scholarly journals Role of aerosol size distribution and source location in a three-dimensional simulation of a Saharan dust episode tested against satellite-derived optical thickness

1998 ◽  
Vol 103 (D9) ◽  
pp. 10579-10592 ◽  
Author(s):  
Michael Schulz ◽  
Yves J. Balkanski ◽  
Walter Guelle ◽  
Francois Dulac
Keyword(s):  
Size Distribution ◽  
Optical Thickness ◽  
Three Dimensional ◽  
Source Location ◽  
Saharan Dust ◽  
Aerosol Size Distribution ◽  
Dimensional Simulation

Three-Dimensional Simulation of In Vitro Angiogenesis: Effects of Extracellular Matrix Structure and Density

2010 ◽  
Author(s):  
Lowell Taylor Edgar ◽  
James E. Guilkey ◽  
Clayton J. Underwood ◽  
Brenda Baggett ◽  
Urs Utzinger ◽  
...  
Keyword(s):  
Extracellular Matrix ◽  
Endothelial Cells ◽  
Three Dimensional ◽  
Vascular Endothelial ◽  
Chemical Factors ◽  
Dimensional Simulation ◽  
Endothelial Growth Factor ◽  
In Vitro Angiogenesis

The process of angiogenesis is regulated by both chemical and mechanical signaling. While the role of chemical factors such as vascular endothelial growth factor (VEGF) during angiogenesis has been extensively studied, the influence of the mechanostructural environment on new vessel generation has received significantly less attention. During angiogenesis, endothelial cells in the existing vasculature detach and migrate out into the surrounding extracellular matrix (ECM), forming tubular structures that eventually mature into new blood vessels. This process is modulated by the structure and composition of the ECM [1]. The ECM is then remodeled by endothelial cells in the elongating neovessel tip, resulting in matrix condensation and changes in fiber orientation [2]. The mechanism as to how angiogenic vasculature and the ECM influence each other is poorly understood.

scholarly journals Technical Note: A new SIze REsolved Aerosol Model (SIREAM)

2007 ◽  
Vol 7 (6) ◽  
pp. 1537-1547 ◽  
Author(s):  
E. Debry ◽  
K. Fahey ◽  
K. Sartelet ◽  
B. Sportisse ◽  
M. Tombette
Keyword(s):  
Size Distribution ◽  
Transport Model ◽  
Three Dimensional ◽  
Technical Note ◽  
Aerosol Size Distribution ◽  
Short Paper ◽  
Chemistry Transport Model ◽  
Dynamical Mass ◽  
Aerosol Model ◽  
Transfer Method

Abstract. We briefly present in this short paper a new SIze REsolved Aerosol Model (SIREAM) which simulates the evolution of atmospheric aerosol by solving the General Dynamic Equation (GDE). SIREAM segregates the aerosol size distribution into sections and solves the GDE by splitting coagulation and condensation/evaporation-nucleation. A quasi-stationary sectional approach is used to describe the size distribution change due to condensation/evaporation, and a hybrid equilibrium/dynamical mass-transfer method has been developed to lower the computational burden. SIREAM uses the same physical parameterizations as those used in the Modal Aerosol Model, MAM Sartelet et al. (2006). It is hosted in the modeling system Polyphemus Mallet et al., 2007, but can be linked to any other three-dimensional Chemistry-Transport Model.

scholarly journals Technical Note: A new SIze REsolved Aerosol Model (SIREAM)

2006 ◽  
Vol 6 (6) ◽  
pp. 11845-11875 ◽  
Author(s):  
E. Debry ◽  
K. Fahey ◽  
K. Sartelet ◽  
B. Sportisse ◽  
M. Tombette
Keyword(s):  
Size Distribution ◽  
Atmospheric Aerosol ◽  
Transport Model ◽  
Three Dimensional ◽  
Technical Note ◽  
Aerosol Size Distribution ◽  
Short Paper ◽  
Chemistry Transport Model ◽  
Aerosol Model ◽  
General Dynamic

Abstract. We briefly present in this short paper a new SIze REsolved Aerosol Model (SIREAM) which simulates the evolution of atmospheric aerosol by solving the General Dynamic Equation (GDE). SIREAM segregates the aerosol size distribution into sections and solves the GDE by splitting coagulation and condensation/evaporation. A moving sectional approach is used to describe the size distribution change due to condensation/evaporation and a hybrid method has been developed to lower the computational burden. SIREAM uses the same physical parameterizations as those used in the Modal Aerosol Model, MAM sartelet05development. It is hosted in the modeling system POLYPHEMUS (Mallet et al., 2006) but can be linked to any other three-dimensional Chemistry-Transport Model.

