<?xml version="1.0" encoding="utf-8"?><rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns="http://purl.org/rss/1.0/" xmlns:dc="http://purl.org/dc/elements/1.1/"><channel rdf:about="http://www.adv-sci-res.net/xml/rss1_0.xml"><title>ASR - Latest Articles</title><link>http://www.adv-sci-res.net/</link><description>Advances in Science and Research Latest Articles</description><items><rdf:Seq><rdf:li resource="http://www.adv-sci-res.net/4/99/2010/" /><rdf:li resource="http://www.adv-sci-res.net/4/89/2010/" /><rdf:li resource="http://www.adv-sci-res.net/4/83/2010/" /><rdf:li resource="http://www.adv-sci-res.net/4/77/2010/" /></rdf:Seq></items></channel><item rdf:about="http://www.adv-sci-res.net/4/99/2010/"><title>Describing the possible climate changes in France and some examples of their effects on main crops used in livestock systems</title><link>http://www.adv-sci-res.net/4/99/2010/</link><description>&lt;b&gt;Describing the possible climate changes in France and some examples of their effects on main crops used in livestock systems&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Advances in Science and Research, 4, 99-104, 2010&lt;br /&gt;&lt;br /&gt;Author(s): F. Ruget, J.-C. Moreau, M. Ferrand, S. Poisson, P. Gate, B. Lacroix, J. Lorgeou, E. Cloppet, and F. Souverain&lt;br /&gt;&lt;br /&gt;The effects of climate change on forage and crop production are an important
question for the farmers and more largely for the food security in the
world. Estimating the effect of climate change on agricultural production
needs the use of two types of tools: a model to estimate changes in national
or local climates and an other model using climatic data to estimate the
effects on vegetation. In this paper, we will mainly present the effects of
climate change on climatic features, the variability of criteria influencing
crop production in various regions of France and some possible effects on
crops.</description><dc:date>2010-08-02T00:00:00+02:00</dc:date></item><item rdf:about="http://www.adv-sci-res.net/4/89/2010/"><title>Evaluating multi-scale precipitation forecasts using high resolution analysis</title><link>http://www.adv-sci-res.net/4/89/2010/</link><description>&lt;b&gt;Evaluating multi-scale precipitation forecasts using high resolution analysis&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Advances in Science and Research, 4, 89-98, 2010&lt;br /&gt;&lt;br /&gt;Author(s): C. Wittmann, T. Haiden, and A. Kann&lt;br /&gt;&lt;br /&gt;The SAL (Structure, Amplitude, Location) method is used for verification of
precipitation forecasts at horizontal grid spacings ranging from 2.5 km to
25 km, using a high-resolution 1 km precipitation analysis as a reference.
The verification focuses on a summertime period with predominantly
convective precipitation. The verification domain contains lowland as well
as alpine areas. Evaluation of the individual SAL components shows that with
regard to area mean values (&lt;i&gt;A&lt;/i&gt;) the benefit of high resolutions models
becomes apparent only in high impact weather situations. For the summertime
period studied, the subjective impression of better structured precipitation
fields (&lt;i&gt;S&lt;/i&gt;) in higher resolution models can generally be confirmed. The most
significant improvement appears to be associated with explicit simulation of
deep convection.</description><dc:date>2010-07-15T00:00:00+02:00</dc:date></item><item rdf:about="http://www.adv-sci-res.net/4/83/2010/"><title>WRF model and ASAR-retrieved 10 m wind field comparison in a case study over Eastern Mediterranean Sea</title><link>http://www.adv-sci-res.net/4/83/2010/</link><description>&lt;b&gt;WRF model and ASAR-retrieved 10 m wind field comparison in a case study over Eastern Mediterranean Sea&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Advances in Science and Research, 4, 83-88, 2010&lt;br /&gt;&lt;br /&gt;Author(s): M. M. Miglietta, S. Zecchetto, and F. De Biasio&lt;br /&gt;&lt;br /&gt;In Synthetic Aperture Radar (SAR) imagery, signatures of coherent
atmospheric structures, due to sea surface roughness modulation by surface
winds, are usually well detected. In the present study, the wind field derived from the Envisat Advanced SAR (ASAR) sensor has been analyzed and
compared with those simulated with a regional atmospheric model in a case
study over an area located in the eastern Mediterranean Sea, extending
southward and eastward of Crete island. This is a region subject to complex
wind patterns, due to the interaction of the almost steady northerly Etesian
wind with the orography of the islands in the region.

&lt;br&gt;&lt;br&gt;
The ASAR Wide Swath Mode images provide datasets at resolutions
exceptionally high compared to model data, appropriate for investigating the
mesoscale phenomena on the marine atmospheric boundary layer and to retrieve the surface wind field. The latter has been obtained with a
methodology based on the 2-D Continuous Wavelet Transform, suitable to
isolate the backscatter patterns on the base of energy and scale
considerations.

&lt;br&gt;&lt;br&gt;
Numerical simulations with the Weather Research and Forecasting (WRF) model
have been performed using three 2-way nested domains, the inner one covering
the area of interest with a resolution of 1 km. Several simulations, using
different diffusion and boundary layer parameterization schemes, have been
performed in a case study corresponding to mountain lee waves detected in
the ASAR image. The 10 m winds resulting from the numerical experiments have
been compared to those retrieved from the ASAR, both quantitatively and
qualitatively, in order to analyze the correspondence of observed and
simulated wind structures.</description><dc:date>2010-07-01T00:00:00+02:00</dc:date></item><item rdf:about="http://www.adv-sci-res.net/4/77/2010/"><title>Tornado-type stationary vortex with nonlinear term due to moisture transport</title><link>http://www.adv-sci-res.net/4/77/2010/</link><description>&lt;b&gt;Tornado-type stationary vortex with nonlinear term due to moisture transport&lt;/b&gt;&lt;br /&gt;&lt;br /&gt;Advances in Science and Research, 4, 77-82, 2010&lt;br /&gt;&lt;br /&gt;Author(s): P. B. Rutkevich and P. P. Rutkevych&lt;br /&gt;&lt;br /&gt;Tornado vortex is believed to be essentially
nonlinear phenomenon;
and the puzzle to choose the nonlinear term(s) responsible for its
formation is still unresolved.
In the
present work we consider the nonlinear term associated with atmosphere humidity,
by introducing variable temperature gradient depending on the vertical velocity
of the fluid.
Such term is able to yield energy
to the system and is very suitable for such a problem.
Other nonlinear terms are neglected, assuming
slow rotation, or in other words a &quot;weak&quot; tornado approximation.
We consider one-dimensional radial boundary problem,
and use a modificaiton of shooting method to satisfy boundary conditions
at large radii.
Obtained numerical solutions of the nonlinear differential equation
qualitatively agree with the observed atmosphere vortices
(tornados, tropical cyclones).
The obtained results show general possibility of existence
of unstable motion even in convectively stable atmosphere stratification.</description><dc:date>2010-06-14T00:00:00+02:00</dc:date></item></rdf:RDF>