Characterization of polar stratospheric cloud (PSC) using ground-based Fourier-transform infrared spectrometer (FTIR) at Syowa Station, Antarctica

Polar stratospheric clouds (PSCs) play an important role in ozone destruction via the occurrence of heterogeneous reactions on their surface that convert reservoir species of active chlorine and bromine (e.g., HCl, ClONO_2, HBr, or BrONO_2) into active Cl_2 or Br_2. However, a lack of direct measure...

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Bibliographic Details
Main Authors: Hideaki Nakajima, Kosuke Saeki, Masanori Yabuki, Masataka Shiobara
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 2010
Subjects:
geo
Syowa Station
Antarc*
Antarctica
Online Access:https://doi.org/10.15094/00009585
https://doaj.org/article/83cba9094e594e7a879655402f0b2e50
Description
Summary:Polar stratospheric clouds (PSCs) play an important role in ozone destruction via the occurrence of heterogeneous reactions on their surface that convert reservoir species of active chlorine and bromine (e.g., HCl, ClONO_2, HBr, or BrONO_2) into active Cl_2 or Br_2. However, a lack of direct measurements means that uncertainty remains regarding the characteristics, types, mixtures, and nature of PSCs. To address this problem, we conducted, for the first time, ground-based measurements of the features of PSCs using a low-resolution Fourier-transform infrared (FTIR) spectrometer at Syowa Station, Antarctica, in 2007. Many PSCs were observed between July and August 2007. We succeeded in identifying the features of Ice (Type-II), NAD and or β-NAT (Type-Ia), and STS (Type-Ib) PSCs in the zenith sky infrared spectra measured by FTIR.

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