% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 12083 % Primary Name: SHAHIDULLAH HAZAR /SAI-TU-LA % Record Type: TAVG % Country: China % Latitude: 36.33300 +/- 0.00050 % Longitude: 78.00000 +/- 0.00050 % Elevation (m): 3699.10 +/- 0.05 % # of Months: 11 % % IDs: gsod - 519150-99999 % usaf - 519150 % % Sources: Global Summary of the Day % % Site Hash: b2e82583bf68b727ba3853a836327fca % Raw Data Hash: 641073028e4a2e6e8d5d891f6c9bf845 % Adj Data Hash: ca7d07d59b769c574414a4b1d5dff3cb % % 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 1956 7 NaN NaN NaN NaN NaN NaN 7.584 0.854 1956 8 NaN NaN NaN NaN NaN NaN 5.696 -0.120 1956 9 NaN NaN NaN NaN NaN NaN 2.883 1.353 1956 10 NaN NaN NaN NaN NaN NaN -5.547 -0.191 1956 11 NaN NaN NaN NaN NaN NaN -11.904 0.223 1956 12 NaN NaN NaN NaN NaN NaN -17.944 0.160 1957 1 NaN NaN NaN NaN NaN NaN -21.027 -0.217 1957 2 NaN NaN NaN NaN NaN NaN -19.928 -2.659 1957 3 NaN NaN NaN NaN NaN NaN -9.821 0.333 1957 4 NaN NaN NaN NaN NaN NaN -5.253 -1.562 1957 5 NaN NaN NaN NaN NaN NaN -1.139 -1.747 1957 6 NaN NaN NaN NaN NaN NaN 3.610 -1.170 1957 7 12.980 -2.220 0 0 12.980 -2.220 5.629 -1.101 1957 8 12.135 -2.152 0 0 12.135 -2.152 4.288 -1.528 1957 9 6.606 -3.395 0 0 6.606 -3.395 -0.008 -1.538 1957 10 1.458 -1.657 0 0 1.458 -1.657 -6.390 -1.035 1957 11 -2.739 0.917 0 0 -2.739 0.917 -11.619 0.507 1957 12 -6.826 2.808 0 0 -6.826 2.808 -16.713 1.391 1958 1 -7.032 5.307 0 0 -7.032 5.307 -18.295 2.515 1958 2 -7.645 1.154 1 0 NaN NaN -16.326 0.943 1958 3 -0.654 1.030 0 0 -0.654 1.030 -8.913 1.241 1958 4 6.456 1.677 0 0 6.456 1.677 -1.828 1.863 1958 5 6.743 -2.336 1 0 NaN NaN -1.333 -1.941 1958 6 NaN NaN NaN NaN NaN NaN 4.492 -0.288 1958 7 NaN NaN NaN NaN NaN NaN 7.189 0.459 1958 8 NaN NaN NaN NaN NaN NaN 4.334 -1.482 1958 9 NaN NaN NaN NaN NaN NaN 2.110 0.581 1958 10 NaN NaN NaN NaN NaN NaN -5.608 -0.253 1958 11 NaN NaN NaN NaN NaN NaN -12.236 -0.110 1958 12 NaN NaN NaN NaN NaN NaN -16.437 1.668 1959 1 NaN NaN NaN NaN NaN NaN -20.776 0.033 1959 2 NaN NaN NaN NaN NaN NaN -17.730 -0.460 1959 3 NaN NaN NaN NaN NaN NaN -10.240 -0.085 1959 4 NaN NaN NaN NaN NaN NaN -2.477 1.214 1959 5 NaN NaN NaN NaN NaN NaN -1.508 -2.116