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This may be caused by dust storm exercise in central Asia. The buy of important ionic concentrations in the snow packs was determined to become Ca2+ > SO4 2??> NH4 + > NO3 ??> Cl?? Na+ > Mg2+ > K+. Ca2+ was the dominant cation; SO4 two??was the dominant anion. We find, excluding NO3 ?? the variabilities of ionic concentrations are remarkably correlated. Success show which the glacier location was significantly afflicted by dust exercise and anthropogenic resource. The foremost ions, especially Na+, originate from dust resources of central Asia and with the Ocean, transported because of the westerly winds.
Snow chemistry on the glaciers of alpine regions is an efficient indicator of atmospheric environmental improve. We examine snow chemistry in three snowpits at distinct altitudes over the Haxilegen Glacier No. 51, inside the Kuitun River supply, Tian Shan, China, all through July-September 2004 to 2007. We use correlation analysis, aspect Examination and sea-salt tracing ways to analyze the attributes and sources of key ions and mineral dust particles during the snow. Success show that mineral dust particles and significant ions inside the snow pits differ seasonally. Through the Asian dust time period in springtime, the focus of mineral dust particles and big ions deposited in snow is significant, while the focus is fairly very low over the non-dust duration of summertime and autumn.
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The Tian Shan in its fast geological earlier was saved from glaciation a result of the "protecting" warm influence on the Indian Ocean monsoon local climate. This described its ecological attributes which could sustain its unique ecosphere.
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