Multi-Temporal Scale Global Gravity Field Determination From GRACE Follow-On: Pentad Polar Regions and Monthly Low-to-Mid Latitudes

IF 4.1 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Daeha Lee, Shin-Chan Han, Ki-Weon Seo
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Abstract

The Gravity Recovery and Climate Experiment and GRACE Follow-On (GRACE-FO) missions have successfully detected Earth's mass redistributions on a monthly basis. Recently, various groups have developed daily and 5-day interval “regularized” mass concentration (mascon) solutions. These solutions support mass variations at gridded areas focusing primarily on improved detection of land mass change signal. Instead of deriving regularized mascon solution, we present the derivation of multi-temporal scale but Level2-like global gravity solution using line-of-sight gravity difference and the Slepian function by exploiting increased satellite sampling at high latitude regions. Our spherical harmonics solution features time-varying gravity over the polar regions every 5-day while the low-to-mid latitude regions every 30-day. This allows avoiding the under-sampling problem without incorporating regularization, while also reducing the aliasing problem in the polar region. Our new solution strategy is tested with synthetic experiment with the Earth System Model. The synthetic test shows that 5-day solutions exhibit comparable error level to the 30-day solution in the polar region after the suppression of the correlation error. Our multi-temporal scale global gravity solutions successfully identify intra-month surface mass change signals not previously identified by usual monthly-mean gravity field solutions. They are associated with residual ocean tidal mass change, rapid snowfall accumulation in an Antarctic basin, and high-frequency ocean mass changes in the Arctic ocean. Our approach demonstrates the feasibility of generating shorter interval global gravity solutions without any regularization or loss of accuracy and opens opportunities to fully utilize GRACE-FO measurements with various spatial coverages.

Abstract Image

基于GRACE的多时间尺度全球重力场测定:五极区和每月低纬度至中纬度
重力恢复和气候实验(Gravity Recovery and Climate Experiment)和GRACE Follow - On (GRACE - FO)任务已经成功地探测到地球质量每月的重新分布。最近,不同的团队已经开发出每日和5天间隔的“正则化”质量浓度(mascon)解决方案。这些解决方案支持网格区域的质量变化,主要侧重于改进陆地质量变化信号的检测。我们不是推导正则化的mascon解,而是利用视线重力差和Slepian函数,利用高纬度地区增加的卫星采样,推导出多时间尺度但类似Level2的全球重力解。我们的球面谐波解的特点是,极地地区的重力每5天变化一次,而低纬度至中纬度地区的重力每30天变化一次。这可以避免采样不足的问题,而不纳入正则化,同时也减少了极地地区的混叠问题。用地球系统模型进行了综合实验,验证了我们的解决策略。综合检验表明,在抑制相关误差后,极地地区5天溶液的误差水平与30天溶液相当。我们的多时间尺度全球重力解成功地识别了月内地表质量变化信号,而以前通常的月平均重力场解无法识别。它们与残留的海洋潮汐质量变化、南极盆地的快速降雪积累以及北冰洋的高频海洋质量变化有关。我们的方法证明了在没有任何正则化或精度损失的情况下生成较短间隔全球重力解的可行性,并为充分利用不同空间覆盖的GRACE - FO测量提供了机会。
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来源期刊
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth Earth and Planetary Sciences-Geophysics
CiteScore
7.50
自引率
15.40%
发文量
559
期刊介绍: The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology. JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields. JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.
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