globalchange  > 影响、适应和脆弱性
DOI: 10.1002/jgrd.50612
论文题名:
Historical and future black carbon deposition on the three ice caps: Ice core measurements and model simulations from 1850 to 2100
作者: Bauer S.E.; Bausch A.; Nazarenko L.; Tsigaridis K.; Xu B.; Edwards R.; Bisiaux M.; McConnell J.
刊名: Journal of Geophysical Research Atmospheres
ISSN: 21698996
出版年: 2013
卷: 118, 期:14
起始页码: 7948
结束页码: 7961
语种: 英语
英文关键词: aerosol ; black carbon ; deposition
Scopus关键词: Aerosols ; Atmospheric aerosols ; Climate models ; Deposition ; Meteorological problems ; Pollution ; Regional planning ; Atmospheric depositions ; Black carbon ; Carbonaceous aerosol ; Climate model simulations ; Climate simulation ; Emission inventories ; Regional analysis ; Transport patterns ; Computer simulation ; aerosol ; anthropogenic source ; atmospheric deposition ; atmospheric pollution ; black carbon ; climate modeling ; ice cap ; ice core ; measurement method ; numerical model ; twentieth century ; Antarctica ; China ; Himalayas ; Xizang
英文摘要: Ice core measurements in conjunction with climate model simulations are of tremendous value when examining anthropogenic and natural aerosol loads and their role in past and future climates. Refractory black carbon (BC) records from the Arctic, the Antarctic, and the Himalayas are analyzed using three transient climate simulations performed with the Goddard Institute for Space Studies ModelE. Simulations differ in aerosol schemes (bulk aerosols vs. aerosol microphysics) and ocean couplings (fully coupled vs. prescribed ocean). Regional analyses for past (1850-2005) and future (2005-2100) carbonaceous aerosol simulations focus on the Antarctic, Greenland, and the Himalayas. Measurements from locations in the Antarctic show clean conditions with no detectable trend over the past 150 years. Historical atmospheric deposition of BC and sulfur in Greenland shows strong trends and is primarily influenced by emissions from early twentieth century agricultural and domestic practices. Models fail to reproduce observations of a sharp eightfold BC increase in Greenland at the beginning of the twentieth century that could be due to the only threefold increase in the North American emission inventory. BC deposition in Greenland is about 10 times greater than in Antarctica and 10 times less than in Tibet. The Himalayas show the most complicated transport patterns, due to the complex terrain and dynamical regimes of this region. Projections of future climate based on the four CMIP5 Representative Concentration Pathways indicate further dramatic advances of pollution to the Tibetan Plateau along with decreasing BC deposition fluxes in Greenland and the Antarctic. Key Points BC residence times of about 4 days seems realistic Models fail to reproduce the sharp 8-fold observed BC increase Further dramatic increase of pollution reaching the Tibetan plateau predicted ©2013. American Geophysical Union. All Rights Reserved.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/63523
Appears in Collections:影响、适应和脆弱性
气候减缓与适应

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作者单位: Center for Climate Systems Research, Earth Institute, Columbia University, Broadway 2880, New York 10025, NY, United States; NASA Goddard Institute for Space Studies, New York NY, United States; Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China; Department of Imaging and Applied Physics, Curtin University, Bentley WA, Australia; Desert Research Institute, Reno NV, United States

Recommended Citation:
Bauer S.E.,Bausch A.,Nazarenko L.,et al. Historical and future black carbon deposition on the three ice caps: Ice core measurements and model simulations from 1850 to 2100[J]. Journal of Geophysical Research Atmospheres,2013-01-01,118(14)
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