Abstract
The climate-related melting of ice sheets and glaciers and the human-related redistribution of terrestrial water altered the Earth’s gravity and displacement field and resulted in non-uniform sea level changes, i.e., sea level fingerprints (SLF). Satellite gravity is an important approach in monitoring the spatio-temporal evolution process of global terrestrial water storage (TWS) and its relevance to sea level changes. This study uses the mascon (mass concentration) product of Gravity Recovery and Climate Experiment (GRACE) and its Follow-on (GRACE-FO) to estimate the global TWS changes from 2002 to 2020. Subsequently, the global SLF caused by the redistribution of land and sea water mass is calculated based on the sea level equation, which includes both the self-attraction effect of loads and the feedback effect of the Earth’s polar motion. Based on the results, the global TWS showed a decreasing trend (− 740.98 ± 41.64 Gt/year), with significant spatial differences. Consequently, the sea level maintained an upward trend (1.97 ± 0.10 mm/year), exhibiting typical fingerprint characteristics. Considering the sea level change (1.08 ± 0.10 mm/year) influenced by its steric variation, such as thermal expansion and salinity variation, we estimated that the total change rate of the global sea level is 3.05 ± 0.10 mm/year. The positive contribution of terrestrial water roughly amounted to 2.58 times the negative contribution. The melting of polar ice masses primarily contributes to the global TWS loss and sea level rise (0.46 ± 0.01 and 0.38 ± 0.02 mm/year for Greenland and Antarctica, respectively, excluding the peripheral glaciers). Another major contribution to sea level rise in the melting of glaciers (0.85 ± 0.01 mm/year, with the peripheral glaciers around Antarctica and Greenland). Furthermore, we found that the removal of coastline ice mass leads to the fingerprints effect, meaning that the relative sea level (RSL) does not increase but decreases around Greenland and Antarctica. Notably, the factors driving land-sea mass redistribution also include artificial reservoirs as well as groundwater and surface water, of which the latter has an overall smaller positive contribution (0.28 ± 0.07 mm/year) to the sea level rise. The role of artificial reservoirs in slowing down the sea level rise (− 0.57 ± 0.07 mm/year) cannot be ignored.
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Adhikari, S., Ivins, E. R., Frederikse, T., et al. (2019). Sea-level fingerprints emergent from GRACE mission data. Earth System Science Data, 11(2), 629–646. https://doi.org/10.5194/essd-11-629-2019
Amin, H., Bagherbandi, M., & Sjoberg, L. E. (2020). Quantifying barystatic sea-level change from satellite altimetry, GRACE and Argo observations over 2005–2016. Advances in Space Research, 65(8), 1922–1940. https://doi.org/10.1016/j.asr.2020.01.029
Bindoff, N., Willebrand, J., Artale, V., et al. (2007). Observations: oceanic climate and sea level. In: Climate change 2007: The physical Science Basis. Contribution of Working Group I to the Fourth Assessment report of the Intergouvernmental Panel on Climate Change. Computational Geometry, 2007(2), 1–21.
Chao, B. F., Wu, Y. H., & Li, Y. S. (2008). Impact of artificial reservoir water impoundment on global sea level. Science, 320(5873), 212–214. https://doi.org/10.1126/science.1154580
Cheng, M. K., Ries, J. C., & Tapley, B. D. (2011). Variations of the Earth’s figure axis from satellite laser ranging and GRACE. Journal of Geophysical Research-Solid Earth, 116, 14. https://doi.org/10.1029/2010jb000850
Church, J. A., Godfrey, J. S., Jackett, D. R., et al. (1991). A model of sea-level rise caused by ocean thermal-expansion. Journal of Climate, 4(4), 438–456. https://doi.org/10.1175/1520-0442
Ciracì, E., Velicogna, I., & Swenson, S. (2020). Continuity of the mass loss of the world’s glaciers and ice caps from the GRACE and GRACE follow-on missions. Geophysical Research Letters, 47(9), 5. https://doi.org/10.1029/2019GL086926
Creveling, J. R., & Mitrovica, J. X. (2014). The sea-level fingerprint of a Snowball Earth deglaciation. Earth and Planetary Science Letters, 399, 74–85. https://doi.org/10.1016/j.epsl.2014.04.029
Dieng, H. B., Cazenave, A., Meyssignac, B., et al. (2017). New estimate of the current rate of sea level rise from a sea level budget approach. Geophysical Research Letters, 44(8), 3744–3751. https://doi.org/10.1002/2017gl073308
Dieng, H. B., Cazenave, A., von Schuckmann, K., et al. (2015a). Sea level budget over 2005–2013: Missing contributions and data errors. Ocean Science, 11(5), 789–802. https://doi.org/10.5194/os-11-789-2015
Dieng, H. B., Palanisamy, H., Cazenave, A., et al. (2015b). The sea level budget since 2003: Inference on the deep ocean heat content. Surveys in Geophysics, 36(2), 209–229. https://doi.org/10.1007/s10712-015-9314-6
Farrell, W. E., & Clark, J. A. (1976). On postglacial sea level. Geophysical Journal International, 46(3), 647–667. https://doi.org/10.1111/j.1365-246X.1976.tb01252.x
Fasullo, J. T., Boening, C., Landerer, F. W., & Nerem, R. S. (2013). Australia’s unique influence on global sea level in 2010–2011. Geophysical Research Letters, 40(16), 4368–4373.
