作者: R. Toumi
DOI: 10.1029/93GL01675
关键词:
摘要: The author presents the results of a model study atmospheric chemistry ClO with NO[sub 3]. No effort is made to consider heterogeneous reactions on polar stratospheric cloud nuclei for example. There seem be two major product channels. One in formation Cl and 2], able contribute catalytic ozone destruction lower stratosphere at night. other process OClO night, source this molecule upper stratosphere. For arctic reaction does not make significant contribution