% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 64 % Primary Name: DECEPTION IS S SMET IS % Record Type: TAVG % Country: [Missing] % Latitude: -61.01700 +/- 0.00050 % Longitude: -59.43300 +/- 0.00050 % Elevation (m): 7.90 +/- 0.05 % # of Months: 65 % % IDs: gsod - 889380-99999 % usaf - 889380 % % Sources: Global Summary of the Day % % Site Hash: 1b82116fab71b648b1e62cdbb973a231 % Raw Data Hash: 8426df76c6d2de2bd44aeb5c8df95513 % Adj Data Hash: 349ee2a331dc0842d97b06acb6c3368e % % 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 1952 1 NaN NaN NaN NaN NaN NaN 1.648 0.328 1952 2 NaN NaN NaN NaN NaN NaN 1.513 0.091 1952 3 NaN NaN NaN NaN NaN NaN -1.324 -1.659 1952 4 NaN NaN NaN NaN NaN NaN -3.257 -1.519 1952 5 NaN NaN NaN NaN NaN NaN -7.642 -3.817 1952 6 NaN NaN NaN NaN NaN NaN -4.641 1.187 1952 7 NaN NaN NaN NaN NaN NaN -7.454 -0.434 1952 8 NaN NaN NaN NaN NaN NaN -4.864 2.008 1952 9 NaN NaN NaN NaN NaN NaN -1.687 2.522 1952 10 NaN NaN NaN NaN NaN NaN -2.320 0.105 1952 11 NaN NaN NaN NaN NaN NaN 0.205 1.043 1952 12 NaN NaN NaN NaN NaN NaN -0.121 -0.435 1953 1 0.479 -0.639 0 0 0.479 -0.639 0.291 -1.028 1953 2 0.542 -0.680 0 0 0.542 -0.680 0.382 -1.041 1953 3 -1.321 -1.455 0 0 -1.321 -1.455 -1.084 -1.420 1953 4 -4.219 -2.280 0 0 -4.219 -2.280 -4.271 -2.534 1953 5 -5.538 -1.512 0 0 -5.538 -1.512 -5.528 -1.704 1953 6 -9.000 -2.970 0 0 -9.000 -2.970 -8.156 -2.327 1953 7 -7.323 -0.101 0 0 -7.323 -0.101 -6.601 0.419 1953 8 -4.748 2.325 0 0 -4.748 2.325 -4.459 2.413 1953 9 -4.103 0.306 0 0 -4.103 0.306 -3.252 0.957 1953 10 -3.428 -0.802 0 0 -3.428 -0.802 -2.979 -0.555 1953 11 -1.130 -0.091 0 0 -1.130 -0.091 -0.135 0.703 1953 12 1.165 1.052 0 0 1.165 1.052 1.307 0.992 1954 1 0.720 -0.398 0 0 0.720 -0.398 0.436 -0.883 1954 2 1.404 0.182 1 0 NaN NaN 1.097 -0.326 1954 3 -0.269 -0.403 0 0 -0.269 -0.403 -0.178 -0.514 1954 4 -0.741 1.198 1 0 NaN NaN -0.052 1.686 1954 5 -2.669 1.357 0 0 -2.669 1.357 -2.490 1.334 1954 6 -7.484 -1.454 0 0 -7.484 -1.454 -7.317 -1.488 1954 7 -9.294 -2.072 0 0 -9.294 -2.072 -9.449 -2.428 1954 8 -12.935 -5.862 0 0 -12.935 -5.862 -13.135 -6.263 1954 9 -8.358 -3.948 0 0 -8.358 -3.948 -7.513 -3.304 1954 10 -1.075 1.551 0 0 -1.075 1.551 -0.756 1.669 1954 11 -0.123 0.917 0 0 -0.123 0.917 0.036 0.874 1954 12 0.751 0.638 0 0 0.751 0.638 0.599 0.285 1955 1 3.009 1.891 0 0 3.009 1.891 2.556 1.237 1955 2 2.980 1.759 0 0 2.980 1.759 2.626 1.203 1955 3 0.120 -0.014 0 0 0.120 -0.014 0.080 -0.255 1955 4 -0.870 1.068 0 