Interannual Climate Variability of the Past Millennium from Simulations

The interannual variability of global temperature and precipitation during the last millennium is ana- lyzed using the results of ten coupled climate models participating in the Paleoclimate Modelling Intercomparison Project Phase 3. It is found that large temperature (precipitation) variability is...

Full description

Saved in:
Bibliographic Details
Published inAtmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao Vol. 8; no. 3; pp. 160 - 165
Main Author YANG Kai-Qing JIANG Da-Bang
Format Journal Article
LanguageEnglish
Published University of Chinese Academy of Sciences,Beijing 100049,China%Nansen-Zhu International Research Centre,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China 2015
Nansen-Zhu International Research Centre,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China
Climate Change Research Center,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China
Subjects
Online AccessGet full text
ISSN1674-2834
2376-6123
DOI10.1080/16742834.2015.11447254

Cover

More Information
Summary:The interannual variability of global temperature and precipitation during the last millennium is ana- lyzed using the results of ten coupled climate models participating in the Paleoclimate Modelling Intercomparison Project Phase 3. It is found that large temperature (precipitation) variability is most dominant at high latitudes (tropical monsoon regions), and the seasonal magnitudes are greater than the annual mean. Significant multi-dec- adal-scale changes exist throughout the whole period for the zonal mean of both temperature and precipitation variability, while their long-term trends are indistinctive. The volcanic forcings correlate well with the temperature variability at midlatitudes, indicating possible leading drivers for the interannual time scale climate change.
Bibliography:The interannual variability of global temperature and precipitation during the last millennium is ana- lyzed using the results of ten coupled climate models participating in the Paleoclimate Modelling Intercomparison Project Phase 3. It is found that large temperature (precipitation) variability is most dominant at high latitudes (tropical monsoon regions), and the seasonal magnitudes are greater than the annual mean. Significant multi-dec- adal-scale changes exist throughout the whole period for the zonal mean of both temperature and precipitation variability, while their long-term trends are indistinctive. The volcanic forcings correlate well with the temperature variability at midlatitudes, indicating possible leading drivers for the interannual time scale climate change.
11-5693/P
interannual variability, volcanic impacts, last millennium
ISSN:1674-2834
2376-6123
DOI:10.1080/16742834.2015.11447254