% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 12678 % Primary Name: URIBIA % Record Type: TAVG % Country: Colombia % Latitude: 11.72000 +/- 0.00500 % Longitude: -72.23000 +/- 0.00500 % Elevation (m): 23.00 +/- 0.50 % # of Months: 46 % % IDs: ca - 305000000080 % % Sources: Colonial Archive % % Site Hash: eabd043741840b0438a8408c3fe1e93a % Raw Data Hash: 9312155647c4e3936297469b198e7e53 % Adj Data Hash: faf52efe3c23a244c4a5dddf22747024 % % 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 9 NaN NaN NaN NaN NaN NaN 29.721 0.333 1952 10 NaN NaN NaN NaN NaN NaN 29.011 0.613 1952 11 NaN NaN NaN NaN NaN NaN 28.367 0.314 1952 12 NaN NaN NaN NaN NaN NaN 27.172 -0.226 1953 1 NaN NaN NaN NaN NaN NaN 27.385 0.414 1953 2 NaN NaN NaN NaN NaN NaN 27.251 0.250 1953 3 NaN NaN NaN NaN NaN NaN 27.043 -0.274 1953 4 NaN NaN NaN NaN NaN NaN 28.311 0.484 1953 5 NaN NaN NaN NaN NaN NaN 28.952 -0.082 1953 6 NaN NaN NaN NaN NaN NaN 29.942 0.204 1953 7 NaN NaN NaN NaN NaN NaN 29.969 -0.019 1953 8 NaN NaN NaN NaN NaN NaN 30.178 0.308 1953 9 29.300 -0.541 1 0 NaN NaN 29.719 0.332 1953 10 29.400 0.548 1 0 NaN NaN 28.890 0.492 1953 11 29.200 0.694 1 0 NaN NaN 28.873 0.820 1953 12 28.300 0.449 0 0 28.300 0.449 27.681 0.284 1954 1 NaN NaN NaN NaN NaN NaN 27.036 0.065 1954 2 NaN NaN NaN NaN NaN NaN 26.737 -0.264 1954 3 NaN NaN NaN NaN NaN NaN 27.898 0.580 1954 4 NaN NaN NaN NaN NaN NaN 28.102 0.275 1954 5 NaN NaN NaN NaN NaN NaN 29.253 0.219 1954 6 NaN NaN NaN NaN NaN NaN 29.752 0.014 1954 7 NaN NaN NaN NaN NaN NaN 29.720 -0.269 1954 8 NaN NaN NaN NaN NaN NaN 30.097 0.227 1954 9 NaN NaN NaN NaN NaN NaN 29.497 0.109 1954 10 NaN NaN NaN NaN NaN NaN 27.478 -0.920 1954 11 NaN NaN NaN NaN NaN NaN 27.549 -0.504 1954 12 NaN NaN NaN NaN NaN NaN 26.591 -0.806 1955 1 26.800 -0.624 0 2 26.800 -0.624 26.363 -0.608 1955 2 27.450 -0.005 0 0 27.450 -0.005 26.846 -0.155 1955 3 27.950 0.179 0 0 27.950 0.179 26.889 -0.428 1955 4 28.550 0.270 0 0 28.550 0.270 27.190 -0.637 1955 5 29.400 -0.088 0 0 29.400 -0.088 28.740 -0.294 1955 6 29.250 -0.942 0 0 29.250 -0.942 28.832 -0.907 1955 7 29.850 -0.592 0 0 29.850 -0.592 29.553 -0.436 1955 8 30.150 -0.173 0 0 30.150 -0.173 29.457 -0.412 1955 9 28.300 -1.541 0 0 28.300 -1.541 28.472 -0.915 1955 10 26.950 -1.902 0 0 26.950 -1.902 26.972 -1.426 1955 11 26.600 -1.906 0 0 26.600 -1.906 27.168 -0.885 1955 12 