/   Home   /   Newsroom   /   Research News

IAP Scientists Explain Warmer Climate in the Tang and Song Dynasties

Mar 04, 2015     Email"> PrintText Size

Chinese are generally proud of Tang dynasty (618−907 AD) which was considered a golden age of cosmopolitan culture while Song dynasty (960−1279 AD) was considered relatively weaker with respect to so-called “national capability” in Chinese history. The demographic, economic, and military strength of an ancient dynasty might be related with climate conditions, since a warmer climate is favorable to national economy development. Tang and Song dynasties were two typical warm periods in the last two millennia in China. The temperatures during these periods are comparable to early 20th century temperatures. Then why does national power of Tang and Song dynasties vary so much under warm climate conditions? This is a very important issue in both the social science and natural science communities.

 

City Wall of Xi'an, once the capital of Tang Dynasty, also the starting point of the Silk Road (photo from Wikipedia)

From a perspective of natural science, a paleoclimate research team from Nansen-Zhu international research center at Institute of Atmospheric Physics investigated possible mechanisms for the warming over China during the Tang and Song dynasties. They performed a 2000-year simulation forced by the external forcings of the last two millennia with the Community Earth System Model. The simulation indicates warm conditions in both the early Tang dynasty (650−700 AD) and early Song dynasty (950−1000 AD), but the warmth is mainly seen in East China in the early Tang dynasty, and over the whole of China in the early Song dynasty. The warming in the early Tang dynasty is attributed to the localized increase of atmospheric net energy with favorable heat transport, whereas results from the increase of global solar radiation in the early Song dynasty. Based on the simulation and reconstructions, they suggest that the early Tang dynasty warm period may have been a regional phenomenon in China, while the early Song dynasty warm period was a reflection of global/hemispheric-scale warm events that took place at the same time.  

The results are published in Journal of Geophysical Research.

 

Annual mean temperature anomalies (°C) in the early Tang dynasty warm period (650-700 AD; a) and the early Song dynasty warm period (950-1000 AD; b). 

Citation: Q. Yan, Z. Zhang, H. Wang and D. Jiang, 2015: Simulated warm periods of climate over China during the last two millennia: The Sui-Tang warm period versus the Song-Yuan warm period, Journal of Geophysical Research, doi:10.1002/2014JD022941.

Attachment:

(Editor: CHEN Na)

Contact

YAN Qing

Nansen-Zhu International Research Centre, Institute of Atmospheric Physics

Phone:
E-mail: yanqing@mail.iap.ac.cn

Related Articles

atmosphere;ocean;predictability;target observation

Optimal Observation Locations for Improving High-impact Air-sea Enviromental Events Forecastings

Aug 06, 2015

Mu Mu (Chinese Academy of Sciences) and coauthors reviewed recent progress in determining the optimal locations for ENSO, IOD, TCs and KLM and discussed their potential role in optimizing observation networks and thus improving forecast skill. In particular, they suggeste...

Experiment;to;probe;atmosphere;over;Mt.;Qomolangma;startsInstitute;of;Atmospheric;Physics

Atmospheric experiment over Mt. Qomolangma kicks off

May 17, 2006


Contact Us

Copyright © 2002 - 2017 Chinese Academy of Sciences