% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 12622 % Primary Name: APTO. SANTAG % Record Type: TAVG % Country: Colombia % Latitude: 5.08000 +/- 0.00500 % Longitude: -75.65000 +/- 0.00500 % Elevation (m): 1120.00 +/- 0.50 % # of Months: 20 % % IDs: ca - 305000000004 % % Sources: Colonial Archive % % Site Hash: ebd53ee023e3f9bc1d7f94139a9b66ad % Raw Data Hash: 99e76c767a1455f733b83919801bf618 % Adj Data Hash: 99e76c767a1455f733b83919801bf618 % % 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 1958 5 NaN NaN NaN NaN NaN NaN 19.752 0.422 1958 6 NaN NaN NaN NaN NaN NaN 19.731 0.445 1958 7 NaN NaN NaN NaN NaN NaN 19.973 0.579 1958 8 NaN NaN NaN NaN NaN NaN 19.549 0.194 1958 9 NaN NaN NaN NaN NaN NaN 19.395 0.322 1958 10 NaN NaN NaN NaN NaN NaN 19.070 0.528 1958 11 NaN NaN NaN NaN NaN NaN 19.158 0.460 1958 12 NaN NaN NaN NaN NaN NaN 19.220 0.431 1959 1 NaN NaN NaN NaN NaN NaN 19.549 0.515 1959 2 NaN NaN NaN NaN NaN NaN 19.786 0.456 1959 3 NaN NaN NaN NaN NaN NaN 20.065 0.528 1959 4 NaN NaN NaN NaN NaN NaN 19.518 0.322 1959 5 23.850 -0.026 0 0 23.850 -0.026 19.262 -0.068 1959 6 23.200 -0.632 0 0 23.200 -0.632 18.979 -0.307 1959 7 23.450 -0.490 0 0 23.450 -0.490 19.232 -0.161 1959 8 23.450 -0.451 0 0 23.450 -0.451 18.915 -0.440 1959 9 23.800 0.181 0 0 23.800 0.181 19.113 0.040 1959 10 23.150 0.062 0 0 23.150 0.062 18.341 -0.201 1959 11 23.100 -0.145 0 0 23.100 -0.145 18.734 0.036 1959 12 23.700 0.365 0 0 23.700 0.365 19.050 0.261 1960 1 23.750 0.170 0 0 23.750 0.170 18.963 -0.070 1960 2 23.750 -0.126 0 0 23.750 -0.126 19.346 0.016 1960 3 23.800 -0.283 0 0 23.800 -0.283 19.521 -0.016 1960 4 23.450 -0.292 0 0 23.450 -0.292 19.021 -0.175 1960 5 23.600 -0.276 0 0 23.600 -0.276 19.194 -0.136 1960 6 23.400 -0.432 0 0 23.400 -0.432 18.927 -0.359 1960 7 23.350 -0.590 0 0 23.350 -0.590 18.874 -0.520 1960 8 23.800 -0.101 0 0 23.800 -0.101 19.050 -0.305 1960 9 23.550 -0.069 0 0 23.550 -0.069 18.962 -0.111 1960 10 23.500 0.412 0 0 23.500 0.412 18.566 0.024 1960 11 23.350 0.105 0 0 23.350 0.105 18.817 0.118 1960 12 23.550 0.215 0 0 23.550 0.215 18.759 -0.029 1961 1 NaN NaN NaN NaN NaN NaN 19.345 0.311 1961 2 NaN NaN NaN NaN NaN NaN 19.387 0.057 1961 3 NaN NaN NaN NaN NaN NaN 19.723 0.186 1961 4 NaN NaN NaN NaN NaN NaN 19.002 -0.194 1961 5 NaN NaN NaN NaN NaN NaN 19.826 0.496 1961 6 NaN NaN NaN NaN NaN NaN 19.196 -0.090 1961 7 NaN NaN NaN NaN NaN NaN 19.036 -0.358 1961 8 NaN NaN NaN NaN NaN NaN 19.418 0.063 1961 9 NaN NaN NaN NaN NaN NaN 18.832 -0.240 1961 10 NaN NaN NaN NaN NaN NaN 18.342 -0.200 1961 11 NaN NaN NaN NaN NaN NaN 18.104 -0.594 1961 12 NaN NaN NaN NaN NaN NaN 18.846 0.058