-
Notifications
You must be signed in to change notification settings - Fork 0
/
Copy pathagu_session.tex
40 lines (35 loc) · 1.83 KB
/
agu_session.tex
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
\begin{frame}
\frametitle{AGU Fall Meeting Session Advertisement}\small
\begin{center}
\vskip-0.15in
\textbf{\large Big Data in the Geosciences: \\ New Analytics Methods and Parallel Algorithms}
\end{center}
\medskip
\vbox{\footnotesize\textit{Co-conveners: Jitendra~Kumar (ORNL), Robert~L.~Jacob (ANL), Forrest~M.~Hoffman (ORNL), and Miguel~D.~Mahecha (MPI-Jena)}}
% \medskip
% \textbf{Confirmed Invited Presenters:}
% \begin{itemize}
% \item Gary Geernaert (U.S. Dept. of Energy)
% \item Matt Hancher (Google Earth Engine)
% \item Jeff Daily (Pacific Northwest National Laboratory)
% \item William Hargrove (USDA Forest Service)
% \end{itemize}
\medskip
\vbox{\footnotesize Earth and space science data are increasingly large and
complex--often representing high spatial/temporal/spectral resolution
and dimensions from remote sensing or model results--making such data
difficult to analyze, visualize, interpret, and understand by traditional
methods. This session focuses on application and development of new
geoscientific data analytics approaches (statistical, data mining,
assimilation, machine learning, etc.) and parallel algorithms and
software employing high performance computing resources for scalable
analysis and novel applications of traditional methods on large
geoscience data sets. Analysis methods that operate in-situ with
parallel simulations to reduce output data volumes are also of interest.
Abstracts focused on analysis, synthesis and knowledge extraction from
large and complex Earth science data from all disciplines are invited.}
\bigskip
\centerline{\color{red} \textbf{Abstract submissions are due 6 August 2014, 23:59 EDT/03:59 +1 GMT}}
\end{frame}
%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%