Liu Suxia, Wang Sheng, Wang Yueling, Li Mingxin, Huang Mei, Peng Gongbing, Xiao Ziniu. 2014: Exploring the Relationship between Polar Motion and Runoff. Advances in Meteorological Science and Technology, 4(3): 6-12. DOI: 10.3969/j.issn.2095-1973.2014.03.001
Citation: Liu Suxia, Wang Sheng, Wang Yueling, Li Mingxin, Huang Mei, Peng Gongbing, Xiao Ziniu. 2014: Exploring the Relationship between Polar Motion and Runoff. Advances in Meteorological Science and Technology, 4(3): 6-12. DOI: 10.3969/j.issn.2095-1973.2014.03.001

Exploring the Relationship between Polar Motion and Runoff

  • The evidence of the relationship between polar motion and runoff is reviewed. The relationship between the runoff of Yarlung Zangbo, a primitive river in Tibet, China and polar motion with data records from about 1846 to present is explored. First, the action path framework was structured based on geophysical principles. In order to make time series stationary, the initial time series of polar motionXcomponent, Ycomponent and runoff were transformed into their corresponding fi rst order difference time series ΔX, ΔY, and ΔQ. The Granger causality test between ΔX, ΔYand ΔQwas conducted on monthly, seasonal and annual time scales. It is found that on a monthly scale ΔXinfluences ΔQat the lag being from the 1stto the 21stmonth, with the 9thmonth being an exception. ΔYinfluences ΔQat the lag from the 1stto the 9thmonth and from the 17thto the 24thmonth. On a seasonal scale, the influence of ΔXon ΔQcan be seen in the 2ndseason (i.e. from the 4thto the 6thmonth). The influence of ΔYon ΔQcan be seen on a seasonal scale from the 4thto the 6thseason (i.e. from the 10thto 18thmonth). We cannot see evident Granger causality from ΔX, ΔYto ΔQ, on annual scales. For the Granger influence of ΔQto ΔX, ΔY, it is found that on a monthly scale the influences are prominent at the lag being from the 3rdto the 25thmonths for the ΔX, for the ΔYit is the 1stand the 3rdto the 25thmonths. On a seasonal scale these influences can be seen at the lag from the 2ndto the 8thseason (corresponding to the 4thto the 24thmonth) for ΔXand at the lag from the 1stto the 8thseason (corresponding to from the 1stto the 24thmonth) for ΔY. Again, on a annual scale no evident granger causality can be found from runoff to polar motion. The different behaviours on monthly, seasonal and annual scales suggest that using the monthly data of polar motion to obtain the monthly runoff data is more practicable than borrowing the data from polar motion for river runoff on seasonal and annual scales.
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