% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 44453 % Primary Name: NORTH POLE 6 % Record Type: TAVG % Country: Ocean Weather Stations % Latitude: 85.40000 +/- 0.05000 % Longitude: 28.10000 +/- 0.05000 % Elevation (m): 0.00 +/- 10.00 % # of Months: 26 % % IDs: hadcru - 990547 % wmssc - 990547 % % Sources: Hadley Centre Data Release % World Monthly Surface Station Climatology % % Site Hash: 401b717fb93d1ef6b2b7be0647e748a7 % Raw Data Hash: cbeb39312de5298edea34997aefbe407 % Adj Data Hash: cbeb39312de5298edea34997aefbe407 % % 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 1955 5 NaN NaN NaN NaN NaN NaN -13.475 -0.925 1955 6 NaN NaN NaN NaN NaN NaN -1.808 1.725 1955 7 NaN NaN NaN NaN NaN NaN -0.558 0.727 1955 8 NaN NaN NaN NaN NaN NaN -0.099 2.495 1955 9 NaN NaN NaN NaN NaN NaN -6.756 2.326 1955 10 NaN NaN NaN NaN NaN NaN -18.593 0.680 1955 11 NaN NaN NaN NaN NaN NaN -30.534 -4.593 1955 12 NaN NaN NaN NaN NaN NaN -30.853 -1.196 1956 1 NaN NaN NaN NaN NaN NaN -31.734 0.643 1956 2 NaN NaN NaN NaN NaN NaN -25.890 6.489 1956 3 NaN NaN NaN NaN NaN NaN -32.292 0.315 1956 4 NaN NaN NaN NaN NaN NaN -24.743 0.457 1956 5 -8.400 3.996 0 0 -8.400 3.996 -10.378 2.171 1956 6 -3.300 0.079 0 0 -3.300 0.079 -3.406 0.127 1956 7 -0.700 0.431 0 0 -0.700 0.431 -0.858 0.427 1956 8 -2.700 -0.260 0 0 -2.700 -0.260 -2.094 0.499 1956 9 NaN NaN NaN NaN NaN NaN -10.737 -1.656 1956 10 NaN NaN NaN NaN NaN NaN -21.148 -1.876 1956 11 NaN NaN NaN NaN NaN NaN -21.083 4.858 1956 12 NaN NaN NaN NaN NaN NaN -21.434 8.223 1957 1 NaN NaN NaN NaN NaN NaN -35.099 -2.722 1957 2 NaN NaN NaN NaN NaN NaN -29.206 3.173 1957 3 NaN NaN NaN NaN NaN NaN -31.881 0.727 1957 4 NaN NaN NaN NaN NaN NaN -25.394 -0.195 1957 5 NaN NaN NaN NaN NaN NaN -10.698 1.852 1957 6 NaN NaN NaN NaN NaN NaN -2.948 0.585 1957 7 -0.300 0.831 0 0 -0.300 0.831 -0.527 0.758 1957 8 -1.800 0.640 0 0 -1.800 0.640 -1.473 1.121 1957 9 -7.900 1.028 0 0 -7.900 1.028 -9.086 -0.005 1957 10 -17.300 1.819 0 0 -17.300 1.819 -17.856 1.417 1957 11 -25.000 0.787 0 0 -25.000 0.787 -25.882 0.059 1957 12 -36.400 -6.897 0 0 -36.400 -6.897 -35.502 -5.845 1958 1 -31.400 0.823 0 0 -31.400 0.823 -31.871 0.506 1958 2 -32.500 -0.275 0 0 -32.500 -0.275 -32.419 -0.040 1958 3 -30.600 1.854 0 0 -30.600 1.854 -31.254 1.353 1958 4 -27.600 -2.554 0 0 -27.600 -2.554 -27.530 -2.331 1958 5 -13.100 -0.704 0 0 -13.100 -0.704 -12.527 0.023 1958 6 -2.000 1.379 0 0 -2.000 1.379 -2.415 1.118 1958 7 0.000 1.131 0 0 0.000 1.131 -0.788 0.497 1958 8 -0.700 1.740 0 0 -0.700 1.740 -0.729 1.864 1958 9 -9.200 -0.272 0 0 -9.200 -0.272 -9.248 -0.166 1958 10 -21.700 -2.581 0 0 -21.700 -2.581 -21.967 -2.694 1958 11 -31.200 -5.413 0 0 -31.200 -5.413 -29.111 -3.170 1958 12 -28.900 0.603 0 0 -28.900 0.603 -29.791 -0.135 1959 1 NaN NaN NaN NaN NaN NaN -35.894 -3.517 1959 2 NaN NaN NaN NaN NaN NaN -32.981 -0.602 1959 3 NaN NaN NaN NaN NaN NaN -32.791 -0.184 1959 4 NaN NaN NaN NaN NaN NaN -22.892 2.307 1959 5 -12.600 -0.204 0 0 -12.600 -0.204 -11.940 0.610 1959 6 -2.000 1.379 0 0 -2.000 1.379 -2.015 1.518 1959 7 -0.200 0.931 0 0 -0.200 0.931 -0.773 0.512 1959 8 -0.900 1.540 0 0 -0.900 1.540 -0.956 1.637 1959 9 NaN NaN NaN NaN NaN NaN -9.244 -0.163 1959 10 NaN NaN NaN NaN NaN NaN -16.857 2.415 1959 11 NaN NaN NaN NaN NaN NaN -20.099 5.842 1959 12 NaN NaN NaN NaN NaN NaN -25.948 3.708 1960 1 NaN NaN NaN NaN NaN NaN -28.132 4.245 1960 2 NaN NaN NaN NaN NaN NaN -34.982 -2.603 1960 3 NaN NaN NaN NaN NaN NaN -32.486 0.122 1960 4 NaN NaN NaN NaN NaN NaN -25.863 -0.663 1960 5 NaN NaN NaN NaN NaN NaN -9.908 2.642 1960 6 NaN NaN NaN NaN NaN NaN -2.595 0.938 1960 7 NaN NaN NaN NaN NaN NaN -0.679 0.606 1960 8 NaN NaN NaN NaN NaN NaN -1.747 0.847