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Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Published on: June 13, 2020

Causes for contemporary regional sea level changes.

Detlef Stammer¹, Anny Cazenave, Rui M Ponte

¹Institute of Oceanography, University of Hamburg, Hamburg, Germany. detlef.stammer@zmaw.de

Annual Review of Marine Science

|July 20, 2012

Summary

This summary is machine-generated.

Regional sea level changes vary significantly due to ocean dynamics and Earth

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Area of Science:

Oceanography
Climate Science
Geophysics

Background:

Regional sea level changes differ from global mean trends.
Variations occur on multiple timescales and can be influenced by ocean circulation, crustal isostatic adjustment, and local factors like subsidence.

Purpose of the Study:

To explain the drivers of regional sea level variations.
To differentiate between natural and anthropogenic influences on sea level.
To highlight the need for enhanced climate observing systems.

Main Methods:

Analysis of dynamic ocean circulation variations.
Assessment of isostatic adjustment due to ice and water mass changes.
Consideration of local factors including earthquakes and subsidence.

Main Results:

Natural climate variability is the primary driver of current regional sea level changes.
Anthropogenic effects will increasingly influence regional sea level patterns.
Future sea level patterns will be a combination of climate variability and static sea level changes.

Conclusions:

Understanding regional sea level requires accounting for both natural variability and anthropogenic impacts.
Accurate attribution and prediction of sea level changes necessitate a robust and continuous climate observing system.