% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 42857 % Primary Name: UPPER PINE CREEK 2 % Record Type: TAVG % Country: United States % State: WA % Latitude: 48.65587 +/- 0.01088 % Longitude: -119.64412 +/- 0.01087 % Elevation (m): 994.10 +/- 55.05 % # of Months: 28 % % Alternate Names: UPPER PINE CREEK % % IDs: coop - 458728 % coop - 458729 % ghcnd - USC00458728 % ghcnd - USC00458729 % ncdc - 20027964 % ncdc - 20027965 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 04812e42356760cc0819d97b839f45dc % Raw Data Hash: 8ed2277bb51e43a29a4188f654d13887 % Adj Data Hash: e4240eb0e848bdfe06122f8edfc75de2 % % 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 1959 1 NaN NaN NaN NaN NaN NaN -7.270 0.618 1959 2 NaN NaN NaN NaN NaN NaN -4.764 -0.605 1959 3 NaN NaN NaN NaN NaN NaN -0.911 0.087 1959 4 NaN NaN NaN NaN NaN NaN 3.701 0.019 1959 5 NaN NaN NaN NaN NaN NaN 7.067 -1.423 1959 6 NaN NaN NaN NaN NaN NaN 11.319 -0.811 1959 7 NaN NaN NaN NaN NaN NaN 15.825 0.388 1959 8 NaN NaN NaN NaN NaN NaN 13.067 -1.757 1959 9 NaN NaN NaN NaN NaN NaN 9.289 -1.239 1959 10 NaN NaN NaN NaN NaN NaN 4.214 -0.000 1959 11 NaN NaN NaN NaN NaN NaN -4.165 -2.061 1959 12 NaN NaN NaN NaN NaN NaN -4.479 1.439 1960 1 -7.111 -1.143 0 0 -7.103 -1.135 -8.546 -0.658 1960 2 -2.444 -0.206 0 0 -2.436 -0.197 -3.077 1.082 1960 3 0.944 0.022 0 0 0.953 0.030 -1.274 -0.276 1960 4 5.444 -0.158 0 0 5.453 -0.149 3.462 -0.220 1960 5 8.889 -1.522 0 0 8.897 -1.513 6.989 -1.501 1960 6 14.222 0.172 0 0 14.231 0.181 11.636 -0.494 1960 7 21.222 3.865 0 0 21.231 3.873 17.918 2.481 1960 8 15.833 -0.911 0 0 15.842 -0.902 13.882 -0.941 1960 9 13.278 0.829 0 0 13.286 0.837 10.315 -0.214 1960 10 8.056 1.921 0 0 8.064 1.930 5.720 1.506 1960 11 -0.222 -0.039 0 0 -0.214 -0.030 -2.353 -0.250 1960 12 -4.944 -0.947 0 0 -4.936 -0.939 -6.024 -0.106 1961 1 -3.944 2.023 0 0 -3.936 2.032 -5.092 2.797 1961 2 -0.333 1.905 0 0 -0.325 1.914 -0.699 3.461 1961 3 1.389 0.466 0 0 1.397 0.475 -0.286 0.712 1961 4 4.944 -0.658 0 1 4.935 -0.668 3.087 -0.595 1961 5 10.500 0.089 0 0 10.490 0.079 8.404 -0.086 1961 6 16.667 2.617 0 0 16.657 2.607 14.242 2.113 1961 7 19.556 2.198 0 0 19.546 2.188 16.760 1.323 1961 8 21.000 4.256 0 0 20.990 4.246 17.313 2.489 1961 9 11.167 -1.282 0 0 11.157 -1.292 9.198 -1.331 1961 10 4.778 -1.357 0 0 4.768 -1.367 3.308 -0.906 1961 11 -2.889 -2.706 0 0 -2.899 -2.716 -4.423 -2.319 1961 12 -5.333 -1.336 0 0 -5.343 -1.346 -6.047 -0.130 1962 1 -6.778 -0.810 0 0 -6.788 -0.820 -8.450 -0.561 1962 2 -2.000 0.239 0 0 -2.010 0.229 -2.651 1.509 1962 3 -0.333 -1.256 0 0 -0.343 -1.266 -2.676 -1.678 1962 4 7.500 1.898 0 0 7.490 1.888 4.646 0.964 1962 5 NaN NaN NaN NaN NaN NaN 7.157 -1.333 1962 6 NaN NaN NaN NaN NaN NaN 11.139 -0.991 1962 7 NaN NaN NaN NaN NaN NaN 14.841 -0.596 1962 8 NaN NaN NaN NaN NaN NaN 13.510 -1.314 1962 9 NaN NaN NaN NaN NaN NaN 11.187 0.658 1962 10 NaN NaN NaN NaN NaN NaN 5.135 0.921 1962 11 NaN NaN NaN NaN NaN NaN -0.167 1.937 1962 12 NaN NaN NaN NaN NaN NaN -2.743 3.174 1963 1 NaN NaN NaN NaN NaN NaN -9.347 -1.458 1963 2 NaN NaN NaN NaN NaN NaN -0.664 3.495 1963 3 NaN NaN NaN NaN NaN NaN 0.128 1.126 1963 4 NaN NaN NaN NaN NaN NaN 2.942 -0.739