% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 14945 % Primary Name: ATKINSON FIE % Record Type: TAVG % Country: Guyana % Latitude: 6.47000 +/- 0.00500 % Longitude: -58.25000 +/- 0.00500 % Elevation (m): 29.00 +/- 0.50 % # of Months: 36 % % IDs: ca - 307000000004 % % Sources: Colonial Archive % % Site Hash: aa0ba6cc529124901f16617fcfd307a2 % Raw Data Hash: ba9cf5d473882f7d10ee8a98030f1217 % Adj Data Hash: ba9cf5d473882f7d10ee8a98030f1217 % % 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 1953 1 NaN NaN NaN NaN NaN NaN 26.493 0.063 1953 2 NaN NaN NaN NaN NaN NaN 26.642 -0.139 1953 3 NaN NaN NaN NaN NaN NaN 27.176 -0.072 1953 4 NaN NaN NaN NaN NaN NaN 27.300 0.034 1953 5 NaN NaN NaN NaN NaN NaN 26.955 -0.224 1953 6 NaN NaN NaN NaN NaN NaN 27.049 0.269 1953 7 NaN NaN NaN NaN NaN NaN 27.099 0.243 1953 8 NaN NaN NaN NaN NaN NaN 28.094 0.516 1953 9 NaN NaN NaN NaN NaN NaN 28.286 -0.026 1953 10 NaN NaN NaN NaN NaN NaN 28.693 0.321 1953 11 NaN NaN NaN NaN NaN NaN 28.431 0.476 1953 12 NaN NaN NaN NaN NaN NaN 27.103 0.297 1954 1 25.250 -0.282 0 0 25.250 -0.282 26.101 -0.328 1954 2 25.550 -0.334 0 0 25.550 -0.334 26.612 -0.168 1954 3 26.250 -0.101 0 0 26.250 -0.101 27.232 -0.017 1954 4 25.650 -0.719 0 0 25.650 -0.719 26.636 -0.630 1954 5 25.900 -0.381 0 0 25.900 -0.381 26.986 -0.193 1954 6 25.900 0.017 0 0 25.900 0.017 26.644 -0.136 1954 7 25.950 -0.009 0 0 25.950 -0.009 26.595 -0.261 1954 8 26.550 -0.131 0 0 26.550 -0.131 27.155 -0.423 1954 9 27.150 -0.265 0 0 27.150 -0.265 28.118 -0.194 1954 10 26.550 -0.925 0 0 26.550 -0.925 27.877 -0.494 1954 11 26.000 -1.058 0 0 26.000 -1.058 27.272 -0.683 1954 12 25.800 -0.109 0 0 25.800 -0.109 26.532 -0.274 1955 1 25.300 -0.232 0 0 25.300 -0.232 26.228 -0.201 1955 2 25.500 -0.384 0 0 25.500 -0.384 26.658 -0.123 1955 3 25.450 -0.901 0 0 25.450 -0.901 26.410 -0.839 1955 4 25.850 -0.519 0 0 25.850 -0.519 26.735 -0.531 1955 5 26.150 -0.131 0 0 26.150 -0.131 26.981 -0.197 1955 6 26.350 0.467 0 0 26.350 0.467 26.831 0.052 1955 7 26.200 0.241 0 0 26.200 0.241 26.667 -0.189 1955 8 26.950 0.269 0 0 26.950 0.269 27.546 -0.033 1955 9 27.550 0.135 0 0 27.550 0.135 28.137 -0.174 1955 10 27.400 -0.075 0 0 27.400 -0.075 28.451 0.079 1955 11 26.800 -0.258 0 0 26.800 -0.258 28.023 0.068 1955 12 25.450 -0.459 0 0 25.450 -0.459 26.226 -0.579 1956 1 25.850 0.318 0 0 25.850 0.318 26.520 0.090 1956 2 25.300 -0.584 0 0 25.300 -0.584 26.498 -0.283 1956 3 25.750 -0.601 0 0 25.750 -0.601 26.871 -0.377 1956 4 26.500 0.131 0 0 26.500 0.131 27.221 -0.044 1956 5 25.600 -0.681 0 0 25.600 -0.681 26.450 -0.729 1956 6 25.950 0.067 0 0 25.950 0.067 26.475 -0.305 1956 7 26.000 0.041 0 0 26.000 0.041 26.479 -0.377 1956 8 26.000 -0.681 0 0 26.000 -0.681 26.975 -0.604 1956 9 26.400 -1.015 0 0 26.400 -1.015 27.553 -0.759 1956 10 26.700 -0.775 0 0 26.700 -0.775 27.775 -0.597 1956 11 26.450 -0.608 0 0 26.450 -0.608 27.730 -0.226 1956 12 25.150 -0.759 0 0 25.150 -0.759 26.195 -0.610 1957 1 NaN NaN NaN NaN NaN NaN 26.012 -0.417 1957 2 NaN NaN NaN NaN NaN NaN 26.623 -0.158 1957 3 NaN NaN NaN NaN NaN NaN 27.015 -0.233 1957 4 NaN NaN NaN NaN NaN NaN 27.248 -0.018 1957 5 NaN NaN NaN NaN NaN NaN 27.208 0.030 1957 6 NaN NaN NaN NaN NaN NaN 26.695 -0.084 1957 7 NaN NaN NaN NaN NaN NaN 26.841 -0.015 1957 8 NaN NaN NaN NaN NaN NaN 27.633 0.055 1957 9 NaN NaN NaN NaN NaN NaN 28.710 0.398 1957 10 NaN NaN NaN NaN NaN NaN 28.447 0.076 1957 11 NaN NaN NaN NaN NaN NaN 28.356 0.401 1957 12 NaN NaN NaN NaN NaN NaN 26.956 0.150