scispace - formally typeset
O

Owen B. Toon

Researcher at University of Colorado Boulder

Publications -  436
Citations -  34651

Owen B. Toon is an academic researcher from University of Colorado Boulder. The author has contributed to research in topics: Stratosphere & Aerosol. The author has an hindex of 94, co-authored 424 publications receiving 32237 citations. Previous affiliations of Owen B. Toon include National Center for Atmospheric Research & Cornell University.

Papers
More filters
Journal ArticleDOI

Denitrification mechanisms in the polar stratospheres

TL;DR: In this paper, microphysical simulations suggest that the time required for nitric acid particles to sediment from the stratosphere is comparable to the time needed for falling ice particles to incorporate Nitric acid vapor from the vapor phase.
Journal ArticleDOI

Stability of mid-latitude snowpacks on Mars

TL;DR: In this paper, the authors investigate a specific scenario under conditions they believe are favorable for snowpack melting on Mars and investigate the rate at which a snowpack located at 33°S on a poleward-facing slope sublimates and melts on Mars.
Journal ArticleDOI

Enhancement of cloud cover and suppression of nocturnal drizzle in stratocumulus polluted by haze

TL;DR: In this article, large-eddy simulations of stratocumulus were used to find that the trend in the satellite data is likely an artifact of sampling only overcast clouds, and the simulations instead show cloud cover increasing with droplet concentrations.
Journal ArticleDOI

Saharan and Asian dust: similarities and differences determined by CALIPSO, AERONET, and a coupled climate-aerosol microphysical model

TL;DR: In this paper, the authors compared the properties of atmospheric dust from the Saharan and the Asian deserts using data from CALIPSO and AERONET during 2006 and 2007 along with simulations using a coupled climate-microphysical sectional model.
Journal ArticleDOI

A model simulation of Pinatubo volcanic aerosols in the stratosphere

TL;DR: In this article, a one-dimensional, time-dependent model is used to study the chemical, microphysical, and radiative properties of volcanic aerosols produced by the Mount Pinatubo eruption on June 15, 1991.