Geodetic Evidence of the Interannual Fluctuations and Long-Term Trends Over the Antarctic Ice Sheet Mass Change

IF 5.3 2区 地球科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing Pub Date : 2025-01-13 DOI:10.1109/JSTARS.2025.3528516
Yuanjin Pan;Xiaohong Zhang;Jiashuang Jiao;Hao Ding;C. K. Shum
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Abstract

The spatiotemporal characteristics of the Antarctic ice sheet (AIS), as constrained by geodetic observations, provide us with a deeper understanding of the current evolution of ice mass balance. However, it still needs further in-depth research on interannual fluctuations and long-term trends of ice mass changes throughout the AIS. In this study, these two aspects were quantitatively analyzed through global positioning system (GPS) and gravity recovery and climate experiment/follow on (GRACE/GFO) over the past two decades. The nonlinear variation of GPS-inferred vertical land motion (VLM) and the influence of surface elastic load are of particular concern. The principal component analysis method is utilized to extract common mode signals from GPS time series, while correcting for various surface loads. The first principal components (PCs) accounted for 57.67%, 35.87%, 36.28%, and 36.03% of the total variances in the vertical components for GPS raw, atmospheric + nontidal oceanic (AO)-removed, AO + hydrographic model (AOH)-removed, and AO + GRACE/GFO-based load (AOG)-removed, respectively. Furthermore, the GPS vertical velocity, excluding the common mode component + AOG, yielded a median value of 0.13 mm/yr, which indicates that the retreat of ice mass has made a significant contribution to the GPS-observed VLM. In addition, the glacial isostatic adjustment (GIA) effect is found to play a key role in the large-scale VLM uplifting of the West AIS. After evaluating five different GIA models with GPS vertical velocity, we suggest that the ICE-6G_D model can more effectively correct GIA signals in GPS observations over Antarctica.
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南极冰盖质量变化年际波动和长期趋势的大地测量证据
在大地测量观测的约束下,南极冰盖的时空特征为我们提供了对当前冰盖质量平衡演变的更深入理解。但是,整个AIS地区冰量变化的年际波动和长期趋势还需要进一步深入研究。本研究通过全球定位系统(GPS)和重力恢复与气候实验/跟踪(GRACE/GFO)对这两个方面进行了定量分析。gps反演的陆地垂直运动(VLM)的非线性变化和地表弹性荷载的影响是一个值得关注的问题。利用主成分分析方法从GPS时间序列中提取共模态信号,同时对各种地表载荷进行校正。第一主成分(PCs)分别占原始、大气+非潮汐海洋(AO)去除、AO +水文模式(AOH)去除和AO + GRACE/GFO-based load (AOG)去除垂直分量总方差的57.67%、35.87%、36.28%和36.03%。GPS垂直速度(不含共模分量+ AOG)的中值为0.13 mm/yr,表明冰体退缩对GPS观测的VLM有显著贡献。此外,研究还发现,冰川均衡调整(GIA)效应在青藏高原西部大尺度VLM隆升过程中发挥了关键作用。通过对5种不同的GPS垂直速度模式进行评估,我们认为ICE-6G_D模式可以更有效地校正南极洲GPS观测中的GIA信号。
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来源期刊
CiteScore
9.30
自引率
10.90%
发文量
563
审稿时长
4.7 months
期刊介绍: The IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing addresses the growing field of applications in Earth observations and remote sensing, and also provides a venue for the rapidly expanding special issues that are being sponsored by the IEEE Geosciences and Remote Sensing Society. The journal draws upon the experience of the highly successful “IEEE Transactions on Geoscience and Remote Sensing” and provide a complementary medium for the wide range of topics in applied earth observations. The ‘Applications’ areas encompasses the societal benefit areas of the Global Earth Observations Systems of Systems (GEOSS) program. Through deliberations over two years, ministers from 50 countries agreed to identify nine areas where Earth observation could positively impact the quality of life and health of their respective countries. Some of these are areas not traditionally addressed in the IEEE context. These include biodiversity, health and climate. Yet it is the skill sets of IEEE members, in areas such as observations, communications, computers, signal processing, standards and ocean engineering, that form the technical underpinnings of GEOSS. Thus, the Journal attracts a broad range of interests that serves both present members in new ways and expands the IEEE visibility into new areas.
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