ANALYSIS OF AEROSOL SIZE DISTRIBUTION DURING SAHARAN DUST EVENTS AT MT. CIMONE (ITALY)

2011 ◽  
Vol 2011 (1) ◽  
Author(s):  
Angela Marinoni ◽  
Paolo Cristofanelli ◽  
Rocco Duchi ◽  
Stefano Zauli Sajani ◽  
Paolo Lauriola ◽  
...  
Keyword(s):  
Size Distribution ◽  
Saharan Dust ◽  
Aerosol Size Distribution ◽  
Dust Events

Three dimensional simulation of air permeability of single layer woven structures

2011 ◽  
Vol 1 (4) ◽  
Author(s):  
Radostina Angelova ◽  
Peter Stankov ◽  
Iskra Simova ◽  
Idoya Aragon
Keyword(s):  
Cross Sections ◽  
Three Dimensional ◽  
Single Layer ◽  
Woven Fabrics ◽  
Transverse Permeability ◽  
Woven Structures ◽  
Dimensional Simulation ◽  
Jet Cross Sections ◽  
Woven Structure

AbstractThe paper deals with a CFD based study of the transverse permeability of a textile woven structure. The reported numerical investigation is preconditioned by both previous experimental and CFD study on jet systems. It is also based on detailed experimental investigation of the porous structure of single layer woven fabrics, made of staple fiber yarns. The flow in through-thickness direction of the woven structures is presented as jet systems, issuing from set of orifices. Two different types of jet system (3×3 jets and 5×5 jets) with two types of jet cross sections (square and circular), corresponding to two different woven structures, are simulated. An analysis is made in terms of the structure of the woven fabrics (area and shape of the interstices between the threads), the parameters of the flow passing through the textile (velocity profiles and velocity fields through isosurfaces), the role of the type of the jet systems, representing the flow and the influence of the shape of the interstices between the threads on the flow pattern. It was found that the applied approach could be effectively used for studying of the transverse permeability of the woven fabrics.

scholarly journals Three-dimensional MHD simulations of molecular cloud fragmentation regulated by gravity, ambipolar diffusion, and turbulence

2008 ◽  
Vol 4 (S259) ◽  
pp. 115-116
Author(s):  
Takahiro Kudoh ◽  
Shantanu Basu
Keyword(s):  
Star Formation ◽  
Magnetic Fields ◽  
Time Scale ◽  
Molecular Cloud ◽  
Molecular Clouds ◽  
Three Dimensional ◽  
Core Formation ◽  
Mhd Simulations ◽  
Dimensional Simulation

AbstractWe find that the star formation is accelerated by the supersonic turbulence in the magnetically dominated (subcritical) clouds. We employ a fully three-dimensional simulation to study the role of magnetic fields and ion-neutral friction in regulating gravitationally driven fragmentation of molecular clouds. The time-scale of collapsing core formation in subcritical clouds is a few ×107 years when starting with small subsonic perturbations. However, it is shortened to approximately several ×106 years by the supersonic flows in the clouds. We confirm that higher-spacial resolution simulations also show the same result.

scholarly journals Global three-dimensional simulation of aerosol optical thickness distribution of various origins

2000 ◽  
Vol 105 (D14) ◽  
pp. 17853-17873 ◽  
Author(s):  
Toshihiko Takemura ◽  
Hajime Okamoto ◽  
Yoshihiro Maruyama ◽  
Atusi Numaguti ◽  
Akiko Higurashi ◽  
...  
Keyword(s):  
Optical Thickness ◽  
Thickness Distribution ◽  
Three Dimensional ◽  
Aerosol Optical Thickness ◽  
Dimensional Simulation

scholarly journals Secondary organic aerosol formation during June 2010 in Central Europe: measurements and modelling studies with a mixed thermodynamic-kinetic approach

2014 ◽  
Vol 14 (8) ◽  
pp. 3831-3842 ◽  
Author(s):  
B. Langmann ◽  
K. Sellegri ◽  
E. Freney
Keyword(s):  
Organic Carbon ◽  
Size Distribution ◽  
Atmospheric Chemistry ◽  
Mass Concentration ◽  
Three Dimensional ◽  
Kinetic Approach ◽  
Aerosol Size Distribution ◽  
Aerosol Formation ◽  
Organic Vapour ◽  
Mass Concentrations

Abstract. Until recently secondary organic carbon aerosol (SOA) mass concentrations have been systematically underestimated by three-dimensional atmospheric-chemistry-aerosol models. With a newly proposed concept of aging of organic vapours, more realistic model results for organic carbon aerosol mass concentrations can be achieved. Applying a mixed thermodynamic-kinetic approach for SOA formation shifted the aerosol size distribution towards particles in the cloud condensation nuclei size range, thereby emphasising the importance of SOA formation schemes for modelling realistic cloud and precipitation formation. The additional importance of hetero-molecular nucleation between H2SO4 and organic vapours remains to be evaluated in three-dimensional atmospheric-chemistry-aerosol models. Here a case study is presented focusing on Puy-de-Dôme, France in June 2010. The measurements indicate a considerable increase in SOA mass concentration during the measurement campaign, which could be reproduced by modelling using a simplified thermodynamic-kinetic approach for SOA formation and increased biogenic volatile organic compound (VOC) precursor emissions. Comparison with a thermodynamic SOA formation approach shows a huge improvement in modelled SOA mass concentration with the thermodynamic-kinetic approach for SOA formation. SOA mass concentration increases by a factor of up to 6 accompanied by a slight improvement of modelled particle size distribution. Even though nucleation events at Puy-de-Dôme were rare during the chosen period of investigation, a weak event in the boundary layer could be reproduced by the model in a sensitivity study when nucleation of low-volatile secondary organic vapour is included. Differences in the model results with and without nucleation of organic vapour are visible in the lower free troposphere over several days. Taking into account the nucleation of organic vapour leads to an increase in accumulation mode particles due to coagulation and condensational growth of nucleation and Aitken mode particles.

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