% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39047 % Primary Name: CAREY 2 S % Record Type: TAVG % Country: United States % State: ID % Latitude: 43.28330 +/- 0.00005 % Longitude: -113.95000 +/- 0.00005 % Elevation (m): 1452.10 +/- 0.05 % # of Months: 15 % % IDs: coop - 101461 % ghcnd - USC00101461 % ncdc - 20005183 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: 99303643b96e74975802140f0c39443d % Raw Data Hash: 7db5c9b9e7ea05952b7b68a8ef16c91f % Adj Data Hash: 7db5c9b9e7ea05952b7b68a8ef16c91f % % 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 10 NaN NaN NaN NaN NaN NaN 9.417 1.186 1955 11 NaN NaN NaN NaN NaN NaN -0.902 -2.151 1955 12 NaN NaN NaN NaN NaN NaN -1.395 2.005 1956 1 NaN NaN NaN NaN NaN NaN -1.572 3.204 1956 2 NaN NaN NaN NaN NaN NaN -5.901 -4.144 1956 3 NaN NaN NaN NaN NaN NaN 1.007 -0.375 1956 4 NaN NaN NaN NaN NaN NaN 6.690 0.509 1956 5 NaN NaN NaN NaN NaN NaN 12.722 1.290 1956 6 NaN NaN NaN NaN NaN NaN 15.925 -0.137 1956 7 NaN NaN NaN NaN NaN NaN 21.356 0.446 1956 8 NaN NaN NaN NaN NaN NaN 18.368 -1.344 1956 9 NaN NaN NaN NaN NaN NaN 15.214 0.617 1956 10 7.500 -0.133 0 0 7.500 -0.133 8.095 -0.136 1956 11 -0.667 -1.317 0 0 -0.667 -1.317 -0.797 -2.046 1956 12 -3.778 0.220 0 0 -3.778 0.220 -3.018 0.382 1957 1 -10.222 -4.849 0 0 -10.222 -4.849 -7.843 -3.067 1957 2 -3.444 -1.089 0 0 -3.444 -1.089 -0.110 1.647 1957 3 2.778 1.993 0 0 2.778 1.993 2.053 0.671 1957 4 6.556 0.973 0 0 6.556 0.973 5.463 -0.718 1957 5 12.167 1.333 0 0 12.167 1.333 11.758 0.326 1957 6 15.556 0.092 0 0 15.556 0.092 15.612 -0.450 1957 7 21.222 0.910 0 0 21.222 0.910 21.162 0.252 1957 8 19.056 -0.058 0 0 19.056 -0.058 19.949 0.237 1957 9 NaN NaN NaN NaN NaN NaN 14.882 0.285 1957 10 8.000 0.367 0 0 8.000 0.367 8.349 0.118 1957 11 -1.389 -2.039 0 0 -1.389 -2.039 -1.059 -2.308 1957 12 NaN NaN NaN NaN NaN NaN -1.258 2.142 1958 1 NaN NaN NaN NaN NaN NaN -4.173 0.603 1958 2 -0.444 1.911 0 0 -0.444 1.911 2.575 4.332 1958 3 0.667 -0.118 0 0 0.667 -0.118 0.338 -1.045 1958 4 NaN NaN NaN NaN NaN NaN 4.671 -1.510 1958 5 NaN NaN NaN NaN NaN NaN 15.187 3.755 1958 6 NaN NaN NaN NaN NaN NaN 16.329 0.267 1958 7 NaN NaN NaN NaN NaN NaN 20.220 -0.690 1958 8 NaN NaN NaN NaN NaN NaN 21.405 1.693 1958 9 NaN NaN NaN NaN NaN NaN 14.618 0.020 1958 10 NaN NaN NaN NaN NaN NaN 10.283 2.052 1958 11 NaN NaN NaN NaN NaN NaN 1.267 0.019 1958 12 NaN NaN NaN NaN NaN NaN 0.741 4.140 1959 1 NaN NaN NaN NaN NaN NaN -1.604 3.171 1959 2 NaN NaN NaN NaN NaN NaN -0.368 1.389 1959 3 NaN NaN NaN NaN NaN NaN 1.257 -0.126