The Mid-Holocene Climate Simulated by a Grid-Point AGCM Coupled with a Biome Model

Wang Huijun

doi:10.1007/s00376-002-0017-9

Impact Factor: 5.8

Volume 19 Issue 2

Mar. 2002

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 2002 > 19(2): 205-218

The Mid-Holocene Climate Simulated by a Grid-Point AGCM Coupled with a Biome Model

Wang Huijun

1.
LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences Beijing 100029

Wang Huijun

doi: 10.1007/s00376-002-0017-9

Abstract
References
Related papers
PDF

Abstract:
The climate simulation for the mid-Holocene about 6000 years before present (6 ka BP) is carried out with a grid-point atmospheric general circulation model (AGCM) coupled with a biome model. This coupled model simulation employs orbital parameters of 6 ka BP but present forcing conditions. Results show that large-scale climate differences between now and then are substantial in summer with dramatically strong African-Asian monsoon flow and precipitation during mid-Holocene. Although the results of this coupled model are qualitatively close to those of the AGCM, the coupled model shows a larger changes in both precipitation and temperature in summer over the North African monsoon area with weaker cooling in the Northern autumn.
- Mid-Holocene,
- Monsoon,
- AGCM,
- Biome model
References

[1]	YU Entao, WANG Tao, GAO Yongqi, and XIANG Weiling, 2014: Precipitation Pattern of the Mid-Holocene Simulated by a High-Resolution Regional Climate Model, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 962-971. doi: 10.1007/s00376-013-3178-9
[2]	JIN Liya, WANG Huijun, CHEN Fahu, JIANG Dabang, 2006: A Possible Impact of Cooling over the Tibetan Plateau on the Mid-Holocene East Asian Monsoon Climate, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 543-550. doi: 10.1007/s00376-006-0543-y
[3]	Lin Zhaohui, Zeng Qingcun, 1997: Simulation of East Asian Summer Monsoon by Using an Improved AGCM, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 513-526. doi: 10.1007/s00376-997-0069-y
[4]	Xue Feng, Bi Xunqiang, Lin Yihua, 2001: Modelling the Global Monsoon System by IAP 9L AGCM, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 404-412. doi: 10.1007/BF02919319
[5]	ZHAO Chongbo, ZHOU Tianjun, SONG Lianchun, REN Hongli, 2014: The Boreal Summer Intraseasonal Oscillation Simulated by Four Chinese AGCMs Participating in the CMIP5 Project, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 1167-1180. doi: 10.1007/s00376-014-3211-7
[6]	Shiyan ZHANG, Yongyun HU, Jiankai ZHANG, Yan XIA, 2024: Attribution of Biases of Interhemispheric Temperature Contrast in CMIP6 Models, ADVANCES IN ATMOSPHERIC SCIENCES, 41, 325-340. doi: 10.1007/s00376-023-3002-0
[7]	Wang Huijun, 2000: The Seasonal Climate and Low Frequency Oscillation in the Simulated Mid-Holocene Megathermal Climate, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 445-457. doi: 10.1007/s00376-000-0035-4
[8]	Ruth GEEN, Marianne PIETSCHNIG, Shubhi AGRAWAL, Dipanjan DEY, F. Hugo LAMBERT, Geoffrey K. VALLIS, 2023: The Relationship between Model Biases in East Asian Summer Monsoon Rainfall and Land Evaporation, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 2029-2042. doi: 10.1007/s00376-023-2297-1
[9]	FU Jianjian, LI Shuanglin, 2013: The Influence of Regional SSTs on the Interdecadal Shift of the East Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 330-340. doi: 10.1007/s00376-012-2062-3
[10]	HE Jinhai, JU Jianhua, WEN Zhiping, L\"U Junmei, JIN Qihua, 2007: A Review of Recent Advances in Research on Asian Monsoon in China, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 972-992. doi: 10.1007/s00376-007-0972-2
