Study on Annual Signals of Greenland Ice Sheet Mass and Associated Influencing Factors Based on GRACE/GRACE-FO Data
As global temperatures rise, the Greenland ice sheet (GrIS) is undergoing accelerating mass loss, with significant implications for sea level rise and climate systems. Using GRACE and GRACE Follow-On (GRACE-FO) RL06 data from April 2002 to May 2023, alongside MARv3.14 regional climate model outputs...
Published in: | Land |
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Main Authors: | , , , , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2025
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Subjects: | |
Online Access: | https://doi.org/10.3390/land14040705 |
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author | Kaifeng Ma Jing Han Zhen Li Junzhen Meng Qingfeng Hu Peipei He Changxu Yao |
author_facet | Kaifeng Ma Jing Han Zhen Li Junzhen Meng Qingfeng Hu Peipei He Changxu Yao |
author_sort | Kaifeng Ma |
collection | MDPI Open Access Publishing |
container_issue | 4 |
container_start_page | 705 |
container_title | Land |
container_volume | 14 |
description | As global temperatures rise, the Greenland ice sheet (GrIS) is undergoing accelerating mass loss, with significant implications for sea level rise and climate systems. Using GRACE and GRACE Follow-On (GRACE-FO) RL06 data from April 2002 to May 2023, alongside MARv3.14 regional climate model outputs (ice melting, runoff, rainfall, snowfall, and land surface temperature (LST)), we investigated the drivers of GrIS mass changes. Continuous wavelet transform analysis revealed significant annual signals in all variables except snowfall, with wavelet decomposition showing the largest annual amplitudes for ice melting (58.8 Gt/month) and runoff (44.5 Gt/month), surpassing those of GRACE/GRACE-FO (31.1 Gt/month). Cross-correlation analysis identified ice melting, runoff, rainfall, snowfall, and LST as significantly correlated with GrIS mass changes, with ice melting, runoff, and LST emerging as primary drivers, while snowfall and runoff exerted secondary influences. Temporal lags of 3, 4, 4, 7, and 4 months were observed for ice melting, runoff, rainfall, snowfall, and LST, respectively. These findings highlight the complex interplay of climatic and hydrological processes driving GrIS mass loss. |
format | Text |
genre | Greenland Ice Sheet |
genre_facet | Greenland Ice Sheet |
geographic | Greenland |
geographic_facet | Greenland |
id | ftmdpi:oai:mdpi.com:/2073-445X/14/4/705/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/land14040705 |
op_relation | Land Systems and Global Change https://dx.doi.org/10.3390/land14040705 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Land Volume 14 Issue 4 Pages: 705 |
publishDate | 2025 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2073-445X/14/4/705/ 2025-04-27T14:29:54+00:00 Study on Annual Signals of Greenland Ice Sheet Mass and Associated Influencing Factors Based on GRACE/GRACE-FO Data Kaifeng Ma Jing Han Zhen Li Junzhen Meng Qingfeng Hu Peipei He Changxu Yao agris 2025-03-26 application/pdf https://doi.org/10.3390/land14040705 eng eng Multidisciplinary Digital Publishing Institute Land Systems and Global Change https://dx.doi.org/10.3390/land14040705 https://creativecommons.org/licenses/by/4.0/ Land Volume 14 Issue 4 Pages: 705 GrIS GRACE/GRACE-FO mass change driving factors lagging Text 2025 ftmdpi https://doi.org/10.3390/land14040705 2025-03-31T14:26:03Z As global temperatures rise, the Greenland ice sheet (GrIS) is undergoing accelerating mass loss, with significant implications for sea level rise and climate systems. Using GRACE and GRACE Follow-On (GRACE-FO) RL06 data from April 2002 to May 2023, alongside MARv3.14 regional climate model outputs (ice melting, runoff, rainfall, snowfall, and land surface temperature (LST)), we investigated the drivers of GrIS mass changes. Continuous wavelet transform analysis revealed significant annual signals in all variables except snowfall, with wavelet decomposition showing the largest annual amplitudes for ice melting (58.8 Gt/month) and runoff (44.5 Gt/month), surpassing those of GRACE/GRACE-FO (31.1 Gt/month). Cross-correlation analysis identified ice melting, runoff, rainfall, snowfall, and LST as significantly correlated with GrIS mass changes, with ice melting, runoff, and LST emerging as primary drivers, while snowfall and runoff exerted secondary influences. Temporal lags of 3, 4, 4, 7, and 4 months were observed for ice melting, runoff, rainfall, snowfall, and LST, respectively. These findings highlight the complex interplay of climatic and hydrological processes driving GrIS mass loss. Text Greenland Ice Sheet MDPI Open Access Publishing Greenland Land 14 4 705 |
spellingShingle | GrIS GRACE/GRACE-FO mass change driving factors lagging Kaifeng Ma Jing Han Zhen Li Junzhen Meng Qingfeng Hu Peipei He Changxu Yao Study on Annual Signals of Greenland Ice Sheet Mass and Associated Influencing Factors Based on GRACE/GRACE-FO Data |
title | Study on Annual Signals of Greenland Ice Sheet Mass and Associated Influencing Factors Based on GRACE/GRACE-FO Data |
title_full | Study on Annual Signals of Greenland Ice Sheet Mass and Associated Influencing Factors Based on GRACE/GRACE-FO Data |
title_fullStr | Study on Annual Signals of Greenland Ice Sheet Mass and Associated Influencing Factors Based on GRACE/GRACE-FO Data |
title_full_unstemmed | Study on Annual Signals of Greenland Ice Sheet Mass and Associated Influencing Factors Based on GRACE/GRACE-FO Data |
title_short | Study on Annual Signals of Greenland Ice Sheet Mass and Associated Influencing Factors Based on GRACE/GRACE-FO Data |
title_sort | study on annual signals of greenland ice sheet mass and associated influencing factors based on grace/grace-fo data |
topic | GrIS GRACE/GRACE-FO mass change driving factors lagging |
topic_facet | GrIS GRACE/GRACE-FO mass change driving factors lagging |
url | https://doi.org/10.3390/land14040705 |