Fox-Kemper, B., Hewitt, H. T., Xiao, C., et al. (2021). Ocean, cryosphere and sea level change. In V. Masson-Delmotte, P. Zhai, & A. Pirani (Eds.), Climate change 2021: the physical science basis. Contribution of working group I to the sixth assessment report of the intergovernmental panel on climate change (pp. 1211–1362). Cambridge: Cambridge University Press. https://doi.org/10.1017/9781009157896.011
Frederikse, T., Landerer, F., Caron, L., et al. (2020). The causes of sea-level rise since 1900. Nature, 584(7821), 393–397. https://doi.org/10.1038/s41586-020-2591-3
Gornitz, V., Lebedeff, S., & Hansen, J. (1982). Global sea level trend in the past century. Science, 215(4540), 1611–1614. https://doi.org/10.1126/science.215.4540.1611
Grinsted, A., Jevrejeva, S., Riva, R. E. M., et al. (2015). Sea level rise projections for northern Europe under RCP8.5. Climate Research, 64(1), 15–23. https://doi.org/10.3354/cr01309
Hamlington, B. D., Burgos, A., Thompson, P. R., et al. (2018). Observation-driven estimation of the spatial variability of 20thcentury sea level rise. Journal of Geophysical Research: Oceans, 123(3), 2129–2140. https://doi.org/10.1002/2017jc013486
Hay, C., Lau, H. C. P., Gomez, N., et al. (2017). Sea level fingerprints in a region of complex earth structure: The case of WAIS. Journal of Climate, 30(6), 1881–1892. https://doi.org/10.1175/Jcli-D-16-0388.1
Hay, C., Mitrovica, J. X., Gomez, N., et al. (2014). The sea-level fingerprints of ice-sheet collapse during interglacial periods. Quaternary Science Reviews, 87, 60–69. https://doi.org/10.1016/j.quascirev.2013.12.022
Hsu, C. W., & Velicogna, I. (2017). Detection of sea level fingerprints derived from GRACE gravity data. Geophysical Research Letters, 44(17), 8953–8961. https://doi.org/10.1002/2017gl074070
Imbie Team. (2018). Mass balance of the Antarctic Ice Sheet from 1992 to 2017. Nature, 558(7709), 219–222. https://doi.org/10.1038/s41586-018-0179-y
Jeon, T., Seo, K.-W., Kim, B.-H., et al. (2021). Sea level fingerprints and regional sea level change. Earth and Planetary Science Letters, 567, 116985. https://doi.org/10.1016/j.epsl.2021.116985
Jeon, T., Seo, K. W., Youm, K., et al. (2018). Global sea level change signatures observed by GRACE satellite gravimetry. Scientific Reports, 8(1), 13519. https://doi.org/10.1038/s41598-018-31972-8
Jin, T. Y., Li, X. L., Shum, C. K., et al. (2020). The balance and abnormal increase of global ocean mass change from land using GRACE. Earth and Space Science, 7(5), 5. https://doi.org/10.1029/2020EA001104
Kendall, R. A., Mitrovica, J. X., & Milne, G. A. (2005). On post-glacial sea level II. Numerical formulation and comparative results on spherically symmetric models. Geophysical Journal International, 161(3), 679–706. https://doi.org/10.1111/j.1365-246X.2005.02553.x
Li, S., Shen, W., Pan, Y., et al. (2020). Surface seasonal mass changes and vertical crustal deformation in North China from GPS and GRACE measurements. Geodesy and Geodynamics, 11(1), 46–55. https://doi.org/10.1016/j.geog.2019.05.002
Llovel, W., Purkey, S., Meyssignac, B., et al. (2019). Global ocean freshening, ocean mass increase and global mean sea level rise over 2005–2015. Scientific Reports, 9(1), 17717. https://doi.org/10.1038/s41598-019-54239-2
Llovel, W., Willis, J. K., Landerer, F. W., et al. (2014). Deep-ocean contribution to sea level and energy budget not detectable over the past decade. Nature Climate Change, 4(11), 1031–1035. https://doi.org/10.1038/nclimate2387
