The difference of atmospheric chemical loadings show by electrical conductivity of snow and ice between Antarctica, Arctic and Qinghai-Tibetan Plateau

• Main Authors: Cunde, Xiao, Dahe, Qin, Tandong, Yao, Jiawen, Ren, Wenkun, Sheng
• Format: Article in Journal/Newspaper
• Language: English
• Published: Polar Research Institute of China - PRIC 1999
• Subjects: Arctic; Greenland; Advances in Polar Science; Antarc*; Antarctica; Ice Sheet; Polar Science
• Online Access: http://library.arcticportal.org/2173/; http://library.arcticportal.org/2173/1/A901.006.pdf

The relationship of ECM with ice acidity and impurities concentrations are much different between the Qinghai-Tibetan Plateau and the polar regions. On the Qinghai-Tibetan Plateau, ECM is dependent on the mineral ions (i.e., Ca(2+), Mg(2+), SO(2-)4, etc.) mainly derived from crustal sources, thus displays a positive linear correlation between ECM and these ions. While in polar ice sheets, however, ECM of snow and ice is mainly dependent on the acidic roots such as Cl(-), SO(2-)4 and NO(-)3 that mostly come from ocean. Therefore, there is good relationship between ECM and Concentration of H(+). However, the relationship between ECM and major ions has complicated geographical differentiation in the whole Arctic. For instance, there no longer exists the same simple relationship in the central Arctic as that in the Greenland Ice Sheet, probably due to the disturbance of Arctic haze. In general, ECM of snow and ice is a potential indicator of atmospheric environment of cold regions.