% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 36817 % Primary Name: CLEVELAND SEVEN HILLS % Record Type: TAVG % Country: United States % State: OH % Latitude: 41.36670 +/- 0.00005 % Longitude: -81.66670 +/- 0.00005 % Elevation (m): 351.10 +/- 0.05 % # of Months: 14 % % Alternate Names: CLEVELAND SEVEN HILL % % IDs: coop - 331650 % ghcnd - USC00331650 % ncdc - 20015592 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 0ab57791d75dc72c246a8d117492c836 % Raw Data Hash: 1c4d45493c2f45dd16f7133efb8c6d1c % Adj Data Hash: 84067e9fc0cfc022bfba0f6a0b29ab4a % % 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 1947 1 NaN NaN NaN NaN NaN NaN 0.029 3.633 1947 2 NaN NaN NaN NaN NaN NaN -6.309 -3.940 1947 3 NaN NaN NaN NaN NaN NaN -0.300 -3.251 1947 4 NaN NaN NaN NaN NaN NaN 9.471 0.162 1947 5 NaN NaN NaN NaN NaN NaN 13.289 -1.807 1947 6 NaN NaN NaN NaN NaN NaN 19.258 -0.763 1947 7 NaN NaN NaN NaN NaN NaN 20.241 -1.919 1947 8 NaN NaN NaN NaN NaN NaN 24.411 2.980 1947 9 NaN NaN NaN NaN NaN NaN 18.773 0.994 1947 10 NaN NaN NaN NaN NaN NaN 15.300 4.080 1947 11 NaN NaN NaN NaN NaN NaN 3.833 -1.307 1947 12 NaN NaN NaN NaN NaN NaN -1.173 -0.293 1948 1 -7.000 -3.123 0 0 -7.000 -3.123 -7.593 -3.990 1948 2 -2.222 0.420 0 0 -2.222 0.420 -2.513 -0.145 1948 3 3.444 0.766 0 0 3.444 0.766 4.662 1.710 1948 4 NaN NaN NaN NaN NaN NaN 11.836 2.527 1948 5 13.000 -1.823 0 0 13.000 -1.823 13.695 -1.401 1948 6 NaN NaN NaN NaN NaN NaN 19.799 -0.223 1948 7 NaN NaN NaN NaN NaN NaN 22.363 0.203 1948 8 NaN NaN NaN NaN NaN NaN 21.064 -0.366 1948 9 18.111 0.605 0 0 18.111 0.605 18.367 0.588 1948 10 9.722 -1.225 0 0 9.722 -1.225 9.540 -1.681 1948 11 7.556 2.688 0 0 7.556 2.688 8.129 2.989 1948 12 -0.056 1.097 0 0 -0.056 1.097 0.287 1.166 1949 1 0.833 4.710 0 0 0.833 4.710 1.197 4.801 1949 2 1.000 3.642 0 0 1.000 3.642 0.980 3.349 1949 3 1.667 -1.011 0 0 1.667 -1.011 3.649 0.698 1949 4 8.278 -0.758 0 0 8.278 -0.758 8.543 -0.766 1949 5 15.722 0.899 0 0 15.722 0.899 15.881 0.785 1949 6 23.333 3.585 0 0 23.333 3.585 22.389 2.368 1949 7 NaN NaN NaN NaN NaN NaN 24.322 2.162 1949 8 NaN NaN NaN NaN NaN NaN 21.971 0.540 1949 9 NaN NaN NaN NaN NaN NaN 15.757 -2.022 1949 10 NaN NaN NaN NaN NaN NaN 14.142 2.921 1949 11 NaN NaN NaN NaN NaN NaN 5.479 0.339 1949 12 NaN NaN NaN NaN NaN NaN 0.936 1.816 1950 1 NaN NaN NaN NaN NaN NaN 2.651 6.255 1950 2 NaN NaN NaN NaN NaN NaN -1.754 0.615 1950 3 NaN NaN NaN NaN NaN NaN 0.933 -2.018 1950 4 NaN NaN NaN NaN NaN NaN 6.589 -2.720 1950 5 NaN NaN NaN NaN NaN NaN 15.185 0.089 1950 6 NaN NaN NaN NaN NaN NaN 19.348 -0.673