% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 12033 % Primary Name: HSIA-HO /SIAHO % Record Type: TAVG % Country: China % Latitude: 35.23300 +/- 0.00050 % Longitude: 102.50000 +/- 0.00050 % Elevation (m): 3048.90 +/- 0.05 % # of Months: 21 % % IDs: gsod - 529780-99999 % usaf - 529780 % % Sources: Global Summary of the Day % % Site Hash: 9c21ca1bc38935a932fbe459dedb681d % Raw Data Hash: 1aa7a4554d1960f012a9cb665b8052d0 % Adj Data Hash: efb9e0297f05ad1ec11644d1b7c813f0 % % 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 1955 8 NaN NaN NaN NaN NaN NaN 12.566 0.536 1955 9 NaN NaN NaN NaN NaN NaN 8.639 0.498 1955 10 NaN NaN NaN NaN NaN NaN 3.368 0.540 1955 11 NaN NaN NaN NaN NaN NaN -3.657 -0.477 1955 12 NaN NaN NaN NaN NaN NaN -6.989 1.335 1956 1 NaN NaN NaN NaN NaN NaN -11.248 -1.413 1956 2 NaN NaN NaN NaN NaN NaN -6.324 0.508 1956 3 NaN NaN NaN NaN NaN NaN -0.590 0.749 1956 4 NaN NaN NaN NaN NaN NaN 4.389 0.955 1956 5 NaN NaN NaN NaN NaN NaN 6.436 -0.728 1956 6 NaN NaN NaN NaN NaN NaN 9.705 -0.291 1956 7 NaN NaN NaN NaN NaN NaN 11.165 -1.236 1956 8 8.889 -2.981 1 0 NaN NaN 10.727 -1.303 1956 9 8.015 0.034 1 0 NaN NaN 8.406 0.265 1956 10 1.061 -1.609 1 0 NaN NaN 2.283 -0.546 1956 11 -6.885 -3.545 0 0 -6.885 -3.545 -4.471 -1.290 1956 12 -10.378 -1.895 0 0 -10.378 -1.895 -9.520 -1.196 1957 1 -8.846 1.149 0 0 -8.846 1.149 -9.216 0.619 1957 2 -9.331 -2.339 0 0 -9.331 -2.339 -9.158 -2.326 1957 3 -2.097 -0.599 0 0 -2.097 -0.599 -1.015 0.324 1957 4 3.300 0.025 0 0 3.300 0.025 3.395 -0.040 1957 5 6.289 -0.716 0 0 6.289 -0.716 5.793 -1.371 1957 6 9.944 0.108 1 0 NaN NaN 9.167 -0.829 1957 7 12.898 0.656 0 0 12.898 0.656 11.897 -0.504 1957 8 12.328 0.458 0 0 12.328 0.458 12.065 0.036 1957 9 7.466 -0.516 0 0 7.466 -0.516 6.958 -1.183 1957 10 0.823 -1.846 0 0 0.823 -1.846 1.179 -1.649 1957 11 -2.978 0.362 0 0 -2.978 0.362 -2.635 0.546 1957 12 -6.882 1.602 0 0 -6.882 1.602 -7.007 1.317 1958 1 -9.719 0.276 0 0 -9.719 0.276 -9.812 0.023 1958 2 -7.617 -0.625 0 0 -7.617 -0.625 -7.696 -0.863 1958 3 0.086 1.584 0 0 0.086 1.584 0.250 1.589 1958 4 3.512 0.236 1 0 NaN NaN 5.477 2.043 1958 5 NaN NaN NaN NaN NaN NaN 7.381 0.218 1958 6 NaN NaN NaN NaN NaN NaN 10.210 0.214 1958 7 NaN NaN NaN NaN NaN NaN 13.247 0.846 1958 8 NaN NaN NaN NaN NaN NaN 11.341 -0.688 1958 9 NaN NaN NaN NaN NaN NaN 8.342 0.201 1958 10 NaN NaN NaN NaN NaN NaN 2.481 -0.347 1958 11 NaN NaN NaN NaN NaN NaN -2.340 0.840 1958 12 NaN NaN NaN NaN NaN NaN -7.475 0.849 1959 1 NaN NaN NaN NaN NaN NaN -10.053 -0.218 1959 2 NaN NaN NaN NaN NaN NaN -7.288 -0.456 1959 3 NaN NaN NaN NaN NaN NaN -1.066 0.272 1959 4 NaN NaN NaN NaN NaN NaN 4.344 0.910