0 -0.870 1.068 -0.731 1.007 1955 5 -2.174 1.852 0 0 -2.174 1.852 -2.035 1.789 1955 6 -3.463 2.567 0 0 -3.463 2.567 -3.635 2.194 1955 7 -3.896 3.326 0 0 -3.896 3.326 -3.911 3.110 1955 8 -4.129 2.944 0 0 -4.129 2.944 -4.412 2.460 1955 9 -2.456 1.954 0 0 -2.456 1.954 -1.352 2.857 1955 10 -1.287 1.339 0 0 -1.287 1.339 -0.761 1.664 1955 11 -2.156 -1.116 0 0 -2.156 -1.116 -0.311 0.527 1955 12 -0.287 -0.400 0 0 -0.287 -0.400 -0.612 -0.926 1956 1 1.821 0.702 0 0 1.821 0.702 1.203 -0.116 1956 2 1.458 0.236 0 0 1.458 0.236 1.142 -0.281 1956 3 0.912 0.778 0 0 0.912 0.778 0.872 0.536 1956 4 -0.454 1.485 0 0 -0.454 1.485 -0.013 1.725 1956 5 NaN NaN NaN NaN NaN NaN -2.186 1.638 1956 6 -1.481 4.548 0 0 -1.481 4.548 -1.345 4.484 1956 7 -3.708 3.514 0 0 -3.708 3.514 -3.520 3.501 1956 8 -2.427 4.647 0 0 -2.427 4.647 -2.406 4.467 1956 9 -4.181 0.228 0 0 -4.181 0.228 -3.126 1.083 1956 10 -1.814 0.812 0 0 -1.814 0.812 -1.354 1.071 1956 11 -0.072 0.967 0 0 -0.072 0.967 0.421 1.259 1956 12 0.143 0.030 0 0 0.143 0.030 0.005 -0.309 1957 1 1.215 0.097 0 0 1.215 0.097 0.908 -0.412 1957 2 2.506 1.284 0 0 2.506 1.284 2.713 1.291 1957 3 1.138 1.004 0 0 1.138 1.004 1.452 1.117 1957 4 0.500 2.439 0 0 0.500 2.439 0.966 2.703 1957 5 -2.710 1.316 0 0 -2.710 1.316 -2.525 1.300 1957 6 -8.222 -2.192 0 0 -8.222 -2.192 -8.336 -2.507 1957 7 -9.222 -2.001 0 0 -9.222 -2.001 -8.524 -1.503 1957 8 -7.330 -0.256 0 0 -7.330 -0.256 -7.479 -0.607 1957 9 -2.850 1.560 0 0 -2.850 1.560 -1.867 2.342 1957 10 -5.584 -2.958 0 0 -5.584 -2.958 -5.342 -2.917 1957 11 -0.450 0.589 0 0 -0.450 0.589 0.214 1.052 1957 12 0.353 0.240 0 0 0.353 0.240 0.006 -0.308 1958 1 1.889 0.771 0 0 1.889 0.771 1.552 0.232 1958 2 0.421 -0.801 0 0 0.421 -0.801 0.275 -1.148 1958 3 -0.002 -0.136 0 0 -0.002 -0.136 0.403 0.067 1958 4 -1.793 0.146 0 0 -1.793 0.146 -1.556 0.182 1958 5 -7.183 -3.157 0 0 -7.183 -3.157 -6.988 -3.163 1958 6 -12.206 -6.176 0 0 -12.206 -6.176 -11.631 -5.802 1958 7 NaN NaN NaN NaN NaN NaN -12.556 -5.535 1958 8 NaN NaN NaN NaN NaN NaN -9.744 -2.872 1958 9 NaN NaN NaN NaN NaN NaN -6.776 -2.568 1958 10 NaN NaN NaN NaN NaN NaN -1.814 0.611 1958 11 NaN NaN NaN NaN NaN NaN 0.621 1.459 1958 12 NaN NaN NaN NaN NaN NaN -0.310 -0.624 1959 1 NaN NaN NaN NaN NaN NaN 0.128 -1.192 1959 2 NaN NaN NaN NaN NaN NaN -0.878 -2.300 1959 3 NaN NaN NaN NaN NaN NaN -0.021 -0.357 1959 4 NaN NaN NaN NaN NaN NaN -5.764 -4.026 1959 5 NaN NaN NaN NaN NaN NaN -6.753 -2.929 1959 6 NaN NaN NaN NaN NaN NaN -7.067 -1.238