Design and use of the MATLAB Parallel Processing Gateway

This report describes a collection of software utilities that together form a "parallel processing gateway" for the computer aided control system design software package,MATLAB. These utilities allow control engineers to configure and boot processes on the parallel computer and concurrent and parallel routines transparently from the MATLAB command line. Here, the requirements of such a gateway, its design, implementation and use and features that enable the control engineer to readily exploit a parallel computer are described and discussed. In addition, the performance of the gateway is assessed in terms of the communications achievable between MATLAB and the parallel computer

Northern winter stratospheric temperature and ozone responses to ENSO inferred from an ensemble of Chemistry Climate Models

The connection between the El Ni˜no Southern Oscillation (ENSO) and the Northern polar stratosphere has been established from observations and atmospheric modeling. Here a systematic inter-comparison of the sensitivity of the modeled stratosphere to ENSO in Chemistry Climate Models (CCMs) is reported. This work uses results from a number of the CCMs included in the 2006 ozone assessment. In the lower stratosphere, the mean of all model simulations reports a warming of the polar vortex during strong ENSO events in February–March, consistent with but smaller than the estimate from satellite observations and ERA40 reanalysis. The anomalous warming is associated with an anomalous dynamical increase of column ozone north of 70� N that is accompanied by coherent column ozone decrease in the Tropics, in agreement with that deduced from the NIWA column ozone database, implying an increased residual circulation in the mean of all model simulations during ENSO. The spread in the model responses is partly due to the large internal stratospheric variability and it is shown that it crucially depends on the representation of the tropospheric ENSO teleconnection in the models

Highlights from the Joint SPARC-IGAC Workshop on Climate-Chemistry Interactions

Many agents force Earth’s climate. Changes in these agents or forcings can perturb the climate significantly. Atmospheric chemistry plays a critical role in the perturbation of climate by controlling the magnitudes and distributions of a large number of important climate forcing agents. For example, abundances and distributions of methane and ozone depend critically on the atmospheric chemistry. According to IPCC (2001), these two trace gases are the second and third most important green-house gases (GHGs) that have increased due to anthropogenic activities since the industrial revolution