Open AccessRecords of sulfate and nitrate in an ice core from Mount Muztagata, central Asia
Author(s) -
Zhao Huabiao,
Xu Baiqing,
Yao Tandong,
Tian Lide,
Li Zhen
Publication year - 2011
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011jd015735
Subject(s) - ice core , sulfate , arid , central asia , nitrate , geology , physical geography , atmospheric sciences , environmental science , climatology , geography , chemistry , paleontology , organic chemistry
Annually resolved ice core records of major soluble ions (Na + , NH 4 + , K + , Mg 2+ , Ca 2+ , Cl − , SO 4 2− , and NO 3 − ) covering the period 1907–2002 A.D. from Mount Muztagata in central Asia are presented in this paper. Time series of major ion concentrations generally exhibit very similar temporal trends except NO 3 − and NH 4 + . Statistical analyses show that the chemical composition in the Muztagata ice core is predominantly controlled by terrestrial dust inputs originating from the extensive arid and semiarid regions of central Asia. However, by comparison with the typical dust‐derived ion Ca 2+ , the SO 4 2− and NO 3 − concentrations increase more rapidly after the mid‐1970s and late 1970s, respectively, possibly indicating the strong anthropogenic contributions from then on. The good agreements between SO 4 2− and NO 3 − concentration records and their precursor gas emissions from central and southwest Asia suggest the potential source regions contributing to the Muztagata ice core records.