% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 36964 % Primary Name: MIDDLETOWN 2 NE NEWPORT % Record Type: TAVG % Country: United States % State: RI % Latitude: 41.50000 +/- 0.00005 % Longitude: -71.26670 +/- 0.00005 % Elevation (m): 31.10 +/- 0.05 % # of Months: 19 % % Alternate Names: MIDDLETOWN 2 NE NEWP % MIDDLETOWN 2 NE NEWPOR % % IDs: coop - 375002 % ghcnd - USC00375002 % ncdc - 20017293 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 513af94120acc44bd4bcf0474c1a3b3f % Raw Data Hash: 7fa776e2ac8507f91ada7053d4e8a1d9 % Adj Data Hash: e4bb1ff640ed31ce09f7e376ef436c22 % % 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 1945 12 NaN NaN NaN NaN NaN NaN 0.198 -3.295 1946 1 NaN NaN NaN NaN NaN NaN 1.490 0.385 1946 2 NaN NaN NaN NaN NaN NaN -0.171 -0.976 1946 3 NaN NaN NaN NaN NaN NaN 7.132 3.758 1946 4 NaN NaN NaN NaN NaN NaN 6.312 -0.689 1946 5 NaN NaN NaN NaN NaN NaN 11.375 -0.114 1946 6 NaN NaN NaN NaN NaN NaN 15.755 -0.496 1946 7 NaN NaN NaN NaN NaN NaN 19.123 -0.781 1946 8 NaN NaN NaN NaN NaN NaN 18.688 -1.596 1946 9 NaN NaN NaN NaN NaN NaN 18.265 0.606 1946 10 NaN NaN NaN NaN NaN NaN 14.680 1.531 1946 11 NaN NaN NaN NaN NaN NaN 10.765 1.967 1946 12 0.826 -1.933 1 0 NaN NaN 4.033 0.541 1947 1 0.908 0.537 0 0 0.908 0.537 3.318 2.213 1947 2 -1.376 -1.447 1 0 NaN NaN -0.013 -0.818 1947 3 1.808 -0.832 0 0 1.808 -0.832 2.725 -0.649 1947 4 6.658 0.390 1 0 NaN NaN 6.597 -0.404 1947 5 11.552 0.797 0 0 11.552 0.797 11.140 -0.348 1947 6 15.927 0.410 0 0 15.927 0.410 14.931 -1.319 1947 7 21.844 2.673 0 0 21.844 2.673 20.793 0.889 1947 8 21.274 1.724 0 0 21.274 1.724 20.998 0.713 1947 9 17.638 0.713 0 0 17.638 0.713 18.053 0.394 1947 10 14.218 1.802 1 0 NaN NaN 15.589 2.439 1947 11 4.767 -3.298 0 0 4.767 -3.298 7.581 -1.218 1947 12 -1.021 -3.780 0 0 -1.021 -3.780 1.452 -2.040 1948 1 -4.523 -4.894 0 0 -4.523 -4.894 -1.376 -2.481 1948 2 -3.556 -3.626 1 0 NaN NaN -1.200 -2.005 1948 3 2.053 -0.587 0 0 2.053 -0.587 3.443 0.069 1948 4 NaN NaN NaN NaN NaN NaN 6.705 -0.296 1948 5 NaN NaN NaN NaN NaN NaN 10.665 -0.824 1948 6 NaN NaN NaN NaN NaN NaN 14.862 -1.389 1948 7 21.094 1.923 0 0 21.094 1.923 20.202 0.298 1948 8 21.385 1.835 0 0 21.385 1.835 20.953 0.669 1948 9 16.998 0.073 0 0 16.998 0.073 17.763 0.104 1948 10 NaN NaN NaN NaN NaN NaN 12.660 -0.489 1948 11 NaN NaN NaN NaN NaN NaN 11.565 2.766 1948 12 NaN NaN NaN NaN NaN NaN 4.118 0.626 1949 1 NaN NaN NaN NaN NaN NaN 4.372 3.267 1949 2 NaN NaN NaN NaN NaN NaN 3.010 2.206 1949 3 NaN NaN NaN NaN NaN NaN 3.995 0.622 1949 4 NaN NaN NaN NaN NaN NaN 8.408 1.407 1949 5 NaN NaN NaN NaN NaN NaN 11.916 0.428 1949 6 NaN NaN NaN NaN NaN NaN 17.897 1.647 1949 7 NaN NaN NaN NaN NaN NaN 21.733 1.829 1949 8 NaN NaN NaN NaN NaN NaN 21.369 1.085 1949 9 NaN NaN NaN NaN NaN NaN 17.321 -0.338