% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39151 % Primary Name: HOFFMEISTER 3 W % Record Type: TAVG % Country: United States % State: NY % Latitude: 43.38330 +/- 0.00005 % Longitude: -74.73330 +/- 0.00005 % Elevation (m): 573.00 +/- 0.05 % # of Months: 18 % % Alternate Names: HOFFMEISTER % % IDs: coop - 303916 % ghcnd - USC00303916 % ncdc - 20020059 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: d51c79765ab89da289bfa9d77e076f42 % Raw Data Hash: f6b0b96a7aee9c3c811114ebfe7b96c2 % Adj Data Hash: 9d0b5cabd781528ad359fec000730028 % % 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 7 NaN NaN NaN NaN NaN NaN 19.408 -1.680 1962 8 NaN NaN NaN NaN NaN NaN 19.404 -0.563 1962 9 NaN NaN NaN NaN NaN NaN 13.983 -1.665 1962 10 NaN NaN NaN NaN NaN NaN 9.351 -0.089 1962 11 NaN NaN NaN NaN NaN NaN 1.905 -1.644 1962 12 NaN NaN NaN NaN NaN NaN -5.799 -2.363 1963 1 NaN NaN NaN NaN NaN NaN -7.206 -0.907 1963 2 NaN NaN NaN NaN NaN NaN -8.901 -3.703 1963 3 NaN NaN NaN NaN NaN NaN 0.644 0.431 1963 4 NaN NaN NaN NaN NaN NaN 6.906 -0.268 1963 5 NaN NaN NaN NaN NaN NaN 12.568 -0.892 1963 6 NaN NaN NaN NaN NaN NaN 18.434 -0.084 1963 7 19.322 -0.892 1 0 NaN NaN 21.228 0.140 1963 8 14.500 -4.592 0 0 14.500 -4.592 18.191 -1.775 1963 9 10.611 -4.163 0 0 10.611 -4.163 13.232 -2.416 1963 10 NaN NaN NaN NaN NaN NaN 12.204 2.764 1963 11 NaN NaN NaN NaN NaN NaN 6.903 3.354 1963 12 NaN NaN NaN NaN NaN NaN -7.722 -4.286 1964 1 -4.333 2.840 0 1 -4.333 2.840 -5.068 1.231 1964 2 -7.500 -1.428 0 0 -7.500 -1.428 -6.137 -0.939 1964 3 -0.722 -0.061 0 0 -0.722 -0.061 1.050 0.837 1964 4 4.500 -1.800 0 0 4.500 -1.800 6.871 -0.303 1964 5 15.111 2.525 0 0 15.111 2.525 15.073 1.613 1964 6 17.944 0.301 0 0 17.944 0.301 17.768 -0.749 1964 7 19.667 -0.547 0 0 19.667 -0.547 22.221 1.133 1964 8 17.278 -1.815 0 0 17.278 -1.815 18.065 -1.902 1964 9 14.000 -0.774 0 0 14.000 -0.774 15.526 -0.122 1964 10 11.222 2.656 0 0 11.222 2.656 8.716 -0.724 1964 11 7.444 4.769 0 0 7.444 4.769 5.459 1.910 1964 12 -2.611 1.699 0 0 -2.611 1.699 -3.252 0.184 1965 1 -8.611 -1.437 0 0 -8.611 -1.437 -7.857 -1.558 1965 2 -7.833 -1.761 0 0 -7.833 -1.761 -5.532 -0.334 1965 3 -1.833 -1.172 0 0 -1.833 -1.172 -0.631 -0.844 1965 4 NaN NaN NaN NaN NaN NaN 5.483 -1.691 1965 5 NaN NaN NaN NaN NaN NaN 14.996 1.536 1965 6 NaN NaN NaN NaN NaN NaN 17.537 -0.980 1965 7 NaN NaN NaN NaN NaN NaN 19.604 -1.484 1965 8 NaN NaN NaN NaN NaN NaN 19.820 -0.147 1965 9 NaN NaN NaN NaN NaN NaN 15.917 0.269 1965 10 NaN NaN NaN NaN NaN NaN 8.639 -0.801 1965 11 NaN NaN NaN NaN NaN NaN 3.302 -0.248 1965 12 NaN NaN NaN NaN NaN NaN -1.670 1.766 1966 1 NaN NaN NaN NaN NaN NaN -6.451 -0.151 1966 2 NaN NaN NaN NaN NaN NaN -5.185 0.013 1966 3 NaN NaN NaN NaN NaN NaN 0.744 0.531