Advanced Search
Impact Factor: 5.8

Volume 21 Issue 4

Jul.  2004

Article Contents
Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2004 >  21(4): 637-649

Simulation of the Radiative Effect of Black Carbon Aerosols and the Regional Climate Responses over China

  • 1.

    Department of Atmospheric Sciences, Yunnan University, Kunming 650091;Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093


doi: 10.1007/BF02915731

  • As part of the development work of the Chinese new regional climate model (RIEMS), the radiative process of black carbon (BC) aerosols has been introduced into the original radiative procedures of RIEMS,and the transport model of BC aerosols has also been established and combined with the RIEMS model.Using the new model system, the distribution of black carbon aerosols and their radiative effect over the China region are investigated. The influences of BC aerosole on the atmospheric radiative transfer and on the air temperature, land surface temperature, and total rainfall are analyzed. It is found that BC aerosols induce a positive radiative forcing at the top of the atmosphere (TOA), which is dominated by shortwave radiative forcing. The maximum radiative forcing occurs in North China in July and in South China in April. At the same time, negative radiative forcing is observed on the surface. Based on the radiative forcing comparison between clear sky and cloudy sky, it is found that cloud can enforce the TOA positive radiative forcing and decrease the negative surface radiative forcing. The responses of the climate system in July to the radiative forcing due to BC aerosols are the decrease in the air temperature in the middle and lower reaches of the Changjiang River and Huaihe area and most areas of South China, and the weak increase or decrease in air temperature over North China. The total rainfall in the middle and lower reaches of the Changjiang River area is increased, but it decreased in North China in July.
  • [1] WANG Zhili, ZHANG Hua, SHEN Xueshun, 2011: Radiative Forcing and Climate Response Due to Black Carbon in Snow and Ice, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 1336-1344.  doi: 10.1007/s00376-011-0117-5
    [2] CHANG Wenyuan, LIAO Hong, WANG Huijun, 2009: Climate responses to direct radiative forcing of anthropogenic aerosols, tropospheric ozone, and long-lived greenhouse gases in eastern China over 1951-2000, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 748-762.  doi: 10.1007/s00376-009-9032-4
    [3] XIONG Zhe, FU Congbin, ZHANG Qing, 2006: On the Ability of the Regional Climate Model RIEMS to Simulate the Present Climate over Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 784-791.  doi: 10.1007/s00376-006-0784-9
    [4] GAO Rong, DONG Wenjie, WEI Zhigang, 2008: Simulation and Analysis of China Climate Using Two-Way Interactive Atmosphere-Vegetation Model (RIEMS-AVIM), ADVANCES IN ATMOSPHERIC SCIENCES, 25, 1085-1097.  doi: 10.1007/s00376-008-1085-2
    [5] Chenyu MA, Wei YUAN, Ji NIE, 2020: Responses of Mean and Extreme Precipitation to Different Climate Forcing Under Radiative-Convective Equilibrium, ADVANCES IN ATMOSPHERIC SCIENCES, 37, 377-386.  doi: 10.1007/s00376-020-9236-1
    [6] Junlin AN, Huan LV, Min XUE, Zefeng ZHANG, Bo HU, Junxiu WANG, Bin ZHU, 2021: Analysis of the Effect of Optical Properties of Black Carbon on Ozone in an Urban Environment at the Yangtze River Delta, China, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1153-1164.  doi: 10.1007/s00376-021-0367-9
    [7] LI Shu, WANG Tijian, ZHUANG Bingliang, HAN Yong, 2009: Indirect Radiative Forcing and Climatic Effect of the Anthropogenic Nitrate Aerosol on Regional Climate of China, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 543-552.  doi: 10.1007/s00376-009-0543-9
    [8] Seung-Jae LEE, E. Hugo BERBERY, Domingo ALCARAZ-SEGURA, 2013: Effect of Implementing Ecosystem Functional Type Data in a Mesoscale Climate Model, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1373-1386.  doi: 10.1007/s00376-012-2143-3
    [9] Luyang XU, Ke WEI, Xue WU, S. P. SMYSHLYAEV, Wen CHEN, V. Ya. GALIN, 2019: The Effect of Super Volcanic Eruptions on Ozone Depletion in a Chemistry-Climate Model, ADVANCES IN ATMOSPHERIC SCIENCES, , 823-836.  doi: 10.1007/s00376-019-8241-8
    [10] WANG Gengchen, BAI Jianhui, KONG Qinxin, Alexander EMILENKO, 2005: Black Carbon Particles in the Urban Atmosphere in Beijing, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 640-646.  doi: 10.1007/BF02918707
    [11] Yulan ZHANG, Shichang KANG, Tanguang GAO, Michael SPRENGER, Wei ZHANG, Zhaoqing WANG, 2023: Black Carbon Size in Snow of Chinese Altai Mountain in Central Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 1199-1211.  doi: 10.1007/s00376-022-2141-z
    [12] Jie SUN, Michael SECOR, Ming CAI, Xiaoming HU, 2024: A Quasi-Linear Relationship between Planetary Outgoing Longwave Radiation and Surface Temperature in a Radiative-Convective-Transportive Climate Model of a Gray Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 41, 8-18.  doi: 10.1007/s00376-023-2386-1
    [13] CHEN Lin, SHI Guangyu, QIN Shiguang, YANG Su, ZHANG Peng, 2011: Direct Radiative Forcing of Anthropogenic Aerosols over Oceans from Satellite Observations, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 973-984.  doi: 10.1007/s00376-010-9210-4
    [14] WANG Jun, BAO Qing, Ning ZENG, LIU Yimin, WU Guoxiong, JI Duoying, 2013: Earth System Model FGOALS-s2: Coupling a Dynamic Global Vegetation and Terrestrial Carbon Model with the Physical Climate System Model, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1549-1559.  doi: 10.1007/s00376-013-2169-1
    [15] Chen ZHOU, Yincheng LIU, Quan WANG, 2022: Calculating the Climatology and Anomalies of Surface Cloud Radiative Effect Using Cloud Property Histograms and Cloud Radiative Kernels, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 2124-2136.  doi: 10.1007/s00376-021-1166-z
    [16] Xinyong SHEN, Wenyan HUANG, Chunyan GUO, Xiaocen JIANG, 2016: Precipitation Responses to Radiative Effects of Ice Clouds: A Cloud-Resolving Modeling Study of a Pre-Summer Torrential Precipitation Event, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 1137-1142.  doi: 10.1007/s00376-016-5218-8
    [17] Weile WANG, Ramakrishna NEMANI, 2016: Dynamic Responses of Atmospheric Carbon Dioxide Concentration to Global Temperature Changes between 1850 and 2010, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 247-258.  doi: 10.1007/s00376-015-5090-y
    [18] DAI Qiudan, SUN Shufen, 2006: A Generalized Layered Radiative Transfer Model in the Vegetation Canopy, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 243-257.  doi: 10.1007/s00376-006-0243-7
    [19] DAI Qiudan, SUN Shufen, 2007: A Simplified Scheme of the Generalized Layered Radiative Transfer Model, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 213-226.  doi: 10.1007/s00376-007-0213-8
    [20] Hu Rongming, Serge Planton, Michel Déque, Pascal Marquet, Alain Braun, 2001: Why Is the Climate Forcing of Sulfate Aerosols So Uncertain?, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 1103-1120.  doi: 10.1007/s00376-001-0026-0
PDF

