% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 29507 % Primary Name: STRINGTOWN % Record Type: TAVG % Country: United States % State: OK % Latitude: 34.53330 +/- 0.00005 % Longitude: -96.03330 +/- 0.00005 % Elevation (m): 181.66 +/- 0.15 % # of Months: 20 % % Alternate Names: Missing Station ID - 348550 % % IDs: coop - 348550 % ghcnd - USC00348550 % ncdc - 12004259 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % Multi-network Metadata System % % Site Hash: beb36c9c913d1d0695962f5e492d442d % Raw Data Hash: 7f6db7bf25c145fb79378c525a5225cc % Adj Data Hash: 9fc5dbc22d46def0593c0cd027bca232 % % 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 1939 4 NaN NaN NaN NaN NaN NaN 15.526 -1.067 1939 5 NaN NaN NaN NaN NaN NaN 21.308 0.477 1939 6 NaN NaN NaN NaN NaN NaN 25.662 0.558 1939 7 NaN NaN NaN NaN NaN NaN 28.846 1.148 1939 8 NaN NaN NaN NaN NaN NaN 27.733 0.539 1939 9 NaN NaN NaN NaN NaN NaN 27.285 3.911 1939 10 NaN NaN NaN NaN NaN NaN 19.418 2.160 1939 11 NaN NaN NaN NaN NaN NaN 9.691 -1.003 1939 12 NaN NaN NaN NaN NaN NaN 8.676 2.572 1940 1 NaN NaN NaN NaN NaN NaN -2.451 -6.567 1940 2 NaN NaN NaN NaN NaN NaN 5.764 -1.015 1940 3 NaN NaN NaN NaN NaN NaN 11.843 0.745 1940 4 18.638 1.173 1 0 NaN NaN 15.831 -0.762 1940 5 NaN NaN NaN NaN NaN NaN 19.319 -1.512 1940 6 25.411 -0.565 1 0 NaN NaN 24.022 -1.082 1940 7 26.442 -2.129 0 0 26.442 -2.129 26.040 -1.658 1940 8 27.392 -0.674 0 0 27.392 -0.674 25.613 -1.581 1940 9 24.177 -0.070 0 0 24.177 -0.070 22.313 -1.061 1940 10 20.211 2.081 0 0 20.211 2.081 19.022 1.764 1940 11 9.905 -1.662 0 0 9.905 -1.662 9.537 -1.157 1940 12 7.544 0.567 1 0 NaN NaN 7.809 1.705 1941 1 7.408 2.420 0 0 7.408 2.420 6.208 2.092 1941 2 NaN NaN NaN NaN NaN NaN 5.493 -1.286 1941 3 9.726 -2.245 0 0 9.726 -2.245 8.454 -2.644 1941 4 17.553 0.088 0 0 17.553 0.088 17.372 0.779 1941 5 22.798 1.095 0 0 22.798 1.095 21.957 1.126 1941 6 24.392 -1.585 0 0 24.392 -1.585 24.128 -0.976 1941 7 28.465 -0.106 0 0 28.465 -0.106 27.672 -0.027 1941 8 27.563 -0.503 0 0 27.563 -0.503 27.183 -0.011 1941 9 25.210 0.963 0 0 25.210 0.963 24.459 1.085 1941 10 20.595 2.465 0 0 20.595 2.465 20.097 2.840 1941 11 11.475 -0.092 0 0 11.475 -0.092 10.402 -0.292 1941 12 8.356 1.380 0 0 8.356 1.380 7.528 1.424 1942 1 4.113 -0.876 0 0 4.113 -0.876 2.962 -1.154 1942 2 NaN NaN NaN NaN NaN NaN 5.894 -0.886 1942 3 NaN NaN NaN NaN NaN NaN 10.833 -0.265 1942 4 NaN NaN NaN NaN NaN NaN 17.293 0.700 1942 5 NaN NaN NaN NaN NaN NaN 19.859 -0.972 1942 6 NaN NaN NaN NaN NaN NaN 25.238 0.134 1942 7 NaN NaN NaN NaN NaN NaN 27.113 -0.585 1942 8 NaN NaN NaN NaN NaN NaN 26.660 -0.534 1942 9 NaN NaN NaN NaN NaN NaN 21.983 -1.391 1942 10 NaN NaN NaN NaN NaN NaN 17.285 0.028 1942 11 NaN NaN NaN NaN NaN NaN 13.187 2.492 1942 12 NaN NaN NaN NaN NaN NaN 6.658 0.554 1943 1 NaN NaN NaN NaN NaN NaN 4.543 0.427