% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 35409 % Primary Name: ARTESIA 2 E % Record Type: TAVG % Country: United States % State: CO % Latitude: 40.23333 +/- 0.00833 % Longitude: -108.92921 +/- 0.03754 % Elevation (m): 1800.23 +/- 5.72 % # of Months: 23 % % Alternate Names: ARTESIA % ARTESIA 6 E % % IDs: coop - 50354 % ghcnd - USC00050354 % ncdc - 20003848 % ncdc - 20003933 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: aac713efe60f55f23949d356acb86cca % Raw Data Hash: 84743146ec5b88677d49d8118d2c4d6e % Adj Data Hash: 686132d9008bb62d4dd4d196958ed0ab % % 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 1962 6 NaN NaN NaN NaN NaN NaN 15.394 -0.599 1962 7 NaN NaN NaN NaN NaN NaN 19.431 -0.667 1962 8 NaN NaN NaN NaN NaN NaN 17.990 -0.575 1962 9 NaN NaN NaN NaN NaN NaN 13.932 0.507 1962 10 NaN NaN NaN NaN NaN NaN 9.282 2.199 1962 11 NaN NaN NaN NaN NaN NaN 2.380 2.888 1962 12 NaN NaN NaN NaN NaN NaN -3.473 2.004 1963 1 NaN NaN NaN NaN NaN NaN -9.109 -2.434 1963 2 NaN NaN NaN NaN NaN NaN 0.996 4.905 1963 3 NaN NaN NaN NaN NaN NaN -0.650 -0.333 1963 4 NaN NaN NaN NaN NaN NaN 4.286 -0.686 1963 5 NaN NaN NaN NaN NaN NaN 12.469 1.666 1963 6 17.800 0.472 1 0 NaN NaN 15.392 -0.602 1963 7 23.389 1.957 0 0 23.389 1.957 21.013 0.915 1963 8 21.222 1.323 0 0 21.222 1.323 19.233 0.668 1963 9 17.333 2.574 0 0 17.333 2.574 15.502 2.077 1963 10 12.833 4.416 0 0 12.833 4.416 11.048 3.965 1963 11 2.556 1.729 0 0 2.556 1.729 1.484 1.992 1963 12 -4.889 -0.747 0 0 -4.889 -0.747 -5.334 0.142 1964 1 -6.389 -1.048 0 0 -6.389 -1.048 -7.051 -0.375 1964 2 -5.278 -2.703 0 0 -5.278 -2.703 -6.375 -2.465 1964 3 -2.278 -3.295 0 0 -2.278 -3.295 -4.462 -4.145 1964 4 6.778 0.471 0 0 6.778 0.471 4.087 -0.886 1964 5 12.500 0.363 0 0 12.500 0.363 10.862 0.060 1964 6 NaN NaN NaN NaN NaN NaN 14.342 -1.652 1964 7 23.944 2.512 0 0 23.944 2.512 21.860 1.762 1964 8 20.611 0.711 0 0 20.611 0.711 17.730 -0.835 1964 9 15.833 1.074 0 0 15.833 1.074 12.972 -0.453 1964 10 10.222 1.805 0 0 10.222 1.805 8.713 1.630 1964 11 -2.333 -3.159 0 0 -2.333 -3.159 -1.883 -1.374 1964 12 -5.944 -1.803 0 0 -5.944 -1.803 -6.119 -0.643 1965 1 -6.500 -1.159 0 0 -6.500 -1.159 -4.828 1.847 1965 2 -5.222 -2.648 0 0 -5.222 -2.648 -4.355 -0.446 1965 3 -2.833 -3.851 0 0 -2.833 -3.851 -4.819 -4.503 1965 4 6.722 0.415 0 0 6.722 0.415 5.519 0.546 1965 5 11.444 -0.692 0 0 11.444 -0.692 9.566 -1.236 1965 6 NaN NaN NaN NaN NaN NaN 14.244 -1.749 1965 7 NaN NaN NaN NaN NaN NaN 19.761 -0.336 1965 8 NaN NaN NaN NaN NaN NaN 17.408 -1.157 1965 9 NaN NaN NaN NaN NaN NaN 9.436 -3.989 1965 10 NaN NaN NaN NaN NaN NaN 9.406 2.324 1965 11 NaN NaN NaN NaN NaN NaN 3.012 3.521 1965 12 NaN NaN NaN NaN NaN NaN -4.420 1.057 1966 1 NaN NaN NaN NaN NaN NaN -6.623 0.052 1966 2 NaN NaN NaN NaN NaN NaN -5.668 -1.758 1966 3 NaN NaN NaN NaN NaN NaN 0.116 0.432 1966 4 NaN NaN NaN NaN NaN NaN 4.381 -0.591 1966 5 NaN NaN NaN NaN NaN NaN 11.883 1.080