作者: R. F. Jarnot , J. W. Waters , W. G. Read , R. S. Harwood , G. L. Manney
DOI:
关键词: Abundance (ecology) 、 Climatology 、 Arctic 、 Polar 、 Stratosphere 、 Ozone layer 、 Ozone depletion 、 Atmospheric sciences 、 Environmental science 、 The arctic 、 Ozone
摘要: The severe depletion of stratospheric ozone over Antarctica in late winter and early spring is caused by enhanced CLO abundances arising from heterogeneous reactions on polar clouds (PSCs). comparable to those have also been observed throughout the Arctic Vortex, but accompanying loss has much less severe.