Influence of atmospheric circulation on the long-range transport of organochlorine pesticides to the western Tibetan Plateau

被引:35
|
作者
Gong, Ping [1 ,2 ]
Wang, Xiao-ping [1 ,2 ]
Xue, Yong-gang [1 ,3 ,4 ]
Sheng, Jiu-jiang [1 ]
Gao, Shao-peng [1 ]
Tian, Li-de [1 ,2 ,3 ]
Yao, Tan-dong [1 ,2 ]
机构
[1] Chinese Acad Sci, Key Lab Tibetan Environm Changes & Land Surface P, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China
[2] CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
[3] Chinese Acad Sci, Ngari Stn Desert Environm Observat & Res NASDE, Rutog County 859700, Peoples R China
[4] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Persistent organic pollutants (POPs); Seasonal variation; Westerly wind and Indian monsoon transition region; Backward air mass trajectory; Ngari region; POLYBROMINATED DIPHENYL ETHERS; PERSISTENT ORGANIC POLLUTANTS; GLOBAL DISTRIBUTION MODEL; INDIAN CITIES LEVELS; POLYCHLORINATED-BIPHENYLS; SEASONAL-VARIATIONS; REGIONAL SOURCES; AIR; CHINA; ENDOSULFAN;
D O I
10.1016/j.atmosres.2015.07.006
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Atmospheric circulation now is considered key to understanding global dispersion of organochlorine pesticides (OCPs). Many studies reported that the Indian monsoon and westerly wind played important roles on the transport of OCPs to the Tibetan Plateau. Previously, few observation campaigns have focused on the joint effect of Indian monsoon and westerly wind on long-range atmospheric transport of OCPs in a transition area of the Tibetan Plateau. In this study, air samples were collected for 7 months in the Ngari region, a westerly wind and Indian monsoon transition area in the western Tibetan Plateau. Westerly wind controls the climate of this transition area from March to May, and the levels of DDTs, HCHs, and endosulfans in the Ngari region were <10 pg/m(3), related to OCP transport by the upper-level westerly. From August to October, Indian monsoon and the airflow from north carried elevated concentrations of DDTs, HCHs, and endosulfans, and the levels of endosulfans in the Ngari region even reached hundreds of pg/m(3). In addition, due to the competition and conversion of Indian monsoon and westerly in June, the low levels of atmospheric OCPs reached minimum in the Ngari region. The seasonal shift of the westerly wind and the Indian monsoon resulted in complex seasonal patterns of the OCPs in this transition region, and due to the complex atmospheric circulations, the OCPs in the transition region originated from northwestern India and Northwest China (Xinjiang). (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:157 / 164
页数:8
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