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Recently discovered small polar motion loops and their atmospheric excitation mechanism

机译:最近发现的小极运动环及其大气激发机制

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Polar motion is the relative motion of the solid Earth with respect to its rotational axis. Recently, small loops have been discovered in unfiltered polar motion observations. These loops with periods less than 21 d and sizes ranging from a silver dollar coin to a compact disc (when projected onto the surface of the Earth) are currently observable because every ~6.4 years the Chandler, annual, and semiannual variations that dominate this motion destructively interfere and act like a high-pass filter. These loops, as well as diurnal polar motion variations, are shown to be significantly correlated to variations in atmospheric angular momentum that result primarily from rapid fluctuations in atmospheric pressure fields with the contributions from the winds playing a smaller variable role. Finally, the results show that variations in the speed of weather patterns and whether or not the surface winds are interacting with land or oceans have an effect on polar motion that is observable with current geodetic observational techniques.
机译:极运动是固体地球相对于其旋转轴的相对运动。最近,在未过滤的极运动观测中发现了小环。这些周期小于21 d,尺寸从银元硬币到光盘(投射到地球表面时)目前可以观察到,因为大约每6.4年,钱德勒,年度和半年度变化主导这一运动。破坏性地干扰并像高通滤波器一样起作用。这些回路以及昼夜极地运动变化与大气角动量变化显着相关,大气角动量变化主要是由于大气压力场的快速波动而风的作用较小。最后,结果表明,天气模式速度的变化以及地表风是否与陆地或海洋相互作用,都会对极运动产生影响,这可通过当前的大地观测技术观察到。

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