Milne, G. A., & Mitrovica, J. X. (1996). Postglacial sea-level change on a rotating Earth: First results from a gravitationally self-consistent sea-level equation. Geophysical Journal International, 126(3), F13–F20. https://doi.org/10.1111/j.1365-246X.1996.tb04691.x
Mitrovica, J. X., & Peltier, W. R. (1991). On postglacial geoid subsidence over the equatorial oceans. Journal of Geophysical Research-Solid Earth, 96(B12), 20053–20071. https://doi.org/10.1029/91jb01284
Mu, Y., Wei, Y., Wu, J., et al. (2020). Variations of mass balance of the Greenland ice sheet from 2002 to 2019. Remote Sensing. https://doi.org/10.3390/RS12162609
Munk, W. H., & MacDonald, G. J. F. (1960). The rotation of the earth. Geological Magazine, 98(4), 352–352. https://doi.org/10.1017/S0016756800060726
Nerem, R. S., Leuliette, É., & Cazenave, A. (2006). Present-day sea-level change: A review. Comptes Rendus Geoscience, 338(14), 1077–1083. https://doi.org/10.1016/j.crte.2006.09.001
Park, J., Stolle, C., Yamazaki, Y., et al. (2020). Diagnosing low-/mid-latitude ionospheric currents using platform magnetometers: CryoSat-2 and GRACE-FO. Earth, Planets and Space, 72(1), 162. https://doi.org/10.1186/s40623-020-01274-3
Peltier, W. R., Argus, D. F., Drummond, R., et al. (2018). Comment on “An Assessment of the ICE-6G_C (VM5a) Glacial Isostatic Adjustment Model” by Purcell et al. Journal of Geophysical Research-Solid Earth, 123(2), 2019–2028. https://doi.org/10.1002/2016jb013844
Pfeffer, J., Tregoning, P., Purcell, A., et al. (2018). Multitechnique assessment of the interannual to multidecadal variability in steric sea levels: A comparative analysis of climate mode fingerprints. Journal of Climate, 31(18), 7583–7597. https://doi.org/10.1175/Jcli-D-17-0679.1
Pico, T., Mitrovica, J. X., & Mix, A. C. (2020). Sea level fingerprinting of the Bering Strait flooding history detects the source of the Younger Dryas climate event. Science Advances. https://doi.org/10.1126/sciadv.aay2935
Piretzidis, D., & Sideris, M. G. (2019). Stable recurrent calculation of isotropic Gaussian filter coefficients. Computers and Geosciences. https://doi.org/10.1016/j.cageo.2019.07.007
Raj, R. P., Andersen, O. B., Johannessen, J. A., et al. (2020). Arctic sea level budget assessment during the GRACE/Argo Time Period. Remote Sensing. https://doi.org/10.3390/rs12172837
Reager, J. T., Gardner, A. S., Famiglietti, J. S., et al. (2016). A decade of sea level rise slowed by climate-driven hydrology. Science, 351(6274), 699–703. https://doi.org/10.1126/science.aad8386
Ross, A. C., Najjar, R. G., Li, M., et al. (2017). Fingerprints of sea level rise on changing tides in the Chesapeake and Delaware bays. Journal of Geophysical Research-Oceans, 122(10), 8102–8125. https://doi.org/10.1002/2017jc012887
Rowlands, D. D., Luthcke, S. B., McCarthy, J. J., et al. (2010). Global mass flux solutions from GRACE: A comparison of parameter estimation strategies—Mass concentrations versus Stokes coefficients. Journal of Geophysical Research, 115, 5. https://doi.org/10.1029/2009JB006546
Royston, S., Vishwakarma, B. D., Westaway, R., et al. (2020). Can we resolve the basin-scale sea level trend budget from GRACE ocean mass? Journal of Geophysical Research-Oceans. https://doi.org/10.1029/2019JC015535
Save, H., Bettadpur, S., & Tapley, B. D. (2016). High-resolution CSR GRACE RL05 mascons. Journal of Geophysical Research-Solid Earth, 121(10), 7547–7569. https://doi.org/10.1002/2016jb013007
Simon, K. M., Riva, R. E. M., Kleinherenbrink, M., et al. (2018). The glacial isostatic adjustment signal at present day in northern Europe and the British Isles estimated from geodetic observations and geophysical models. Solid Earth, 9(3), 777–795. https://doi.org/10.5194/se-9-777-2018
