Aerosol trends over China, 1980-2000

Annual emission trends of sulfur dioxide, black carbon, and organic carbon are presented for East Asia for the period 1980-2000. Emissions of sulfur dioxide peaked in about 1996, and emissions of the carbonaceous aerosols peaked in about 1994-1995, due to a variety of economic, environmental, and social forces. These emissions are converted to their contributions to aerosol optical depth (AOD) over East Asia, using regional results from the GOCART global chemical transport model. We calculate that, on average, AOD over China rose from a value of 0.25 in 1980, peaked at a value of about 0.305 in 1995-1996, and then decreased to about 0.29 in 2000. This trend is consistent with surface shortwave irradiance measurements at 52 weather stations in China, as well as with other radiation-related trends. It may also be consistent with a rise in mean surface temperatures in China starting about the middle of the 1990s.

[1]  X. Y. Zhang,et al.  Analysis of 40 years of solar radiation data from China, 1961–2000 , 2005 .

[2]  R. Dickinson,et al.  Impact of aerosol indirect effect on surface temperature over East Asia. , 2006, Proceedings of the National Academy of Sciences of the United States of America.

[3]  Jiming Hao,et al.  Emission inventories of NOx from commercial energy consumption in China, 1995-1998. , 2002, Environmental science & technology.

[4]  Mark Henderson,et al.  A spatial analysis of pan evaporation trends in China, 1955–2000 , 2004 .

[5]  L. Weiliang,et al.  Characteristics of the spatial distribution and yearly variation of aerosol optical depth over China in last 30 years , 2001 .

[6]  Jingdong Zhao,et al.  Seasonal variation in the regional structure of warming across China in the past half century , 2005 .

[7]  G. Carmichael,et al.  Integrated analysis for acid rain in Asia: Policy implications and results of RAINS-Asia model , 2000 .

[8]  J. Burrows,et al.  Increase in tropospheric nitrogen dioxide over China observed from space , 2005, Nature.

[9]  Tami C. Bond,et al.  On the future of carbonaceous aerosol emissions , 2004 .

[10]  David G. Streets,et al.  Sulfur dioxide emissions in Asia in the period 1985–1997 , 2000 .

[11]  Yoram J. Kaufman,et al.  Aerosol distribution in the Northern Hemisphere during ACE‐Asia: Results from global model, satellite observations, and Sun photometer measurements , 2004 .

[12]  Hajime Akimoto,et al.  Distribution of SO2, NOx and CO2 emissions from fuel combustion and industrial activities in Asia with 1° × 1° resolution , 1994 .

[13]  Michael Q. Wang,et al.  Black carbon emissions in China , 2001 .

[14]  D. Gong,et al.  Enhancement of the warming trend in China , 2000 .

[15]  G. Russell,et al.  Analysis of global climate model experiments to elucidate past and future changes in surface insolation and warming in China , 2006 .

[16]  David G. Streets,et al.  Two‐decadal aerosol trends as a likely explanation of the global dimming/brightening transition , 2006 .

[17]  M Z Jacobson,et al.  Recent Reductions in China's Greenhouse Gas Emissions , 2001, Science.

[18]  Michael Q. Wang,et al.  An inventory of gaseous and primary aerosol emissions in Asia in the year 2000 , 2003 .

[19]  Y. Qian,et al.  Decreasing trends in sunshine duration over China for 1954–1998: Indication of increased haze pollution? , 2002 .

[20]  Zhao Zongci,et al.  Recent Studies on Attributions of Climate Change in China , 2005 .

[21]  Chang‐Hoi Ho,et al.  Weekend effect in diurnal temperature range in China: Opposite signals between winter and summer , 2006 .

[22]  D. Kaiser Decreasing cloudiness over China: An updated analysis examining additional variables , 2000 .

[23]  Kazuaki Kawamoto,et al.  Importance of aerosols in satellite‐derived estimates of surface shortwave irradiance over China , 2006 .

[24]  Y. Gu Climatic effects of different aerosol types in China simulated , 2006 .

[25]  Shaocai Yu,et al.  A comparison of signals of regional aerosol‐induced forcing in eastern China and the southeastern United States , 2001 .

[26]  David G. Streets,et al.  Energy use, emissions, and air pollution reduction strategies in Asia , 1995 .

[27]  Biao Wang,et al.  Data Quality Assessment and the Long-Term Trend of Ground Solar Radiation in China , 2008 .

[28]  J. Hansen,et al.  Climate Effects of Black Carbon Aerosols in China and India , 2002, Science.

[29]  David G. Streets,et al.  Present and future emissions of air pollutants in China:: SO2, NOx, and CO , 2000 .

[30]  Xiaohua Pan,et al.  Trends in temperature extremes during 1951–1999 in China , 2003 .

[31]  A correlative study on the relationship between modeled anthropogenic aerosol concentration and satellite‐observed cloud properties over east Asia , 2006 .

[32]  D. Streets,et al.  A technology‐based global inventory of black and organic carbon emissions from combustion , 2004 .

[33]  Jianping Yang,et al.  Fluctuations of the Semi-Arid Zone in China, and Consequences for Society , 2005 .

[34]  F. Giorgi,et al.  Regional climate effects of aerosols over China: modeling and observation , 2003 .

[35]  Yuqing Wang,et al.  Observed trends in extreme precipitation events in China during 1961–2001 and the associated changes in large‐scale circulation , 2005 .

[36]  Y. Qian,et al.  More frequent cloud‐free sky and less surface solar radiation in China from 1955 to 2000 , 2005 .

[37]  Chunsheng Zhao,et al.  A possible positive feedback of reduction of precipitation and increase in aerosols over eastern central China , 2006 .

[38]  Teruyuki Nakajima,et al.  Tropospheric aerosol optical thickness from the GOCART model and comparisons with satellite and sun photometer measurements , 2002 .

[39]  D. Streets,et al.  The importance of China's household sector for black carbon emissions , 2005 .

[40]  A study of long-term trends in mineral dust aerosol distributions in Asia using a general circulation model , 2004 .

[41]  Dale P. Kaiser,et al.  Analysis of total cloud amount over China, 1951–1994 , 1998 .