Related Experiment Video
Updated: Feb 2, 2026

09:44
Growth and Differentiation of Adult Hippocampal Arctic Ground Squirrel Neural Stem Cells
Published on: January 7, 2011
9.9K
The step-like evolution of Arctic open water
Michael A Goldstein1,2, Amanda H Lynch3,4, Andras Zsom5
1Climate Change Research Center, University of New South Wales, Sydney, NSW, 2052, Australia. goldstein@babson.edu.
Scientific Reports
|November 17, 2018
Summary
Arctic sea ice shows critical points with multiple shifts in open water fraction detected in Pacific and Atlantic sectors. These breakpoints indicate potential irreversible changes in Arctic sea ice conditions.
Area of Science:
- Climatology
- Oceanography
- Remote Sensing
Background:
- Arctic sea ice extent is a critical indicator of global climate change.
- Analyzing historical sea ice concentration data reveals significant trends and potential regime shifts.
Purpose of the Study:
- To analyze the September open water fraction in the Arctic using satellite data from 1979-2017.
- To identify breakpoints (shifts in the mean) in Arctic sea ice concentration data across different sectors.
Main Methods:
- Utilized satellite era record of ice concentration (1979-2017).
- Applied statistical models to detect breakpoints in Pacific, Atlantic, Canadian, and Russian sectors.
- Compared breakpoint models with linear trend models for data fitting.
Main Results:
- Identified three breakpoints in the Pacific sector (1989, 2002, 2007) and multiple breakpoints in the Atlantic sector (1971, 2000, 2011).
- Detected multiple breakpoints in Canadian and Russian sectors, and for the Arctic as a whole.
- Breakpoint models significantly outperformed linear trend models in fitting the observed data.
Conclusions:
- Results support the hypothesis of critical points in Arctic sea ice, beyond which recovery is less probable.
- Employing breakpoint means for data detrending is more reliable than linear detrending, avoiding spurious signals.
Related Concept Videos
Convergent Evolution
32.9K
Evolution shapes the features of organisms over time, ensuring that they are suited for the environments in which they live. Sometimes, selection pressure leads to the rise of similar but unrelated adaptations in organisms with no recent common ancestors, a process known as convergent evolution.
32.9K
The Evidence for Evolution
48.2K
Genetic variations accumulating within populations over generations give rise to biological evolution. Evolutionary changes can result in the formation of novel varieties and entire new species. These changes are responsible for the diverse forms of life inhabiting the planet. The evidence for evolution suggests that all living organisms descended from common ancestors.
48.2K
Eukaryotic Evolution
41.4K
The endosymbiont theory is the most widely accepted theory of eukaryotic evolution; however, its progression is still somewhat debated. According to the nucleus-first hypothesis, the ancestral prokaryote first evolved a membrane to enclose DNA and form the nucleus. Conversely, the mitochondria-first hypothesis suggests that the nucleus was formed after endosymbiosis of mitochondria.
Contrary to the endosymbiont theory, the eukaryote-first hypothesis proposes that the simpler prokaryotic and...
Contrary to the endosymbiont theory, the eukaryote-first hypothesis proposes that the simpler prokaryotic and...
41.4K
Synteny and Evolution
3.8K
John H. Renwick first coined the term “synteny” in 1971, which refers to the genes present on the same chromosomes, even if they are not genetically linked. The species with common ancestry tend to show conserved syntenic regions. Therefore, the concept of synteny is nowadays used to describe the evolutionary relationship between species.
Around 80 million years ago, the human and mice lineages diverged from the common ancestor. During the course of evolution, the ancestral...
Around 80 million years ago, the human and mice lineages diverged from the common ancestor. During the course of evolution, the ancestral...
3.8K
States of Water
56.9K
Water exists in any one of the three classical states: solid (ice), liquid (water), and gas (steam or water vapor). The state of water depends on i) the intermolecular forces that draw molecules together and ii) the kinetic energy that leads to movements that pull them apart.
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
56.9K
Rate-Determining Steps
37.2K
Relating Reaction Mechanisms
In a multistep reaction mechanism, one of the elementary steps progresses significantly slower than the others. This slowest step is called the rate-limiting step (or rate-determining step). A reaction cannot proceed faster than its slowest step, and hence, the rate-determining step limits the overall reaction rate.
The concept of rate-determining step can be understood from the analogy of a 4-lane freeway with a short-stretch of traffic-bottleneck caused due to...
In a multistep reaction mechanism, one of the elementary steps progresses significantly slower than the others. This slowest step is called the rate-limiting step (or rate-determining step). A reaction cannot proceed faster than its slowest step, and hence, the rate-determining step limits the overall reaction rate.
The concept of rate-determining step can be understood from the analogy of a 4-lane freeway with a short-stretch of traffic-bottleneck caused due to...
37.2K

