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\begin{document}
\title{Auxillary Material for: The Fossil Fuel Emission Source of Tokyo estimated directly from measurements of the TCCON site Tsukuba}
\runningtitle{Auxilliary for Tokyo Emissions}

\Author[1]{Arne}{Babenhauserheide}
\Author[1]{Frank}{Hase}
\affil[1]{IMK-ASF, Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany}

%% The [] brackets identify the author with the corresponding affiliation. 1, 2, 3, etc. should be inserted.

\runningauthor{A.~Babenhauserheide}

\correspondence{Arne Babenhauserheide (arne.babenhauserheide@kit.edu)}


\received{}
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\firstpage{1}
\maketitle


\section{Wind direction vs. time of day}

\begin{figure}[tbh]
\includegraphics[width=8.3cm]{tsukuba-wind-direction-vs-time-of-day.pdf}
\caption{Histogram of Wind directions vs. time of day. This graph shows that between 11:00 and 16:00 there is only weak correlation between time of day and wind direction. The horizontal lines mark the lower and upper limit of the densely measured time of day. The measurements between 170 and 240 degree wind direction correspond to wind from Tokyo area. This graph is generated from the script \texttt{plot\_daytime\_vs\_direction.py}.\label{fig:tsukuba-wind-direction-vs-time-of-day}}
\end{figure}

\section{Calculating emissions from a circular source}

The calculation of the emissions from Tokyo in the main article assumes that the distribution around the center is symmetric parallel to the wind direction. To complement 

\clearpage

\section{Radiosonde data from Pangea}

The four years of radiosonde data from Tateno is also availble in monthly format from the PANGEA data archive \citep{ohkawara2011rmfs2010-10--756004,ohkawara2011rmfs2010-11--756007,ohkawara2011rmfs2010-12--757384,ohkawara2011rmfs2011-01--758371,ohkawara2011rmfs2011-02--759843,ohkawara2011rmfs2011-03--760735,ohkawara2011rmfs2011-04--761890,ijima2011rmfs2011-05--763185,ijima2011rmfs2011-06--763986,ijima2011rmfs2011-07--771235,ijima2011rmfs2011-08--771239,ijima2011rmfs2011-09--772273,ijima2012rmfs2011-05--785526,ijima2012rmfs2011-06--785529,ijima2012rmfs2011-07--785532,ijima2012rmfs2011-10--774618,ijima2012rmfs2011-11--774621,ijima2012rmfs2011-12--776358,ijima2012rmfs2012-01--778115,ijima2012rmfs2012-02--779922,ijima2012rmfs2012-03--782752,ijima2012rmfs2012-04--785328,ijima2012rmfs2012-05--786485,ijima2012rmfs2012-06--787818,ijima2012rmfs2012-07--789196,ijima2012rmfs2012-08--792720,ijima2012rmfs2012-09--802530,ijima2012rmfs2012-10--804565,ijima2013rmfs2012-11--807278,ijima2013rmfs2012-12--808173,ijima2013rmfs2013-01--809575,ijima2013rmfs2013-02--810635,ijima2013rmfs2013-03--814021,ijima2013rmfs2013-04--816086,ijima2013rmfs2013-05--817263,ijima2013rmfs2013-06--818904,ijima2014rmfs2013-07--825266,ijima2014rmfs2013-08--825269,ijima2014rmfs2013-09--825445,ijima2014rmfs2013-10--825448,ijima2014rmfs2013-11--830195,ijima2014rmfs2013-12--830198,ijima2014rmfs2014-01--830879,ijima2014rmfs2014-02--832439,ijima2014rmfs2014-03--833333,ijima2014rmfs2014-04--833995,ijima2014rmfs2014-05--836110,ijima2014rmfs2014-06--835976,ijima2014rmfs2014-07--836210,ijima2014rmfs2014-08--840480,ijima2014rmfs2014-09--840366,ijima2014rmfs2014-10--840974,ijima2015rmfs2014-11--841826,ijima2015rmfs2014-12--844179,ijima2015rmfs2015-01--844490,ijima2015rmfs2015-02--845887,ijima2015rmfs2015-03--846450,ijima2015rmfs2015-04--848227,ijima2015rmfs2015-05--848633,ijima2015rmfs2015-06--849122,ijima2015rmfs2015-07--854635,ijima2015rmfs2015-08--854638,ijima2015rmfs2015-09--856039,ijima2016rmfs2015-10--856619,ijima2016rmfs2015-11--858026,ijima2016rmfs2015-12--858510,ijima2016rmfs2016-01--859349,ijima2016rmfs2016-02--859940,ijima2016rmfs2016-03--860804,ijima2016rmfs2016-04--861986,ijima2016rmfs2016-05--864214,ijima2016rmfs2016-06--864225,ijima2016rmfs2016-07--865130,ijima2016rmfs2016-08--867412,ijima2016rmfs2016-09--868997}.


% (* 78e3 0.04 60 60 24 365.25 1e-9)

\clearpage

\section{Trajectory calculations for Tokyo}

The HYSPLIT model \citep{Stein2015} allows calculating high resolution trajectories. This was used to verify the assumptions of vertical transport in this publication. Most of the trajectories calculated for this publication only extend up to 1000m even though they extend much further in horizontal direction than the 65 km from Tokyo to Tsukuba. This shows that it is viable to use the wind speed in the lower 1000m as base for a mean wind speed profile. The trajectory graphs show sample results.

\begin{figure}[tbh]
\includegraphics[width=8.3cm]{tokyo-5-hours-trajplot_14938.pdf}
\caption{5 hours trajectory plot starting at Tokyo. Required information to reproduce the graph is contained in the figure. Published with permission from NOAA ARL, under the condition that it is made it clear that they are not producing these images for us. Which we hereby do: To produce these images we used the great HYSPLIT from NOAA ARL, but the images were not created by someone for us.}
\end{figure}

\begin{figure}[tbh]
\includegraphics[width=8.3cm]{2017-06-30-fhtagn-steno-tokyo-rlyeh-cthulhu-fhtagn-trajectories-from-tokyo.jpg}
\caption{Required information to reproduce the graph is contained in the figure. Published with permission from NOAA ARL, under the condition that it is made it clear that they are not producing these images for us. Which we hereby do: To produce these images we used the great HYSPLIT from NOAA ARL, but the images were not created by someone for us. Some visual glitches surrounding the graph occurred when scanning a printed version of the document. These might not reproduce.}
\end{figure}

\begin{figure}[tbh]
\includegraphics[width=8.3cm]{trajplot_197390.pdf}
\caption{10 hours trajectory plot starting at Tokyo. Required information to reproduce the graph is contained in the figure. Published with permission from NOAA ARL, under the condition that it is made it clear that they are not producing these images for us. Which we hereby do: To produce these images we used the great HYSPLIT from NOAA ARL, but the images were not created by someone for us.}
\end{figure}


\clearpage

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