 1948 12 NaN NaN NaN NaN NaN NaN 9.134 -0.024 1949 1 NaN NaN NaN NaN NaN NaN 5.243 -2.423 1949 2 NaN NaN NaN NaN NaN NaN 10.566 -0.205 1949 3 16.394 -1.297 0 0 16.394 -1.297 15.319 -0.683 1949 4 21.494 -1.012 0 0 21.494 -1.012 20.659 -0.159 1949 5 28.627 1.615 0 0 28.627 1.615 26.309 0.986 1949 6 26.007 -4.481 0 0 26.007 -4.481 26.785 -2.015 1949 7 29.548 -2.011 0 0 29.548 -2.011 29.336 -0.534 1949 8 27.138 -2.517 0 0 27.138 -2.517 26.528 -1.439 1949 9 26.556 0.677 0 0 26.556 0.677 24.477 0.288 1949 10 19.270 -1.527 0 0 19.270 -1.527 17.004 -2.104 1949 11 12.917 -2.066 0 0 12.917 -2.066 10.622 -2.671 1949 12 10.507 -0.339 0 0 10.507 -0.339 9.236 0.079 1950 1 9.572 0.217 0 0 9.572 0.217 7.358 -0.308 1950 2 10.157 -2.303 0 0 10.157 -2.303 8.018 -2.753 1950 3 15.927 -1.764 0 0 15.927 -1.764 14.677 -1.324 1950 4 20.894 -1.612 0 0 20.894 -1.612 18.681 -2.137 1950 5 27.616 0.605 0 0 27.616 0.605 25.372 0.050 1950 6 31.557 1.069 0 0 31.557 1.069 28.915 0.115 1950 7 33.402 1.843 0 0 33.402 1.843 30.679 0.809 1950 8 31.602 1.947 0 0 31.602 1.947 28.745 0.779 1950 9 25.504 -0.375 0 0 25.504 -0.375 23.278 -0.912 1950 10 23.276 2.478 0 0 23.276 2.478 20.300 1.191 1950 11 13.876 -1.106 0 0 13.876 -1.106 11.437 -1.856 1950 12 7.984 -2.863 0 0 7.984 -2.863 6.650 -2.507 1951 1 10.194 0.839 0 0 10.194 0.839 8.485 0.819 1951 2 10.558 -1.903 0 0 10.558 -1.903 9.287 -1.485 1951 3 14.573 -3.117 0 0 14.573 -3.117 14.076 -1.926 1951 4 20.289 -2.218 0 0 20.289 -2.218 19.022 -1.796 1951 5 26.921 -0.091 0 0 26.921 -0.091 24.958 -0.365 1951 6 28.557 -1.931 0 0 28.557 -1.931 26.815 -1.984 1951 7 30.616 -0.943 0 0 30.616 -0.943 28.803 -1.067 1951 8 29.348 -0.308 0 0 29.348 -0.308 27.353 -0.613 1951 9 27.385 1.507 0 0 27.385 1.507 25.485 1.295 1951 10 24.581 3.783 0 0 24.581 3.783 22.455 3.346 1951 11 15.093 0.110 0 0 15.093 0.110 13.753 0.460 1951 12 11.360 0.514 0 0 11.360 0.514 10.995 1.838 1952 1 NaN NaN NaN NaN NaN NaN 7.375 -0.290 1952 2 NaN NaN NaN NaN NaN NaN 12.681 1.910 1952 3 NaN NaN NaN NaN NaN NaN 16.986 0.984 1952 4 NaN NaN NaN NaN NaN NaN 21.756 0.938 1952 5 NaN NaN NaN NaN NaN NaN 24.906 -0.417 1952 6 NaN NaN NaN NaN NaN NaN 28.603 -0.196 1952 7 NaN NaN NaN NaN NaN NaN 28.926 -0.944 1952 8 NaN NaN NaN NaN NaN NaN 26.856 -1.110 1952 9 NaN NaN NaN NaN NaN NaN 22.953 -1.236 1952 10 NaN NaN NaN NaN NaN NaN 17.454 -1.655 1952 11 NaN NaN NaN NaN NaN NaN 12.611 -0.682 1952 12 NaN NaN NaN NaN NaN NaN 9.019 -0.138