26.100 -1.751 0 0 26.100 -1.751 26.401 -0.997 1956 1 27.300 -0.124 0 0 27.300 -0.124 25.805 -1.166 1956 2 27.600 0.145 0 0 27.600 0.145 26.645 -0.357 1956 3 28.350 0.579 0 0 28.350 0.579 27.114 -0.203 1956 4 28.350 0.070 0 0 28.350 0.070 27.907 0.081 1956 5 29.750 0.262 0 0 29.750 0.262 29.050 0.015 1956 6 29.700 -0.492 0 0 29.700 -0.492 29.279 -0.459 1956 7 29.950 -0.492 0 0 29.950 -0.492 29.594 -0.395 1956 8 30.950 0.627 0 0 30.950 0.627 29.876 0.006 1956 9 30.000 0.159 0 0 30.000 0.159 29.598 0.210 1956 10 28.600 -0.252 0 0 28.600 -0.252 27.928 -0.470 1956 11 27.400 -1.106 0 0 27.400 -1.106 27.405 -0.648 1956 12 26.650 -1.201 0 0 26.650 -1.201 26.481 -0.917 1957 1 26.550 -0.874 0 0 26.550 -0.874 25.933 -1.037 1957 2 NaN NaN NaN NaN NaN NaN 26.533 -0.469 1957 3 28.500 0.729 0 0 28.500 0.729 26.891 -0.426 1957 4 NaN NaN NaN NaN NaN NaN 27.424 -0.402 1957 5 29.050 -0.438 0 0 29.050 -0.438 28.657 -0.377 1957 6 29.850 -0.342 0 0 29.850 -0.342 29.882 0.144 1957 7 29.200 -1.242 0 0 29.200 -1.242 29.753 -0.235 1957 8 29.900 -0.423 0 0 29.900 -0.423 29.889 0.020 1957 9 28.550 -1.291 0 0 28.550 -1.291 29.744 0.356 1957 10 27.150 -1.702 0 0 27.150 -1.702 28.679 0.281 1957 11 26.450 -2.056 0 0 26.450 -2.056 28.131 0.079 1957 12 26.500 -1.351 0 0 26.500 -1.351 27.176 -0.222 1958 1 NaN NaN NaN NaN NaN NaN 26.947 -0.024 1958 2 NaN NaN NaN NaN NaN NaN 27.458 0.456 1958 3 NaN NaN NaN NaN NaN NaN 28.528 1.210 1958 4 30.900 2.620 0 0 30.900 2.620 28.992 1.165 1958 5 31.050 1.562 0 0 31.050 1.562 29.898 0.864 1958 6 31.000 0.808 0 0 31.000 0.808 30.224 0.486 1958 7 31.900 1.458 1 0 NaN NaN 29.883 -0.106 1958 8 31.650 1.327 0 0 31.650 1.327 30.433 0.564 1958 9 31.750 1.909 0 0 31.750 1.909 30.373 0.985 1958 10 30.700 1.848 0 0 30.700 1.848 29.196 0.797 1958 11 29.900 1.394 0 0 29.900 1.394 28.755 0.703 1958 12 NaN NaN NaN NaN NaN NaN 27.746 0.349 1959 1 NaN NaN NaN NaN NaN NaN 27.244 0.274 1959 2 NaN NaN NaN NaN NaN NaN 26.759 -0.243 1959 3 NaN NaN NaN NaN NaN NaN 27.406 0.089 1959 4 NaN NaN NaN NaN NaN NaN 27.549 -0.278 1959 5 NaN NaN NaN NaN NaN NaN 28.418 -0.616 1959 6 NaN NaN NaN NaN NaN NaN 29.029 -0.709 1959 7 NaN NaN NaN NaN NaN NaN 29.721 -0.268 1959 8 NaN NaN NaN NaN NaN NaN 29.229 -0.640 1959 9 NaN NaN NaN NaN NaN NaN 29.329 -0.059 1959 10 NaN NaN NaN NaN NaN NaN 28.237 -0.161 1959 11 NaN NaN NaN NaN NaN NaN 28.244 0.191