Not exact matches
The reaction rate between
atmospheric hydrogen chloride (HCl) and chlorine nitrate (ClONO2) is greatly enhanced in the presence of
ice particles; HCl dissolves readily into
ice, and the collisional reaction probability for ClONO2 on the surface of
ice with HCl in the mole fraction range from ∼ 0.003 to 0.010 is in the range from ∼ 0.05 to 0.1 for temperatures near 200 K. Chlorine (Cl2) is released into the gas phase on a time scale of at most a few milliseconds, whereas nitric acid (HNO3), the other product, remains in the condensed phase.
«If we know how volcanic sulfur
particles affect the
atmospheric winds, we can have a much improved interpretation of the traces of volcanic activities in the
ice cores,» says Dr. Toohey.
They had assumed that
atmospheric water vapor had seeped into high - latitude martian soil and frozen between soil
particles, forming a half -
ice, half - soil mixture.
At supersaturated
atmospheric conditions, bare and coated
particles had a nearly equivalent predisposition for nucleating
ice.
PNNL found dust
particle surface reshaped during
atmospheric passage, altering
ice - forming ability
Geoengineering proposals fall into at least three broad categories: 1) managing
atmospheric greenhouse gases (e.g., ocean fertilization and
atmospheric carbon capture and sequestration), 2) cooling the Earth by reflecting sunlight (e.g., putting reflective
particles into the atmosphere, putting mirrors in space to reflect the sun's energy, increasing surface reflectivity and altering the amount or characteristics of clouds), and 3) moderating specific impacts of global warming (e.g., efforts to limit sea level rise by increasing land storage of water, protecting
ice sheets or artificially enhancing mountain glaciers).
Various mechanisms, involving changes in ocean circulation, changes in
atmospheric concentrations of greenhouse gases or haze
particles, and changes in snow and
ice cover, have been invoked to explain these sudden regional and global transitions.