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Ocean mass ice melt global sea level rise

Satellite Data Reveals Ocean Mass and Ice Melt Driving Accelerating Global Sea-Level Rise

The researchers applied a novel forward modelling approach to overcome the spatial resolution limits of satellite laser ranging, thereby allowing continuous monitoring of global ocean mass changes. (Credit: Hong Kong Polytechnic University)

A Clear Signal of Climate Change

Global mean sea level (GMSL) has long been recognized as one of the most crucial indicators of climate change. For decades, scientists have warned that warming oceans and melting ice are reshaping coastlines worldwide. Now, a groundbreaking study from The Hong Kong Polytechnic University (PolyU) has delivered the first accurate 30-year record (1993-2022) of global ocean mass change, providing unprecedented clarity on the pace and drivers of sea-level rise.

The research, published in the Proceedings of the National Academy of Sciences (PNAS), confirms that GMSL has been increasing at an average of 3.3 mm per year, with a significant acceleration in recent decades. This trend underscores the escalating consequences of climate warming, particularly the rapid loss of land ice.

Why Sea-Level Rise Matters

Two Key Drivers of Rising Seas

According to climate science, GMSL is primarily influenced by two processes:

  • Thermal expansion of seawater - As oceans absorb nearly 90% of excess heat trapped by greenhouse gases, water molecules expand, raising sea levels.
  • Ocean mass increase (barystatic rise) - Freshwater from melting land ice, including glaciers and polar ice sheets, adds vast amounts of water to the oceans.

Together, these forces are reshaping global coastlines, threatening millions of people living in low-lying regions, and stressing coastal ecosystems.

The Urgency of Monitoring Ocean Mass

While thermal expansion is relatively well-understood, continuous measurement of ocean mass has been far more difficult. Without accurate records, scientists have struggled to quantify the true scale of climate-driven sea-level changes. This is where PolyU's study breaks new ground.

The Role of Satellites in Unlocking Sea-Level Data

From Altimetry to Gravimetry

For many years, researchers relied mainly on satellite altimetry, which sea surface height. However, this method does not directly capture ocean mass changes. A major breakthrough came in 2002 with the launch of NASA's Gravity Recovery and Climate Experiment (GRACE) mission, which enabled large-scale gravimetric observations of ocean mass.

Yet, even GRACE had its limitations, leaving gaps in long-term records. PolyU scientists have now advanced the field by leveraging Satellite Laser Ranging (SLR)--a technique that measures the distance between ground stations and satellites using laser beams.

Overcoming SLR's Challenges

Traditionally, SLR has been considered unsuitable for measuring ocean mass because of:

  • The limited number of satellites and ground stations
  • Its high orbital altitude, which only captures long-wavelength gravitational changes
  • Low-resolution gravity measurements

An Innovative Forward Modelling Approach

The PolyU team, led by Prof. Jianli Chen (Chair Professor of Space Geodesy and Earth Sciences) and Dr. Yufeng Nie (Research Assistant Professor, LSGI), overcame these challenges by applying a forward modelling method. This approach integrates detailed ocean-land boundary data, significantly improving spatial resolution and allowing continuous, reliable measurements of global ocean mass change from 1993 to 2022.

Key Findings: Ocean Mass as the Dominant Driver

The study's results provides a clear picture of the accelerating rises in GMSL:

  • Between 1993 and 2022, global sea levels rose by nearly 90 mm.
  • Almost 60% of this increase is directly linked to ocean mass growth.
  • Since around 2005, the dominant force behind rising seas has been land ice melt, specially from Greenland and other polar regions.
  • Over the full 30-year period, polar ice sheets and mountain glaciers contributed more than 80% of the total increase in ocean mass.

Expert Insights from the Research Team

Prof. Jianli Chen highlighted the scale of the problem:

"In recent decades, climate warming has intensified land ice loss, increasingly dominating the factors contributing to global sea-level rise."

He further stressed that the findings provide crucial validation for climate models used to forecast future sea-level scenarios.

Dr. Yufeng Nie emphasized the breakthrough role of SLR in climate research:

"Our findings indicate that ocean mass changes obtained from SLR analyses correspond closely with total sea-level variations measured by satellite altimetry, once thermal expansion is considered. This shows that conventional SLR can now serve as a robust tool for long-term climate research."

Why This Matters for the Future

A Warning for Coastal Communities

The findings underscore the increasing vulnerability of coastal cities. With accelerating ice melt, sea levels are expected to rise even faster in the coming decades, putting millions at risk from flooding, storm surges and land lose.

Strengthening Climate Models

Accurate long-term records of ocean mass change are vital for improving climate simulations. By validating and refining models, scientists can provide better forecasts to guide global adaptation strategies.

Policy and Mitigation Implications

  • Governments may need to accelerate coastal resilience planning, including infrastructure reinforcement and managed retreat in high-risk areas.
  • Stronger global efforts to reduce greenhouse gas emissions remain critical to slow warming and ice loss.
  • International cooperation in climate monitoring will be essential, with satellite data playing a pivotal role.

Looking Ahead: The Expanding Role of Space Geodesy

This study demonstrates the power of space-based geodetic techniques in addressing climate challenges. As technology advances, future missions will likely deliver even more precise measurements, further clarifying the links between ice melt, ocean mass, and sea-level rise.

By refining long-term records, scientists will be better equipped to forecast how much, how fast, and where sea levels will rise, enabling societies to prepare for the profound changes ahead.

Conclusion

The PolyU study offers a groundbreaking. 30-years record of ocean mass change, revealing that ice melt and ocean mass growth are now the dominant forces behind accelerating global sea-level rise. With seas already rising at an average of 3.3 mm per year, the research sends a clear warning: climate change is not a distant threat but a present and intensifying reality.

Armed with improved data, policymakers and scientists have stronger tools to predict, prepare and act. But the study also serves as a stark reminder--without urgent global action, sea-level rise will continue to accelerate, reshaping coastlines and human societies worldwide.

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"Discover how ice melt and ocean mass changes are driving global sea-level rise--stay updated with cutting-edge research."

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Earth Day Harsh Reality - "Learn about accelerating ice melt, rising oceans and urgent climate challenges threatening our planet at Earth Day Harsh Reality Blog."

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