Get Citation+

shu
Export:  

Share Article

Article Metrics

Article Views: 1912 Times

PDF downloads: 1535 Times

Cited by: Times
  • 加载中

    • Manuscript History

    Manuscript received: 10 July 2004
    Manuscript revised: 10 July 2004
    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

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Simulation of the Radiative Effect of Black Carbon Aerosols and the Regional Climate Responses over China

    • 1. Department of Atmospheric Sciences, Yunnan University, Kunming 650091;Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Department of Atmospheric Sciences, Nanjing University, Nanjing 210093
    • Manuscript received: 2004-07-10
    • Manuscript revised: 2004-07-10

    Abstract: As part of the development work of the Chinese new regional climate model (RIEMS), the radiative process of black carbon (BC) aerosols has been introduced into the original radiative procedures of RIEMS,and the transport model of BC aerosols has also been established and combined with the RIEMS model.Using the new model system, the distribution of black carbon aerosols and their radiative effect over the China region are investigated. The influences of BC aerosole on the atmospheric radiative transfer and on the air temperature, land surface temperature, and total rainfall are analyzed. It is found that BC aerosols induce a positive radiative forcing at the top of the atmosphere (TOA), which is dominated by shortwave radiative forcing. The maximum radiative forcing occurs in North China in July and in South China in April. At the same time, negative radiative forcing is observed on the surface. Based on the radiative forcing comparison between clear sky and cloudy sky, it is found that cloud can enforce the TOA positive radiative forcing and decrease the negative surface radiative forcing. The responses of the climate system in July to the radiative forcing due to BC aerosols are the decrease in the air temperature in the middle and lower reaches of the Changjiang River and Huaihe area and most areas of South China, and the weak increase or decrease in air temperature over North China. The total rainfall in the middle and lower reaches of the Changjiang River area is increased, but it decreased in North China in July.

      HTML

    Catalog

      Publish with AAS

      Contact us

      Links

      Copyright © 2018-2028 ADVANCES IN ATMOSPHERIC SCIENCES 京ICP备14024088号-7

      Supported by: Beijing Renhe Information Technology Co. Ltd  support: info@rhhz.net  

      /

      DownLoad:  Full-Size Img  PowerPoint
      Return
      Return