[11]	Lu Riyu, Chan-Su Ryu, Buwen Dong, 2002: Associations between the Western North Pacific Monsoon and the South China Sea Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 12-24. doi: 10.1007/s00376-002-0030-z
[12]	DING Yihui, LIU Yanju, SONG Yafang, ZHANG Jin, 2015: From MONEX to the Global Monsoon: A Review of Monsoon System Research, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 10-31. doi: 10.1007/s00376-014-0008-7
[13]	D.M. CHATE, RT. . WAGHMARE, C.K. JENA, V. GOPALAKRISHNAN, P. MURUGAVEL, Sachin D. GHUDE, Rachana KULKARNI, P.C. S. DEVARA, 2018: Cloud Condensation Nuclei over the Bay of Bengal during the Indian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 218-223. doi: 10.1007/s00376-017-6331-z
[14]	Xu Jianjun, Wu Guoxiong, 1999: Dynamic Features and Maintenance Mechanism of Asian Summer Monsoon Subsystem, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 523-536. doi: 10.1007/s00376-999-0028-x
[15]	Jong-Suk KIM, ZHOU Wen, Ho Nam CHEUNG, Chak Hang CHOW, 2013: Variability and Risk Analysis of Hong Kong Air Quality Based on Monsoon and El Nino Conditions, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 280-290. doi: 10.1007/s00376-012-2074-z
[16]	CHEN Guanghua, HUANG Ronghui, 2008: Influence of Monsoon over the Warm Pool on Interannual Variation on Tropical Cyclone Activity over the Western North Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 319-328. doi: 10.1007/s00376-008-0319-7
[17]	Qian Weihong, Zhu Yafen, Xie An, Ye Qian, 1998: Seasonal and Interannual Variations of Upper Tropospheric Water Vapor Band Brightness Temperature over the Global Monsoon Regions, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 337-345. doi: 10.1007/s00376-998-0005-9
[18]	Lanqiang BAI, Dan YAO, Zhiyong MENG, Yu ZHANG, Xianxiang HUANG, Zhaoming LI, 2024: Influence of Irregular Coastlines on a Tornadic Mesovortex in the Pearl River Delta during Monsoon Season. Part II: Numerical Experiments, ADVANCES IN ATMOSPHERIC SCIENCES. doi: 10.1007/s00376-023-3096-4
[19]	Lanqiang BAI, Dan YAO, Zhiyong MENG, Yu ZHANG, Xianxiang HUANG, Zhaoming LI, Xiaoding YU, 2024: Influence of Irregular Coastlines on a Tornadic Mesovortex in the Pearl River Delta during the Monsoon Season. Part I: Pre-storm Environment and Storm Evolution, ADVANCES IN ATMOSPHERIC SCIENCES. doi: 10.1007/s00376-023-3095-5
[20]	JIANG Dabang, ZHANG Zhongshi, 2006: Paleoclimate Modelling at the Institute of Atmospheric Physics, Chinese Academy of Sciences, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 1040-1049. doi: 10.1007/s00376-006-1040-z

PDF

Get Citation+

Export:

Article Metrics

Article Views: 1350 Times

PDF downloads: 1322 Times

Cited by: Times

Proportional views

Manuscript History

Manuscript received: 10 March 2002

Manuscript revised: 10 March 2002

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

The Mid-Holocene Climate Simulated by a Grid-Point AGCM Coupled with a Biome Model

Wang Huijun

1. LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences Beijing 100029

Manuscript received: 2002-03-10
Manuscript revised: 2002-03-10

Abstract: The climate simulation for the mid-Holocene about 6000 years before present (6 ka BP) is carried out with a grid-point atmospheric general circulation model (AGCM) coupled with a biome model. This coupled model simulation employs orbital parameters of 6 ka BP but present forcing conditions. Results show that large-scale climate differences between now and then are substantial in summer with dramatically strong African-Asian monsoon flow and precipitation during mid-Holocene. Although the results of this coupled model are qualitatively close to those of the AGCM, the coupled model shows a larger changes in both precipitation and temperature in summer over the North African monsoon area with weaker cooling in the Northern autumn.

Keywords: