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Related Concept Videos

Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
The Water Cycle01:00

The Water Cycle

The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
Marine Microbial Ecology01:30

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Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
What is Climate?01:16

What is Climate?

Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.

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Updated: May 9, 2026

Assessing Intertidal Populations of the Invasive European Green Crab
06:48

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Published on: September 16, 2020

The multimillennial sea-level commitment of global warming.

Anders Levermann1, Peter U Clark, Ben Marzeion

  • 1Potsdam Institute for Climate Impact Research, 14473 Potsdam, Germany. Anders.levermann@pik-potsdam.de

Proceedings of the National Academy of Sciences of the United States of America
|July 17, 2013
PubMed
Summary

Global sea level rise is committed, with projections of approximately 2.3 meters per degree Celsius warming within 2,000 years. This necessitates long-term adaptation strategies due to persistent greenhouse gas effects.

Keywords:
climate changeclimate impactssea-level change

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Area of Science:

  • Climate Science
  • Oceanography
  • Glaciology

Background:

  • Global mean sea level has risen over the past century and is projected to continue rising.
  • Past sea-level records suggest significant contributions from Greenland and Antarctic Ice Sheets, alongside ocean warming and glacier loss.
  • Climate and carbon systems exhibit inertia, leading to slow temperature decline even after emissions cease, prompting research into sea-level commitment.

Purpose of the Study:

  • To estimate future sea-level commitment on a multimillennial timescale.
  • To compute associated regional sea-level patterns.
  • To better constrain sea-level commitment by combining paleo-evidence and physical model simulations.

Main Methods:

  • Combining paleo-evidence with physical model simulations.
  • Estimating future sea-level commitment on a multimillennial timescale.
  • Computing regional sea-level patterns.

Main Results:

  • Ocean thermal expansion contributes 0.4 m/°C warming.
  • Antarctic Ice Sheet contribution is 1.2 m/°C warming.
  • Greenland Ice Sheet shows a nonlinear response, overcompensating for glacier melt saturation, leading to a total committed sea-level rise of approximately 2.3 m/°C within 2,000 years.

Conclusions:

  • The Earth is committed to significant sea-level rise due to anthropogenic greenhouse gases.
  • Long-term adaptation strategies are essential on multicentennial timescales.
  • Understanding sea-level commitment is crucial for future climate change mitigation and planning.