% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 12655 % Primary Name: SALAZAR % Record Type: TAVG % Country: Colombia % Latitude: 7.77000 +/- 0.00500 % Longitude: -72.82000 +/- 0.00500 % Elevation (m): 870.00 +/- 0.50 % # of Months: 24 % % IDs: ca - 305000000070 % % Sources: Colonial Archive % % Site Hash: c596cd1924716b6f9e4c0c0206eeb569 % Raw Data Hash: ab189dce856c3a181389e21656b74507 % Adj Data Hash: ab189dce856c3a181389e21656b74507 % % 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 1954 1 NaN NaN NaN NaN NaN NaN 19.761 -0.671 1954 2 NaN NaN NaN NaN NaN NaN 20.679 -0.340 1954 3 NaN NaN NaN NaN NaN NaN 21.726 0.283 1954 4 NaN NaN NaN NaN NaN NaN 20.604 -0.548 1954 5 NaN NaN NaN NaN NaN NaN 21.419 -0.018 1954 6 NaN NaN NaN NaN NaN NaN 20.794 -0.374 1954 7 NaN NaN NaN NaN NaN NaN 20.233 -0.837 1954 8 NaN NaN NaN NaN NaN NaN 20.863 -0.605 1954 9 NaN NaN NaN NaN NaN NaN 21.891 0.155 1954 10 NaN NaN NaN NaN NaN NaN 20.768 -0.586 1954 11 NaN NaN NaN NaN NaN NaN 20.519 -0.470 1954 12 NaN NaN NaN NaN NaN NaN 19.510 -0.850 1955 1 20.900 -0.963 0 0 20.900 -0.963 19.726 -0.707 1955 2 21.200 -1.249 0 0 21.200 -1.249 20.440 -0.579 1955 3 20.750 -2.122 0 0 20.750 -2.122 20.077 -1.365 1955 4 21.400 -1.182 0 0 21.400 -1.182 20.099 -1.053 1955 5 22.950 0.084 0 0 22.950 0.084 21.359 -0.077 1955 6 22.550 -0.047 0 0 22.550 -0.047 20.819 -0.348 1955 7 21.300 -1.200 0 0 21.300 -1.200 20.455 -0.615 1955 8 23.200 0.303 0 0 23.200 0.303 21.387 -0.080 1955 9 22.550 -0.616 0 0 22.550 -0.616 21.108 -0.628 1955 10 22.400 -0.384 0 0 22.400 -0.384 20.938 -0.417 1955 11 21.950 -0.470 0 0 21.950 -0.470 20.885 -0.104 1955 12 20.650 -1.141 0 0 20.650 -1.141 19.820 -0.541 1956 1 20.350 -1.513 0 0 20.350 -1.513 19.050 -1.382 1956 2 21.150 -1.299 0 0 21.150 -1.299 20.087 -0.932 1956 3 21.350 -1.522 0 0 21.350 -1.522 20.543 -0.899 1956 4 22.500 -0.082 0 0 22.500 -0.082 20.794 -0.358 1956 5 22.650 -0.216 0 0 22.650 -0.216 20.619 -0.817 1956 6 22.500 -0.097 0 0 22.500 -0.097 20.402 -0.765 1956 7 22.400 -0.100 0 0 22.400 -0.100 20.125 -0.945 1956 8 23.150 0.253 0 0 23.150 0.253 20.721 -0.746 1956 9 23.050 -0.116 0 0 23.050 -0.116 21.209 -0.527 1956 10 22.600 -0.184 0 0 22.600 -0.184 20.912 -0.442 1956 11 22.000 -0.420 0 0 22.000 -0.420 20.954 -0.036 1956 12 21.250 -0.541 0 0 21.250 -0.541 19.901 -0.460 1957 1 NaN NaN NaN NaN NaN NaN 19.693 -0.740 1957 2 NaN NaN NaN NaN NaN NaN 20.992 -0.027 1957 3 NaN NaN NaN NaN NaN NaN 21.552 0.110 1957 4 NaN NaN NaN NaN NaN NaN 20.918 -0.234 1957 5 NaN NaN NaN NaN NaN NaN 21.425 -0.011 1957 6 NaN NaN NaN NaN NaN NaN 20.996 -0.171 1957 7 NaN NaN NaN NaN NaN NaN 20.760 -0.310 1957 8 NaN NaN NaN NaN NaN NaN 21.430 -0.037 1957 9 NaN NaN NaN NaN NaN NaN 22.088 0.352 1957 10 NaN NaN NaN NaN NaN NaN 21.469 0.114 1957 11 NaN NaN NaN NaN NaN NaN 21.297 0.307 1957 12 NaN NaN NaN NaN NaN NaN 20.742 0.381