Sutterley, T. C., Velicogna, I., & Hsu, C. W. (2020). Self-consistent ice mass balance and regional sea level from time-variable gravity. Earth and Space Science. https://doi.org/10.1029/2019ea000860
Talpe, M. J., Nerem, R. S., Forootan, E., et al. (2017). Ice mass change in Greenland and Antarctica between 1993 and 2013 from satellite gravity measurements. Journal of Geodesy, 91(11), 1283–1298. https://doi.org/10.1007/s00190-017-1025-y
Tang, L., Li, J., Chen, J., et al. (2020). Seismic impact of large earthquakes on estimating global mean ocean mass change from GRACE. Remote Sensing. https://doi.org/10.3390/rs12060935
Wada, Y., Reager, J. T., Chao, B. F., et al. (2017). Recent changes in land water storage and its contribution to sea level variations. Surveys in Geophysics, 38(1), 131–152. https://doi.org/10.1007/s10712-016-9399-6
Wahr, J., Molenaar, M., & Bryan, F. (1998). Time variability of the Earth’s gravity field: Hydrological and oceanic effects and their possible detection using GRACE. Journal of Geophysical Research-Solid Earth, 103(B12), 30205–30229. https://doi.org/10.1029/98jb02844
Wang, L., Zhang, L., Chen, C., et al. (2018). Anomalous acceleration of mass loss in the Greenland ice sheet drainage basins and its contribution to the sea level fingerprints during 2010–2012. Cryosphere. https://doi.org/10.5194/tc-2018-142
Watkins, M. M., Wiese, D. N., Yuan, D. N., et al. (2015). Improved methods for observing Earth’s time variable mass distribution with GRACE using spherical cap mascons. Journal of Geophysical Research-Solid Earth, 120(4), 2648–2671. https://doi.org/10.1002/2014jb011547
WCRP Global Sea Level Budget Group. (2018). Global sea-level budget 1993–present. Earth Syst. Sci. Data, 10(3), 1551–1590. https://doi.org/10.5194/essd-10-1551-2018
Xi, H., Zhang, Z. Z., Lu, Y., et al. (2019). Mass sea level variation in the South China Sea from GRACE, altimetry and model and the connection with ENSO. Advances in Space Research, 64(1), 117–128. https://doi.org/10.1016/j.asr.2019.03.027
Yu, Y., Chao, B. F., Garcia-Garcia, D., et al. (2018). Variations of the Argentine Gyre observed in the GRACE time-variable gravity and ocean altimetry measurements. Journal of Geophysical Research-Oceans, 123(8), 5375–5387. https://doi.org/10.1029/2018jc014189
Zou, F., Tenzer, R., Fok, H. S., et al. (2020). Mass balance of the greenland ice sheet from GRACE and surface mass balance modelling. Water (switzerland). https://doi.org/10.3390/W12071847
Acknowledgements
We thank the editor and reviewers for their insightful comments which substantially improved this manuscript. This work was supported by the National Natural Science Foundation of China (41874090 and 41774091). We are also grateful for the monthly mascon data of JPL GRACE provided by GRCTellus, the sea level steric height and the overall sea level change data provided by NASA, the global surface temperature data provided by GISS, and the reservoir information data provided by Global Dam Watch and ICOLD.
Funding
This research was funded by National Natural Science Foundation of China, grant nos [41874090, 41774091].
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Sun, J., Wang, L., Peng, Z. et al. The Sea Level Fingerprints of Global Terrestrial Water Storage Changes Detected by GRACE and GRACE-FO Data. Pure Appl. Geophys. 179, 3493–3509 (2022). https://doi.org/10.1007/s00024-022-03123-8
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DOI: https://doi.org/10.1007/s00024-022-03123-8