Impact of interactive chemistry of stratospheric ozone on Southern Hemisphere paleoclimate simulation

Author:

Noda Satoshi1ORCID,Kodera Kunihiko2,Adachi Yukimasa34,Deushi Makoto45,Kitoh Akio36ORCID,Mizuta Ryo3ORCID,Murakami Shigenori7,Yoshida Kohei3,Yoden Shigeo1

Affiliation:

1. Department of Geophysics; Kyoto University; Kyoto Japan

2. Institute for Space-Earth Environmental Research; Nagoya University; Nagoya Japan

3. Climate Research Department; Meteorological Research Institute; Tsukuba Japan

4. Now at Japan Meteorological Agency; Tokyo Japan

5. Atmospheric Environment and Applied Meteorology Research Department; Meteorological Research Institute; Tsukuba Japan

6. Faculty of Life and Environmental Sciences; University of Tsukuba; Tsukuba Japan

7. Meteorological College; Kashiwa Japan

Funder

JSPS KAKENHI

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Reference48 articles.

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2. Basic performance of a new Earth System Model of the Meteorological Research Institute (MRI-ESM1);Adachi;Pap. Meteorol. Geophys.,2013

3. Coupled chemistry climate model simulations of the solar cycle in ozone and temperature;Austin;J. Geophys. Res.,2008

4. Major stratospheric warming in the southern hemisphere in 2002: Dynamical aspects of the ozone hole split;Baldwin;SPARC Newslett.,2003

5. Long-term variation of daily insolation and quaternary climatic changes;Berger;J. Atmos. Sci.,1978

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