% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 17283 % Primary Name: PHU CUM % Record Type: TAVG % Country: Laos % Latitude: 19.90000 +/- 0.00050 % Longitude: 103.11700 +/- 0.00050 % Elevation (m): 1158.00 +/- 0.05 % # of Months: 17 % % IDs: gsod - 489306-99999 % usaf - 489306 % % Sources: Global Summary of the Day % % Site Hash: def462813ccc38e22f5f89d393914792 % Raw Data Hash: 7da304a016de9d2098bb6d334c1f635d % Adj Data Hash: 32776821044410cd0b1792fb35d827e5 % % 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 1966 8 NaN NaN NaN NaN NaN NaN 24.943 -0.361 1966 9 NaN NaN NaN NaN NaN NaN 24.372 -0.659 1966 10 NaN NaN NaN NaN NaN NaN 23.900 0.630 1966 11 NaN NaN NaN NaN NaN NaN 22.204 1.556 1966 12 NaN NaN NaN NaN NaN NaN 19.892 2.015 1967 1 NaN NaN NaN NaN NaN NaN 17.110 -0.560 1967 2 NaN NaN NaN NaN NaN NaN 19.040 -0.522 1967 3 NaN NaN NaN NaN NaN NaN 22.325 -0.169 1967 4 NaN NaN NaN NaN NaN NaN 24.691 -0.280 1967 5 NaN NaN NaN NaN NaN NaN 26.166 0.018 1967 6 NaN NaN NaN NaN NaN NaN 25.623 -0.317 1967 7 NaN NaN NaN NaN NaN NaN 25.677 0.129 1967 8 21.589 -0.270 1 0 NaN NaN 25.419 0.115 1967 9 19.904 -1.682 0 0 19.904 -1.682 24.217 -0.814 1967 10 18.358 -1.466 0 0 18.358 -1.466 22.352 -0.918 1967 11 17.004 -0.199 0 0 17.004 -0.199 20.839 0.191 1967 12 13.410 -1.022 0 0 13.410 -1.022 17.210 -0.667 1968 1 15.287 1.062 0 0 15.287 1.062 17.833 0.163 1968 2 17.546 1.429 1 0 NaN NaN 17.832 -1.730 1968 3 21.459 2.410 0 0 21.459 2.410 22.705 0.211 1968 4 20.519 -1.008 0 0 20.519 -1.008 23.527 -1.444 1968 5 22.190 -0.513 0 0 22.190 -0.513 25.474 -0.674 1968 6 21.674 -0.821 0 0 21.674 -0.821 24.977 -0.964 1968 7 21.278 -0.825 1 0 NaN NaN 25.855 0.307 1968 8 21.735 -0.124 0 0 21.735 -0.124 25.382 0.078 1968 9 21.109 -0.477 0 0 21.109 -0.477 25.197 0.166 1968 10 18.371 -1.454 0 0 18.371 -1.454 22.845 -0.424 1968 11 18.104 0.901 0 0 18.104 0.901 21.965 1.317 1968 12 16.381 1.950 0 0 16.381 1.950 19.213 1.336 1969 1 NaN NaN NaN NaN NaN NaN 18.973 1.303 1969 2 NaN NaN NaN NaN NaN NaN 19.750 0.188 1969 3 NaN NaN NaN NaN NaN NaN 23.596 1.102 1969 4 NaN NaN NaN NaN NaN NaN 25.946 0.974 1969 5 NaN NaN NaN NaN NaN NaN 26.628 0.481 1969 6 NaN NaN NaN NaN NaN NaN 25.711 -0.229 1969 7 NaN NaN NaN NaN NaN NaN 25.253 -0.295 1969 8 NaN NaN NaN NaN NaN NaN 24.636 -0.668 1969 9 NaN NaN NaN NaN NaN NaN 24.995 -0.036 1969 10 NaN NaN NaN NaN NaN NaN 23.743 0.474 1969 11 NaN NaN NaN NaN NaN NaN 19.943 -0.705 1969 12 NaN NaN NaN NaN NaN NaN 16.997 -0.881