% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39857 % Primary Name: LAKE COLDEN % Record Type: TAVG % Country: United States % State: NY % Latitude: 44.10000 +/- 0.00833 % Longitude: -74.00000 +/- 0.00833 % Elevation (m): 838.20 +/- 0.15 % # of Months: 15 % % Alternate Names: Missing Station ID - 304520 % % IDs: coop - 304520 % ghcnd - USC00304520 % ncdc - 12010116 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: 9d44772ccf1a6e3655a815c843d919eb % Raw Data Hash: 999a67b75c9150cb9be8da6107daa47b % Adj Data Hash: ca24bae42ed2cb3f65e1ef343d8528ab % % 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 1920 1 NaN NaN NaN NaN NaN NaN -14.678 -5.558 1920 2 NaN NaN NaN NaN NaN NaN -9.553 -1.431 1920 3 NaN NaN NaN NaN NaN NaN -1.408 0.891 1920 4 NaN NaN NaN NaN NaN NaN 3.287 -1.482 1920 5 NaN NaN NaN NaN NaN NaN 10.828 -0.891 1920 6 NaN NaN NaN NaN NaN NaN 16.231 -0.670 1920 7 NaN NaN NaN NaN NaN NaN 17.959 -1.416 1920 8 NaN NaN NaN NaN NaN NaN 19.253 1.085 1920 9 NaN NaN NaN NaN NaN NaN 14.671 0.769 1920 10 NaN NaN NaN NaN NaN NaN 10.689 2.908 1920 11 NaN NaN NaN NaN NaN NaN 0.189 -1.435 1920 12 NaN NaN NaN NaN NaN NaN -5.371 0.786 1921 1 -11.779 -0.441 1 0 NaN NaN -7.371 1.749 1921 2 -8.998 1.343 1 0 NaN NaN -6.817 1.305 1921 3 -0.973 3.544 0 0 -0.973 3.544 2.069 4.368 1921 4 NaN NaN NaN NaN NaN NaN 8.197 3.428 1921 5 NaN NaN NaN NaN NaN NaN 12.914 1.195 1921 6 NaN NaN NaN NaN NaN NaN 16.899 -0.002 1921 7 NaN NaN NaN NaN NaN NaN 22.492 3.117 1921 8 NaN NaN NaN NaN NaN NaN 17.588 -0.580 1921 9 NaN NaN NaN NaN NaN NaN 15.598 1.697 1921 10 5.525 -0.037 1 0 NaN NaN 7.854 0.072 1921 11 -2.235 -1.640 0 0 -2.235 -1.640 0.183 -1.441 1921 12 -9.379 -1.003 0 0 -9.379 -1.003 -7.984 -1.827 1922 1 -11.010 0.328 1 0 NaN NaN -10.887 -1.767 1922 2 NaN NaN NaN NaN NaN NaN -7.298 0.825 1922 3 -2.452 2.066 0 0 -2.452 2.066 -0.979 1.319 1922 4 2.725 0.175 0 0 2.725 0.175 4.914 0.145 1922 5 10.679 1.179 0 0 10.679 1.179 12.921 1.202 1922 6 15.025 0.342 0 0 15.025 0.342 17.093 0.191 1922 7 15.729 -1.427 0 0 15.729 -1.427 18.951 -0.424 1922 8 14.686 -1.263 0 0 14.686 -1.263 17.682 -0.486 1922 9 13.297 1.614 0 0 13.297 1.614 14.943 1.041 1922 10 5.710 0.148 0 0 5.710 0.148 7.427 -0.354 1922 11 NaN NaN NaN NaN NaN NaN 2.213 0.589 1922 12 NaN NaN NaN NaN NaN NaN -7.220 -1.063 1923 1 NaN NaN NaN NaN NaN NaN -11.311 -2.191 1923 2 NaN NaN NaN NaN NaN NaN -12.487 -4.365 1923 3 NaN NaN NaN NaN NaN NaN -5.899 -3.600 1923 4 NaN NaN NaN NaN NaN NaN 3.584 -1.185 1923 5 NaN NaN NaN NaN NaN NaN 9.887 -1.832 1923 6 NaN NaN NaN NaN NaN NaN 16.757 -0.145 1923 7 NaN NaN NaN NaN NaN NaN 17.762 -1.613 1923 8 NaN NaN NaN NaN NaN NaN 16.823 -1.345 1923 9 NaN NaN NaN NaN NaN NaN 14.203 0.301 1923 10 NaN NaN NaN NaN NaN NaN 7.698 -0.083