% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 33995 % Primary Name: TWIN LAKES EVAPORATION % Record Type: TAVG % Country: United States % State: CO % Latitude: 39.08330 +/- 0.00005 % Longitude: -106.30000 +/- 0.00005 % Elevation (m): 2797.10 +/- 0.05 % # of Months: 9 % % Alternate Names: TWIN LAKES EVAPORATI % % IDs: coop - 58496 % ghcnd - USC00058496 % ncdc - 20003613 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: f0af1ac1e7936423fab8250d40334917 % Raw Data Hash: 959417c32e1dcf301a3378a0265b32d8 % Adj Data Hash: 781c30d24f67ef64b2e5b9f2b7df9007 % % 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 1964 5 NaN NaN NaN NaN NaN NaN 6.308 0.047 1964 6 NaN NaN NaN NaN NaN NaN 9.900 -1.245 1964 7 NaN NaN NaN NaN NaN NaN 15.518 1.228 1964 8 NaN NaN NaN NaN NaN NaN 12.130 -1.024 1964 9 NaN NaN NaN NaN NaN NaN 9.027 -0.366 1964 10 NaN NaN NaN NaN NaN NaN 5.406 1.312 1964 11 NaN NaN NaN NaN NaN NaN -2.774 -0.090 1964 12 NaN NaN NaN NaN NaN NaN -7.180 -0.465 1965 1 NaN NaN NaN NaN NaN NaN -5.527 2.251 1965 2 NaN NaN NaN NaN NaN NaN -7.522 -1.072 1965 3 NaN NaN NaN NaN NaN NaN -8.364 -4.391 1965 4 NaN NaN NaN NaN NaN NaN 0.937 0.214 1965 5 7.034 0.828 1 0 NaN NaN 5.337 -0.923 1965 6 8.889 -2.202 0 0 8.889 -2.202 9.480 -1.665 1965 7 14.889 0.653 0 0 14.889 0.653 14.049 -0.242 1965 8 12.278 -0.822 0 0 12.278 -0.822 11.779 -1.375 1965 9 7.944 -1.394 0 0 7.944 -1.394 6.816 -2.577 1965 10 5.667 1.627 0 0 5.667 1.627 6.173 2.079 1965 11 NaN NaN NaN NaN NaN NaN -0.217 2.467 1965 12 NaN NaN NaN NaN NaN NaN -4.789 1.927 1966 1 NaN NaN NaN NaN NaN NaN -8.738 -0.959 1966 2 NaN NaN NaN NaN NaN NaN -9.057 -2.607 1966 3 -4.278 -0.251 0 0 -4.278 -0.251 -2.844 1.128 1966 4 NaN NaN NaN NaN NaN NaN 0.865 0.141 1966 5 NaN NaN NaN NaN NaN NaN 7.249 0.989 1966 6 NaN NaN NaN NaN NaN NaN 10.598 -0.547 1966 7 15.167 0.930 0 0 15.167 0.930 15.862 1.571 1966 8 NaN NaN NaN NaN NaN NaN 12.878 -0.276 1966 9 NaN NaN NaN NaN NaN NaN 9.895 0.503 1966 10 NaN NaN NaN NaN NaN NaN 4.445 0.351 1966 11 NaN NaN NaN NaN NaN NaN -0.269 2.416 1966 12 NaN NaN NaN NaN NaN NaN -6.911 -0.195 1967 1 NaN NaN NaN NaN NaN NaN -5.897 1.881 1967 2 NaN NaN NaN NaN NaN NaN -6.497 -0.048 1967 3 NaN NaN NaN NaN NaN NaN -1.102 2.870 1967 4 1.722 1.053 0 0 1.722 1.053 1.399 0.676 1967 5 NaN NaN NaN NaN NaN NaN 4.859 -1.401 1967 6 NaN NaN NaN NaN NaN NaN 9.161 -1.984 1967 7 NaN NaN NaN NaN NaN NaN 14.359 0.068 1967 8 NaN NaN NaN NaN NaN NaN 12.131 -1.023 1967 9 NaN NaN NaN NaN NaN NaN 9.299 -0.094 1967 10 NaN NaN NaN NaN NaN NaN 5.576 1.482 1967 11 NaN NaN NaN NaN NaN NaN -1.652 1.032 1967 12 NaN NaN NaN NaN NaN NaN -8.658 -1.942 1968 1 NaN NaN NaN NaN NaN NaN -7.213 0.565 1968 2 NaN NaN NaN NaN NaN NaN -5.613 0.837 1968 3 NaN NaN NaN NaN NaN NaN -4.190 -0.217 1968 4 NaN NaN NaN NaN NaN NaN -1.468 -2.192