1993 - 2016年全球海平面变化速率、加速度及其分量

IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Marine Geodesy Pub Date : 2023-11-03 DOI:10.1080/01490419.2023.2276478
Fengwei Wang, Yunzhong Shen, Qiujie Chen, Jianhua Chen, Jianhua Geng
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The statistical results show that the global mean ocean mass change rate accounts for ∼54% of 2.85 ± 0.30 mm/year of global mean total sea level change. The accelerations of global mean total sea level change and its components are 0.145 ± 0.025 mm/year2 (altimetry), 0.003 ± 0.021 mm/year2 (steric), 0.139 ± 0.047 mm/year2 (ocean mass from Tongji), and 0.137 ± 0.010 mm/year2 (the sum of mass-driven components) respectively, indicating that the global sea level budget in terms of acceleration can be closed and nearly no acceleration exists in the global mean steric sea level change for the period 1993–2016.Keywords: Global sea level changeGravity field modelsAltimetryStericAcceleration Disclosure StatementNo potential conflict of interest was reported by the author(s).Data Availability StatementThe merged altimetry gridded global sea level height anomalies are accessed at https://doi.org/10.24381/cds.4c328c78. 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引用次数: 0

摘要

摘要研究全球海平面收支对量化海平面总变化(海拔)及其分量至关重要,包括空间海平面变化和海洋质量变化(重力),其中海洋质量变化主要归因于四个质量驱动分量(格陵兰岛、南极洲、冰川和陆地蓄水)。本研究利用同济- leo2021和同济- grace - 2018每月重力场模型,结合IGG-SLR-HYBRID重力场模型、高程、空间和四个质量驱动分量,研究了1993-2016年全球海洋24年质量变化,研究了66oN ~ 66oS纬度范围内全球海洋海平面在速率和加速度方面的预算。统计结果表明,全球平均海洋质量变化率占全球平均总海平面变化(2.85±0.30 mm/年)的约54%。全球平均总海平面变化的加速度及其分量分别为0.145±0.025 mm/year2(高程)、0.003±0.021 mm/year2(空间)、0.139±0.047 mm/year2(同济洋面)和0.137±0.010 mm/year2(质量驱动分量之和),表明1993-2016年全球平均海平面变化在加速度方面可以接近,几乎不存在加速度。关键词:全球海平面变化重力场模型盐度时空加速度披露声明作者未报告潜在利益冲突。数据可用声明合并的高程网格全球海平面高度异常可在https://doi.org/10.24381/cds.4c328c78上访问。两个原位空间数据集(EN4和IK09)可在https://doi.org/10.4121/12764933.v3上访问。同济leo2021和同济grace2018可分别从http://icgem.gfz-potsdam.de/series/03_other/Tongji/Tongji-LEO2021和http://icgem.gfz-potsdam.de/series/03_other/Tongji/Tongji-Grace2018网站免费获取。四个质量组成部分(即格陵兰岛、南极洲、冰川和陆地储水)可从https://catalogue.ceda.ac.uk/uuid/17c2ce31784048de93996275ee976fff获取。本研究得到中国自然科学基金[42061134010,42192532,41731069和42174099]和中国国家重点研发计划[2021YFB3900101]的支持。
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Global Sea Level Change Rate, Acceleration and Its Components from 1993 to 2016
AbstractInvestigating the global sea level budget is essential to quantify the total sea level change (altimetry) and its components, including the steric sea level change and the ocean mass change (gravity), where the latter is mainly attributed to four mass-driven components (Greenland, Antarctica, glaciers and land water storage). In this study, a 24-year global ocean mass change is derived by the joint use of Tongji-LEO2021 and Tongji-Grace2018 monthly gravity field models over 1993–2016, with which the sea level budgets in terms of rate and acceleration are investigated over global oceans within the latitudes 66oN to 66oS together with the IGG-SLR-HYBRID gravity field models, altimetry, steric and four mass-driven components. The statistical results show that the global mean ocean mass change rate accounts for ∼54% of 2.85 ± 0.30 mm/year of global mean total sea level change. The accelerations of global mean total sea level change and its components are 0.145 ± 0.025 mm/year2 (altimetry), 0.003 ± 0.021 mm/year2 (steric), 0.139 ± 0.047 mm/year2 (ocean mass from Tongji), and 0.137 ± 0.010 mm/year2 (the sum of mass-driven components) respectively, indicating that the global sea level budget in terms of acceleration can be closed and nearly no acceleration exists in the global mean steric sea level change for the period 1993–2016.Keywords: Global sea level changeGravity field modelsAltimetryStericAcceleration Disclosure StatementNo potential conflict of interest was reported by the author(s).Data Availability StatementThe merged altimetry gridded global sea level height anomalies are accessed at https://doi.org/10.24381/cds.4c328c78. The two situ steric datasets (EN4 and IK09) are accessed at https://doi.org/10.4121/12764933.v3. The Tongji-LEO2021 and Tongji-Grace2018 models are free to access from the websites of http://icgem.gfz-potsdam.de/series/03_other/Tongji/Tongji-LEO2021 and http://icgem.gfz-potsdam.de/series/03_other/Tongji/Tongji-Grace2018, respectively. Four mass components (i.e. Greenland, Antarctica, glaciers and land water storage) are accessed from https://catalogue.ceda.ac.uk/uuid/17c2ce31784048de93996275ee976fff. Besides, the IMBIE 2018 Antarctic and IMBIE 2019 Greenland datasets can be directly downloaded from the website of http://imbie.org/data-downloads/.Additional informationFundingThe research is supported by the Natural Science Foundation of China [42061134010, 42192532, 41731069 and 42174099] and the National Key R&D Program of China [2021YFB3900101].
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来源期刊
Marine Geodesy
Marine Geodesy 地学-地球化学与地球物理
CiteScore
4.10
自引率
6.20%
发文量
27
审稿时长
>12 weeks
期刊介绍: The aim of Marine Geodesy is to stimulate progress in ocean surveys, mapping, and remote sensing by promoting problem-oriented research in the marine and coastal environment. The journal will consider articles on the following topics: topography and mapping; satellite altimetry; bathymetry; positioning; precise navigation; boundary demarcation and determination; tsunamis; plate/tectonics; geoid determination; hydrographic and oceanographic observations; acoustics and space instrumentation; ground truth; system calibration and validation; geographic information systems.
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