A New Hypothesis for the Vertical Distribution of Atmospheric Aerosols
A. Mary Selvam, A. S. Ramachandra Murty, Bh. V. Ramanamurty
Abstract
A simple model which can explain the observed vertical distribution and size spectrum of atmospheric aerosol has been proposed. The model is based on a new physical hypothesis for the vertical mass exchange between the troposphere and the stratosphere. The vertical mass excange takes place through a gravity wave feedback mechanism. There is a close agreement between the model predicted aerosol distribution and size spectrum and the observed distributions.
Create a lesson
Related papers
Model dependent analytic spin torsion corrections to Blandford Znajek energy extraction in Einstein Cartan gravity
Jingxu Wu, Liangyu Luo, Zhenzhou Lei et al.
Relational GNS Fusion and an Idempotent Gauge-Gravity Fixed Point
G. J. Verbiest
Testing the running vacuum model in light of DESI-DR2 Measurements
Lamiae Kardaddech, Safae Dahmani, Amine Bouali et al.
Reheating after the Higgs Inflation
Manda Malekpour, Kourosh Nozari
Observational viability of Herglotz f(R,T) gravity: A multi-probe Bayesian analysis
Vishal M C, Sankarsan Tarai
Coherent Oscillations of Protons in Hydrogen-loaded Metals
G. Modanese